Construction Materials
Volume 166 Issue CM3
Undercut anchorage in dimension stone
cladding
Camposinhos
ice | proceedings
Proceedings of the Institution of Civil Engineers
Construction Materials 166 June 2013 Issue CM3
Pages 158–174 http://dx.doi.org/10.1680/coma.11.00050
Paper 1100050
Received 17/08/2011
Accepted 17/10/2011
Published online 02/08/2012
Keywords: anchors & anchorages/design methods & aids/
stress analysis
ICE Publishing: All rights reserved
Undercut anchorage in
dimension stone cladding
Rui S. Camposinhos PhD
Coordinator Professor, ISEP, Polytechnic of Porto, School of Engineering,
Porto, Portugal
This paper analyses undercut anchorage technology, in particular its behaviour and performance as a fixing system for
dimension stone cladding of rainscreen façades. Based on a number of mechanical tests using various types of
Portuguese stone – three igneous, two sedimentary and one metamorphic – a study was carried out to investigate the
relationship between the flexural strength and breaking load of specific and very common stone types. Several
physical and mechanical characterisation tests and 130 pull-out tests with 6 and 8 mm cone bolt threads were
performed to determine the pull-out load failure on six different stone types: three granite, two limestone and one
marble. Finite-element stress analyses were carried out, and the test results were the basis for calibrating a simple
formula that can be used to estimate the stone’s breaking load at the undercut anchorage. Stress concentration
factors are proposed to take into account the undercut drill hole geometry and the specific properties of each type of
stone. Stone specimens from the same batches were subject to pull-out force tests using dowel anchorages, whose
values were then compared with the breaking load of undercut anchorages. Results are discussed and conclusions are
drawn based on tensile stress values by comparing the test results, the finite-element method and the proposed semiempirical formulations for the same breaking load.
Notation
Acf
du
em
F
Ku
r
sm
t
a
am
wt
wu
smax
st
stm
sRf
sRtf
sRf1
sRf2
1.
area of the projected cone failure surface
anchorage depth
minimum edge distance
applied force at failure
stress concentration factor
radius of the specimen (disc)
minimum space between anchors
thickness of the disc
average angle of the cone failure surface
average spall angle
diameter of the cylindrical drill hole
diameter of the undercut
actual maximum stress
tensile strength of the stone
medium tensile stress
strength of a brittle material under flexure
axial tension
flexural strength of specimen with volume v1
flexural strength of specimen with volume v2
Introduction
Art and science must come together in the design of stone
façades. The beauty and quality of natural stone make it an
ideal material for prestigious projects using successful
construction methods in many countries. Rainscreen cladding
systems, using the more expensive fixing option, in terms of
materials and fixing, can offer other benefits resulting in cost
and time savings in the overall project.
Resistance to lateral loading, mainly wind and seismic action,
is usually achieved by means of stainless steel anchors inserted
into kerfs or holes that are drilled or cut into the edges of the
stone panels. These anchors are mechanically connected to the
building’s structure, thus providing the essential mechanical
connection between the stone and the structure. One structural
weak point in this type of stone construction is to be found at
the kerfs or anchor holes on the edges of the stone slabs. These
cuts need to leave sufficient stone thickness to provide the
necessary strength to resist the various forces or actions to
which the stone panels are subject.
The failure of any stone panel may have significant consequences. Many engineers and architects have an overconfident attitude toward these issues and, although they
may not fully understand the engineering aspects of natural
stone and the behaviour of natural stone veneers, this
drawback does not seem to be a constraint when they specify
the selection, manufacture and use of natural stone as a façade
cladding material. This attitude, when combined with a lack of
regulatory controls and standards stipulating appropriate
practices, has often led to situations of serious flaws in the
selection, design, and installation of natural stone cladding
panels.
