Accepted Manuscript
Lightweight geopolymer-based hybrid materials
Giuseppina Roviello, Costantino Menna, Oreste Tarallo, Laura Ricciotti, Francesco
Messina, Claudio Ferone, Domenico Asprone, Raffaele Cioffi
PII:
S1359-8368(17)31039-9
DOI:
10.1016/j.compositesb.2017.07.020
Reference:
JCOMB 5155
To appear in:
Composites Part B
Received Date: 22 March 2017
Revised Date:
14 June 2017
Accepted Date: 13 July 2017
Please cite this article as: Roviello G, Menna C, Tarallo O, Ricciotti L, Messina F, Ferone C, Asprone
D, Cioffi R, Lightweight geopolymer-based hybrid materials, Composites Part B (2017), doi: 10.1016/
j.compositesb.2017.07.020.
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ACCEPTED MANUSCRIPT
Lightweight geopolymer-based hybrid materials
Giuseppina Rovielloa,b, Costantino Mennac, Oreste Tarallod, Laura Ricciottic, Francesco Messinaa,b, Claudio Ferone,a,b,
Domenico Asproncc, Raffaele Cioffi,a,b
Dipartimento di Ingegneria, Università di Napoli ‘Parthenope’, Centro Direzionale, Isola C4, 80143 Napoli, Italy
b
INSTM Research Group Napoli Parthenope, National Consortium for Science and Technology of Materials, Via G.
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a
Giusti, 9 50121 Firenze (ITALY)
c
Dipartimento di Strutture per l’Ingegneria e l’Architettura, Università di Napoli Federico II, Napoli 80125, Italy;
d
Dipartimento di Scienze Chimiche, Università degli Studi di Napoli “Federico II”, Complesso Universitario di Monte
*
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S. Angelo, via Cintia, 80126 Napoli, Italy
Corresponding Author: tel. +39-081-5476781; fax: +39-081-5476777;
e-mail address:
[email protected] (G. Roviello)
_______________________________________________________________________________
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Graphical abstract
G-Ep
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G-Sil
1
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Lightweight geopolymer-based hybrid materials
Giuseppina Rovielloa,b, Costantino Mennac, Oreste Tarallod, Laura Ricciottic, Francesco Messinaa,b, Claudio Ferone,a,b,
Domenico Aspronec, Raffaele Cioffi,a,b
Dipartimento di Ingegneria, Università di Napoli ‘Parthenope’, Centro Direzionale, Isola C4, 80143 Napoli, Italy
b
INSTM Research Group Napoli Parthenope, National Consortium for Science and Technology of Materials, Via G.
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a
Giusti, 9 50121 Firenze (ITALY)
c
Dipartimento di Strutture per l’Ingegneria e l’Architettura, Università di Napoli Federico II, Napoli 80125, Italy;
d
Dipartimento di Scienze Chimiche, Università degli Studi di Napoli “Federico II”, Complesso Universitario di Monte
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S. Angelo, via Cintia, 80126 Napoli, Italy
Abstract
The present study reports on the preparation and characterization of new organic-inorganic
geopolymer based hybrid foams obtained by reacting an aluminosilicate source and an alkalisilicate
solution with mixtures of dialkylsiloxane oligomers or organic resins precursors. By using different
amounts of Si0 powder as in situ foaming agent, hybrid geopolymer-based foams with densities
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ranging from 0.25 to 0.85 g/cm3 were successfully prepared. These new materials are characterized
by remarkable mechanical properties, good fire resistance and low thermal conductivity,
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significantly better than those shown by neat geopolymer foams reported in the literature and
comparable or even better than those of typical (not geopolymer) inorganic foamed materials with
1.
Introduction
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similar densities.
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Porous materials are widely used in several applications including membranes, high-efficiency
adsorption materials, catalysis, as well as in the construction industry where they find their
application as insulating or sound-proof panels or for the production of lightweight structural
components. To these aims, organic polymers, metals or inorganic materials can be successfully
used as source raw material for the foamed products. In particular, thanks to their low mass, low
heat conductivity and good sound-proofing properties, organic polymer foams are particularly
suitable as insulating components and are extensively used in civil engineering. However, most
polymeric systems suffer from thermal degradation under high temperatures, affecting their
structural integrity and releasing toxic or flammable gases into the atmosphere.
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In the case of high temperature applications, as an alternative to polymeric foams, inorganic porous
materials can be used. Such materials are usually divided in two main classes, relying on the
specific use. One class comprises materials obtained by employing lightweight aggregates while the
other one is represented by highly porous materials. Several studies have been carried out about
lightweight and eco-compatible materials/aggregates [1-5] employing cold bonding techniques but
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the obtained densities (even less than 2000 kg/m3 defining lightweight aggregates) are, however,
still considerable. Slightly lower values have been obtained by employing thermal processes [6] but
such processes typically imply a high environmental impact (production of CO2). Among inorganic
porous materials, great attention has been devoted to porous geopolymers due to i) the possibility of
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using low cost raw materials [7,8], ii) their chemical resistance [9], iii) their good thermal properties
[10] and iv) their environmental friendly nature [11,12].
The term ‘‘geopolymer’’ was originally introduced by Davidovits [13] to describe the amorphous
inorganic aluminosilicate framework produced by reacting natural Si- and Al-rich materials, such as
metakaolin or industrial by-products (fly ash, blast furnace slag), with highly alkaline aqueous
solutions. Geopolymers exhibit a wide variety of technologically relevant properties, such as high
compressive strength [14], fire resistance and low shrinkage [15]. For these reasons, geopolymers
seem to be a desirable alternative to ordinary Portland cement also thanks to their environmentally
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sustainable characteristics [16] mainly associated with the reduced CO2 emissions arising from the
production of the raw materials from which they are obtained [17].
