On the Modelling of
Mechanical Dewatering in
Papermaking
Vinicius Lobosco
Doctoral Dissertation
Stockholm 2004
Royal Institute of Technology
Department of Fibre and Polymer Technology
Division of Paper Technology
SE-100 44 Stockholm, Sweden
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Stockholm 2004, Universitetsservice US-AB tryckeri
To Hanna & Julia
Viagem Literal
Se alguém telefonar,
diga lhe que tenho saudades,
e que o mundo só girou a metade.
Num terço ou quarto de volta a gente se encontra.
E outra vez gira o céu e a saudade volta a te abraçar.
O ciclo nunca pára.
As curvas tendem a ser tortas.
As almas, vidas vivas,
as podres personalidades mortas,
são um jogo sem fim da poesia infinita,
a obra de Deus que Ele não terminou,
o ponto de mutação sempre próximo a nova estação.
Se cegarmos os olhos, veremos com o coração:
têm frango assado no forno,
pêssego em calda na geladeira,
e muito som na caixa.
Lobosco, Vinicius (2004)
On the Modelling of Mechanical Dewatering in Papermaking
Abstract
Most of the water fed into a paper machine is removed mechanically in
the forming and press sections. One of the factor which has an important
influence on mechanical dewatering, i.e. in both forming and pressing, is the
stress-strain behaviour of the fibre network.
The focus of this thesis is on the development of improved mathematical
descriptions of the stress-strain behaviour exhibited by fibre networks in the
forming and press sections. The first part of the thesis presents a physically
based model of the forming and densification of fibre mats in twin-wire formers. The model can calculate the effect of the application of a varied load
through the forming section. It was developed from mass and momentum
balances of the fibre and liquid phases, the fibre mat stress-porosity relation
and an expression for the permeability as a function of the porosity. The
fibre-mat stress-porosity relation used is rate-independent and presents hysteresis. Simulations have been conducted to study the effects of roll pressure,
blade pulses, wire tension and beating. The effect of sequential blade pressure pulses after the forming roll on the dewatering and the concentration
gradients could be characterised. The simulations also exhibited rewetting by
expansion when the fibre mats left the forming roll. Increasing wire tension
resulted in increased dewatering, but the rate of increase diminished rapidly
with increasing tension. The simulation results also indicated that beating
has a large influence on dewatering.
The second part of the thesis presents two models of the rate-dependent
stress-strain behaviour of the fibre network that is observed in wet pressing.
The first model was based on the approach pioneered by Perzyna (1966)
for strain-rate dependent plasticity and was quite satisfactory for calculating
the stress-strain behaviour of the fibre network in single press nips. It was
successfully applied for studying densification and dewatering in both normal
wet pressing and high temperature wet pressing. However, the first model
only includes rate dependence in the compression phase of the compressionexpansion cycle; the expansion phase is treated as being rate independent
The second model of the stress-strain behaviour of the fibre network treats
both compression and expansion as being rate dependent, according to experimental observations. It is based on the idea that the wet fibre web may
v
be conceived as a layered network of restricted swelling gels. A swollen fibre
is a restricted gel, the inner swelling pressure in a swollen fibre wall being
balanced by the stresses in the fibre wall structure. The observed rate dependence of wet webs in both compression and expansion phases was attributed
to the flow of water out of and into the fibre walls. The second model gave
predictions that are in good agreement with results from uniaxial experiments using pressure pulses of arbitrary shape for both a single pulse and a
sequence of pulses. It may therefore be used as a general model for the rheological behaviour of the wet fibre network in wet pressing, provided the model
parameters are estimated from experimental data with small experimental
error.
KEYWORDS: Paper, modelling, dewatering, forming, wet pressing, fibre
network stress, rheology, hysteresis, intra-fibre water, compressibility, structural stress, stress-strain, restricted gels, swelling.
vi
Preface
“There is no duty more indispensable than that of returning a kindness. All men distrust
one forgetful of a benefit.”
Cicero.
The mechanical dewatering that takes place in the forming and press
sections is of crucial importance for papermaking, not only because most of
the water in papermaking is removed mechanically, but also because several
of the final paper properties are influenced by these two sections. A factor
which plays an important role in mechanical dewatering, in both forming and
pressing, is the stress-strain behaviour of the fibre network.
The focus of this thesis is on developing improved mathematical descriptions of the stress-strain behaviour exhibited by fibre networks in the forming
and press sections. The first part of the thesis presents a model of the forming
and densification of fibre mats in twin-wire formers (Paper 1). The model
includes hysteresis in the stress-strain relationship of the fibre network.
The second part of this thesis deals with the stress-strain behaviour of
the fibre network during wet pressing. Since the work of Gustav Carlsson it
is generally accepted that the intra-fibre water flow also contributes to the
stress-strain behaviour of the fibre network in the press section. Both Carlsson and later researchers have stressed the importance of that phenomenon
for wet pressing.
Two models of the stress-strain behaviour of the fibre network in wet
pressing are presented. The first model follows the approach proposed by
Perzyna for rate sensitive plasticity and is here called the Perzyna model. It
could describe the rate-dependent stress-strain behaviour of the fibre network
in conditions typical for a single press nip (Paper 2). The model could simulate the stress-strain behaviour of different types of pulps and the effect of
web temperature (Paper 3). The Perzyna model allowed for rate sensitivity
in the compression phase of the nip but not in the expansion phase.
A press sections normally has a sequence of press nips and the fibre network expands in the unloaded region in-between the nips. To model the
stress-strain behaviour in a sequence of press nips, it is therefore necessary
to allow for rate sensitivity in both the compression and expansion phases of
the pressure pulse. Hence, a second model, which is here referred to as the
vii
gel-network model, was developed based on the idea that the fibre web may
be conceived as a layered network of restricted swelling gels (Paper 4). It
gave predictions which are in good agreement with experimental results for
both a single pulse and a sequence of pulses.
Since I started this project in September 1997, I have been helped and
supported by many people that I would like to thank. First, I would like to
greatly thank my supervisor at STFI and co-author in the last three papers,
Vikram Kaul, who believed in me, and gave me the opportunity to start
working as a postgraduate student at STFI. I would also like to thank him for
all the help and advice, and for being so unusually present in the development
of my work even after he retired. I would also like to thank the co-authors
of the first paper, Bo Norman and Sören Östlund, for their very valuable
discussions and comments. Sören Östlund is also thanked for guiding me
in – for me – new fields of solid mechanics, and believing in me in critical
moments of my work. I feel very much in debt to these three people. I am also
in debt with Raul Tempone, for giving me support regarding the numerical
methods and with Antônio Ponce de Leon for his help with statistics. Hannes
Vomhoff is thanked for making his experimental results available. I am very
greatful to Jean-Francis Bloch, Jan-Erik Gustafsson and Eric Schmidt for
reading the drafts and I also would like to thank Jonas Funkquist, Inger
van Heesch, Richard Holmqvist, Sune Karlsson, Marianne Lockner, Marco
Lucisano and Ali Moosavifar for their help and support. Finally, I would like
to acknowledge the Joule Project of the European Community, the Center
for Chemical Process Design and Control and STFI for providing the funds
necessary for this project.
I hope I will be able to return their kindness.
Stockholm, Autumn 2003
Vinicius Lobosco
viii
List of Publications
This thesis is based on the following four papers:
1. Modelling of Forming and Densification of Fibre Mats in Twin-Wire
Formers.
Lobosco, V., Norman, B. and Östlund, S., to be submitted for publication to Nordic Pulp and Paper Research Journal.
2. An Elastic/Viscoplastic Model of the Fibre Network Stress in Wet
Pressing: Part I
Lobosco, V. and Kaul, V. (2001), Nordic Pulp and Paper Research
Journal, 16(1):12–17.
3. An Elastic/Viscoplastic Model of the Fibre Network Stress in Wet
Pressing: Part 2. Accounting for Pulp Properties and Web Temperature
Lobosco, V. and Kaul, V. (2001), Nordic Pulp and Paper Research
Journal, 16(4):313–318.
4. The Stress-Strain Relationship of the Fibre Network in Wet Pressing.
Lobosco, V. and Kaul, V., to be submitted for publication to Nordic
Pulp and Paper Research Journal.
ix
Other relevant publications not included in the thesis:
1. An Elastic-Viscoplastic Model of the Rheological Behaviour of Wet Fibre Networks in Compression
Lobosco, V. and Kaul, V. (1999), International Paper Physics Conference, San Diego, CA, USA, 26-30 Sept. 1999, pp 403-410.
2. A Rheological Model of the Paper Fibre Network in Wet Pressing
Lobosco, V. (2000), Licentiate Thesis, Department of Pulp and Paper
Chemistry and Technology, Royal Institute of Technology, Stockholm.
3. Densification and Dewatering in High Temperature Wet Pressing
Gustafsson, J. E., Kaul, V. and Lobosco, V. (2001), The Science of
Papermaking, 12th Fundamental Research Symposium, Oxford, UK,
17-21, Sept. 2001, vol. 1, pp 679-708.
4. A Rheological Model of the Fibre Network in Wet Pressing
Lobosco, V. (2002), Nordic Rheology Conference 2002, Gothenburg,
Sweden, June 12-14 2002, pp 83-88.
5. High Temperature Pressing of Fibrous Materials
Kaul, V., Gustafsson, J.-E., Lobosco V., Bloch, J.-F., Thibault, X.,
Reverdy, N., Costa, C. A. V., Aguilar, H., Mendes, P., Norman, B.,
Nilsson, F., Stenström, S., Nilsson, J., Olsson, L., Todorovich, A.
(2002), STFI report PUB 7, Stockholm, Sweden: STFI Swedish Pulp
and Paper Research Institute, 19pp
6. Modélisation du Pressage du Papier : Consolidation et Expression de
l’eau du Gâteau Fibreux Humide
Gustafsson, J. E., Kaul, V., Lobosco, V. and Bloch, J.-F. (2003), Rev.
ATIP vol. 57, no. 4, Oct. 2003, pp 22, 24, 26-30, 32-35.
x
Contents
1 Introduction
1
1.1
The Papermaking Process . . . . . . . . . . . . . . . . . . . .
1
1.2
Mechanical Dewatering . . . . . . . . . . . . . . . . . . . . . .
3
1.2.1
Forming Section . . . . . . . . . . . . . . . . . . . . . .
3
1.2.2
Wet Pressing Section . . . . . . . . . . . . . . . . . . .
5
Fibre/Water Separation Process . . . . . . . . . . . . . . . . .
6
1.3.1
Flow Through Porous Media . . . . . . . . . . . . . . .
6
1.3.2
Fibre Network Compression . . . . . . . . . . . . . . .
9
1.3.3
Flow with Compression . . . . . . . . . . . . . . . . . . 12
1.3
1.4
Modelling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15
1.4.1
Forming . . . . . . . . . . . . . . . . . . . . . . . . . . 15
1.4.2
Wet Pressing . . . . . . . . . . . . . . . . . . . . . . . 16
1.5
Summarising
. . . . . . . . . . . . . . . . . . . . . . . . . . . 17
1.6
Objectives . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17
2 Modelling of Dewatering in Forming
2.1
19
Model . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20
2.1.1
Constitutive Equations and Physical Properties . . . . 20
2.1.2
Initial and Boundary Conditions . . . . . . . . . . . . . 21
2.1.3
Numerical Solution . . . . . . . . . . . . . . . . . . . . 22
2.2
Results and Discussions . . . . . . . . . . . . . . . . . . . . . 23
2.3
Concluding Remarks . . . . . . . . . . . . . . . . . . . . . . . 26
xi
3 The Perzyna Model
3.1
27
Experiments . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28
3.1.1
Sources of Error . . . . . . . . . . . . . . . . . . . . . . 29
3.2
Model . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32
3.3
Results and Discussions . . . . . . . . . . . . . . . . . . . . . 34
3.4
3.3.1
Parameters Estimation . . . . . . . . . . . . . . . . . . 34
3.3.2
Validation . . . . . . . . . . . . . . . . . . . . . . . . . 36
Concluding Remarks . . . . . . . . . . . . . . . . . . . . . . . 38
4 The Gel-Network Model
39
4.1
Experiments . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40
4.2
Model . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40
4.3
4.4
4.2.1
The Micro- and Macroscopic Perspectives . . . . . . . 40
4.2.2
The Macroscopic Model . . . . . . . . . . . . . . . . . 42
Results and Discussions . . . . . . . . . . . . . . . . . . . . . 44
4.3.1
The Equilibrium Curve . . . . . . . . . . . . . . . . . . 44
4.3.2
Parameters Estimation . . . . . . . . . . . . . . . . . . 44
4.3.3
Validation . . . . . . . . . . . . . . . . . . . . . . . . . 45
Concluding Remarks . . . . . . . . . . . . . . . . . . . . . . . 47
A Model Derivation
59
A.1 Continuity Equations . . . . . . . . . . . . . . . . . . . . . . . 59
A.2 Momentum Equations . . . . . . . . . . . . . . . . . . . . . . 60
A.3 Momentum Transfer Equations . . . . . . . . . . . . . . . . . 63
B Rate-Independent Fibre-Network Stress
65
C Numerical Solution with FEM
71
xii
Chapter 1
Introduction
“...rå materialet stötes i stenmortlar tillsammans med vatten. [...]de tidigaste pappersarken
formades genom att man förtunnade pappersmassan med vatten tills man hade en
slags fibervälling och därefter slog den över en ram med ett utspänt nät.”
Bo Rudin about the art of paper production in China at Ts’ai Lun’s time. Ts’ai Lun is
often named as the first papermaker.
In this chapter, first, the basic principles of the papermaking process
are shortly described. Then, the phenomena that are relevant for mechanical
dewatering in papermaking are presented together with experimental results,
which give support for the assumptions made in the development of the
models.
1.1
The Papermaking Process
The basic principles of producing paper from fibre suspensions have not
changed since the time of Ts’ai Lun in China 105 BC. This is also the principle in the first industrial paper machines (Figure 1.1) as well as in present
modern machines. However, production capacity has increased several orders
of magnitude, and paper quality has improved dramatically.
When the fibre suspension1 enters the paper machine, it has a solids content of approximately 0.5 percent, while the finished paper has a dry material
content in excess of 90 percent. Hence, 200 times the weight of the paper
produced has to be removed before it reaches the consumer (Figure 1.2).
1
The suspension contains fibres and water. When the fibres are entangled enough to
become a structure, they are called fibre mat or wet web, which sometimes also includes
air. The fibre network comprehends only the intra-fibre water and the fibres.
1
2
CHAPTER 1. INTRODUCTION
Figure 1.1: The paper machine presented by Donkin in Germany 1818
(Pires and Kuan, 1988)
Moreover, it is vital for the final paper quality the way water is removed.
Therefore, mechanical dewatering plays a central role in paper research.
Figure 1.2: A squematic picture of a paper machine showing the dewatering sections, and the approximate fibre concentration at different stages
(Pires and Kuan, 1988)
Water is removed from the fibre suspension, and later from the fibre web,
in three basic parts of a paper machine: in the forming, the press and the
drying sections. In the forming and wet pressing sections, water is removed
mechanically, whereas it is removed by evaporation in the drying section.
In the forming section, a jet with the fibre suspension is distributed onto
one or between two wires, where the paper is basically formed. Most of the
dewatering takes place in this section by wire tension as well as vacuum, with
the fibre web reaching a solids content of approximately 20 percent, when
it enters the press section. In the press section, water is also mechanically
removed from the web, but now with much higher pressure levels. A mechanical load is applied in a press nip, when the fibre web – covered with
one or two felts – passes between two rotating press rolls or between a press
roll and a press shoe. Usually, there are three or four press nips in a paper
1.2. MECHANICAL DEWATERING
3
machine, and these lead to an increase in the solids content to approximately
45 percent when the web leaves this section. In the drying section, most of
the remaining water is dried by evaporation as it passes over a number of
steam-heated cylinders, thus finalising the dewatering process.