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Construction Materials
Volume 166 Issue CM3
Undercut anchorage in
dimension stone cladding
Camposinhos
Developing innovative fastening products requires in-depth
knowledge about the physical phenomena involved in the
complete process of installation and loading.
stainless steel. The sleeve is made of stainless steel or carbon.
The nut is in stainless steel or aluminium.
Generally, fasteners can be subdivided into three different
working principles according to the load transfer mechanism,
namely friction, bonding and keying.
For friction-type anchors, the tensile load is transferred from
the anchor to the base material due to the friction created by
expanded segments. For bonding anchors, the tensile load is
transferred mainly through the adhesive bond between the
anchor rod and the stone which may cause a combined shear
and cone type failure.
Keying-type anchors carry the tensile load through main keys
at the end of the anchor, resulting in a cone shape failure or in
the yielding of the steel rod. This is the case of undercut
anchoring. This technology, combined with a suitable support
framework, allows the engineer to implement a safe and high
performance fixing system for stone cladding façades. The
main aspects of this technology are described in the next
section.
2.
Undercut anchoring
Since anchoring is only a small part of the whole façade
system, all other influencing factors must be given an equal
amount of consideration for a successful design. However, to
comprehend how undercut anchors are used, a basic understanding of the most important issues of this type of
technology must be addressed.
There are mainly two types of undercut technologies to provide
a keying-type anchorage in the interior of the dimension stone
or slab’s thickness.
Anchors are installed by driving the anchor sleeve against the
locking ring, thus forcing it to expand within the undercut hole
form and locking it within the stone, which provides a stressfree anchorage under zero applied load. This system is
generally identified with the Fischer-type technology
(Deutsches Institut für Bautechnik, 2009).
The other system consists of a special anchor made of a
crosswise slotted anchor sleeve with an internal thread. The
anchor’s upper edge has a hexagon formed to it and the
respective hexagon bolt with a tooth lock washer formed to it.
The anchor sleeve and the hexagon bolt with a tooth lock
washer formed to it are also made of stainless steel. The anchor
is fitted into an undercut drill hole and, by driving the sleeve in
it is deformed (Figure 2). The anchor sleeve is expanded to its
original dimension by inserting the screw to a controlled depth,
so that the sleeve sits snugly against the undercut section of the
hole in the façade panel. This system is identified in general
with the Keil-type technology (Deutsches Institut für
Bautechnik, 2004).
In each case the anchor embedment depth may vary and is
directly related to the anchor’s tensile capacity. The greater the
embedment depth the higher the load bearing capacity,
providing the steel has the required load bearing capacity.
The undercut drilling is performed with a proper drill bit and a
special drilling device in order to obtain the correct shape and
dimension according to the size and type of anchors to be fitted
(Figure 3).
a
One system is illustrated in Figure 1 in which the undercut
anchors have a cone bolt, either with external thread or
internal thread and generally 6 or 8 mm in diameter, an
expansion ring with three or four convolutions, a sleeve and,
optionally, a nut. Cone bolts and expansion rings are made of
a
b
a
c
b
c
b
d
c
e
d
Anchor with external thread
Anchor with internal thread
Figure 1. Undercut anchors with external and internal thread:
(a) expansion ring; (b) sleeve; (c) cone bolt; and (d) nut
Figure 2. System using a crosswise slotted sleeve and an internal
thread with a hexagon bolt: (a) slotted sleeve; (b) hexagon bolt
with internal thread and tooth lock; (c) dimension stone; and
(d) panel bracket
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Volume 166 Issue CM3
Undercut anchorage in
dimension stone cladding
Camposinhos
t
hv
du
t
Z
u
Figure 3. Typical cross-section of a stone slab showing undercut
drilling: wt, diameter of the cylindrical drill hole; wu, diameter of the
undercut; du, anchorage depth; hv, constant diameter hole depth;
z, variable diameter hole depth; t, panel thickness
In general, the undrilled depth (t2du) is equal to or greater
than 0?4t. This may be justified by the fact that the undercut
anchorage resistance is governed by the stone thickness in
tension under negative wind pressure on façades. For positive
pressures, the majority of resultant forces are transmitted
directly to the frame supporting system and/or the façade
backup structure.