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Geopolymers are produced by means of a polycondensation reaction (the so called
“geopolymerization”). During this reaction, a gel network is formed, consisting of SiO4 and AlO4
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tetrahedra sharing oxygen corners and forming rings of various sizes analogous to those found in
zeolites. If foaming agents are added into the geopolymer paste during its consolidation, porous
materials can be obtained. Well know blowing agents are hydrogen peroxide, metallic Al or Si
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powder [18-20]. By following this synthesis approach, porous materials with pore size ranging from
nanometers to few millimetres and a total porosity up to 90% were obtained [21,22] without using
high temperature treatments (such as burn out of organics and sintering) that are, by contrast,
necessary for the production of porous ceramics through conventional techniques [23].
In general, the geopolymer-based porous materials developed to date exhibit very interesting
properties in terms of thermal and acoustic conductivity but the presence of pores and the extremely
heterogeneous structure affect unavoidably their mechanical properties, sometimes resulting in low
compressive strengths (found to be about 1 MPa or less depending on the corresponding apparent
density) [20]. In detail, consolidated foams characterized by thermal conductivity values of
approximately 0.15 Wm-1K-1 or less were successfully obtained with the addition of silica fume or
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silicon powder [21] as a foaming agent to sodium silicate and kaolin [24] or potassium silicate
based [25] geopolymers. In the cited studies, the authors exploited the capability of free silicon
contained inside the silica fume to generate porosity by releasing molecular hydrogen from silicon
oxidization in alkaline solution, achieving significant percentages of pore volume (> 60% ) [26].
Porous geopolymer materials were also produced starting from fly ash precursors and in
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combination with hydrogen peroxide [27] or sodium perborate [28] as foaming agent, resulting in
consolidated foams with a porosity of ≈ 80 %, thermal conductivity of ≈ 0.08 Wm-1K-1 and
compressive strengths ranging between 0.80 and 0.40 MPa. Higher compressive strengths were
recorded in the case of fly ash based geopolymer foams with bulk densities in the range of 400–800
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kg/m3 and obtained with the use of aluminium powder as blowing agent [29] . Furthermore, in the
case of geopolymer and fly ash foam concretes, the higher densities of the obtained materials
(typically from 720 to 1600 kg/m3) led to very high compressive strengths ranging from 3 to 48
MPa, with thermal conductivity values in the range of 0.15–0.48 Wm-1K-1 [30] which are
reasonably low for concrete applications.
Recently we succeeded in obtaining organic-inorganic hybrid materials by reacting an
aluminosilicate source and an aqueous alkali hydroxide and/or alkalisilicate solution with mixtures
of dialkylsiloxane oligomers or organic resins precursors [31-38]. Compared to neat geopolymers
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with analogous Si/Al ratio, these materials are characterized by enhanced mechanical properties,
along with good temperature and fire resistance [39-42].
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In this study, for the first time, we report on the synthesis and characterization of high performance
organic-inorganic hybrid foams obtained by in situ foaming of the hybrid materials described before
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through the addition of silicon powder. These foams show remarkable mechanical properties, good
fire resistance and low thermal conductivity, significantly enhanced in respect to those
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characterizing neat geopolymer foams reported in the literature and comparable, or even better, than
those of typical (not geopolymeric) inorganic foamed materials with similar densities.
Considering that commonly used organic insulating materials are flammable while inorganic ones
need complex processing conditions and/or high sintering temperatures (increasing the
manufacturing cost), the hybrid porous geopolymer-based materials described in this study have
good application potential as an effective alternative for thermal insulation or fire-resistant sealant
materials.
2. Experimental Section
2.1. Materials
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Metakaolin was kindly provided by Neuchem S.r.l. (Milan, Italy) and its composition is reported in
Table 1. Sodium hydroxide with reagent grade, was supplied by Sigma-Aldrich. The sodium silicate
solution was supplied by Prochin Italia S.r.l (Caserta, Italy). with the composition reported in Table
1. A commercial oligomeric dimethylsiloxane mixture was purchased from Globalchimica S.r.l
(Turin, Italy) with the name of Globasil AL20. The epoxy resin used in this paper, called Epojet®,
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was purchased by Mapei S.p.A (Milan, Italy) [43]: it is a commercial two-component epoxy
adhesive for injection, which, after the mixing, takes the aspect of a low viscosity liquid and it is
usable for 40 minutes at room temperature. Silicon powder ~325 mesh was purchased from Sigma-
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Aldrich. Additional experimental details are reported in references 32 and 33.
Table 1. Chemical composition (weight %) of the metakaolin and sodium silicate solution used in
this paper.
Metakaolin
Al2O3 SiO2
K2O
Fe2O3 TiO2
MgO
CaO
others
41.90
0.77
1.60
0.19
0.17
0.67
52.90
Sodium silicate solution
Na2O
H2O
27.40
8.15
64.45
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2.2 Specimen Preparation
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SiO2
1.80
2.2.1. Geopolymer (G-MK)
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The alkaline activating solution was prepared by dissolving solid sodium hydroxide into the sodium
silicate solution. The solution was then allowed to equilibrate and cool for 24 h. The composition of
the solution can be expressed as Na2O 1.4SiO2 10.5H2O. Metakaolin was then incorporated into the
activating solution with a liquid to solid ratio of 1.4:1 by weight, and mixed by a mechanical mixer
for 10 min at 800 rpm. As revealed by EDS analysis on the cured samples, the composition of the
whole geopolymeric system can be expressed as Al2O3 3.5SiO2 1.0Na2O 10.5H2O, corresponding to
a complete geopolymerization process. Neat geopolymer sample was indicated as G-MK.
2.2.2. Foamed Geopolymer Composites (G-Ep)
Geopolymer-based foamed composites were obtained by adding 10% by weight of Epojet® resin to
the freshly-prepared geopolymeric suspension, and quickly incorporated by controlled mixing (5
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min at 1350 rpm) [32]. Before being added to the geopolymeric mixture, Epojet® was cured at
room temperature for 10 minutes, when it was still easily workable and long before its complete
crosslinking and hardening (that takes place in about 5–7 hours at 23 °C).