As may be expected, the effort for removing water increases as the water
content decreases, which has consequences for the costs. The drying section has by far the largest costs as water is removed by evaporation. It is,
therefore, preferable to remove water, as much as possible, mechanically in
the cost-effective forming and pressing sections. Even small improvements in
mechanical dewatering could lead to significant cost reductions.
Reliable mathematical models of mechanical dewatering may contribute
to a better design and the optimisation of dewatering in the forming and
pressing sections. Furthermore, various important characteristics of the final
paper are determined by mechanical dewatering. Hence, a better understanding of the process, with the help of reliable physically based models,
may also lead to improvements in paper quality.
1.2
1.2.1
Mechanical Dewatering
Forming Section
The first generation of forming sections was the so-called Fourdrinier form- Types of formers
ing, where dewatering took place on a horizontal wire by the action of the
gravity. In the 1970’s, the second generation, twin-wire formers, started being increasingly used. The main advantages of twin-wire formers are the
increased dewatering rate (approximately four times dewatering in a Fourdrinier former), and the lessened two-sidedness. Although the retention is
worsened, the advantages, especially of being able to run the paper machine
at much faster velocities, exceed the disadvantages, and nowadays most machines have a twin-wire former.
Basically, there are two dewatering principles normally used in twin-wire
formers, viz. roll and blade formers. In roll formers, the suspension is fed
between two wires that wrap a roll. The applied pressure is approximately
constant and equal to the wire tension divided by the radius of curvature.
In blade formers, the suspension and the wires are deflected through a series
of opposing blades. In this case, the suspension experiences a series of small
pressure pulses.
4
CHAPTER 1. INTRODUCTION
Blade formers generate paper with good formation. There is, however, a
trade-off between formation and retention. Usually, to improve formation one
worsens retention. The pressure pulses generated by the blades are believed
to disrupt the larger flocs in the suspension by stretching, improving large
scale formation. The price to pay is the deteriorated retention, which requires
the addition of retention aids to keep it at an acceptable level. Roll formers,
on the other hand, usually produce paper with bad formation, but with a
good retention. Therefore, as pointed out in Nordström and Norman (1994),
roll-blade formers endeavour to achieve the best of both giving up as little as
possible. The initial mat is formed at a high retention. Later, in the blade
former region, the partially formed fibre mats help to enhance retention in
the formation-improving phase by acting as filters.
Dewatering
mechanisms
Baines (1967) divided conceptually dewatering in the forming section in
a twin-wire former in three zones, viz: the free-jet, the wedge and the press
zones2 (Figure 1.3). The free-jet zone is the region the suspension travels
after leaving the headbox until it impinges onto the wires. At the impinging
point the wedge zone starts, where the fibre mats – separated by the fibre
suspension in between them – are built up on the wires until they meet. In
this region, drainage occurs by filtration (Hisey, 1956; Parker, 1972). After
the contact point, dewatering occurs through compression of the fibre mats.
This is the press zone, where dewatering occurs by thickening, i.e. compression of the fibre mat. Comprehensive description of the forming process can
be found in Wrist (1962), Norman (1989) and Norman and Söderberg (2001).
Figure 1.3: A squematic figure with the different zones in the forming
section. The dewatering mechanisms in each zone are indicated.
2
Press zone should not be confused with the press section. Although the dewatering
mechanism is the same, they are two distinct things, and occupy different regions in the
paper machine.
1.2. MECHANICAL DEWATERING
1.2.2
5
Wet Pressing Section
The dewatering principle in wet pressing can be described as an intense
thickening. In wet pressing as well as in the press zone in forming, the
stress applied on the fibre network is balanced by two components, viz. the
hydraulic pressure and the fibre network stress (often called the structural
stress). The hydraulic pressure causes water to flow in-between the fibres,
whereas the fibre network stress deforms the fibre network. In wet pressing,
the difference is that, as the loads applied are much higher, the water flow
from the fibre walls may play an important role.
Campbell (1947) was the first researcher to make a detailed account of the
physics of wet pressing. He introduced Terzaghi’s principle (1944) from soil
mechanics into paper science. According to this principle, the total applied
stress in the nip, σT , is balanced by the sum of the hydraulic pressure, pw ,
and the fibre network stress (also called structural stress), σs . Nevertheless,
one should note that the Terzaghi’s principle is just a particular case of the
of the more general expression (Biot, 1941; Auriault and Sanchez-Palencia,
1977):
σT = φeff
a pw + σs ,
Stress
decomposition
Terzaghi’s
principle
(1.1)
eff
when φeff
a is equal to the unity. The parameter φa is called the effective areal
porosity and have to be determined experimentally (Kataja et al., 1995).
Although the total applied stress is approximately constant in the direction of application, the two components vary due to the flow. The hydraulic
pressure decreases in the direction of flow and the fibre network stress increases accordingly. Therefore, the layers closest to the surface where the
water leaves the medium are the most compressed. This phenomenon is
called stratification (MacGregor, 1989).
Still based on the stress decomposition in the nip, Wahlström (1969)
introduced the concepts of flow-controlled and pressure-controlled dewatering
according to the importance of each component in the right-hand side of
Equation (1.1). The idea of flow-controlled nips makes it easier to understand
the advantage of extended nip presses (ENP)3 , where one roll is replaced
by a press shoe. In these cases, the resistance imposed by the liquid flow
in-between the fibres is the limiting factor for dewatering. Therefore, the
3
Nevertheless, pressure-controlled nips may also experience dewatering improvements
(Wahlström, 1990).
Stratification
Flow- and
pressurecontrolled
nips
6
CHAPTER 1. INTRODUCTION
increased residence time in ENP enables a longer water flow time from the
web, improving dewatering.
1.3
Fibre/Water Separation Process
The physical modelling of the fibre/water separation process involves mass
and momentum balances of the components and some constitutive equations. As the geometry of the fibres is complex, simplifying assumptions are
frequently done, and the different phases are usually treated as continua. A
short survey of the of the experiments relevant for mathematical modelling
of mechanical dewatering is given below.
1.3.1
Darcy’s law
Flow Through Porous Media
Momentum exchange between the phases is often postulated to obey Darcy’s
law for homogeneous media subject to a pressure difference:
v=
Forchheimer
equation
K ∆pw
,
µ L
(1.2)
where v is the superficial velocity, pw is the hydraulic pressure, L and K
are the medium length and permeability, repectively, and µ is the fluid viscosity. Equation (1.2) neglects inertial forces, which seems to be reasonable
for Reynolds number, Re = ρrv/µ, less than unity (Bear, 1972; Scheidegger,
1974; Greenkorn, 1983). r is the average pore size radius4 and ρ is the fluid
velocity.Equation (1.2) has been extended in cases where inertial terms are
significant into:
∆pw
= av + bv 2 ,
L
(1.3)
where a and b are constants (Scheidegger, 1974; Dullien, 1979). This equation
is usually called the Forchheimer equation, and was suggested in the first
decade of the 20th century. It applies for Reynolds numbers larger than
unity.
4
Some researchers use the average fibre radius instead. However, some fibre modificating processes, e.g. beating, alter considerably the flow conditions without changing
markedly the average fibre radius.
1.3. FIBRE/WATER SEPARATION PROCESS
7
Equation (1.2) was originally presented by Darcy for isotropic, homogeneous5 porous media. However, fibre mats are highly compressible, and many
interesting separation processes have non-constant concentration or composition and therefore varying permeability through the medium. Moreover, the
flow resistance in the medium may also vary with direction. Equation (1.2)
is heuristically extended to heterogeneous, anisotropic media by expressing
it in the differential form:
v=
K
gradpw ,
µ
(1.4)
where K is the permeability tensor, which has to be described in the whole
medium. Thus, Darcy’s law may also be used in compressible anisotropic
media.
Permeability
measurements
Several researchers have examined the influence of porous media concentration on the permeability, using thick media in compression-permeability
(CP) cells (Collicutt, 1947; Robertson and Mason, 1949; Ingmanson, 1952,
1953; Nilsson and Larsson, 1968; Gren and Ljungkvist, 1983; Ljungkvist,
1983; Carlsson et al., 1983; Rasi et al., 1999). Their experimental results
for several different kinds of pulp fit well to Equation (1.2), which suggests
that inertial terms are negligible in those experimental conditions. Indeed,
Mantar et al. (1995) and Wildfong et al. (2000a) conclude that inertial effects
may be present but play only a secondary role in the flow through fibre mats.
Different relationships are employed to fit the measured permeability data
at different concentrations. Usually, at concentrations typical for wet press- Kozeny-Carman
ing, empirical relationships are used for fitting (Nilsson and Larsson, 1968;
Carlsson et al., 1983; Bloch, 1995), although considerable advances have been
achieved lately in modelling liquid flow through a unstructured medium (Koponen et al., 1998). At concentrations typical for forming, theoretical considerations underpinning the semi-empirical equations are employed to describe
the observed data. The theoretical model by Kozeny and Carman is the
one most used. It is an extrapolation of the Poiseuille equation to porous
medium by using the concept of hydraulic radius (Dullien, 1979). According
to this formulation, permeability, K, as a function of the concentration (or
porosity) is given by:
5
Homogenity is said of a property that is independent of the position, whereas isotropy
is said of a property that varies with the direction. As this text only considers heterogenities and anysotropies in the flow resistance, i.e. with respect to the permeability, this
property will be omitted for simplicity.
8
CHAPTER 1. INTRODUCTION
K=
φ3ext
,
k0 Sv2 (1 − φext )2
(1.5)
where k0 is the Kozeny constant, Sv is the specific surface area – i.e. the
external area per unit volume – in contact with the fluid and φext is the
external porosity, i.e. the ratio between the volume available for flow and the
total volume. According to the measurements by Ingmanson et al. (1959), k0
is approximately constant (= 5.55) for values of effective porosity until 0.8,
above which k0 increases dramatically.
The external porosity, φext , can be expressed as 1 − ac, where a is the effective volume and c is the concentration. Substituting it into Equation (1.5),
one obtains, after some rearrangement:
Kc
2
31
=
1
5.55Sw
13
(1 − ac) ,
(1.6)
where Sw = Sv a is the external surface area per weight of fibrous material.
Robertson and Mason (1949) examined the permeability of kraft and sulphite pulps beaten to different degrees over a concentration range between
five and twelve percent. They calculated the permeability parameters a and
Sw based on their measurements for trials with two kraft pulps and five
with sulphite pulp. Robertson and Mason’s (1949) and also Ingmanson’s
(1952) permeability data are in good agreement with Equation (1.6) for concentrations up to slightly above 15 percent solids content for sulphite pulp,
Figure 1.4.
Nevertheless, in order to obtain Equation (1.6), it was assumed that the
volume not available for flow in the fibre mats is constant, which definitely
is not true at high solids content. As the fibre network gets compressed, the
specific volume of the fibres diminishes, which will eventually lead to water
expression out of the fibre walls. It is also possible that water actually flows
through the fibres in conditions typical for pressing (Gustafsson et al., 2001;
Lucisano and Martinez, 2001). Both these phenomena would imply somewhat higher permeability values than the Kozeny-Carman equation reckons
(indeed, it gives negative permeability for concentrations, c, higher than 1/a);
the deviation increasing the higher the solids content is. Therefore, Meyer
(1969) suggest that a and Sw were a function of the stress in the fibre network. Wang et al. (2002) give another solution to this problem. They suggest
an exponential expression for φext as a function of concentration, in order to
avoid that porosity reaches zero.
1.3. FIBRE/WATER SEPARATION PROCESS
9
Figure 1.4: Left: Rectified permeability data as a function of the concentration for a series of beaten samples of sulphite pulp. The freeness
numbers are given in the diagram (Robertson and Mason, 1949). Right:
Similar results by Ingmanson (1952).
1.3.2
Fibre Network Compression
Fibre mats are highly compressible, and the fibre network stress induced by
fluid flow through the porous medium has a cumulative effect, resulting in
a heterogeneous porous medium. Also, as pointed out above, permeability
depends on the porosity. Therefore, in order to quantify the dewatering rate
in a heterogeneous medium with the help of Equation (1.4), a mathematical
description of the concentration as a function of the fibre network stress is
required.
Low Loads
Several researchers have reported the stress-strain behaviour of the fibre network at low mechanical loads and concentrations (Campbell, 1947; Ingmanson, 1952; Jones, 1963; Han, 1969; Gren and Ljungkvist, 1983; Vomhoff and
Schmidt, 1997; Jong, 1998; Boxer and Dodson, 1999). Usually the concentration is expressed as a function of the stress, σ, according to a power law
(Campbell, 1947):
Stress-strain
behaviour
10
CHAPTER 1. INTRODUCTION
c=M
σ
pr
N
,
(1.7)
where c is the concentration, pr is a reference pressure and M and N are
fitting constants6 (Gren and Ljungkvist, 1983).
In the forming section, fibre networks are at low concentrations (normally
below 20 percent). In this range, the fibre network is not compressed to such a
high extent that a considerable amount of water from inside the fibre walls is
squeezed out. Therefore, one would not expect the stress-strain behaviour of
the fibre mats would be rate-dependent in this range. Wilder (1960) studied
the influence of creep in the behaviour of a fibre network at low loads. For
short compression times (<40 ms) creep is of relatively little importance.
Nevertheless, based on the modelling of constant-flow drainage experiments,
Sayegh and Gonzalez (1995) obtained good agreement by assuming that the
fibre network behaves as a Maxwell element. However, one could suspect
that this might also be due to fines distribution in the thickness direction
(see section 1.3.3).
Hysteresis
Jones (1963) observed hysteresis in the compressibility behaviour of the
fibre networks (Figure 1.5). It is clear that the strain not only depends on
the applied stress, but also on the history of the compression. Therefore, the
following notation may be preferred:
σ ≡ σ[φ],
(1.8)
where the square brackets mean that σ at a given time depends on the whole
history of φ until that given instant.
High Loads
In saturated fibre mats, the water located in the interstices between fibres and
Intra- and
in the fibre lumens is called the extra-fibre water. In contrast, a considerable
extra-fibre water amount of water is also held in the porous structure of the fibre wall, the intrafibre water. The intra-fibre water can be estimated by different techniques
(Lindström, 1986), amongst the most common is the water retention value
(WRV).
The first evidence of the importance of the intra-fibre-water flow for pressing comes from experiments showing the expression of water out of fibre walls
6
pr is introduced just to avoid complex units in M and N .
1.3. FIBRE/WATER SEPARATION PROCESS
11
Figure 1.5: Hysteresis behaviour of solids concentration against applied
stress for a fibre network made of loblolly pine summerwood (Jones, 1963).
Carlsson et al. (1977). Therefore, in the wet-press section, the intra-fibre water flow may play an important role in the dewatering process.
Later, the effect of pressing on the intra-fibre water has been shown using different techniques (Laivins and Scallan, 1993b; Maloney et al., 1997;
Häggkvist, 1999). Maloney et al.’s (1997) and Häggkvist’s (1999) results
show that larger pores are closed first followed by continuously smaller pores,
and some pores are permanently closed (hornification). Moreover, some
intra-fibre pores can be reopened by dispersion (Maloney et al., 1997). Drying and beating are also shown to influence the amount of intra-fibre water
(Laivins and Scallan, 1993a, 1995).