2.1
Frame supporting systems
In both systems, the screw or nut is screwed in until exerting
slight pressure on a panel bracket forming a rigid unit with a
backup supporting façade system.
The support system for a dimension stone panel in most cases
consists of a suitable framework in aluminium or stainless
steel. Generally, the framework consists of four brackets
attached to the back of the façade panel by means of an
appropriate undercut anchor. These brackets are then placed
into or onto a corresponding continuous horizontal rail.
Stone types and specimens from the same quarry and batch
were also used to evaluate the force of dowel anchorages and,
thereby, compare the resistance of these two anchorage
systems.
A semi-empirical formulation is proposed based on results
from testing mechanical stone properties and the geometry of
the anchorage.
Finite-element computer analyses of the stress states induced in
the stone panels by the undercut anchorage were also carried
out. These analyses were the basis for calibrating a simple
formula that can be used to estimate the breaking load of the
stone at the undercut anchorage.
3.1
Stone type and specimens
A photo with samples of the six studied rock types is shown in
Figure 4.
A brief lithological description of these stones is a prerequisite
to fully understand the study and its results.
3.1.1 The granites
The study included three different granites: Cinzento de
Alpalhão (C.A.), Pedras Salgadas (P.S.) and Amarelo Real
(A.R.).
(a)
The Cinzento Alpalhão (C.A.) granite is grey with a thin
grain and a very uniform background. Its colour varies
somewhat, from light to dark grey. It is a hard natural
stone containing the following essential minerals:
In most cases the horizontal rails are attached to vertical
mullions which are fixed to the building’s main structure,
structural concrete or masonry.
C.A.
As for the other fixing systems, it must be possible to adjust
undercut anchorage systems both horizontally and vertically.
Relative movement between the panel and the framework must
also be taken into account.
3.
P.S.
A.R
Case study
The main goal of this study is to investigate the relationship
between flexural strength and breaking load at the undercut
anchorage and also to gain a better understanding of the
undercut anchorage’s rupture behaviour. Hence, several tests
were performed to determine the physical and mechanical
properties of the different stone types. Pull-out tests were also
performed to study the strength behaviour of this anchorage
system.
ML.
S.R.
ET.
Figure 4. Prismatic samples after flexural strength test: C.A.,
Cinzento Alpalhão granite; P.S., Pedras Salgadas granite; A.R.,
Amarelo Real granite; M.L., Moleanos Limestone; S.R., Semi Rijo
limestone; E.T., Estremoz marble
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(b)
(c)
plagioclase (35%); quartz (30%), microcline (20%) and
biotite (10%).
The Pedras Salgadas (P.A.) granite is of a light grey
colour with a thin to medium grain and a uniform
background. It is predominantly light grey but also has
some brownish and white coloured areas. It is also a hard
natural stone containing the following essential minerals:
microcline (36%); oligoclase (32%); quartz (25%) and
biotite (6%).
The Amarelo Real (A.R.) granite is of a white-yellow
colour, with a slight brownish tonality, and has a medium
to gross grain and a uniform background. This granite
varies according to its colour uniformity and grain
thickness. It is a medium or medium to coarse-grained
whitish-yellow to brownish-yellow granite, showing some
porphyroid tendency and a somewhat pronounced
weathering and incipient foliation. This granite is also
known as Amarelo Vila Real. Its essential minerals are:
microcline (32%); quartz (27%); plagioclase (26%); and
muscovite (11%).
3.1.2 The limestones
The Moleanos Macio (M.L.) and the Semi Rijo (S.R.) were the
two studied limestones
(a)
(b)
The Moleanos Macio limestone is whitish-grey to light
beige, of an oolitic tendency, calciclastic and bioclastic,
with some dispersed darkish spots.