In order to obtain a smooth but effective foaming process, silicon powder was then added as
foaming agent with different wt% ratios, ranging between 0.03 and 0.24%; afterwards, the system
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was mixed for further 5 min at 1000 rpm. The consolidated geopolymer/organic resin samples
obtained through the above mentioned procedure are hereafter indicated as G-EpXX, where XX
refers to the decimal units by weight (percentage) of silicon foaming agent added to the geopolymer
composite paste (e.g. G-Ep03 refers to a Geopolymer-Epojet composite with 0.03% by weight of Si
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content; G-Ep12 corresponds to 0.12% wt% of Si content). The composite sample that did not
undergo the foaming process was indicated as G-Ep. The mix design details of G-Ep specimens are
reported in Table 2.
2.2.3. Foamed Geopolymer Hybrids (G-Sil)
Hybrid polysiloxane-geopolymer foamed samples were prepared by incorporating 10% by weight
of a commercial oligomeric dimethylsiloxane mixture into the freshly prepared geopolymeric
suspension under mechanical stirring, when the polycondensation reaction of both geopolymer and
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dimethylsiloxane were already started but far to be completed. In order to obtain a set of samples
with a different degree of porosity, silicon powder was added to the geopolymer-hybrid suspension
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as foaming agent in different wt% ratios, ranging between 0.03 and 0.24%; then, the system was
mixed for further 5 min at 1000 rpm. These samples are hereafter indicated as G-SilXX, where XX
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refers to the decimal units by weight (percentage) of silicon foaming agent added to the geopolymer
paste (e.g. G-Sil03 refers to a polysiloxane-geopolymer hybrid sample with 0.03% by weight of Si
content while G-Sil12 corresponds to 0.12% wt% of Si content). The hybrid sample that did not
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undergo the foaming process was indicated as G-Sil. The mix design details of G-Sil specimens are
reported in Table 2.
Table 2. Mix composition (wt%), apparent density and open porosity of the studied samples.
Sample
MK
SS
NaOH
Epoxy
Resin
G-MK
41.55
50
8.45
G-Ep
37.4
45.0
7.6
10
G-Ep03
37.4
45.0
7.6
10
Open
DMS
Si
porosity
(%)
-
0.03
Apparent
density (g cm–3)
15%
1.524
22%
1.425
38%
0.860
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37.4
45.0
7.6
10
-
0.06
41%
0.629
G-Ep12
37.4
45.0
7.6
10
-
0.12
48%
0.500
G-Ep14
37.4
45.0
7.6
10
-
0.14
49%
0.431
G-Ep18
37.4
45.0
7.6
10
-
0.18
50%
0.363
G-Ep24
37.4
45.0
7.6
10
-
0.24
52%
0.312
G-Sil
37.4
45.0
7.6
-
10
7%
1.339
G-Sil03
37.4
45.0
7.6
-
10
0.03
27%
G-Sil06
37.4
45.0
7.6
-
10
0.06
41%
G-Sil12
37.4
45.0
7.6
-
10
0.12
46%
G-Sil14
37.4
45.0
7.6
-
10
0.14
54%%
G-Sil18
37.4
45.0
7.6
-
GSil24
37.4
45.0
7.6
-
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G-Ep06
0.701
0.508
0.396
0.365
10
0.18
60%
0.320
10
0.24
75%
0.252
MK = metakaolin; SS = sodium silicate solution; epoxy resin = Epojet® resin; DMS = oligomeric
dimethylsiloxane mixture; Si = silicon powder
2.2.4. Curing treatments
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As soon as prepared, all the specimens were casted in cubic molds and cured in >95% relative
humidity conditions at room temperature (≈ 22°C) for 24 h and then at 60 C for further 24 h.
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Subsequently, the specimens were kept at room temperature for further 5 days in >95% relative
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2.3 Methods
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humidity conditions and then for further 21 days in air.
2.3.1 Physical testing and microstructure
SEM analysis was carried out by means of a Nova NanoSem 450 FEI Microscope.
Hydrostatic weighing for apparent density and open porosity measurements was carried out by
means of a balance OHAUS-PA213 provided by Pioneer.
Average pores diameter was determined by optical image analysis of polished surfaces. The
analysis was performed by means of an in-house routine developed using a commercial software
package (Matlab R2015a) [44].
2.3.2 Rheological measurement
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Simple flow measurements related to pastes can be performed by means of the minislump cone test
[36]. This testing technique represents a simple procedure that is employed quite frequently in
literature since it allows making both qualitative and quantitative observations on fresh slurries.
However, the geometry of the experimental setup is not standardized and varies in a wide range
[45-49]. In this work, the geometry of the minislump cone was had the following dimensions: top
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diameter equal to 5.0 cm; bottom diameter equal to 6.8 cm; height equal to 6.5 cm (corresponding
to a paste volume equal to 179.1 cm3). Freshly prepared slurries were slowly poured in the cone
placed on a horizontal plane and carefully compacted by means of a thin steel rod. Slump
orthogonal diameters were measured and the average diameter was used to calculate minislump
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area. Mini-slump measurements were repeated at 0, 15, 30, 60 and 120 minutes in order to enlighten
workability loss depending on time, by keeping the fresh slurries in controlled environment
(T=20±2°C; sealed container). Apparent viscosity of geopolymeric mixtures was assessed by means
of a Brookfield viscometer DV2T. Test were carried out with different spindles considering the
variation of rheological features of investigated mixtures. Spindles used are standardized for the
indicated device and are indicated by numbers, namely n° 4, 5, 6 and 7.
Additional tests were carried out in order to understand the capability of geopolymer slurries to
retain liquid phase. Hence, washout tests were performed by means of a modified experimental
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setup with respect to the one used in literature [50]. In particular, instead of 750 mL beakers, 500
compared to the initial mass.