Arguably, the water inside the fibre wall is more difficult to be removed
than the water in-between the fibres. Therefore, in press nips where a limited
impulse is available, the intra-fibre water appears to be the limiting solids
content that can be achieved after the press section (Figure 1.6).
Hence, it is now widely accepted that the effect of intra-fibre-water flow
should be included in the description of the stress-strain behaviour of the fibre
network. Accordingly, Wahlström (1990) proposes the further decomposition
of the total stress:
σT = pw + σs = pw + σs,eq + σs,f l ,
(1.9)
12
CHAPTER 1. INTRODUCTION
Figure 1.6: Influence of the water retention value on the final solids
content for several different pulps (Busker and Cronin, 1982).
where, the fibre network stress is decomposed in σs,eq and σs,f l , the static
compression curve and the resistance to compression due to flow out of the
fibre wall, respectively.
Expansion
Dynamic measurements of the stress-strain behaviour of the fibre network
show considerable rate dependence (Ellis, 1981; Szikla and Paulapuro, 1989;
Vomhoff, 1998; Lobosco, 2000). Further, during the unloading phase, there is
usually little or no expansion of the fibre network before the applied pressure
comes to zero (Vomhoff, 1998). However, some slow but significant expansion
does occur if the web is unloaded completely.
1.3.3
Specific
Resistance
Flow with Compression
In several experiments, for practical reasons, the fibre mat flow resistance is
measured by filtration where a considerable compression of the fibre network
takes place due to flow. The fibre mat flow resistance is thus given in terms
of flow specific resistance 7 , Rw , independent of the thickness, which is a
function of the pressure drop through the medium and is given by:
7
When, for simplicity, the term resistance is used, it is referred to the flow specific
resistance.
1.3. FIBRE/WATER SEPARATION PROCESS
Rw =
∆pw
,
vµw
13
(1.10)
where v is the superficial velocity and w is the grammage (Ingmanson, 1952).
Notwithstanding the fibre mat compression, the medium permeability parameters can be obtained from the specific resistance by taking into account
the fibre network deformation with the help of Equation (1.7). Ingmanson
(1952, 1953) obtains permeability parameters in good agreement with permeability results from a CP-cell. However, it is usual to just study the specific
resistance of fibre mats under different conditions.
Herzig and Johnson (1999) have studied the flow resistance due to the
wires. Their results fit well to Equation (1.3), i.e. Forchheimer’s. Wildfong
et al. (2000b) draw the same conclusion based on results from a laboratorydrainage tester. However, the influence of the resistance to flow due to the
wire is acknowledged to be much greater than could be accounted for by
simply adding it to the fibre mat resistance (Meyer, 1969; Radvan, 1980).
The interaction between fibre mat/wire implies an additional flow resistance,
due to the self-healing effect, i.e. the fibres are deposited in apertures in the
wires.
This phenomenon has been acknowledged as early as in 1962 by Han. His
data from an experimental vacuum former show a fast resistance increase
until 10–20 g/m2 , of approximately the same order as can be seen in the
measurements of Herzig and Johnson (1999) and Jong et al. (1999). Jong
et al.’s results show a fast resistance increase until a mat of approximately
20 g/m2 is formed, followed by a monotonic decrease. However, neither of
them attribute these phenomena to an interfacial resistance. In fact, by
expressing the effective resistance as a sum of the interfacial resistance, Ri ,
and the mat resistance, Rw , one obtains for grammages above w0 :
Reff =
Ri w0 + Rw (w − w0 )
,
w
(1.11)
where w0 is the grammage in the interfacial layer (here w0 ∽ 20 g/m2 ) and
Reff is the overall (effective) resistance of the mat and the interface. The
interfacial resistance, Ri , is given by the average resistance in the interface,
w0 (Figure 1.7). Equation (1.11) can be applied to the experimental results
by Han (1962) and Jong et al. (1999). For small Ri or large8 w, Reff is
approximately Rw .
8
CP-cells usually use high fibre grammages.
Wire
Interface
14
CHAPTER 1. INTRODUCTION
Concluding, flow resistance due to the wires is significant only in the
cases of fast-draining pulps and over the initial impingement area (Herzig and
Johnson, 1999). Further, the interfacial resistance may play an important
role in mechanical dewatering. However, there is not much data on this
subject, nor a stablished form of how to model it.
Figure 1.7: A possible dependence of the incremental specific resistance,
R, on grammage, w, for an unbeaten pulp.
Fines
Mantar et al. (1995) estimate the fibre-mat resistance to flow using a
constant-pressure drainage tester. They show a fibre mat flow resistance increasing with fines content in the pulp. In contrast to Jong et al. (1999), the
estimated resistance does not include the contribution from the interfacial
resistance, which was accounted together with the wire resistance instead.
Therefore, Mantar et al. (1995) do not observe the decaying pattern shown
by Jong et al. (1999). Mantar et al.’s results (1995) show an increase in resistance with grammage for pulps where fines are present, and approximately
contant resistance for an unbeaten pulp. They attribute this phenomenon
to an increase in entrapment of fines with grammage. This is corroborated
by the results of Han (1962) and Wildfong et al. (2000a,b), although the
supposed interfacial resistance was included in the resistance in their case.
In this case, the interfacial resistance must have been small. Han (1962) and
Wildfong et al. (2000a) measured the retention as a function of grammage.
They observed an increase of retention with grammage, which was attributed
to be the reason of the increased flow resistance.
Mantar et al. (1995) also studied the influence of the slurry concentration
on the fibre-mat resistance, and observed a maximum value at approximately
0.5 percent for bleached softwood kraft pulp. At lower concentrations the
1.4. MODELLING
15
fines concentration decreases, whereas, at higher concentrations, flocculation
increases. Both lead to decreasing flow resistance.
Concluding, fines and flocculation may play an important role in the
resistance to flow. Therefore, a fibre mat with constant concentration may
not have a constant permeability due to changes in flocculation condition
and the fines content.
Accordingly, Sayegh and Gonzalez’s (1995) results could be reinterpreted
in a different way than the authors’. They attributed the increase in flow
resistance to the visco-elastic compression of the fibre network. However,
in opposition to what one would intuitively expect, groundwood pulp presented a viscous parameter that was approximately five times larger than
that for unbleached hardwood kraft pulp, which has far more intra-fibre water. Further, the viscous contribution increased with decreasing CSF, which
one expects to correlate with the amount of fine material. In contrast to
that, the increased flow resistance could be attributed to the increasing fines
retention, which enhances flow resistance, as the experimental results by Han
(1962), Mantar et al. (1995) and Wildfong et al. (2000a,b) have shown.
1.4
1.4.1
Modelling
Forming
All the models that take into account the effect of the fibre mat deformation
use a power law to describe the relationship between the concentration and
the fibre mat stress (Meyer, 1962; Emmons, 1965; Martinez, 1998; Zahrai
et al., 1998). There are no models hitherto that take into account the behaviour of the fibre mats during unloading or reloading. Therefore, these
models are limited to situations where the applied stress in the fibre mats
never decreases, and it is not possible to use these models to study the dewatering of the fibre mats after they leave the forming roll, for instance.
Several researchers have modelled dewatering in roll formers (Baines,
1967; Wahren et al., 1975; Hauptmann and Mardon, 1973; Norman, 1979;
Miyanishi et al., 1989) and the pressure distribution around blades (Zhao
and Kerekes, 1995; Nigam and Bark, 1997; Zahrai et al., 1997; Holmqvist,
2002) without considering the fibre network deformation and effect on permeability. There are, however, a few exceptions.
16
CHAPTER 1. INTRODUCTION
Martinez (1998) developed a physically based model of the dewatering
rate in twin-wire roll formers taking into account the deformation of the
fibre mats. The model disregards the time derivative, which means that
the diffusion term balances the convective one completely. As Boxer et al.
(2000) pointed out, this assumption implicitly means that the model only
can handle constant pressures as a boundary condition on the wires.
1.4.2
Wet Pressing
Several models of wet pressing has been proposed. However, most of them
show stress-strain relationships of the fibre network, which do not present rate
dependence. Some consider the fibre network to be only elastic (Roux and
Vincent, 1991; Bloch, 1995), whereas others also consider (rate-independent)
plasticity (El-Hosseiny, 1990; Kataja et al., 1992; Riepen et al., 1996; Bezanovic
et al., 2002).
In contrast to those, Ceckler and Thompson (1982) presented a model of
wet pressing, which includes a rate-dependent description of fibre-network
compression. This description presents an elastic part, attributed to fibre
bending, and a rate-dependent part, attributed to the expulsion of the water
from the inside the fibres. However, this mathematical description shows
too large an expansion during unloading, which has not been observed in
experiments (Vomhoff, 1998).
McDonald and Kerekes (1991a,b, 1994) presented an alternative solution
to include intra-fibre-water dewatering, the decreasing permeability model.
They suggest a model of wet pressing, in which intra- and extra-fibre flow
resistance is considered, but the mechanical stiffness of the fibre network is
ignored. The model is useful for solids content determination within the operability regions where the parameters were estimated. However, it gives little
insight into the real physical phenomena taking place in web consolidation.
Concluding, models of the fibre network rheology, which can be used in
reliable physically based models of wet pressing are needed, but are not yet
available. Indeed, according to Börje Wahlström (1990):
“None of the serious attempts of mathematical modeling of water
removal by pressing, [...], have taken water in the fiber wall into
account and have therefore been unable to properly describe wet
pressing.”
1.5. SUMMARISING
1.5
17
Summarising
Forming There are good experimental results supporting the modelling of
mechanical dewatering by considering the suspesion and the wires as continua. However, the following conclusions can be drawn, which are not taken
into account in the modelling of dewatering:
❼ The fibre mats are heterogeneous due to flocculation and the uneven
distribution of fines.
❼ The interfacial flow resistance, i.e. due to the first layers of fibres on
the wire (10–20 g/m2 ), may play an important role.
❼ The stress-strain relationship may be considered rate independent but
presents hysteresis.
Wet Pressing In wet pressing, intra-fibre water is pressed out of the fibre walls, which results in a rate dependent stress-strain relationship of the
fibre network. Rate dependence is also observed in the slow but significant
expansion taking place after the end of the pressure pulse. There is no mathematical model that captures these phenomena.
1.6
Objectives
The specific objectives of the work reported in this thesis were:
1. To develop a model of dewatering in twin-wire formers with special
focus on the fibre network stress and the deformation gradients in the
thickness direction that are generated. Further:
❼ The model should be able to calculate the effects of complex pressure profiles that are generated through the forming section.
❼ The stress-strain relationship used should include hysteresis.
2. To develop a model of the stress-strain behaviour of saturated fibre
networks when subjected to pressure pulses that are typical for wet
pressing.
18
CHAPTER 1. INTRODUCTION
Chapter 2
Modelling of Dewatering in
Forming
”I have always found it difficult to read books that cannot be understood without too much
meditation. For when following one’s own meditation, one follows a certain natural
inclination and gains profit along with pleasure; but one is enormously cramped when
having to follow the meditation of others.”
Gottfried Wilhelm von Leibniz (1646–1716)
In this chapter, a physically based model of the forming and densification
of fibre mats in twin-wire formers is presented. The model was used to
estimate the dewatering and the concentration gradients in the fibre mats
along the forming section.
This model can handle time-varying stress as boundary conditions on the
wires. Also, the stress-strain behaviour of the fibre mats presents hysteresis1 , which enables to use the model to study dewatering and concentration
gradients after the fibre mats leave the forming roll.
A number of numerical studies were performed. The effect of sequential
blade pressure pulses after the forming roll on the dewatering and the concentration gradients could be characterised. Increasing wire tension resulted
in increasing dewatering, but the rate of increase diminished rapidly. The
simulations also exhibited an elastic expansion of the fibre mats against the
suspension and the wires, sucking back water, when they left the forming
roll. The effect of beating showed a large influence on dewatering.
1
This description is rate independent, as intra-fibre water is assumed not to leave the
fibre walls. Other sources of rate-dependence were also assumed negligible.
19
20
CHAPTER 2. MODELLING OF DEWATERING IN FORMING
2.1
Model
It was assumed that there is no air, that the two wires are symmetrical and
that dewatering occurs only in the z-direction (Figure 2.1). Further, inertial
terms were neglected. Terzaghi’s principle was considered applicable, and
Darcy’s law was assumed to apply. The detailed derivation of the equation
used here is presented in the Appendix A. The final convective-diffusive
equation obtained for the porosity, φ, obtained was:
∂
∂φ
∂
+
(φvf ) −
∂t
∂z
∂z
K ∂σf 0
µ ∂z
= 0,
(2.1)
where vf is the fibres velocity, σf 0 is the stress in the fibre network and K
and µ are the medium permeability and the viscosity, respectively.
Figure 2.1: The system being modelled and the coordinate system used.
2.1.1
Constitutive Equations and Physical Properties
Equation (2.1) involves physical properties and constitutive equations, which
had to be provided in order for the equations to be solved. Permeability was assumed to obey the Kozeny-Carman relation (Equation (1.5)) and
the parameters were taken from Robertson and Mason (1949) presented in
Table 2.1. The paramenter k0 was assumed constant and equal to 5.55.
Equation (1.5) is a rather simplified description compared to what actually
2.1. MODEL
21
happens in between the wires. It does not take into account the variations
in permeability due to the non-homogeneous distribution of fines and flocs
in the forming web mats.
The mathematical description of the fibre network stress, σf 0 , used here
is thoroughly explained in Appendix B. The fluid viscosity, µ, was assumed
constant and equal to 10−3 Pa ➲ s (Perry et al., 1984).
Table 2.1: The effect of beating in terms of the Canadian Standard Freeness (CSF) on the permeability parameters (Robertson and Mason, 1949).
CSF
718
708
598
454
384
2.1.2
kraft 1
a
[ cm3 /g]
4.27
4.60
4.60
4.70
4.91
Sw
CSF
[ cm2 /g]
9100
738
11500
703
28300
541
37300
429
43000
292
kraft 2
a
[ cm3 /g]
3.66
4.57
4.70
4.87
4.67
Sw
[ cm2 /g]
9500
9700
31600
41600
58400
Initial and Boundary Conditions
The mathematical model also requires an initial and two boundary conditions.
Initial Condition. The porosity at t = 0 has to be given for every z:
φ(t = 0, z) = φ0 (z) = 0.99.
(2.2)
Boundary Conditions. At the symmetry plane, z = 0, the water velocity
was assumed to be equal to the fibre velocity, therefore the hydraulic pressure gradient vanishes at that point for every t. Consequently, the porosity
gradient was assumed to vanish:
vv (t, z = 0) − vf (t, z = 0) = 0 ⇒
∂φ
∂z
= 0.
z=0
(2.3)
22
CHAPTER 2. MODELLING OF DEWATERING IN FORMING
For some wires, the superficial open area is large enough to render a
negligibly small flow resistance even in comparison to very thin fibre mats
(Radvan, 1980). The flow resistance imposed by the wire was thus neglected.
However, the fibre/wire interaction may have a significant resistance. This
was not, however, taken into account because of lack of reliable data. Nevertheless, the model could be easily extended to also include those effects by
attributing the interfacial properties to the first deposited layers of fibres.
At the upper boundary, z = h (where h is half of the suspension thickness2 ), the fibre network stress was given, as the hydraulic pressure was
assumed zero. Therefore, the fibre network stress was set equal to the total
pressure experienced by the suspension and the formed web, i.e.
σf 0 (t, z = h) = σT (t) .
(2.4)
Moreover, with the help of the stress-porosity constitutive equation, the
porosity, φ(t, z = h), can be calculated for the given applied stress, σT .