The Semi Rijo limestone is white coloured, with thin grain
and a very uniform background. It has some small darker
spots throughout its surface and may have some slight
signs of fossils. It is a soft natural stone and its main
variations depend on the amount of darker spots, grain
and signs of fossils.
3.1.3 The Marble
The Estremoz Branco Extra (E.T.) marble is white coloured,
with thin to medium grain and a very discreet bluish coloured
vein. It is a fairly hard natural stone, and its main variations
depend on the vein intensity as well as the type of white
background and structure.
3.2
Physical and mechanical properties
Samples were tested both wet and dry. The wet samples were
soaked in water at 22 ˚C for a minimum of 48 h and a
maximum of 120 h. The dry samples were dried prior to testing
in a humidity-controlled oven at 65 ˚C and gradually cooled to
22 ˚C. The samples’ relevant physical characteristics, determined according to EN 13755 (CEN, 2008) and EN 1936
(CEN, 2007b), are shown in Table 1.
The stones were tested in accordance with EN 1926 (CEN,
2007a) to determine their unconfined compressive strength
Undercut anchorage in
dimension stone cladding
Camposinhos
(UCS). Sixty cylindrical samples were tested in dried conditions. The test results are shown in Table 2.
Flexural strength was determined with three-point load tests.
These tests were carried out on 54 prism samples with a
50 mm 6 30 mm cross-section and on 54 slab samples with a
200 mm 6 30 mm cross-section in accordance with European
Standard EN 12372 (CEN, 2006). Hence, the prism specimens
had a total length of 200 mm and were placed on rollers with a
150 mm gap; the slabs had a total length of 400 mm and were
placed on rollers with a 300 mm gap. The samples were tested
in dried conditions with a gangsawn finish on the lower
surface. The bending strength per stone type and the number of
tests are shown in Table 3.
The pull-out breaking load in undercut tests mobilises mainly
the stone’s tensile strength. The tensile strength is a very
important characteristic which governs the cracking and thus
the rupture.
Tensile strength is formally defined as the tensile stress
required in order to cause a failure of an unconfined cylindrical
or cubical stone specimen, divided by the cross-sectional area
of the specimen perpendicular to the axis of loading. This is the
direct tensile strength; because of the difficulties related to
gripping the specimens, this is a very unusual test.
Otherwise, the tensile strength can be found indirectly, that is
by relying on another type of test. One of these indirect tensile
strength methods is the so-called Brazilian test where a circular
solid disc is compressed until failure across a diameter; tensile
stresses perpendicular to that diameter plane are developed; as
such, compressive loading machines are used in this test. In the
Brazilian test a stone’s indirect tensile strength is generally
defined as:
1.
F
sRt ~{ : :
prt
where F is the applied force at failure; r is the radius of the
specimen (disc); and t is the thickness of the disc.
Yet, it must be said that the above formula for determining the
indirect tensile strength of stone, which has been extensively
applied in rock engineering and research fields for more than
30 years, is erroneous when the disc has a significant thickness
(Yu et al., 2006).
Another simple procedure to obtain the indirect tensile
strength is via flexural strength tests (Weibull, 1939). The
flexural strength of a stone specimen is the maximum tensile
stress when it is about to break. This stress is calculated based
on the formula for linearly elastic bodies. Yet, what matters is
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Rock type
Undercut anchorage in
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Stone identification (Figure 4)
Water absorption: %
(EN 13755)
Volumic mass: kg/m3
(EN 1936)
Open porosity: %
(EN 1936)
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
0?3
0?4
0?7
2?4
8?0
0?1
2640
2610
2610
2540
2190
2710
0?7
0?8
1?8
6?3
19?1
0?3
Granite
Limestone
Marble
Table 1. Water absorption, volumic mass and open porosity of the
studied stones
the tensile stress value instead of the flexural strength. It is
known that the calculated maximum flexural stress is greater
than the actual stress in the test specimen because, during the
testing of a stone prism or slab under flexure, a number of
factors operate to change the stress distribution in the specimen
so as to reduce the maximum stress. It follows that the tensile
strength of a stone in the conditions of a flexure test is higher
than in direct testing under tension (Burshtein, 1967).