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2.3.3 Mechanical testing
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mL ones were used. Washout loss after dilution in distilled water was expressed in percentage
Uniaxial compression tests were carried out according to of ASTM D 1621 on 50×50×50 mm cubic
specimens by using a MTS 810 servo-hydraulic universal testing machine. For each sample type,
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three specimens were tested under displacement control in order to obtain the corresponding stressstrain curve, compressive strength and Young’s modulus. Compression tests were performed until
the sample densified and/or ruptured at a constant displacement velocity of 0.60 mm/min. The
measurement of the displacement was performed through the crosshead displacement while the
Young’s modulus of each sample was computed from the initial linear stress-strain response
recorded during the test. All values presented in the current work are an average of three samples.
2.3.4 Thermal characterization
The thermal conductivity measurement was performed in accordance with UNI EN 1745 and UNI
EN 12664, by means of the Guarded Hot Plate Method on air-dry samples with conditioning at
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50°C. The measurement equipment used follows ASTM E1530. For each sample examined, three
specimens with diameter 50.8±0.3 mm and thick 4.3 mm at 10°C were tested.
The test specimens were installed between heating and cooling plates. A constant heat flow flowed
through the test specimens in the stationary temperature state. Thermal conductivity was determined
by the heat flow and the temperature difference between the sample surfaces. The calibration was
conductivity λ (W/mK) can be determined according to the following:
=
(1)
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where s is the specimen thickness and Rs is the thermal resistance.
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performed on a series of reference samples with certified thermal characteristics. The thermal
2.3.5 Fire testing
Flame tests were performed by a cone calorimeter in accordance with the procedure described in
ISO5660 standard method. The heat flux produced was 50kW/m2 on the specimen, which had an
exposed surface of 100×100 mm. The testing equipment consisted of a radiant electric heater in
trunk-conic shape, an exhaust gas system with oxygen monitoring and instrumentation to measure
the gas flux, an electric spark for ignition, and a load cell to measure the weight loss. The test was
Results and discussion
3.1 Foaming process
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terminated after 600 s of exposure.
As described in the previous section, different amounts of silicon powder were added as foaming
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agent to the neat geopolymer slurry (G-MK) and to the two hybrid organic-geopolymer systems GEp and G-Sil. As far as G-MK slurry is concerned, due to its very low viscosity (see section 3.2),
the foaming process yielded the rapid collapse of the foamed structure initially formed. For this
reason, foamed G-MK samples were not considered in this discussion. On the contrary, the addition
of the foaming agent to G-Ep and to G-Sil slurries produced homogeneously foamed structures.
Volume expansion and density of the different G-Ep and G-Sil foamed samples obtained are
reported in Figure 1.
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Figure 1. Density values (red bars) and volume expansion (black bars) of G-Ep and G-Sil foamed
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samples. Volume expansion was evaluated by the percentage ratio between the volume of the
specimen after the foaming process and the starting volume of the slurry.
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As expected, the effectiveness of the foaming process was strictly dependent on the Si amount
added to the G-Ep and G-Sil slurry as foaming agent. The volume expansion of the not cured slurry
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increases with increasing the amount of the foaming agent while the density of the cured porous
materials decreases as the amount of foaming agent used increases. For silicon amount ranging
from 0.03% to 0.24 wt%, high resolution optical photographs of the specimens after expansion and
curing, are reported in Figure 2.
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G-Sil
G-Ep
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Fig. 2: Optical images of polished section surfaces of some representative G-Sil (left column) and
G-Ep (right column) specimens.
By examining the morphologies shown in Figure 2, it is clearly apparent that macropores are
observable in all samples and, for each composition, they are rather uniformly distributed in the
specimens, resulting in good homogeneity also in terms of dimension and shape. Only a minor
amount of egg-shaped pores was detected, parallel to the expansion direction, probably attributable
to the shape and dimensions of the used mold.
As expected, a low quantity of silicon powder added as foaming agent led to poorly expanded
structures with small and regularly distributed rounded pores while high Si content produced the
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coalescence of the pores. Average diameters of pores were equal to 0.70, 1.33, 2.28 and 4.84 mm
for G-Sil03, G-Sil06, G-Sil12 and G-Sil24, respectively while were equal to 0.57, 0.85, 1.28 and
3.13 for G-Ep03, G-Ep06, G-Ep12 and G-Ep24, respectively. Although not reported in this study,
it’s worth pointing out that the addition of Si in amounts of more than 0.24 wt% caused the unstable
collapse of the foamed microstructure. The morphological characterization is very useful to receive
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information about the micromechanical model [51-53].
By examining the morphologies of the foams by SEM micrographs (Figure 3), it is worth pointing
out that, as expected, the surfaces of both samples appeared to be very different from the typical
microstructure of an unfoamed geopolymer matrix [32, 33]. In particular, in the case of G-Ep series
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of samples, a 3D pore structure was detected and characterized by interconnected channels passing
throughout the specimen. In the case of G-Sil foams, the microstructure was characterized by
isolated pores uniformly distributed within the specimens, showing good homogeneity, also in
terms of dimensions and shape. This different morphology was rationalized in terms of rheological
properties of the two slurries (next paragraph).
As discussed in paragraph 3.4, these different microstructures of the two sets of samples turned out
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in different mechanical behaviours.
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Figure 3 SEM images at 100 (A, C) and 2000 (B, D) magnification of G-Ep03 (A, B) and G-Sil03
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(C, D). In B and D, images of the wall between large pores are shown.
3.2 Rheology
Slump test results are reported in Figure 4 and refer to the G-MK, G-Sil and G-Ep slurries tested as
soon as prepared and for different resting times. The system exhibiting the largest flow is G-MK,
while an intermediate performance was obtained for G-Sil. At variance, G-Ep was able to keep
almost unchanged the shape of the slump cone after cone lifting due to very high values of viscosity
and yield stress, thus indicating a strongly different rheological performance respect other
investigated materials. In terms of workability loss, the two “flowable” systems, i.e. G-MK and GSIL, exhibited a similar behaviour. Particularly, the system G-MK was able to keep its
characteristic flow area for at least 30 minutes; this represents a significant parameter for most of
the technological processing procedures on laboratory and industrial scale. G-Sil exhibited a faster
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workability loss with respect to G-MK, since after flow measured after 30 minutes was about 10%
of initial slump value. G-Ep did not experience any significant change over time since the starting
value of mini slump area, which was substantially similar to the bottom area of the cone, was kept
almost constant for all subsequent measurements.