2.1.3
Numerical Solution
The final Equation (2.1) together with its initial, Equation (2.2) and boundary conditions, Equations (2.3) and (2.4), the constitutive equations and
physical properties were solved with the finite element method. This is described in Appendix C.
The model output is porosity, φ (together with φmin and φmax ), as a
function of t and z. Based on these results, several different quantities can
be calculated, e.g. dewatering rate, fibre and water velocity, structural stress,
hydraulic pressure, etc. The results were transformed to solids content, SC,
according to the relation:
SC =
1
1+
φ ρw
1−φ ρf
.
The specific dewatering rate, i.e. the Darcian water velocity at z = h, was
calculated from:
qv (t, z = h) = −
Z
0
2
h
∂φ
dz.
∂t
(2.5)
In order to calculate the suspension thickness, the fibre material density, here assumed
to be 1550 kg/m2 (Carlsson et al., 1983), and the grammage, which in all the simulations
was 100 g/m2 , is required.
2.2. RESULTS AND DISCUSSIONS
2.2
23
Results and Discussions
The model was used to simulate the effects of blade pulses, wire tension
and beating. Typical simulation results are shown in Figure 2.2, where
it is demonstrated how the fibre mats are being formed on the wires, and
how the dewatering rate decreases with the amount of deposited fibres3 .
The simulations show that the suspension between the fibre mats was being
dewatered by filtration. Further, it shows concentration gradients in the fibre
mats, indicating they were being dewatered by thickening even when there
was a suspension in between them.
Figure 2.2: Left: Model predictions for the solids content in a roll-blade
former of unbeaten kraft pulp. The dewatering pressure profile was a
constant pressure of 8 kPa during 20 ms and two haversine pulses with
peak pressures of 15 and 20 kPa and pulse lengths of 10 ms and separated
in time by 10 ms. Right: The dewatering rate for this simulation.
When the fibre mats left the roll, there was a partial expansion of the
mats, which sucked water back into the mat, showing that rewetting may
occur at the very early stages in a paper machine. The calculations showed
that the fibre mats also expanded into the suspension, contributing to an
increase of the amount of deposited fibres, although the average solids content
obviously decreased.
3
There was, however, no sharp distinction between the suspension and the fibre mats
in the model. The initial concentration of the suspension was already above the sediment
concentration, and the fluid-like behaviour of the suspension, which depends on shear
forces, was not considered in this study. The suspension region was arbitrarily considered
to be determined as the region where less than a 20-percent-concentration change occurred
in each simulation.
Rewetting
24
CHAPTER 2. MODELLING OF DEWATERING IN FORMING
Two blades could be modelled assuming a blade pressure profile. This
required the insertion of the pressure profile as a boundary condition but no
other modification. The simulations show sharp gradients in solids content
at regions close to the wire. Note that this region with large gradients expands after each successive pulse. This was probably a consequence of the
compressibility behaviour of the fibre mat, which includes hysteresis.
Unfortunately, the model has a limitation with respect to the pressure
profile that can be used in the simulations. The “blade pulses” must have a
large enough impulse as to deform the elements at least as much as the previous pulse, in order to give a proper description of the fibre network stress
during unloading. In order to describe the fibre network stress throughoutly,
one needs either more internal variables from the porosity history or a hysteresis operator.
Wire tension
Model simulations confirmed the phenomenon that dewatering increases
nonlinearly with increasing wire tension, T (Figure 2.3). This is related
to the rapid decrease of permeability as the fibre mats get compacted. This
result has been observed in pilot paper machines but cannot be obtained with
models where the compressibility, and consequently the strong reduction in
permeability of the fibre mats, are not taken into account.
Figure 2.3: Model predictions of the final average solids content as a
function of the constant wire generated stress during 20 ms and no stress
during 20 ms (pressure profiles analogue to those used in Figure 2.4).
Beating
The influence of beating was studied by comparing the effect of a beaten
(CSF 598) and an unbeaten (CSF 718) kraft pulp on the dewatering and
forming of fibre mats in the roll section prior to the first blade (Figure 2.4).
2.2. RESULTS AND DISCUSSIONS
25
A constant pressure pulse of 8 kPa under 20 ms followed by no load during
the next 20 ms was applied as boundary condition.
Figure 2.4: Model predictions for the solids content in a roll-former
at two different beating degrees. Left: unbeaten kraft pulp (CSF 718).
Right: beaten kraft pulp (CSF 598). The dewatering pressure was 8 kPa
under 20 ms and no pressure under the following 20 ms.
There was a large difference in dewatering rate between the two beating
levels. In the unbeaten case, approximately 80 percent of the suspension was
dewatered, whereas for the beaten pulp only approximately 20 percent of
the water was removed in the first 20 ms. This was due to the difference in
permeability of the two fibre mats, as the stress-strain behaviour of the fibre
network shows not to be dependent on beating (Han, 1969). It is possible
that the model is overestimating the effect of beating in dewatering since it
has a simplified description of permeability. To get more accurate results
it will be necessary to consider the variations in permeability due to the
heterogeneous distribution of fines in the forming web mats.
The model does not take into account the effect of the wire- and the interfacial wire/fibre-flow resistances. However, wire permeability is important
only in the very beginning of the dewatering process, therefore, the results
would probably not have changed significantly, if it had been included. The
wire/fibre-flow resistance was not taken into account because of lack of data.
Its influence should probably increase with increasing number of openings
per unit area for modern wires.
26
2.3
CHAPTER 2. MODELLING OF DEWATERING IN FORMING
Concluding Remarks
This section presents a model of the forming and densification of the fibre
mats in twin-wire formers, which endeavours to overcome two limitations
in previously published models. First, it allows for time-varying stress in
the boundary condition. Second, it can account for hysteresis in the fibre
network stress. Therefore, it was possible to simulate the fibre mat recovery
at the end of the roll former and pressure pulses in the blade section.
Model simulations indicate that increasing wire tension resulted in increasing dewatering, but the rate of increase diminished rapidly. The effect
of sequential blade pressure pulses after the forming roll on the dewatering
and the concentration gradients could be characterised. Model simulations
also indicate the possibility of rewetting when the fibre mats leave the forming
roll. The effect of beating showed a large influence on dewatering. However,
this influence may be overestimated as the permeability relation employed
did not consider the effect of the heterogeneous distribution of fines in the
fibre mats.
Chapter 3
The Perzyna Model
”The felling of awed wonder that science can give us is one of the highest experiences of
which the human psyche is capable. It is a deep aesthetic passion to rank with the
finest that music and poetry can deliver. It is truly one of the things that makes life
worth living and it does so, if anything, more effectively if it convinces us that the
time we have for living is finite.”
Richard Dawkins (1941 – ) in Unweaving the Rainbow 1998
This and the next chapters deal with wet pressing. The mathematical
modelling of wet pressing, analogously to the modelling of the forming section
described in the previous chapter, requires constitutive equations in order to
be solved. One of these, is the relation between the fibre network stress1 ,
σf 0 , and the porosity, usually called stress-strain or rheological behaviour.
However, the term rheological is used only to describe stress rate dependence.
Also, as an abuse of the terminology, sometimes the model is referred to as
a model of the fibre network stress, even though the strain that is modelled.
Rheological
behaviour
As pointed out in the introduction, the stress-strain behaviour of the
fibre networks at high loads is rate dependent, and it is, at least partially,
dependent on the intra-fibre-water flow.
Initially, a model based on the concept of strain-rate dependent plasticity,
including a rate-independent elasticity, was developed in order to describe the
observed experimental data (Perzyna, 1966). This model is presented in this
chapter and is called the Perzyna model. Models of this kind is sometimes
referred to in the literature as elastic/viscoplastic models. It showed good
agreement with experimental results for the compression phase, therefore it is
employed in physically based models of wet pressing (Gustafsson and Kaul,
2001; Gustafsson et al., 2001). However, the Perzyna model gave poorer
1
For simplicity, the subspript will be omitted in this and next chapters.
27
Elastic/
viscoplastic
model
28
CHAPTER 3. THE PERZYNA MODEL
results, when describing unloading as a rate-independent process. Moreover,
it could not describe the experimentally observed behaviour of a sequence of
pressure pulses. Therefore the Perzyna model was further developed. This
is shown in the next chapter.
3.1
Experiments
Vomhoff and Norman (2001) conceived a special measuring cell (Figure 3.1),
with which measurements of the rheological behaviour of the fibre networks
can be obtained. This cell can be placed in a material testing machine to
conduct uniaxial compression tests on saturated fibre networks.
Figure 3.1: The compression device conceived by Vomhoff (1998). The
inset shows the water flow pattern.
Webs placed in the test cell are compressed between a smooth non-porous
surface on one side and 1 mm thick bars spaced 1 mm apart on the other.
The pressure pulses applied by the testing machine can vary greatly in shape,
pulse length, peak pressure and the cell even allow measurements at different
temperatures (Vomhoff and Norman, 2001).
3.1. EXPERIMENTS
29
The experimental trials were performed using webs of 20 or 30 g/m2 of
thermo-mechanical pulp (TMP) and softwood bleached kraft pulp (SBK)
beaten to different levels. The response of the web thickness to the pressure
pulse was recorded as a function of time (Figure 3.2). The modified strain
was calculated based on web thickness according to:
ǫ = ln
h
h0
,
(3.1)
where h0 = w/ρf is the thickness the web would have at zero porosity, and
w and ρf are the grammage and the fibre material density. Expressing the
experimental results in modified strain reduced greatly the variation between
different tests, as it does not require the initial strain, which is difficult to
determine experimentally. The results were, however, presented as a function
of solids content, SC, according to:
SC =
ρf
,
ρf + ρw (hρf /w − 1)
(3.2)
as it is a better known quantity for the papermaker. The fibre material
density, ρf was assumed to be 1550 kg/m3 for bleached sulphate (Carlsson
et al., 1983).
MODIFIED STRAIN [−]
STRESS [MPa]
−1
−2
−3
−4
−5
−6
−7
−8
2.6
0
2.4
−1
2.2
STRESS [MPa]
0
2
1.8
1.6
1.4
20
40
60
80
100
120
−3
−4
−5
−6
1.2
−7
1
0
−2
0.8
0
20
TIME [ms]
40
60
TIME [ms]
80
100
120
−8
0.8
1
1.2
1.4
1.6
1.8
2
2.2
2.4
MODIFIED STRAIN [−]
Figure 3.2: Left: An arbitrary pulse applied to the wet web. Centre:
the response in thickness measured as a function of time. Right: the
experimental response in a stress-modified strain graph.
3.1.1
Sources of Error
The water from the saturated web flows primarily in the in-plane direction,
to the grooves between the bars. Since the design of the test cell ensures
2.6
30
CHAPTER 3. THE PERZYNA MODEL
that water flows primarily in the in-plane directions, the compression of the
web is assumed to be uniform in the thickness direction, which is one of the
requirements to obtain a reliable uniaxial measurements of the stress-strain
behaviour of the fibre network.
Experimental
error
Nevertheless, the stress measured is not exactly the fibre network stress.
Part of the applied stress is balanced by the hydraulic pressure developed
in the extra-fibre space (Vomhoff and Norman, 2001). On the other hand,
according to them, the contribution of the hydraulic pressure due to the inplane flow amounts to only seven percent of the total work performed for the
fastest of their pulses (20 ms) for a similar pulp with almost the same beating
level (23.3 SR in contrast to 25.2 SR used here). For the case for SBK pulps
with 16.3, 35.1 and 62.7 SR, no reliable permeability data were available, and
the influence of the hydraulic pressure from the flow in between the fibres
was not studied. It was probably negligible for the case of 16.3 SR, but could
be significant for the cases with 35.1 and 62.7, especially for the shortest
pulses. Vomhoff (2000) reports high influence of the hydraulic pressure for
the shortest pulses performed with TMP (75 percent of the work for pulses
of 25 ms).
A second type of experimental error is observed in comparing results
from trials with nearly the same pulse profile (Vomhoff and Norman, 2001).
They report relative error at minimum achieved modified strain to be less
than ten percent. These two contributions are henceforth referred to as the
experimental error.
In conclusion, although the best experimental equipment available was
used, these is, nevertheless, some error in the experimental data obtained.
Consequently, the estimated parameter values of the model will carry conModelling error tributions from the experimental error in addition to any eventual modelling
error.
Initially, the behaviour of TMP was examined, and then the material parameters were estimated. Finally, the constitutive equations were validated.
The tests were performed with webs of 20 g/m2 . The experimental data in
Table 3.2 were used in the study of the influence of temperature and intrafibre water in the rheological behaviour of the fibre network stress for SBK.
The tests were performed with webs of 30 g/m2 made of SBK pulp. Some
tests were kindly made available by Vomhoff (1998).
3.1. EXPERIMENTS
31
Table 3.1: Tests performed with webs of 20 g/m2 made of TMP (CSF
235 ml, except the three last rows which have CSF 123 ml). The tests
marked with the symbol ‘*’ were conducted by Vomhoff (1998). The
quasi-static tests were performed with a pulse length of 130 s made of SBK.
Pulse Length Peak Pressure Temperature
[ms]
[MPa]
[o C]
(25, 75)*
3, 8, 23
23
250, 2500
3, 8*, 23*
23
27
3, 10, 20
23
270
3
23
25, 75, 250, 2500
8, 23
23
130000
23
23
699000
15
23
699000
15
50
699000
15
80
Pulse Shape
—
Roll
Roll
Shoe-press
Shoe-press
Strain ramp
Strain ramp
Strain ramp
Strain ramp
Strain ramp
Table 3.2: Tests performed with webs of 30 g/m2 made of SBK pulp.
The tests marked with the symbol * were conducted by Vomhoff (1998).
The quasi-static tests were performed with a pulse length of 349 or 699 s
made of SBK.
Pulse Length
Peak Pressure WRV
[ms]
[MPa]
[g/g]
20, 200, 2000, 349000
8
1.26
20, 200, 2000, 349000
8
1.43
20, 200, 2000, 349000
8
1.51
20, 200, 2000, 349000
8
1.65
(20, 200, 2000)*
5, 10, 20
—
(20, 200, 2000)*
5, 10, 20
—
(20, 200, 2000)*
5, 10, 20
—
699000
20
—
699000
20
—
699000
20
—
SR Temp.
[cl]
[o C]
16.3
23
25.2
23
35.1
23
62.7
23
22.3
23
23.7
50
22.3
80
22.3
23
23.7
50
22.3
80
32
CHAPTER 3. THE PERZYNA MODEL
Figure 3.3: Two experimentally determined stress-solids content curves
obtained from tests with nearly identical applied pulses (8 MPa and
75 ms). The difference between the curves exemplifies the order of magnitude of the highest experimental errors.
3.2
Model
A model of the stress-strain behaviour of the fibre network in wet pressing
should present rate-dependent strains, as observed in the experimental work
of several researchers (Ellis, 1981; Szikla and Paulapuro, 1989; Vomhoff and
Norman, 2001). In our first attempts to model the fibre network force we
applied the standard approaches to visco-elasticity. However, we were not
able to obtain a model which gave good agreement with experimental results.
We concluded it would be necessary to apply plasticity theory, and that led
us to Perzyna’s approach to visco-plasticity (1966). It has two desirable
properties, viz. it allows for time-varying stress and the terms can be nonlinear. Moreover, it could also easily incorporate a term making the ratedependent plasticity also dependent on the strain. Therefore it was employed.
In Perzyna’s approach, the total strain rate is decomposed into elastic (recoverable) and plastic (non-recoverable) parts. Using a logarithmic definition
of strain, ǫ, the total strain rate is then given by
dǫpl
dǫel
dǫij
ij
ij
=
+
.
dt
dt
dt
(3.3)
pl
where ǫel
ij are the components of the elastic strain, and ǫij the components of
the plastic strain tensor. This is a reasonable assumption even for large total
3.2. MODEL
33
strains, provided the elastic strain is small compared to the plastic strain.