The fact that flexural strength is physically greater than axial
tension (according to Davidenkov (1947), and Frenkel and
Kontorova (1943)) since, during flexure, the maximum tensile
stress is experienced only by a filament on the convex surface
of the specimen whereas during axial tension all points of the
cross-section experience the maximum tensile stress.
Based on the statistical theory, Weibull (1939) derived relations
between the strength of a brittle material under flexure, sRf,
and the axial tension, sRt, if data from specimens of different
volumes are known.
Thus, for pure flexure the following relation can be applied:
2.
1
sRt ~ ðsRf1 zsRf2 Þ:ð2mz2Þð{1=mÞ
2
Rock type
Granite
Limestone
Marble
Stone
identification
(Figure 4)
UCS: MPa
(average)
Quantity
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
253
237
83
92
55
97
10
10
10
10
10
10
Table 2. Average unconfined compressive strength of stones
studied as per EN 1926
For simple flexure
3.
h
ið{1=mÞ
1
sRt ~ ðsRf1 zsRf2 Þ:2ð{1=mÞ : ðmz1Þ2
2
where sRf1 and sRf2 are the flexural strengths of specimens
with volumes v1 and v2, respectively.
The value of m is given by the following formula:
4.
m~ln
v2
sRf1
: ln
v1
sRf2
Considering the values from Table 3, the tested stone’s indirect
tensile strength can be estimated by means of Equations 3 and
4. The results are shown in Table 4.
3.3
Undercut anchorage strength tests
Axial tension tests were performed on the slab specimens with a
nominal thickness, t, of 30 mm to evaluate the anchoring strength
with Fischer type anchorages. Two external thread M6 or M8
cone bolts with carbon sleeves (see Figures 1 and 6) were used with
a corresponding nominal diameter drill hole, wt, of 11 and 13 mm,
respectively. The corresponding undercut diameters, wu, are of
13?5 and 15?5 mm, with a tolerance of 0?3 mm for both undercuts.
All anchorage strength tests were performed with a digital pulloff strength tester with a 16 kN capacity (Figure 5). The pulloff tester is fitted with a load cell and a high resolution large
digital display unit, thus being suitable for measurements with
a resolution of 10 N. The direct tensile force is applied by
rotating a hand wheel, through a seat ball which ensures axial
and central load application.
In order to limit tested slabs from bending along the unit’s
three-foot span, they were positioned over a stiff steel plate
with a 120 mm diameter circular hole with its centre aligned
with the vertical axis of the load cell. The 250 mm 6 250 mm
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Undercut anchorage in
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Flexural strength (F.S.), coefficient of variation (c.v.) and number of tests (qty)
Rock type
Granite
Limestone
Marble
Stone
identification
(Figure 4)
Prisms flexural
strength: MPa
c.v.: %
Qty
Slabs flexural
strength: MPa
c.v.: %
Qty
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
21?03
16?82
8?81
15?90
7?40
18?30
4?25
9?74
8?28
8?78
7?00
9?94
9
9
9
9
9
9
15?72
12?85
6?66
11?73
4?97
11?32
6?14
8?12
13?31
7?37
9?10
8?46
9
9
9
9
9
9
Table 3. Flexural strength of tested stones according to EN 12372
square steel plate was 12 mm thick and the 120 mm diameter
centre hole was sufficiently large not to interfere with the pulloff resistance of the undercut anchorages.
lead to a relevant discrepancy in the anchorages’ bearing
capacities.
4.
This procedure limited splitting of the specimens by bending,
even though splitting occurred in a few cases and the
consequent results were obviously rejected (Figure 6).