500
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G-MK
G-Sil
G-Ep
450
350
300
250
200
150
100
50
0
20
40
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2
Slump Area (cm )
400
60
80
100
120
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Figure 4. Variation of slump area with time for G-MK (black squares), G-Sil (red circles) and G-Ep
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(blue triangles) slurries. Lines are a guide for the eyes.
Apparent viscosity measurements related to G-MK, G-Sil and G-Ep slurries are reported in Figure
5. Measurements were performed with different rotating spindles in order to provide further
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information and ensure a better reproducibility of the results. The possibility of using several
spindles depends on the viscosity of the investigated suspension: for relatively high viscosity
values, the number of suitable spindles is limited. In Figure 5, it is evident that G-Sil is
characterized by higher viscosity than G-MK since the number of suitable spindles (spindle n°5 and
spindle n°6) is limited with respect to those that are suitable for G-MK (spindles n°4, n°5 and n°6).
In the torque range investigated, the two mixtures exhibited a very different rheological behaviour.
First, for G-MK, a plateau of apparent viscosity was clearly detected, while for G-Sil, a slight
decrease was detected as a function of torque growth.
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G-MK slurry, spindle n°4
G-MK slurry, spindle n°5
G-MK slurry, spindle n°6
G-Sil slurry, spindle n°5
G-Sil slurry, spindle n°6
G-Ep slurry, spindle n°7
5
8x10
5
5
6x10
4
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1.8x10
4
1.6x10
4
1.4x10
4
1.2x10
4
1.0x10
3
8.0x10
3
6.0x10
3
4.0x10
3
2.0x10
0.0
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Apparent Viscosity (cP)
7x10
20 25 30 35 40 45 50 55 60 65 70 75 80 85 90 95 100
Torque (%)
Figure 5. Apparent viscosity of G-MK (squares), G-Sil (circles) and G-Ep (triangles) slurries as
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measured with the spindle indicated. Lines are a guide for the eyes.
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With regard to the apparent viscosity related to G-Ep slurry, it must be pointed out that
measurement was strongly influenced by the applied shear regime. Hence, a significant variation of
apparent viscosity was experienced depending on different torque applied. In the same range of
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investigated torque for other systems, G-Ep slurry exhibited an apparent viscosity equal to
6.8·105±0.4·105 cP. The presence of a plateau viscosity value was shifted at higher torque (torque >
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80%). The apparent viscosity values are evidently much higher than in the other cases
corresponding to G-MK and G-Sil slurries. This fact corresponds also to the restrained choice in
terms of suitable spindles, which was limited only to spindle n°7.
Finally, Figure 6 shows washout loss values for the three investigated slurries: for all the systems, a
highly promising water retention capability was detected thus indicating a good processability of
the material before its hardening.
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8
6
4
2
0
G-Sil
G-Ep
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G-MK
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Washout loss (%)
10
Figure 6. Washout loss values for G-MK, G-Sil, G-Ep as determined on their freshly prepared
slurries.
The different rheological behaviours herein discussed allowed for a possible interpretation of the
different foaming performances observe for the three investigated systems. Actually, we can infer
that the neat geopolymer prepared in this study was not able to develop a properly foamed
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microstructure, due to the very low viscosity of the slurry. The addition of silicone or epoxy resin to
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the geopolymer slurry turned out in a significant increase of the viscosity of the system that allows
the development of stable pores, thus resulting in a properly foamed microstructure. Moreover, the
different rheological behaviour of the G-Sil and G-Ep systems is probably connected with the
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different microstructure of the two samples [32, 33]. In fact, G-Ep is a geopolymer based composite
system containing discrete microspheres of epoxy resin (mean diameter 10-20 µm), homogenously
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dispersed in the geopolymer matrix (see Figure 3B). At variance, G-Sil is a hybrid geopolymer
material obtained through the chemical bonding between silicon atoms of the geopolymer structure
with the silicon atoms of the dimethylsiloxane oligomer moieties, characterized by a single phase,
with compact and continuous microstructure, up to nanometric level (see Figure 3D) [32, 33].
3.4. Physical and Mechanical Properties
Physical and mechanical properties of foamed hybrid and composite geopolymers are herein
discussed in terms of material apparent density and uniaxial compressive behaviour, including
compressive strength and Young’s modulus results.
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The average apparent densities of G-Sil (blue symbols) and G-Ep (red symbols) foams are reported
in Figure 7 as a function of the wt% of Si powder added to the geopolymer slurry during foaming
procedure. The two foamed materials exhibited a decrease of bulk density with increasing the Si
content in the range 0.03-0.24 wt%, following a 2nd order polynomial law. The obtained trends
suggested that lower densities were achieved as a consequence of the coalescence of individual cells
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of roughly constant smaller pore size (see Figures 2 and 3) into large voids. However, G-Sil foamed
material was able to reach lower density values than G-Ep foamed material when using an equal
content of foaming agent. In particular, G-Sil foamed material exhibited an average apparent
density varying between 0.25 and 0.70 g/cm3 whereas, in the case of G-Ep foamed material, the
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density values varied between 0.31 and 0.86 g/cm3. In other words, within the density range
obtained with the same amount of foaming agent, G-Sil foam was averagely less dense by 20%.
This feature is mainly related to the rheological proprieties of the two different initial materials
which affected cell nucleation, growth and coarsening mechanisms taking place during the foaming
process. Indeed, as reported in the previous section, the G-Ep system was characterized by very
high values of viscosity and yield stress. During the expansion process, the gas volume in the
growing cell increases driven by the gas pressure generating inside the cell itself, until the pressure
inside the cell equals to its surrounding pressure, which is a function of surface tension and
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viscosity of the fresh matrix material. Because of greater viscosity of G-Ep material, a lower surface
area is required to make the cell in equilibrium with its surrounding matrix which turns in smaller
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cell sizes of the foamed material (Figure 2). Furthermore, the dense spheres of epoxy resin forming
the heterogeneous microstructure of G-Ep system may have acted as physical obstacle for cell
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growth phase. On the contrary, in the case of G-Sil material, the lower viscosity of the system
allowed for a larger volume growth, which led to a decrease of the stability of the foam, causing, in
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turn, individual cells to coalesce producing larger voids (Figure 2).