The two components of the total strain rate were modelled independently,
and the plastic part of the strain rate included rate-dependent effects. The
proposed model may therefore be classified as elastic/viscoplastic.
Non-linear elasticity The submodel proposed for the observed non-linear
elasticity was:
σ/3 − pt
,
ǫ = ln 1 − Dln
−pt
el
(3.4)
where σ is the (uniaxial) applied stress, pt and D are parameters. This (rateindependent) expression was used in modelling the elastic part of the total
strain.
Rate-sensitive plasticity The approach proposed by Perzyna (1966) for
modelling rate-sensitive plasticity is followed here. He introduces a static
load function, F , in the form:
F (σij , ǫpl
kl )
=
f (σij , ǫpl
kl )
κ(ǫpl
e )
− 1,
(3.5)
where the function f is the dynamic load function, κ(ǫpl
e ) is a hardening funcpl
tion , and ǫkl are the components of the plastic strain tensor (Perzyna, 1966).
When the dynamic load function, f , is less or equal to the hardening function,
κ(ǫpl
e ), then the static load function, F , is equal to the yield criterion in the
inviscid plasticity theory. However, in Perzyna’s approach to viscoplasticity,
f is allowed to exceed the yield limit, κ(ǫpl
e ). The positive difference between
pl
f and κ(ǫe ) is called the overstress. The function, F , may be interpreted
as a normalised overstress. Perzyna proposes that the plastic strain rate be
expressed as a function of the normalised overstress, F , according to:
dǫpl
∂f
ij
= γc hΩc (F )i
,
dt
∂σij
(3.6)
where γc is a viscosity parameter, and hΩc (F )i is a function that has be chosen
to represent the results of tests under dynamic loading2 . A representation of
2
The symbol hai denotes the Macauley brackets having a value of a for a > 0 and
vanishing otherwise.
34
CHAPTER 3. THE PERZYNA MODEL
the results of the available uniaxial dynamic tests can be given by (Lobosco,
2000):
Nc
c
,
Ωc (F ) = Ψm
c F
(3.7)
where
Ψc =
− κ(ǫpl
ref )
pl
κ(ǫref )
κ(ǫpl
e )
!2
mc
+ 1
.
(3.8)
ǫpl
ref is a reference plastic strain assumed to be 1.9 for any pulp, and mc and
Nc are material parameters.
As only uniaxial compression was considered here, the dynamic load function, f (σij , ǫpl
kl ), was taken to be the applied uniaxial stress, σ, and the hardening function, κ(ǫpl
e ), reduced to the static stress-plastic strain relation,
pl
σy (ǫ ). Thus, the static yield function became:
F =
σ
− 1.
σy (ǫpl )
(3.9)
Finally, rewriting Equation (3.6) for the uniaxial case, and using Equation (3.7), one obtains:
dǫpl
= γc Ψmc F Nc ,
dt
(3.10)
which was solved numerically with a Runge-Kutta algorithm together with
Equation (3.8) in order to obtain dynamic expressions for the modified strain,
i.e ǫpl from σ(t) as input variable.
3.3
3.3.1
Results and Discussions
Parameters Estimation
The elastic parameters of Equation (3.4), pt and D, and the plastic ones from
Equation (3.10), γc , mc and Nc , are different for different pulps, and may
3.3. RESULTS AND DISCUSSIONS
35
change with beating and temperature. Obviously, they should not change
with peak pressure, nor with pressure pulse shape and nor with pulse length.
The parameters were estimated using a small subset of the available experimental data for each experimental setting. The remaining tests were
used to validate the model. The elastic parameters were estimated from the
tests with the shortest pulse length, viz. 25 ms pulse length for TMP and
20 ms for SBK. They were estimated from the region of the stress-modified
strain curve, where the total modified strain starts to recover. The estimated
values for TMP were: D = 0.037 and pt = 0.2 MPa.
Webs made of TMP showed a significant elastic strain, whereas webs
made of SBK showed a much smaller, almost insignificant elastic strain.
Therefore, the elastic strain may be disregarded in the case of SBK, without
any markedly change in the final results.
Having estimated the elastic parameters, the experimental plastic strain
was determined by subtracting the calculated elastic part from the modified
total strain, according to:
ǫpl = ǫ − ǫel .
(3.11)
The strain decomposition being allowed because the compression is uniaxial.
For TMP, the parameters γc , Nc and mc were estimated by varying them
in an iterative procedure to minimise the differences between the experimental plastic strain and the calculated plastic strain. The three tests with 25 ms
pulses were used in this procedure. The estimated parameter values obtained
in this way were Nc = 4.43, γc = -1.2 s−1 and mc = -0.58. Evidently, the
estimated parameter values were kept fixed for the prediction of the tests in
the same conditions.
In the temperature study, the sub-set of tests performed with the highest
peak pressure, i.e. 20 MPa with pulse lengths 20, 200 and 2000 ms (see Table 3.2), were used for parameter estimation. In the case of fibre swelling,
the two tests with pulse lengths 20 and 2000 ms (for each WRV) were used
for parameter estimation. The tests with pulse lengths of 200 ms were used
to test the model predictive capability.
pl
The plastic strain rate, dǫdt , the functions F and Ψm∗ were calculated
from the experimental plastic strain, and the parameters were obtained by
multiple regression.
36
CHAPTER 3. THE PERZYNA MODEL
As m∗c did not show a significant change with temperature nor with fibre
swelling – reflected in the WRV –, it was considered independent of both
temperature and fibre swelling. The influence of temperature on the first
compression could be observed on γc and Nc . The values are presented in
Table 3.3. The influence of fibre swelling on the first compression could be
observed on γc . The values are presented in Table 3.4.
Table 3.3: Estimated values of γc and Nc for webs made of SBK
compressed at different temperatures.
Temperature γc ➲ 10−3
23
-0.140
50
-0.178
80
-0.255
mc
Nc
-0.60 1.146
-0.60 1.036
-0.60 0.930
Table 3.4: Estimated values of γc for webs made of SBK beaten at with
different WRV.
WRV γc ➲ 10−3
1.26
-0.027
1.43
-0.012
1.51
-0.007
1.65
-0.004
3.3.2
mc
-0.40
-0.40
-0.40
-0.40
Nc
1.61
1.61
1.61
1.61
Validation
The Perzyna model presented above was validated by comparing predictions
of web behaviour for all the remaining pressure pulses (i.e. those not used in
the parameters estimation, see Tables 3.1 and 3.2) with the corresponding
experimental results. In each case, the applied pressure pulse (as recorded
in the experiment) was used as the input to the model. The first sampled
thickness in the experiment was used as the initial condition.
On the left-hand side of Figure 3.4, is shown predictions compared with
experimental results for some roll-nip-like pressure pulses with 75 ms in pulse
length (Table 3.1). The rate-dependent behaviour of the webs can be seen
more clearly on the right-hand side of Figure 3.4 showing the experimental
results and the predictions for pulses with 25, 250 and 2500 ms in pulse length
(Table 3.1).
3.3. RESULTS AND DISCUSSIONS
37
Figure 3.4: Left: Comparison between test results for 75 ms roll-press
type pulses with max peak pressures of 3, 8 and 23 MPa, and predictions.
Right: Comparison between test results for roll-press type pulses with
length of 25, 250 and 2500 ms and with max peak of 23 MPa and Perzyna
model predictions (only loading). The quasi-static curve (pulse length
130 s) is also shown (as a reference).
On the left-hand side of Figure 3.5, is presented the predicted and the
experimental results for two different degrees of swelling, 1.26 and 1.65 g/g
with 200 ms (Table 3.1). In both cases, the pressure pulse was 200 ms in
length and achieved 8 MPa in the peak pressure.
Figure 3.5: Left: Experimental and predicted results for two different
degrees of fibre swelling of SBK pulps. The tests were performed with
pulse lengths of 200 ms. Right: Experimental and predicted results for
two different web temperatures of SBK pulps. The tests were performed
with pulse lengths of 20 ms.
38
CHAPTER 3. THE PERZYNA MODEL
On the right-hand side of Figure 3.5, is shown predicted and experimental results for two incoming web temperatures with pressure pulses of 20 ms
length and 10 MPa peak pressure (Table 3.1).
3.4
Concluding Remarks
A mathematical model of the stress-strain behaviour of the fibre network,
here called the Perzyna model was presented and validated. The model
predictions were in good agreement with the experimentally observed fibre
network rheological behaviour over the whole range of peak pressure, pulse
lengths and pulse shapes studied (single pulses). The agreement was good
also for different pulps (TMP and SBK), temperatures, and intra-fibre-water
content (reflected by pulps WRV). The Perzyna model may therefore be a
useful tool to calculate the stress-strain behaviour of fibre network in physically based models of wet pressing for one pulse without relaxation, provided
the model parameters are estimated from experimental data with small experimental error.
Chapter 4
The Gel-Network Model
“We shall never be able to study, by any method, their chemical composition or their
mineralogical structure... Our positive knowledge of stars is necessarily limited to
their geometric and mechanical phenomena.”
August Comte (1798 – 1857) in Cours de philosofie positive 1835
”Credulity is the man’s weakness, but the child’s strength.”
Charles Lamb (1775 – 1834) in Essays of Elia 1823
In order to model the fibre network stress in a sequence of press nips, as
are common in press sections, it is necessary to allow for the unloaded expansion between the nips. This requires rate sensivity in both the compression
and expansion phases, i.e. the web has to be treasted as a material that shows
rate dependence in both the elastic and plastic regions. The determination
of the yield conditions for such a material is very difficult and has not yet
been done (Perzyna, 1966).
Therefore, a new model was developed that utilizes information about
the structure of the web. The wet web may concieved as layered network
of restricted swelling gels. A fibre in a saturated web is a restricted swollen
gel, the inner swelling pressure in a swollen fibre wall being balanced by the
stress in the fibre wall structure (Flory, 1953; Christensen and Giertz, 1965).
The resistance to deformation of a wet web may therefore to be dependent
on the swelling behaviour of the web fibres. The new model is refered to as
restricted gel-network model, or just shortly gel-network model.
The gel-network model could take into account the experimentally observed rate dependence of saturated webs in both compression and expansion and its predictions were in good agreement with results from uniaxial
experiments for both a single nip and a series of consecutive nips, for a wide
range of experimental conditions.
39
Compression,
expansion and
recompression
Restricted
swelling gels
40
CHAPTER 4. THE GEL-NETWORK MODEL
4.1
Experiments
The experimental procedure was the same as in the former chapter. Only
some tests were conducted with different shapes in order to explore the effect
of unloading. The experimental data in Table 4.1 were employed in the generalisation of the mathematical description for expansion and recompression
of fibre sheets.
Regarding the hydraulic pressure contribution on the successive pulses,
it was assumed that they should be smaller than those observed in the first
compression. According to Lindsay and Brady (1993) and Reverdy-Bruas
et al. (2001), permeability for previously compressed webs increases at the
same porosity. Further, previously dried webs also demonstrate increased
permeability (Lindsay, 1994), indicating that the closure of internal pores,
leave external pores more open, for a given total porosity.
Table 4.1: Tests performed with pulp fibre webs of 30 g/m2 made of
SBK. In the cases marked with ‘*’, only one compression pulse was
performed.
Pulse Length
Interval
Pulse Shape
[ms]
[ms]
–
20 and 2000
0, 100 and 300
roll
50 and 500
0, 100 and 300
shoe
2000*
—
see Figure 4.2
20, 200 and 2000*
—
roll
4.2
4.2.1
SR Peak Pressure
[cl]
[MPa]
25.2
9
26.2
8
25.2
5
25.2
9
Model
The Micro- and Macroscopic Perspectives
In this section, we present our view of the relationship between the microscopic concept of a swollen fibre (restricted gel) and the macroscopic variables, viz. applied stress and wet web strain.
A swollen cellulose is a restricted swelling gel (Flory, 1953; Christensen
and Giertz, 1965) and the fibre web may be regarded as a layered network of
restricted gels. From a macroscopic perspective, however, the fibre web may
be considered a continuum. Here we were only concerned with situations
4.2. MODEL
41
where the fibre web is immersed in water and the pressure of the inter-fibre
water (in the pores between the fibres) is negligible. Therefore, the applied
stress perpendicular to the plane of the web was balanced only by the fibre
network stress.
It is hypothesised that if a stress is applied to the uncompressed web, the
hydraulic pressure of the water inside the fibre walls increases, resulting in
an outflow of water until static equilibrium is achieved (Laivins and Scallan,
1993b) at a higher swelling pressure. At the macroscopic level, the applied
stress on the web in a state of static equilibrium is called the equilibrium
stress, σe , which is a function of the history of the web strain1 , ǫ (Figure 4.1).
The function σe can be approximated experimentally by uniaxial, quasi-static
compression tests.
Whenever the applied stress on the web is greater than the equilibrium
stress, the web will be compressed, and some intra-fibre water will be pressed
out of the fibre walls until equilibrium is attained. If instead the applied stress
on the web is less than the equilibrium stress, the web will expand, and, at
the microscopic level, water will flow into the fibre walls until equilibrium is
attained at a lower swelling pressure, as indicated by the experimental results
shown in (Figure 4.2).
Figure 4.1: Experimentally determined equilibrium stress under loading and unloading starting from two different initial strains (loading and
unloading).
1
ρ
The solids content is a function of the strain, ǫ, according to: SC = ρf +ρwf(eǫ −1) ,
where ρw and ρf are the density of the water and fibre material respectively.
Equilibrium
stress
Reaching
equilibrium
42
CHAPTER 4. THE GEL-NETWORK MODEL
Figure 4.2: Experimental response to a half-haversine (1000 ms) pulse
with sudden change to two different stress levels. The load was kept at a
constant level for several minutes. It can be clearly seen how the response
approaches the equilibrium curve during the loading (left) and unloading
(right) phases.
Swelling
The stress-strain behaviour of the fibre network was considered to be
dependent on the swelling properties of the fibres. The observed rate dependence of wet webs in both compression and expansion phases was attributed
to the water flow out of and into the fibre walls. This motivates the use
of the concept of overstress – i.e. the difference between the applied stress
and the equilibrium stress – under both the compression and the expansion
phases. A macroscopic model that is consistent with the hypothesis regarding the swelling and the flow phenomena taking place at the microscopic level
is presented below.
4.2.2
Overstress
The Macroscopic Model
The mathematical description of the rheological behaviour of the fibre network stress, proposed here is based on the hypothesis that compression occurs
with positive normalised overstress, i.e.
F =
σ − σe
,
σe
(4.1)
whereas expansion occurs when F is negative. The model represents the rate
of fibre network deformation by the following set of expressions:
4.2. MODEL
43
dǫ
= γc Ωc (F ) for
dt
dǫ
=
0
for
dt
dǫ
= γe Ωe (F ) for
dt
F > 0,
(4.2)
F = 0,
(4.3)
F < 0.
(4.4)
The functions Ωc (F ) and Ωe (F ) need to be chosen so that they adequately
represent the results of uniaxial tests under dynamic compression/expansion
(Figure 4.2). Analysis of the compression parts of the results of such dynamic tests indicates that Ωc (F ) is a function not only of the excess applied
structural stress but also of the strain (Lobosco, 2000). The expansion part
of the test results showed that Ωe (F ) was also a function of the strain and
the maximum strain. A good representation of the test results was given by
the functions:
Nc
c
,
Ωc = Ψm
c F
me N e
Ωe = Ψe F ,
(4.5)
(4.6)
where2
2
σy (ǫ)
Ψc (ǫ) =
− 1 + 1,
σy (ǫref )
Ψe (ǫ, ǫmax ) = (ǫ − 0.9ǫmax ) .