Results
Fifty pull-out tests with M6 cone bolts and 81 pull-out tests with
M8 cone bolts were performed to determine the pullout load failure
on the six stone types. The typical failure mode was brittle with a
detaching radial cone shape and eventually, spall (Figure 7).
The load was applied at a constant rate of approximately
0?02 kN/s and all specimens were tested after being kept in dry
storage for over 1 week, without any additional wetting or
drying procedures.
The diameter of the cylindrical drill hole, wt, the anchorage
depth, du and the slab thickness were measured before the load
was applied.
Cone bolt anchors of sizes M6 and M8 with external thread
were used. The cone bolt and expansion ring were made of
stainless steel and the sleeve was made of carbon. The anchors
were placed in the undercut drill holes whose typical
dimensions are shown in Table 5 according to Figure 3. It is
worth pointing out that the difference in the geometry of the
drills for M6 and M8 cone bolt threads is very small – a 2 mm
variation for the diameter of the cylindrical drill hole, wt and
for the diameter of the undercut, wu – and probably will not
After a cone type failure, the medium length of the spalls and
their thickness was measured in order to determine the average
angle of the cone failure surface a as illustrated in Figure 8.
The results for the M6 and M8 thread cone bolts are presented
in Tables 6 and 7, respectively. Both tables also indicate the
coefficients of variation (c.v.) of the breaking load and the spall
angles.
Flexural strength (F.S.) and estimated tensile strength (T.S.) (mean values)
Rock type
Granite
Limestone
Marble
Stone
identification
(Figure 4)
Prisms flexural
strength: MPa
Slabs flexural strength:
MPa
m (Equation 3)
Indirect tensile strength: MPa
(Equation 1)
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
21?033
16?824
8?810
15?900
7?396
18?300
15?720
12?850
6?662
11?730
4?967
11?320
6?946
8?495
7?037
6?946
5?290
4?311
9?16
8?05
3?88
6?88
2?71
5?81
Table 4. Flexural and indirect tensile strength of tested stone
according to Equations 2 and 4
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Figure 6. Splitting failure in a limestone slab and undercut
anchorage cone bolt after split failure
Substituting the value of the average spall angle, am, in
Equation 5, the minimum edge distance, em, for anchorage
depths of 15 mm will be given by:
.
Figure 5. Digital pull-off strength tester and stiff steel plate to
deter bending of the specimens
For the M8 cone bolts, since it was not possible to obtain
samples of Estremoz marble from the same quarry and batch,
there is no available data.
which is in good agreement with the value recommend in the
ETA document (Deutsches Institut für Bautechnik, 2009).
With this minimum space between anchors, sm, may be
derived:
6.
A preliminary observation to the results reveals that the
breaking load does not vary with the thread size for the same
stone type, as was expected.
For each stone type, a global appreciation of the breaking load
values and the respective mean value is shown in the graph of
Figure 9. The gross horizontal lines indicate the average of the
breaking load values shown in Tables 6 and 7.
It must be noted that the spall angles are very similar in all the
tested specimens, even for the six stone types. The observed
mean value for all stone types is of 18?1 ˚ with a coefficient of
variation of 9?84%. These values are slightly inferior to the 20 ˚
value reported by Lammert and Hoigard (2007).
The characteristic spall angle value (5% lower percentile),
assuming a normal distribution, will be given by:
5.
ak ~am :ð1{1:64|9:84%Þ&0:839am
em ~15|cotð0:839|180 Þ&55 mm
sm ~2hv :cotð0:839am Þ
A suitable substitution in Equation 6 makes sm equal to 7?4hv,
which is practically the same as the recommended value in the
Fischer ETA document, 8du (Deutsches Institut für (Bautechnik, 2009).