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1.00
G-Sil
G-Ep
0.60
0.40
0.20
0.00
0.10
0.20
0.30
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% wt of Si
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Density [g/cm3]
0.80
Figure 7: Average apparent densities (over three samples) of G-Sil (blue symbols) and G-Ep (red
symbols) foamed materials as a function of the foaming agent content (wt% of Si powder).
Because of the large number of specimens tested, only the stress-strain curves of the samples that
revealed a representative mechanical performance were reported in Figure 8. The stress–strain
curves for each tested foam type were found to be similar kind. In details, all the investigated
foamed materials exhibited a well defined elastic regime, which was noticeable at the early stages of
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stress (stage 1). The linear elastic regime remained with an almost constant slope until reaching the
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yield or unstable collapse point (stage 2) characterized by a sharp load loss on the stress strain-curve
up to a plateau or softening region in the case of G-Sil and G-Ep foam, respectively (stage 3). In
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stage 3, the compression stress was almost constant with strain for higher densities of G-Sil foams
(i.e. for density values of 0.50 and 0.70 g/cm3) as the cells deformed plastically; in those cases, after
the yield stress was reached, the specimen continued to carry 3 MPa of stress up to relatively large
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strains, i.e. 25% of axial deformation. On the contrary, G-Ep foams showed a softening behaviour
in stage 3 up to lower ultimate strains compared to G-Sil foams. The recorded discrepancy was
probably due to the heterogeneous microstructure [32] of G-Ep matrix which was not able to
accommodate the increased local deformation associated with the progressive collapse mechanism
of the cells. A further region of rapidly increasing load (densification region, stage 4) was recorded
only in the case of higher density G-Sil foams.
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G-Sil06
12
G-Sil12
G-Sil24
9
6
3
0
0.00
0.05
0.10
0.15
0.20
0.25
G-Ep03
G-Ep06
12
Stress [MPa]
Stress [MPa]
15
G-Sil03
0.30
Strain [mm/mm]
G-Ep12
G-Ep24
9
6
3
0
0.00
0.05
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15
0.10
0.15
0.20
0.25
0.30
Strain [mm/mm]
(b)
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(a)
Figure 8: Stress-strain curves in compression of G-Sil (a) and G-Ep (b) samples.
The compressive strength of tested foamed materials was calculated from the maximum load
applied to the specimens (corresponding to the yield or unstable collapse point - stage 2) while the
Young's modulus under compression was derived from the slope of the initial linear region of the
stress-strain diagram. The average values of compressive strength and Young’s modulus (computed
from measurements on three samples) are shown in Figure 9a and Figure 9b for G-Sil (blue
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symbols) and G-Ep (red symbols) foamed materials as a function of the relative density ρ*/ρs, i.e.
the ratio between the actual apparent density of the foam, ρ*, and the density of the fully dense neat
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G-Sil and G-Ep materials, ρs, equal to 1.34 and 1.42 g/cm3, respectively. For both foam material
types, the overall results showed that the foaming process was able to produce satisfactory
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mechanical performances in reference to similar materials [20, 22, 30]. In particular, considering
that average compressive strengths of fully dense neat G-Sil and G-Ep materials was 65 and 41
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MPa, respectively [33], the corresponding compressive strengths of foamed samples varied between
11 and 0.67 MPa in the density range of 0.25-0.86 g/cm3 (corresponding to 0.19 and 0.60 of relative
density, respectively). As general tendency, G-Sil foamed material developed higher compressive
strengths than G-Ep foam type in the density range of 0.45-0.70 g/cm3 (0.34-0.52 ρ*/ρs). The
greatest difference was estimated in correspondence of a density value 0.70 g/cm3 and was equal to
47%. Below the density threshold of 0.45 g/cm3 (corresponding to a relative density between 0.350.40), this tendency was reversed in favour of G-Ep foams which exhibited, for instance, a
compressive strength 40% greater than G-Sil foam in the case of 0.30 g/cm3 of density (1.62 vs 1.15
MPa, respectively). This behaviour can be correlated to the deformation response of the two
different cellular materials which is strongly influenced by corresponding value of relative density.
At higher densities, the mechanical performance of the foamed material under compression
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typically approaches the compressive behaviour of the full dense material. Indeed, as reported in a
previous study by the authors [27], in the full dense state, G-Sil material has averagely improved
mechanical performances (either stiffness and strength) compared to G-Ep systems. On the other
side, at low densities, compressive failure is typically caused by tensile failure of the bent cell walls
of a given diameter. In this respect, full dense G-Sil was found to behave as a brittle material under
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failure [33] while G-Ep exhibited a moderate toughening mechanism (with regard to fracture) due
to the presence of the discrete resin particles. Consequently, the tougher G-Ep was able to
accommodate larger tensile strains under bending loads and, in turn, provide a more effective
resistant mechanism to failure in compression at lower densities.
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Stress-strain curves obtained by compressive tests allowed determining also the Young’s modulus
in compression of all samples (Figure 8b). The elastic stiffness of the two foamed materials showed
a similar dependency on the density values, resulting in Young’s modulus values approximately
ranging between 100 and 1400 MPa in the density interval of 0.25-0.86 g/cm3 (corresponding to
0.19 and 0.60 of relative density, respectively). Moreover, the overall trend of the results as a
function of material density, resulted very similar to the one observed for the compressive strength,
i.e. with an inversion point in correspondence of a material density of approximately 0.45 g/cm3
(corresponding to a relative density between 0.35-0.40). In particular, for densities below 0.45
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g/cm3, the Young's modulus of the foams is largely controlled by the volume fraction of large
coalesced voids. In the case of G-Sil foam, brittle micro-cracking of bent coalesced voids may act
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as an additional contribution to deformation within the foam matrix, decreasing the initial stiffness.