(4.7)
(4.8)
Equations (4.2) and (4.4) combined with Equations (4.5) and (4.6) respectively, yield:
dǫ
Nc
c
,
= γc Ψm
c F
dt
dǫ
Ne
e
.
= γe Ψm
e F
dt
(4.9)
(4.10)
The constants γc , γe , Nc , Ne , mc and me are parameters to be estimated from
the experimental data. These equations can be solved using a Runge-Kutta
algorithm.
2
The factor 0.9 multiplying ǫmax is just to avoid singularities problems when ǫ = ǫmax ,
as the parameter me obtained was negative.
44
4.3
4.3.1
Hysteresis
CHAPTER 4. THE GEL-NETWORK MODEL
Results and Discussions
The Equilibrium Curve
In order to estimate the parameters of the model and to make predictions, one
needs to know the equilibrium stress function, σe , approximated by quasistatic measurements of the fibre network. The experimentally determined
equilibrium curves observed were quite complex (Figure 4.1) and could be
expected to require a hysteresis operator if the responses to arbitrary pulses
were to be simulated (e.g. Bergqvist, 1994). However, a much simpler mathematical expression was found to give adequate description of the equilibrium
stress functions of the fibre network obtained in this study (Appendix B).
The proposed expressions showed good agreement with the experimental results, and were used in the estimation of the dynamic parameters.
Figure 4.1 shows a typical example of the equilibrium curves obtained by
us. Laivins and Scallan (1993b) have presented experimentally determined
curves of the water content of wet webs as functions of the applied compressive pressure which are, in principle, equivalent to the first compression
part of the equilibrium curve shown in Figure 4.1. Their results show that
the water contents of pads pressed to high pressures (and allowed to achieve
equilibrium) correlate linearly with the initial levels of swelling of the fibres
(the fibre saturation points). This implies that the solids content at the end
of the first compression in our equilibrium curve are linearly correlated with
the fibre saturation points of the web fibres. Typically, the curves for successive compressions come closer at higher pressures but never pass through
the same point. This can be interpreted as being the result of hornification,
i.e. the closing of pores in the fibre walls (Maloney et al., 1997, 1998).
4.3.2
Parameters Estimation
Equations (4.9) and (4.10) are intrinsically linear, which means that they
can be transformed to linear equations (with respect to the parameters) by
a logarithmic transformation, viz.
dǫ
ln
= ln(γc ) + mc ln(Ψc ) + Nc ln(F )
dt
dǫ
ln
= ln(γe ) + me ln(Ψe ) + Ne ln(F ).
dt
(4.11)
(4.12)
4.3. RESULTS AND DISCUSSIONS
45
The compression parameters, γc , mc and Nc , and the analogue expansion
ones, γe , me and Ne in these two equations could then be straightforwardly
estimated by the weighted least-square method (Draper and Smith, 1981).
Experimental results for several pulses with a large range of strain rate
were used in the estimation, as they provided a larger operation window
for the regressed model. Pulses with pulse lengths of 20, 200 and 2000 ms
without interval (see Table 4.1), were used for parameter estimation. This
multiple regression had to be weighted because the variance of the residuals
was clearly not constant.
Table 4.2: Material parameters estimated with the weighted least-square
method for webs made of SBK.
γ
m
N
Compression -0.0095 -0.59 1.68
Expansion
0.0011 -0.38 1.08
The residuals obtained were small for the compression phase, but not
for the expansion one. Better suggestions for Ωe will probably improve the
residuals. The model parameters were assumed to be the same for all the
pulses.
4.3.3
Validation
The gel-network model was validated by comparing predictions with all experimental results not used in the parameters estimation (Table 4.1). Parameter estimation was required only once and could be done using any
suitable pulse shape. Predictions could then be made for widely different
pulse shapes as shown in Figures 4.3 and 4.4.
The results shown in Figure 4.4 are consistent with the hypothesis that
the webs resistance to deformation is influenced by the swelling behaviour
of the component fibres. The left hand side of Figure 4.4 indicates that
equilibrium was achieved by static compression and the flow out of the fibre
wall, the static applied stress being initially higher than the equilibrium
stress. The right hand side of Figure 4.4 shows a situation where the static
applied stress was initially lower than the equilibrium stress and equilibrium
was achieved by static expansion, partly driven by the swelling of the fibre
walls. This expansion is not captured by the Perzyna model, nor, to the
knowledge of the authors, by any other published model.
Weighted least
squares
46
CHAPTER 4. THE GEL-NETWORK MODEL
Figure 4.3: Left: The roll press-like pulse with 20 and 2000 ms used
to estimate the gel-network model parameters and the model predictions.
Right: Comparison between the experimental response and the gel-model
prediction for an experiment with a shoe-press-like pulse of 50 ms.
Figure 4.4: Comparison between experimental and model responses for
half roll-press-like pulses with incomplete unloading to two different load
levels.
Figure 4.5 compares the gel-network model predictions with the observed response of the web to a series of roll-like press pulses, with and
without unloaded periods in-between. Keeping in mind the difficulty of measuring web thickness accurately at near zero load, the agreement is quite satisfactory. Figure 4.6 compares the experimentally observed development of
solids content with predictions from the Perzyna and the gel-network models
for a sequence of four pressure pulses. The Perzyna model fails to capture
the reductions in solids content during the unloaded intervals in-between
the pulses, whereas the gel-network model showed good agreement with the
experimental data, capturing the general pattern.
4.4. CONCLUDING REMARKS
47
Figure 4.5: Left: Comparison between the experimental and the mathematical prediction for a sequence of roll-press-like pulses without unloaded
periods in-between pulses. Right: Similar comparison with unloaded intervals of 100 ms in-between pulses.
Figure 4.6: Comparison of the experimental, Perzyna model and gelnetwork model responses for four consecutive roll-press-like pulses with
10 MPa in peak pressure with unloaded periods in-between the pulses
4.4
Concluding Remarks
This section presents a new model of the fibre network rheology, the gelnetwork model. It was based on the idea that the wet fibre web may be
conceived as a layered network of restricted swelling gels. Further, it gave
predictions that agree well with the results of uniaxial experiment. It could
simulate the fibre network response to a sequence of pulses of arbitrary shapes
with only a single set of estimated parameters. The gel-network model may
therefore be used as a general model for the rheological behaviour of the wet
48
CHAPTER 4. THE GEL-NETWORK MODEL
fibre network in wet pressing, provided the parameters are estimated from
data with small experimental error.
Bibliography
Auriault, J.-L. and E. Sanchez-Palencia (1977), ‘Etude du comportement
macroscopique d’un milieu poreux saturé déformable’, J. Mécanique
16(4), 575–603. in French.
Baines, W. D. (1967), ‘The papriformer part ii. flow in the formation zone of a
twin-wire machine’, Pulp and Paper Magazine of Canada pp. T497–T505.
Bear, J. (1972), Dynamics of Fluids in Porous Media, Dover, New York.
Bergqvist, A. (1994), On Magnetic Hysteresis Modeling, PhD thesis, Royal
Institute of Technology, Stockholm.
Bezanovic, D., E. F. Kaasschieter and C. J. van Duijn (2002), A onedimensional model for pressure drying of paper, in ‘Progress in Paper
Physics Seminar’, Syracuse, NY, pp. 250–253.
Biot, M. A. (1941), ‘General theory of three-dimensional consolidation’, Journal of Applied Physics 12, 155–164.
Bird, B. R., W. E. Stewart and E. N. Lightfoot (1960), Transport Phenomena,
John Wiley & Sons, New York.
Bloch, J.-F. (1995), Transferts de Masse et de Chaleur dans les Milieux
Poreux Deformables Non Satures: Application au Pressage du Papier, PhD
thesis, Institut National Polytechnique de Grenoble – Centre Technique du
Papier, Grenoble. in French.
Boxer, T. and C. T. J. Dodson (1999), Compression of fibre networks by
ultracentrifugation, in ‘TAPPI International Paper Physics Conference’,
San Diego, CA USA, pp. 391–402.
Boxer, T., C. T. J. Dodson and W. W. Sampson (2000), ‘Analytic solution
to the martinez dewatering equations for roll gap formers’, Journal of Pulp
and Paper Science 26(11), 391–394.
49
50
BIBLIOGRAPHY
Brokate, M. and J. Sprekels (1996), Hysteresis and Phase Transition, first
edn, Springer-Verlag, New York.
Brownell Jr., D. H., S. K. Garg and J. W. Pritchett (1977), ‘Governing
equations for geothermal reservoirs’, Water Resources Research 13(6), 929–
934.
Busker, L. H. and D. C. Cronin (1982), The relative importance of wet press
variables in water removal, in ‘Int. Water Removal Symp.’, Vancouver,
pp. 25–34.
Campbell, W. B. (1947), ‘The physics of water removal’, Pulp and Paper
Magazine of Canada 48(3), 103–109, 122.
Carlsson, G., T. Lindström and T. Florén (1983), ‘Permeability to water of
compressed pulp fibre mats’, Svensk Papperstidning 86(12), R128–R134.
Carlsson, G., T. Linström and C. Söremark (1977), Expression of water
from cellulosic fibers under compressive load, in ‘Fibre-Water Interactions
in Papermaking’, Vol. 1, British Paper and Board Industry Federation,
Oxford, pp. 389–409.
Ceckler, W. T. and E. V. Thompson (1982), The university of maine at orono
wet pressing project, Technical Report DOE/CS/40064-3 (DE83009342),
United States Department of Energy, Orono.
Chadrasekharaiah, D. S. and L. Debnath (1994), Continuum Mechanics, Academic Press, San Diego.
Christensen, P. K. and H. W. Giertz (1965), The cellulose/water relationship, in ‘Consolidation of the Paper Web – Third Fundamental Research
Symposium’, Vol. 1, FRC, Cambridge, pp. 59–84.
Collicutt, S. A. (1947), ‘Drainage characteristics of groundwood pulp’, Pulp
and Paper Magazine of Canada pp. 66–78.
Draper, N. R. and H. Smith (1981), Applied Regression Analysis, Wiley Series
in Probability and Mathematical Statistics, second edn, John Wiley &
Sons, New York.
Drew, D. A. (1983), ‘Mathematical modeling of two-phase flow’, Ann. Rev.
Fluid Mechanics 15, 261–291.
Dullien, F. A. L. (1979), Porous Media: Fluid Transport and Pore Structure,
Academic Press, Inc., San Diego, CA.
BIBLIOGRAPHY
51
El-Hosseiny, F. (1990), ‘Compression behaviour of press felts and wet webs’,
Nordic Pulp and Paper Research Journal 5(1), 28–32.
Ellis, E. R. (1981), Compressibility and Permeability of never Dried Bleached
Softwood Kraft Pulp and its Application to the Prediction of Wet Press
Behavior., PhD thesis, University of Maine at Orono, Orono.
Emmons, H. W. (1965), ‘The continuum properties of fibre suspension’, Tappi
Journal 48(12), 679–687.
Enwald, H., E. Peirano and A.-E. Almstedt (1996), ‘Eulerian two-phase flow
theoy applied to fluidization’, Int. J. of Multiphase Flow 22, 21–66.
Eriksson, K., D. Estep, P. Hansbo and C. Johnson (1996), Computational
Differential Equations, Cambridge University Press, Cambridge.
Flory, R. J. (1953), Principles of Polymer Chemistry, Cornell University
Press, New York.
Fung, Y. C. and P. Tong (2001), Classical and Computational Solid Mechanics, River Edge, NJ : World Scientific, Singapore.
Garg, S. K., Brownell Jr. D. H., J. W. Pritchett and R. G. Hermann (1975),
‘Shock-wave propagation in fluid-saturated porous media’, Jornal of Applied Physics 46(2), 701–713.
Greenkorn, R. A. (1983), Flow Phenomena in Porous Media, Marcel Dekker,
Inc., New York.
Gren, U. and K. Ljungkvist (1983), ‘Compressibility and permeability of
chemical pulps. some notes on the effect of beating.’, Cellul. Chem. Technol. 17(Sept.–Oct.), 515–523.
Gustafsson, J.-E. and V. Kaul (2001), ‘A general model of deformation and
flow in wet fibre webs under compression’, Nordic Pulp and Paper Research
Journal 16(2), 149–155.
Gustafsson, J.-E., V. Kaul and V. Lobosco (2001), Densification and dewatering in high temperature wet pressing, in ‘The Science of Papermaking’,
Vol. 1, FRC, pp. 149–155.
Häggkvist, M. (1999), ‘Porous structure in paper studied by nmr’, Teknologie
Lincentiate Thesis. Royal Institute of Technology – Division of Pulp and
Paper.
52
BIBLIOGRAPHY
Han, S. T. (1962), ‘Drainage in a vacuum former’, Tappi Journal 45(4), 292–
295.
Han, S. T. (1969), ‘Compressibility and permeability of fibre mats.’, Pulp
and Paper Magazine of Canada pp. T134–T146.
Hauptmann, E. G. and J. Mardon (1973), ‘The hydrodynamics of curved
wire formers’, Pulp and Paper Magazine of Canada 74(2), 72–77.
Herzig, R. and D. B. Johnson (1999), ‘Investigation of thin fiber mats formed
at high velocity’, Tappi Journal 82(1), 226–230.
Hisey, R. W. (1956), ‘An investigation of the mechanism of dewatering of
compressible beds’, Tappi Journal 39(10), 690–696.
Holmqvist, C. (2002), ‘Modelling of the pressure distributions in twin-wire
blade formers’, Licentiate Thesis. Royal Institute of Technology, Stockholm.
Ingmanson, W. L. (1952), ‘An investigation of the mechanism of water removal from paper slurries.’, Tappi Journal 35(10), 439–448.
Ingmanson, W. L. (1953), ‘Filtration resistance of compressible materials’,
Chem. Eng. Prog. 49(11), 577–584.
Ingmanson, W. L., B. D. Andrews and R. C. Johnson (1959), ‘Internal pressure distribution in compressible mats under fluid stress’, Tappi Journal
42(10), 840–849.
Ishii, M. (1975), Thermo-fluid Dynamic Theory of Two-phase Flow, Eyrolles,
Paris.
Jacob, C. E. (1950), Engineering Hydraulics, John Wiley, New York, chapter
Flow of Ground Water, pp. 321–386.
Jones, R. L. (1963), ‘The effect of the structure properties on the compression
response of fiber beds.’, Tappi Journal 46(1), 20–28.
Jong, J. H. (1998), Characteristics of Jet Impingement, Drainage and Compression in a Forming Roll of a Twin-wire Machine, PhD thesis, Department of Mechanical and Industrial Engineering, University of Toronto,
Toronto.
Jong, J. H., W. D. Baines and I. G. Currie (1999), ‘Experimental characteristics of forming fabrics and fibre mats’, Journal of Pulp and Paper Science
25(3), 95–99.
BIBLIOGRAPHY
53
Jönsson, K. A.-S. and B. T. L. Jönsson (1992), ‘Fluid flow in compressible
porous media: I: Dynamic behavior.’, AIChE Journal 38(9), 1349–1356.
Kataja, M., J. Kirmanen and Timonen J. (1995), ‘Hydrostatic and structural
pressure in compressed paper webs and press felts’, Nordic Pulp and Paper
Research Journal 10(3), 162–166.
Kataja, M., K. Hiltunen and Timonen J. (1992), ‘Flow of water and air in a
compressible porous medium. a model of wet pressing’, Journal of Applied
Physics 25, 1053–1063.
Kaviany, M. (1995), Principles of Heat Transfer in Porous Media, second
edn, Springer-Verlag, New York.
Kirmanen, J., M. Kataja and J. Timonen (1994), ‘Stress balance in soft
porous media.’, Appl. Phys. Lett. 64(19), 2605–2607.
Koponen, A., D. Kandhai, E. Hellen, M. Alava, A. Hoekstra, M. Kataja,
K. Niskanen, P. Sloot and J. Timonen (1998), ‘Permeability of threedimensional random fibre network’, Physical Review Letters 80(4), 716–
719.
Lagarias, J. C., J. A. Reeds, M. H. Wright and P. E. Wright (1998), ‘Convergence properties of the nelder-mead simplex method in low dimensions’,
Society for Industrial and Applied Mathematics Journal on Optmization
9(1), 112–147.
Laivins, G. V. and A. M. Scallan (1993a), The mechanism of hornification of
wood pulps, in ‘Products of Papermaking – Tenth Fundamental Research
Symposium’, Vol. 2, FRC, Oxford, pp. 1235–1260.
Laivins, G. V. and A. M. Scallan (1993b), Removal of water from pulps by
pressing — part i: Inter- and intra-wall water, in ‘Engineering Conference’,
Vol. 2, TAPPI, Orlando, pp. 741–748.
Laivins, G. V. and A. M. Scallan (1995), The influence of drying and beating
on the swelling of fines, in ‘Third Research Forum on Recycling’, Canadian
Pulp and Paper Association, Vancouver, pp. 153–161.
Landau, L. D. and E. M. Lifchitz (1987), Fluid Mechanics, Vol. 6 of Theoretical Physics, second edn, Pergamon Press, Oxford.
Landau, L. D. and E. M. Lifchitz (1990), Théorie d’elasticité, Vol. 7 of
Physique Théorique, second edn, Mir, Moscow.
54
BIBLIOGRAPHY
Lewis, R. W. and B. A. Scherefler (1998), The Finite Element Method in
the Static and Dynamic Deformation and Consolidation of Porous Media,
second edn, John Wiley & Sons, West Sussex, England.
Lindsay, J. D. (1994), ‘Relative flow porosity in fibrous media: Measurements
and analysis, including dispersion effects’, Tappi Journal 77(6), 225–239.
Lindsay, J. D and P. H. Brady (1993), ‘Studies of anisotropic permeability
with applications to water removal in fibrous webs — part 1: Experimental
methods, sheet anisotropy and relationship to freeness’, Tappi Journal
76(9), 119–127.
Lindström, T. (1986), Paper – Structure and Properties, Marcel Dekker, New
York, chapter The Concept of Measurement of Fiber Swelling, pp. 75–98.
Ljungkvist, K. (1983), Pulp Characterization by Permeability Measurements,
PhD thesis, Department of Chemical Engineering Design, Chalmers,
Gothenburg.
Lobosco, V. (2000), ‘A rheological model of the paper fibre network in wet
pressing’, Teknologie Licentiate Thesis, Department of Pulp and Paper
Chemistry and Technology, Royal Institute of Technology, Stockholm.
Lucisano, M. F. C. and D. M. Martinez (2001), ‘On the characterization of
the delamination process during impulse pressing’, Nordic Pulp and Paper
Research Journal 16(4), 338–344.
MacGregor, M. A. (1989), Wet pressing in 1989 — an historic perspective, analysis and commentary, in ‘Transactions of the 9th Fundamental
Research Symposium’, Vol. 2, Mechanical Engineering Publications Ltd.,
London, pp. 511–586.
Maloney, T., A. Todorovic and H. Paulapuro (1998), ‘The effect of fiber
swelling in press dewatering’, Nordic Pulp and Paper Research Journal
13(4), 285–291.
Maloney, T. C., T. Li, U. Weise and H. Paulapuro (1997), ‘Intra- and interfibre pore closure in wet pressing’, Appita Journal 50(37), 301–306.
Mantar, E., A. Co and J. M. Genco (1995), ‘Drainage characteristics of pulp
slurries under dynamic conditions’, Journal of Pulp and Paper Science
21(2), J44–J50.
Martinez, D. M. (1998), ‘Characterizing the dewatering rate in roll gap formers’, Journal of Pulp and Paper Science 24(1), 7–13.
BIBLIOGRAPHY
55
McDonald, J. D. and R. J. Kerekes (1991a), A decreasing permeability model
of wet pressing: Applications, in ‘Engineering Conference’, Vol. 2, TAPPI,
Nashville, pp. 559–568.
McDonald, J. D. and R. J. Kerekes (1991b), A decreasing permeability model
of wet pressing: Theory, in ‘Engineering Conference’, Vol. 2, TAPPI,
Nashville, pp. 551–558.
McDonald, J. D. and R. J. Kerekes (1994), A decreasing permeability model
of wet pressing with rewetting, in ‘Engineering Conference’, TAPPI, Atlanta, GA, pp. 109–116.
Meyer, H. (1962), ‘A filtration theory for compressible fibrous beds formed
from dilute suspensions’, Tappi Journal 45(4), 296–310.
Meyer, H. (1969), ‘The effect of wire screen on forming fiber mats’, Tappi
Journal 52(9), 1716–1723.
Mitchell, C. and R. Johnson (2001), Modelling water removal from water
fibre mats., in ‘55th Appita Annual Conference’, Hobart, Australia.
Miyanishi, T., Iida K. and T. Iwatsu (1989), ‘Drainage analysis of curved
forming shoes on twin-wire formers’, Tappi Journal pp. 81–85.
Nigam, M. and F. Bark (1997), ‘An analytical method to calculate the flow
past a blade in twin-wire formers’, Tech. Rep. Department of Mechanics,
Royal Institute of Technology.
Nilsson, P. and K. O. Larsson (1968), ‘Paper web performance in a press
nip’, Pulp and Paper Magazine of Canada 69(24), 66–73.
Nordström, B. and B. Norman (1994), ‘Development of the stfi-former’,
Nordic Pulp and Paper Research Journal 9(3), 176–181.
Norman, B. (1979), ‘Principles of twin-wire forming’, Svensk Papperstidning
82(11), 330–336.
Norman, B. (1989), Overview of the physics of forming, in ‘Fundamentals of
Papermaking’, Vol. 3, Mech. Eng. Publ. Ltd., pp. 73–150.
Norman, B. and D. Söderberg (2001), Overview of forming literature, 1990–
2000, in ‘The Science of Papermaking’, Vol. 2, pp. 431–558.
Parker, J. D. (1972), The Sheet-forming Process, Tappi Special Technical
Association Publication, Atlanta.
56
BIBLIOGRAPHY
Perry, R. H., D. W. Green and J. O. Maloney, eds (1984), Chemical Engineers’ Handbook, 6th edn, McGraw-Hill, New York.
Perzyna, P. (1966), ‘Fundamental problems in viscoelasticity’, Advances in
Applied Mechanics 9, 243–377.
Pires, F. S. and G. S. S. Kuan (1988), Celulose e Papel, SENAI/IPT, chapter 6. in Portuguese.
Radvan, B. (1980), The Raw Materials and Processing of Papermaking,
Vol. 1, Elsevier Scientific Publishing Company, Amsterdam, chapter Forming the Web of the Paper, pp. 165–208.
Rasi, M., A. Koponen, J. Asltosalmi, U. Timonen and M. Kataja (1999),
Permeability of paper: Experiments and numerical simulations., in ‘International Paper Physics Conference’, Forest Products Laboratory, San
Diego, CA, USA.
Reverdy-Bruas, N. R, J.-M. Serra-Tosio, Y. Chave and J.-F. Bloch (2001),
‘Investigation of the transverse permeability of saturated paper sheets’,
Drying Technology 19(4), 2421–2433.
Riepen, M., A. M. J. Sinon and B. M. P. Mulder (1996), The integrated paper
machine dewatering model (ipm), in ‘International Drying Symposium’,
Vol. B, Krakow, Poland, pp. 1197–1204.
Robertson, A. A. and S. G. Mason (1949), ‘Specific surface of cellulose
fibers by liquid permeability method.’, Pulp Paper Magazine of Canada
50(13), 103–110.
Roshanzamir, A., S. I. Green and R. J. Kerekes (2000), ‘Two-dimensional
simulation of suction shoes in gap formers’, Journal of Pulp and Paper
Science 26(4), 158–162.
Roux, J. C. and J. P. Vincent (1991), ‘A proposed model in the analysis of
wet pressing’, Tappi Journal 74(2), 189–196.
Sayegh, N. N. and T. O. Gonzalez (1995), ‘Compressibility of fibre mats
during drainage’, Journal of Pulp and Paper Science 21(7), J255–J261.
Scheidegger, A. E. (1974), The Physics of Flow through Porous Media, University of Toronto Press, Toronto.
Soo, S. L. (1990), Multiphase Fluid Dynamics, Science Press, Beijing.
BIBLIOGRAPHY
57
Szikla, Z. and H. Paulapuro (1989), Compression behaviour of fibre mats in
wet pressing, in ‘Ninth Fundamental Research Symposium’, Vol. 3, Cambridge, pp. 583–636.
Terzaghi, K. (1944), Theoretical Soil Mechanics, John Wiley & Sons, New
York.
Visintin, A. (1991), Differential Models of Hysteresis, first edn, SpringerVerlag, New York.
Vomhoff, H. (1998), Dynamic Compressibility of Water-Saturated Fibre Networks and Influence of Local Stress Variations in Wet Pressing, PhD thesis,
Royal Institute of Technology, Stockholm.
Vomhoff, H. (2000), Studies of the dynamic compressibility of watersaturated fibre networks, in ‘TAPPI Engineering Conference’, TAPPI
Press, Atlanta, GA.
Vomhoff, H. and A. Schmidt (1997), ‘The steady-state compressibility of
saturated fibres at low pressures’, Nordic Pulp and Paper Research Journal
12(4), 267–269.
Vomhoff, H. and B. Norman (2001), ‘Method for the investigation of the
dynamic compressibility of wet fibre networks’, Nordic Pulp and Paper
Research Journal 16(1), 57–62.
Wahlström, P. B. (1969), ‘Our present understanding of the fundamentals of
pressing’, Pulp and Paper Magazine of Canada 70(10), 76–96.
Wahlström, P. B. (1990), Effect of water in the fibre wall in wet pressing, in
‘Pre-prints 44th APPITA Annual General Meeting’, Rotoroa, pp. A21.1–
A21.24.
Wahren, D., L. Dufva and B. Wahlström (1975), ‘Mechanics of water removal
in webster-type formers’, Paper Tech. Ind. 16(2), 98–105.
Wang, J., A. N. Hrymark and R. H. Pelton (2002), ‘Specific surface and effective volume of water removal of water-swollen pulp fibres by a permeability
method’, Journal of Pulp and Paper Science 28(1), 13–16.
Wilder, H. D. (1960), ‘The compression creep properties of wet pulp mats.’,
Tappi Journal 43(8), 715–720.
Wildfong, V. J., J. M. Genco, J. A. Shands and D. W. Bousfield (2000a),
‘Filtration mechanics of sheet forming. part ii: Influence of fine material
and compression’, Journal of Pulp and Paper Science 26(8), 280–283.
58
BIBLIOGRAPHY
Wildfong, V. J., J. M. Genco, J. A. Shands and D. W. Bousfield (2000b),
‘Filtration mechanics of sheet forming. part i: Apparatus for determination of constant-pressure filtration resistance’, Journal of Pulp and Paper
Science 26(7), 250–254.
Wrist, P. E. (1962), Dynamics of Sheet Formation on the Fourdrinier Machine, Vol. 2, BPBMA, pp. 839–888.
Zahrai, S., F. Bark and B. Norman (1997), ‘An analysis of blade dewatering in a twin-wire paper machine’, Journal of Pulp and Paper Science
23(9), J452–459.
Zahrai, S., M. D. Martinez and A. A. Dahlkild (1998), ‘Estimating the thickness of the web during twin-wire forming’, Journal of Pulp and Paper
Science 24(2), 67–72.
Zhao, R. and R. Kerekes (1995), ‘Pressure distribution between forming fabrics in blade gaps formers: Thin blades’, Journal of Pulp and Paper Science
21(3), 97–103.
Appendix A
Model Derivation
Several researchers have examined and studied the physics of multi-phase
flow using a continuum mechanics approach, where averaging techniques
have been applied (e.g. Ishii, 1975; Drew, 1983; Soo, 1990; Kaviany, 1995;
Enwald et al., 1996). This procedure has the advantage that it shows more
clearly how the macroscopic quantities stem from microscopic considerations.
Therefore, it was followed here. The system being modelled is shown in Figure 2.1.
Accordingly, a volumetric averaging (Kaviany, 1995), i.e.
1
hψk i = ψ˜k φk =
V
Z
ψk dV,
(A.1)
Vk
was performed on the continuity and momentumR equations below for a given
quantity, ψk , of phase k (Figure A.1). φk = V1 Vk dV is the volume fraction
of phase k = {w, f } (water and fibre)1 . The tilde designates volumetric
average whereas the cap designates massic average, viz.
R
V
ψ̂ = Rk
A.1
ρk ψk dV
ρ dV
Vk k
.
(A.2)
Continuity Equations
The continuity equation for phase k becomes:
1
Water volume fraction is the porosity, which is the terminology used henceforth.
59
60
APPENDIX A. MODEL DERIVATION
Figure A.1: A representative picture of the region being averaged composed of phase k and k.
∂φk ρ˜k
+ div(φk ρ˜k v̂k ) = 0.
∂t
(A.3)
No mass flux between the phases was assumed. If both phases are incompressible, Equation (A.3) becomes:
∂φk
+ div (φk v̂k ) = 0
∂t
A.2
(A.4)
Momentum Equations
Similarly, the equation for conservation of momentum is obtained by volumetric averaging:
1
∂
+
(φk ρ˜k v̂k ) + div (φk ρ˜k v̂k v̂k ) = div φk T̃k + φk T̃Re
k
∂t
V
Z
Sk
Tk ➲ nk dS,
k
(A.5)
where nk is the unit vector normal to the surface2 , Sk k , between the phases
and T̃k and T̃Re
k are the stress tensor in the phase k and the stress due
to the (microscopic) velocity variations inside the integration volume, the
so-called Reynolds stresses (Bird et al., 1960), respectively. According to
Bear (1972) and Kaviany (1995), the deviations observed from Darcy’s law
2
k refers to the adjoining phase to k.
A.2. MOMENTUM EQUATIONS
61
at Reynolds numbers higher than unity are attributed to inertial effects, and
not to turbulence. Arguably, the Reynolds stresses were supposed to be
responsible for this effect.
Accordingly, the experiments performed by Wildfong et al. (2000b) give
evidences for assuming T̃Re
k negligible for the fluid phase. It is obviously
negligible for the solid phase too. According to experiments performed by
Herzig and Johnson (1999) and Wildfong et al. (2000a), T̃Re
k is probably
relevant for the water phase flowing through wires at early dewatering stages.
Simulations of blade dewatering performed by Roshanzamir et al. (2000)
show that this term plays only a modest role in later parts of the forming
sections. The macroscopic inertial terms (the two terms on the left-hand
side of Equation (A.5)) were neglected as the water velocity variation in the
z-direction is very small.
The last term on the right hand side accounts for the (diffusive) momentum transfer between phases for a system without phase transition. How this
term was taken into account is described in the next section.