For densities above 0.45 g/cm3, the volume fraction of large coalesced voids is small and the
9
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3
Analytical
3
2
1
0
0.14
0
0.10
Young's Modulus [MPa]
12
G-Ep
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G-Sil
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Compressive Strength [MPa]
Young's modulus of the G-Sil foam is controlled by the stiffer matrix compared with G-Ep one.
0.30
0.26
0.50
Relative Density, ρ*/ρs [-]
a)
G-Sil
1000
450
500
300
150
0
0.14
0.38
0.70
Analytical
G-Ep
1500
0
0.10
0.30
0.50
0.26
0.38
0.70
Relative Density, ρ*/ρs [-]
b)
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Figure 9: Average (over three samples) compressive strengths (a) and Young’s modulus (b) for GSil (blue symbols) and G-Ep (red symbols) foamed materials as a function of the relative density.
It’s worth noting that within the density range 0.20-0.45 g/cm3 both foamed materials exhibited
interesting compression properties, especially with reference to that density interval which
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represents an important range for technological applications of lightweight materials [23]
In terms of analytical interpretation of the results, we refer to the classical relationships between the
strength (eq. 1) or Young’s modulus (eq. 2) of a cellular material and its relative density proposed
ρ *
σ c*
= C1
s
σc
ρs
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by Gibson-Ashby [54]:
m
ρ *
Ec*
= C2
s
Ec
ρs
(1)
n
(2)
where σ c* , Ec* and ρ * are the compressive or yield strength, the Young’s modulus (in
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compression) and the relative density of the foam material, respectively; σ c , Ec and ρs are the
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corresponding properties referred to the fully dense solid of which the foam is made or, in an
equivalent manner, the properties of the solid cell wall material; C1, C2 are dimensionless constants
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and the exponents m, n depend on the cell morphology and can be established both by experiment
and by numerical computation. These relationships can be successfully used to model the
mechanical properties of most foams, whether open or closed cell, with a bending-dominated
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deformation behaviour. Dotted lines in Fig. 9 a,b represent the best fit of equations (1) and (2), the
parameters of which are reported in Table 3.
Table 3: Parameters of data fitting reported in Fig. 9 a,b (dotted lines) according to equations (1)
and (2).
Compressive Strength
G-Ep-foam
Young's modulus
C1
[-]
0.79
C2
[-]
1.52
m
[-]
2.05
n
[-]
1.95
σ cs [MPa] [27]
40.8
Ecs [MPa] [27]
2600
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G-Sil-Foam
C1
[-]
1.15
C2
[-]
2.35
m
[-]
2.85
n
[-]
2.90
σ cs [MPa] [27]
62.0
Ecs [MPa] [27]
4160
As discussed in this section, the G-Sil and G-Ep foams behave as a linear elastic material up to the
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elastic limit under compression, at which point the cell edges failure takes place. The variations of
Young’s modulus with the relative density follows equation (2) with the exponent n equal to 2 (GEp) or 3 (G-Sil), in agreement with previous results dealing with inorganic (cementitious) foams
[55]; the different values of the exponent, n, between the two foamed materials can be related to the
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elastic properties of the corresponding fully dense solid ones.
A similar analysis can be conducted for the variation of the compressive strength with the relative
density (equation (1)). The exponents m obtained from the best fit of the experimental data resulted
higher that the ones suggested by Gibson-Ashby [54] (i.e. m = 3/2) probably due to several reasons.
Primarily, the possibility of having mixed closed and open cells along with the presence of pores in
most of the cell walls may have affected the failure initiation under compression deformation.
Secondly, the hybrid nature of the foams’ microstructure may act as positive stabilization for the
collapse limit especially at higher densities, for which the contribution of axial and shear stresses in
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the cell wall is dominant.
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3.3 Thermal conductivity
Thermal conductivity tests were carried out on G-Sil12 and G-Ep12 samples. Table 4 shows the
Sample
Density (kg/m3)
λ10, dry (W/mK)
G-Ep12_1
480.1
0.101 ± 0.002
G-Ep12_2
500.5
0.103± 0.002
G-Ep12_3
523.6
0.105± 0.002
G-Sil12_1
396.2
0.101 ± 0.002
G-Sil12_2
395.5
0.105± 0.002
G-Sil12_3
398.0
0.103± 0.002
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values.
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values of the volumetric density (kg/m3) for each examined specimens and the corresponding λ10,dry
Table 4: Density and λ10, dry of three different specimens of G-Ep12 and G-Sil12.
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In both cases, the values of thermal conductivity are in the range 0.101-0.105 W/mK.
Figure 10 shows the relation between the experimental thermal conductivity and the measured
density for G-Ep12 and G-Sil12 specimens. These results are compared with the values reported in
Tables A of EN 12664 for some representative lightweight materials used for masonry products.
Each line refers to 50% fractiles for each category of materials. As far as G-Sil12, the results
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obtained are in the same range with those found for reference materials with the same density, while
in the case of G-Ep12 the conductivity values obtained are far lower than 50% of the values
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reported in the reference materials with the same density thus indicating better insulating properties.
Figure 10: Relation between λ10, dry and density for G-Ep12 (black square); G-Sil12 (black circle);
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masonry mortars, Tab.A12 (red square); autoclaved aerated concrete, Table A10 (blue circle);
concrete with polystyrene aggregates, Table A5 (magenta triangle); concrete with expanded clay
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aggregates, Table A6 (green rhombus). All the straight lines represent P = 50% of the data.
3.2.5. Flame Tests
In order to obtain information on the combustion behaviour of the investigated materials under
ventilated conditions, fire resistance tests were performed on G-Ep18 and G-Sil12 (i.e. samples
showing similar apparent density values, see Table 2). The optical images of these samples before
and after the cone calorimeter test are reported in Figure 11.