The influence of a potential (gravitational) field was disregarded for both
phases, as this contribution is small in comparison to the stresses applied in
twin-wire formers. Equation (A.5) then becomes:
div φk T̃k
1
+
V
Z
Sk
Tk ➲ nk dS = 0.
(A.6)
k
On the boundary between phases, the forces that each phase exerts on each
other have the same magnitude and opposite direction according to Cauchy’s
formula (Landau and Lifchitz, 1987; Chadrasekharaiah and Debnath, 1994),
i.e.
Tk ➲ nk = −T k ➲ n k ,
(A.7)
where n k = −nk . Thus, adding the momentum equations for the two phases,
one obtains:
divTt = div −φw p̃w I + (1 − φw )T̃f = 0,
(A.8)
where Tt is the total stress and T̃w reduces to the hydraulic pressure, i.e
T̃w = −p̃w I (I is the identity matrix ), as the internal shear stresses balance
62
APPENDIX A. MODEL DERIVATION
out in the volume averaging (Jacob, 1950; Bear, 1972; Lewis and Scherefler,
1998).
The stress in the fibre network, k = f , has two contributions (Biot, 1941;
Drew, 1983; Kataja et al., 1995), viz.
T̃f = T̃f 0 + T̃f h ,
(A.9)
where T̃f 0 is the stress in the fibre network disregarding the effect of hydraulic
pressure, i.e. the fibre network stress, and T̃f h is the stress in the fibre network
induced by the hydraulic pressure acting on its surface. Rendulic (p.13 in
Terzaghi, 1944) concludes that the mechanical effects of a given state of total
stress depend only on T̃f 0 . Kirmanen et al. (1994) conjecture the induced
structural pressure to be proportional to the hydraulic pressure, i.e.
T̃f h = −C p̃w I
(A.10)
where the constant C (≤ 1) depends on the material and the contact between
particles. For instance, C = 1 for completely immerse solids (Emmons, 1965;
Landau and Lifchitz, 1990). Therefore, it depends on the straining of the
material.
Equation (A.8) can, with the help of Equations (A.9) and (A.10), be
rewritten as:
Tt =
X
φk T̃k = hTf 0 i − φeff
a p̃w I,
(A.11)
k
where φeff
a is called the effective areal porosity (Kataja et al., 1995). The
fibre network stress is given by:
hTf 0 i = (1 − φw )T̃f 0 ,
(A.12)
and φeff
a is a function of C according to:
φeff
a = C + (1 − C)φw .
(A.13)
According to measurements by Kataja et al. (1995), φeff
a is very close to
unity (∽ 0.99) even for an extreme case in the forming section (40 kPa and
A.3. MOMENTUM TRANSFER EQUATIONS
63
25 percent solids content ⇒ φeff
a = 0.99). Accordingly, Terzaghi’s principle
was assumed in the forming section, i.e.
Tt = hTf 0 i − p̃w I.
A.3
(A.14)
Momentum Transfer Equations
The momentum transfer term given by the last term in Equation (A.5) is
most frequently described by an empirical equation. It includes a dilatational
contribution (Garg et al., 1975; Brownell Jr. et al., 1977), i.e. p̃w gradφw ,
which can be obtained by volumetric averaging in static stress conditions, i.e.
when the fluid is under a constant pressure. Expanding, Tk into −p̃w I + Tdk ,
the momentum transfer term becomes:
1
V
1
Tk ➲ nk dS = p̃w gradφk +
V
Sk k
Z
1
(p̃w − pw ) nk dS +
V
Sk k
Z
Z
Sk
Tdk ➲ nk dS,
k
(A.15)
The second term on the right-hand side of Equation (A.15) comprehend
the buoyant and the form effects, whereas the last term accounts for the
drag. The last two terms are postulated to have the form (Garg et al., 1975;
Brownell Jr. et al., 1977; Lewis and Scherefler, 1998):
1
V
1
(p̃w − pw ) nk dS +
V
Sk k
Z
Z
Sk
Tdk ➲ nk dS = −µφ2w K−1 (v̂k − v̂ k ) , (A.16)
k
where K is the so-called permeability of the medium, and µ is the viscosity
of the fluid. As expressed by Equation (A.7), Equation (A.16) has the same
magnitude but opposite signs for the two phases.
The final equation was obtained from Equations (A.4), (A.6), (A.14),
(A.15) and (A.16) after some rearrangement:
∂φw
+ div (φw v̂f ) − div
∂t
K
divhTf 0 i = 0
µ
(A.17)
As the porosity gradients are much larger in the thickness direction than
those in the MD and the roll radius is large in relation to the suspension
64
APPENDIX A. MODEL DERIVATION
thickness, only the uniaxial problem was considered here. Furthermore, only
symmetrical dewatering was assumed, i.e. centrifugal forces were neglected,
and the blades were considered not to impede the water flow (Figure 2.1).
Equation (A.17) then becomes:
∂φw
∂
∂
+
(φw v̂f,z ) −
∂t
∂z
∂z
Kzz ∂hσf o,zz i
µ
∂z
= 0,
(A.18)
where only the vectorial and tensorial components in the z-direction have
been considered. The indexes z and zz indicate the z-components of the
vectors and tensors in Equation (A.17). By an abuse of notation, they, as
well as the “hi” brackets, were omitted and φw was denoted as φ in the
following for simplicity.
Appendix B
Rate-Independent
Fibre-Network Stress
Here mathematical expressions, which can give good descriptions of the fibre
network stress, σf 0 (discussed in Chapter 2), and the fibre network equilibrium stress, σe (discussed in Chapter 4), are suggested. Both stresses are
rate-independent.
As it was pointed out in the introduction (see Equation (1.8)), the fibre
network stress depends on the entire compression history of the fibre mat.
The same is valid for the fibre network equilibrium stress. However, here a
simplification was made. Those stresses were assumed to be a function of
ǫ, ǫmin and ǫmax , instead of taking into account the entire history of ǫ, i.e.1
σ ≡ σ(ǫ, ǫmin , ǫmax ).
(B.1)
where ǫmin and ǫmax are the onset unloading and the onset reloading modified
strain, respectively. Therefore, this description could be divided into three
parts, viz. first compression, unloading and reloading.
There are some limitations with this approach, but it simplified the solving of the final equations. The numerical solution of the partial differential
equations with hysteresis operators is a more complex issue (see e.g. Visintin,
1991; Bergqvist, 1994; Brokate and Sprekels, 1996) than the solution with the
proposed Equation (B.1).
The expressions had a specific pattern for the three loading situations.
Several authors have measured the first compression of wet fibre networks
1
The modified strain can be readily converted to porosity, φ, according to φ = 1 −
65
1
eǫ .
66 APPENDIX B. RATE-INDEPENDENT FIBRE-NETWORK STRESS
quasi-statically (Campbell, 1947; Han, 1969; Vomhoff and Schmidt, 1997).
According to Campbell (1947), Ingmanson (1952), Han (1969), Gren and
Ljungkvist (1983) and Lobosco (2000), beating does not have any significant
influence on the compressibility behaviour of fibre networks. Campbell (1947)
suggests a mathematical description of this behaviour according to:
p
σf c
= N c/M ,
pr
(B.2)
where c is the concentration (c = ρf /eǫ ), σf c is the applied stress, pr is a
reference pressure and M and N are fitting constants. This equation was
employed in this study as there are several experimental data for different
kind of pulps expressed in this form.
The unloading behaviour was described with the relation:
B−
σun (ǫ, ǫmin ) = σf c (ǫmin )
ǫmin −ǫ0
ǫ−ǫ0
B−1
β
,
(B.3)
where
B=
ǫmin − ǫ0
ǫf c − ǫ 0
β
,
(B.4)
and ǫf c , and σ are parameters dependent on ǫmin (see below). Equation B.3
is intrinsically non-linear, which requires a non-linear algorithm in order to
estimate the parameters. Therefore β, ǫ0 and ǫf c , were estimated for experimental unloading curves using an iterative algorithm (Nelder-Mead simplex
method (Lagarias et al., 1998)).
From the results presented in Figure B.1, β was assumed constant and
equal to 2.3. The two other parameters was considered dependent on ǫmin ,
viz.
β = 2.3
ǫ0 = −0.055 + 0.95ǫmin
ǫf c = 0.3 + 1.15ǫmin
(B.5)
(B.6)
(B.7)
67
Figure B.1: Parameters as a function of the modified strain for several
unloading experiments (high loads).
Figure B.2: Experimental (unloading only) responses to the quasi-static
pulses, and the results obtained with the mathematical expression.
68 APPENDIX B. RATE-INDEPENDENT FIBRE-NETWORK STRESS
Figure B.3: The experimentally measured fibre network compressibility
behaviour at low loads (Vomhoff and Schmidt, 1997). The results obtained
with the mathematical expression are also presented for comparison.
The fit between the mathematical description suggested for the unloading
curves and the experimental results are shown in Figure B.2 and Figure B.3.
In order to describe consecutive compressions, it is necessary to know
not only the strain at which unloading started, but also the strain at which
reloading starts. The following equation was used to describe reloading equilibrium curves starting at zero stress, σ = 0:
1/α ǫ
σre,0 (ǫ, ǫmin ) = σf c (ǫmin )
e
ǫ−ǫmin
min −ǫf c
− e−1/α
1 − e−1/α
.
(B.8)
The parameter α, was chosen to be: α(ǫmin ) = −0.02 + 0.12ǫmin for high
loads, where as for low loads, α showed to behave according to: α(ǫmin ) =
−0.016 + 0.3ǫmin .
For reloading curves starting at σ 6= 0, a weighted average of Equations (B.3) and (B.8) was proposed, viz.
σre (ǫ, ǫmin , ǫre ) = σre,0 +
ǫmin − ǫ
(σun (ǫre ) − σre,0 (ǫre )) .
ǫmin − ǫre
(B.9)
SOLIDS CONTENT [%]
69
STRESS [MPa]
Figure B.4: Stress-strain behaviour for cyclic compression according to
Equation (B.9). The sign of the compression is shown with an arrow. The
first compression is closet to the arrow.
Equation (B.9) could describe qualitatively the behaviour observed in
Jones (1963), see Figure B.4 cf. Figure 1.5.
The mathematical description approximated well the quasi-static curves
in different experiments (Figure B.5). However, as the error is accumulated,
some significant discrepancies was observed at the successive pulses. This
accumulated error is not shown, as the experimental ǫmin and ǫmax were used
in Equation (B.9).
Figure B.5: The experimental response to consecutive completely unloaded quasi-static pulses.
70 APPENDIX B. RATE-INDEPENDENT FIBRE-NETWORK STRESS
Appendix C
Numerical Solution with FEM
Equation (A.18) is markedly more easily solved if the z-coordinate is changed
to a convective coordinate, ζ, according to (Jönsson and Jönsson, 1992;
Mitchell and Johnson, 2001; Fung and Tong, 2001):
dζ =
ρ̃f
(1 − φ (z, t)) dz
w
⇒
∂ζ
ρ̃f
= − (1 − φ)v̂f ,
∂t
w
(C.1)
where w is the suspension grammage. Applying this coordinate transformation and expanding ∂σf 0 /∂ζ by applying the chain rule, Equation (A.18)
becomes:
∂φ (1 − φ)2 ρ̃2f ∂
−
∂t
w2
∂ζ
(1 − φ)K ∂σf 0 [φ] ∂φ
µ
∂φ ∂ζ
= 0.
(C.2)
In order to obtain Equation (C.2) in a dimensionless form, one needs just to
multiply by a time constant, for instance, the process time, tf inal ,
∂
∂φ
− (1 − φ)2
∂τ
∂φ
∂φ
1
De(1 − φ) ∂ζ
= 0.
(C.3)
where τ = t/tf inal and De is a Deborah number1 :
De =
µ (w/ρ̃f (1 − φ))2
.
tf inal K (∂σf 0 [φ]/∂φ)
1
(C.4)
The Deborah number is called in reference to the Biblical prophet Deborah: She said
the mountains flow according to the Lord’s time scale and not humans’.
71
72
APPENDIX C. NUMERICAL SOLUTION WITH FEM
The process is flow controlled for high De and press controlled, otherwise.
The most important advantage with this formulation is that the spatial
domain is constant, Ω = [0, 1], yielding a rectangular space-time domain
Q = Ω × I, where I = [0, tf inal ].
Equation (C.3) can be rewritten as:
1
∂φ
∂
+
2
∂ζ
− (1 − φ) ∂τ
∂σf 0 [φ] ∂φ
1
Ev (1 − φ) ∂φ ∂ζ
= 0,
(C.5)
by dividing the Deborah number into a viscous stress, Ev =
µ(w/ρ̃f (1−φ))2
,
tf inal K
∂σ
[φ]
f0
. The dimensionless forms of the initial and boundary conditions
and ∂φ
are straightforward. Substitutiong σf 0 [φ] for σf 0 (φ, φmini , φmax ), and then
expressing Equation (C.5) in the weak form and integrating the second term
by parts, one obtains:
1
1
∂φ
vdζ
2
0 − (1 − φ) ∂τ
Z 1
1
∂σf 0 ∂φmini
∂σf 0 ∂φmaxi ∂v
∂σf 0 ∂φ
+
+
+
dζ = 0,
∂φ ∂ζ
∂φmini ∂ζ
∂φmaxi ∂ζ
∂ζ
0 Ev (1 − φ)
(C.6)
Z
where v is a test function belonging to the infinite space, V , of bounded continuous functions and piecewise continuous derivatives on [0, 1] with v(0) =
v(1). Partionining the interval (0, 1) in 0 = ζ0 < ζ1 < · · · < ζN < ζN +1 = 1,
we can then introduce the basis functions 2 , ϕi , of the finite-dimensional subspace Vh ∈ V :
ϕi =
0,
ζ−ζi−1
,
ζi −ζi−1
ζ−ζi+1
,
ζi −ζi+1
if ζ ∈
/ [ζi−1 , ζi+1 ]
if ζ ∈ [ζi−1 , ζi ]
(C.7)
if ζ ∈ [ζi , ζi+1 ].
So, Vh is the space of continuous functions v that are piecewise linear with
respect to the partitioning suggested such that v(0) = v(1) = 0. In this
subspace, the solution can be written as a linear combination of the basis
functions:
2
The are the so-called hat functions.
73
φn
φmini,n
φmaxi,n
PN +1
=
i=0 Ai (τ ) ϕi (ζ)
PN
+1
=
Bi (τ ) ϕi (ζ) .
Pi=0
N +1
=
i=0 Ci (τ ) ϕi (ζ)
Substituting Equations (C.8) and v =
yields:
X ∂Ai Z
i
∂τ
0
1
PN +1
j=0
(C.8)
ϕj (ζ) in Equation (C.6), it
Z 1
1
∂σf 0 ∂ϕi ∂ϕj
1
dζ
2 ϕi ϕj dζ + Ai
− (1 − φ)
0 Ev (1 − φ) ∂φ ∂ζ ∂ζ
Z 1
∂σf 0 ∂ϕi ∂ϕj
1
dζ
+ Bi
0 Ev (1 − φ) ∂φmini ∂ζ ∂ζ
Z 1
1
∂σf 0 ∂ϕi ∂ϕj
+ Ci
dζ, (C.9)
0 Ev (1 − φ) ∂φmaxi ∂ζ ∂ζ
where the derivatives ∂σf 0 /∂φ, ∂σf 0 /∂φmini and ∂σf 0 /∂φmaxi were calculated
numerically by finite diferences, and the integral was calculated according
to Simpson’s rule. Equations (C.9) were then solved using a Runge-Kutta
scheme. For the first compression, fewer elements were required by using the
scheme described by Equation (16.26) in Eriksson et al. (1996).