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Figure 11 Images of G-Ep18 (A, B) and G-Sil12 (C, D) before (A, C) and after (B, D) the cone
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calorimeter test.
The cone calorimeter showed that these specimens did not ignite, burn or release appreciable smoke
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even after extended heat flux exposure. Moreover, the heat release rate (HRR), that represents the
contribution in terms of heat released by the material in case of fire, was minimal and also the CO,
CO2 and the produced fumes were of a negligible amount. In particular, G-Sil12 sample showed
specimen.
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HRR and THR values (see Table 5), CO and CO2 production (see Figure 12) lower than G-Ep18
Therefore, the foamed organic-inorganic materials described in the present paper can be considered
as not-flammable, with a not significant production of toxic fumes and smokes. Thus they can
efficiently replace the neat geopolymers in all the applications where exposure to flames and
lightness are desired.
Table 5 summarizes the main outcomes of cone calorimeter tests conducted on the investigated
foamed specimens.
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HRR (peak)
HRR (60 s)
HRR (180 s)
THR
(kW/m2)
(kW/m2)
(kW/m2)
(MJ/m2)
G-Ep18
16.6
3.9
9.4
6.0
G-Sil12
7.4
2.1
1.4
1.1
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Table 5 Flame tests results of G-Ep18 and G-Sil12, HRR= heat release rate, THR= total heat
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release.
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Figure 12 Flame test results: (A) HRR-Heat Release Rate (kW/m2) vs time (s); (B) THR-Total Heat
Release (MJ/m2) vs time; (C) SPR-Smoke production rate (m2/s) vs time (s); (D) CO production
(%) vs time (s); (E) CO2 production (%) vs time (s) for G-Ep18 and G-Sil12.
4. Conclusions
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Two different types of novel organic-inorganic geopolymer based foams were successfully
manufactured by mixing metakaolin and an aqueous alkalisilicate solution with mixtures of
dialkylsiloxane oligomers or organic resins precursors, respectively. The density of the obtained
materials (ranging from 0.25 to 0.85 g/cm3) was tailored by simply controlling the amounts of
silicon powder added to the slurry as in situ foaming agent.
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In both cases, the addition of the organic components or of the dialkylsiloxane oligomers, turned
out in a significant change of the intrinsic viscosity of the geopolymeric slurry, thus allowing the
obtainment of a homogeneous and very regular foaming process. In particular, in the case of the
composite foamed materials obtained by adding the organic resin precursor to the geopolymeric
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slurry (G-Ep), the very high viscosity of the fresh mixture (in respect to neat geopolymeric one) has
allowed obtaining a microstructure characterized by pore cells with a mean diameter up to 3 mm, in
which, the dense spheres of epoxy resin forming the heterogeneous microstructure of the cell walls
could have likely acted as physical hindrance for cell growth phase. At variance, in the case of GSil foams, the lower viscosity of the slurry allowed for a larger volume growth of the cells, which
led to a decrease of the stability of the foam, causing, in turn, individual cells to coalesce thus
producing larger voids.
These new porous materials, despite their cellular morphology, are still characterized by interesting
mechanical properties. In particular, it is worth pointing out that, for both foamed materials, average
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compressive strengths up 5 MPa were recorded within the density range 0.2-0.5 g/cm3, which
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represents an important range for technological applications of lightweight materials.
Moreover, within the same density range, both G-Sil and G-Ep foams exhibit good fire resistance
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and low thermal conductivity with λ values in the range 0.101-0.105 W/mK.
These properties are significantly better than those shown by neat geopolymer foams reported in the
literature and comparable or even better than that of typical (not geopolymeric) inorganic foamed
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materials with similar densities and could be related to the hybrid nature of the materials used. In
fact, as already shown in the case of their dense form, the synergistic effect of the organic and
inorganic components of the developed materials has a beneficial effect on their properties.
For these reasons, it can be reasonably concluded that these new hybrid materials could represent a
valid alternative to commonly used inorganic foams (e.g. Portland Cement foams) for insulation
and lightweight applications, since they combine performance benefits and operational energy
savings.
Acknowledgement
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The authors thank Neuvendis S.p.A. for the metakaolin supply and Prochin Italia S.r.l. for the
silicate solution supply. Dr. Giovanni Morieri and Dr. Luciana Cimino are warmly acknowledged
for assistance in laboratory activities. Università di Napoli “Parthenope” is acknowledged for
financial support to research activities with a grant within the call “Support for Individual Research
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for the 2015-17 Period” issued by Rectoral Decree no. 727/2015.
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ACCEPTED MANUSCRIPT
Lightweight geopolymer-based hybrid materials
Giuseppina Rovielloa,b, Costantino Mennac, Oreste Tarallod, Laura Ricciottic, Francesco Messinaa,b, Claudio Ferone,a,b,
Domenico Asproncc, Raffaele Cioffi,a,b
Dipartimento di Ingegneria, Università di Napoli ‘Parthenope’, Centro Direzionale, Isola C4, 80143 Napoli, Italy
b
INSTM Research Group Napoli Parthenope, National Consortium for Science and Technology of Materials, Via G.
RI
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a
Giusti, 9 50121 Firenze (ITALY)
c
Dipartimento di Strutture per l’Ingegneria e l’Architettura, Università di Napoli Federico II, Napoli 80125, Italy;
d
Dipartimento di Scienze Chimiche, Università degli Studi di Napoli “Federico II”, Complesso Universitario di Monte
*
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AN
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S. Angelo, via Cintia, 80126 Napoli, Italy
Corresponding Author: tel. +39-081-5476781; fax: +39-081-5476777; e-mail address:
[email protected] (G. Roviello)
Highlights
1. Hybrid geopolymer-based foams with densities ranging from 0.25 to 0.85 g/cm3 were
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obtained.
process was obtained.
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2. By using Si0 powder as in situ foaming agent, a homogeneous and very regular foaming
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3. Mechanical and thermal performances significantly better than those shown by neat
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geopolymeric foams and inorganic foamed-materials with similar densities.