4.1
Breaking load in the dowel hole comparison
For the same stone types and batch, 10 samples of each type
were used in tests designed to determine the breaking load at
the dowel hole in terms of EN 13364 (CEN, 2002). The
samples, measuring 200 mm 6 200 mm, were prepared from
slabs with a nominal thickness of 30 mm. The holes were
located 100 mm from either side, measured to the nearest
0?5 mm. The thickness of stone between the edge of the hole
and the two sides was 12 mm, measured to the nearest 0?5 mm.
The holes were 8 mm in diameter and 35 mm deep. The load
was exerted in a direction perpendicular to the axis of the
dowel at a maximum distance of 2 mm from the edge of the
sample and using the system shown in Figure 10.
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External thread gauge
M6
M8
Undercut anchorage in
dimension stone cladding
Camposinhos
wt: mm
wu: mm
du: mm
z: mm
11
13
13?5
15?5
15
15
4
4
Table 5. Undercut drill geometry for M6 and M8 diameter thread
applied to tested anchorages
The dowel hole failure mode is characterised by a brittle
detachment of a wedge. A sample, after being tested, is
illustrated in Figure 11.
found that the average anchorage capacity of undercut anchors
was three times greater than that of the dowel hole.
4.2
Semi-empirical formulation
The mean breaking load values at the dowel load are compared
with the mean breaking load values with undercut anchorages
for the six stone types. The results are shown in Figure 12.
In this section, the undercut geometry and the pull-out test
results were used to develop a formulation of the maximum
tensile stress installed in the stone’s anchorage zone.
The comparison is quite clear and, as expected, the anchorage
capacity with undercut holes is much superior to the dowel
hole at the slab’s edges. This fact has been already referred to
by other authors (Camposinhos, 2009; Camposinhos and
Camposinhos, 2009; Lammert and Hoigard, 2007; Stein,
2000). In the present case, the difference in percentage varied
from 245% for C.A. granite to 78% for S.R. limestone. This
difference increased with the stone’s tensile strength as revealed
when compared with the breaking load values with the tensile
strength values in Table 4. For the six studied types, it was
Hence, the spalls created during the undercut cone bolt anchor
tests were traced, digitised and the projected spall area
calculated.
By projecting the failure surface in a plane perpendicular to the
cone axis and assuming a uniform distribution of the tensile
strength over an equivalent circular idealised area according to
Figure 13, it is possible to establish a relation based on the
maximum principal stress theory (Rankine, Lamé) which is
satisfactorily applicable to brittle or quasi-brittle materials,
such as stone. The theory is based on limiting normal stress.
Failure occurs when the normal stress reaches a specified upper
limit. Failure is predicted when the principal stresses equal the
ultimate strength of the material.
The presence of cuts, grooves, holes, etc., modify stress
distributions, which are obtained through elementary stress
design formulas and are based on the members having a
constant section or a section with a gradual contour change, so
that localised high stresses occur and are measured by a stress
concentration factor (Albrecht and Yamada, 1977; Pilkey and
Pilkey, 2007). In this case, a stress concentration factor must be
considered for the given geometry of the undercut drill hole.
This factor, Ku, is defined by the ratio between the actual
maximum stress, smax, and the medium stress, stm according to
Figure 14, Ku is given by Equation 7 as follows:
t
du
Figure 7. Typical cone mode failure in two tested specimens
t
Figure 8. Cone mode failure and spall angle a
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Undercut anchorage in
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Camposinhos
Breaking load
Stone
identification
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
Spall angle
Number
of tests
F: kN
c.v.: %
a: ˚
c.v.: %
t: mm
wt: mm
du: mm
5
5
7
8
5
20
10?26
7?71
3?86
5?64
2?34
4?92
2?80
4?83
8?92
22?24
3?70
8?02
17?79
19?94
15?44
18?62
19?12
15?14
12?4
15?0
9?6
19?7
14?0
13?4
31?8
30?9
32?9
29?7
28?5
30?7
10?9
10?9
10?9
10?9
10?9
10?8
15?2
15?2
15?3
15?3
15?3
15?3
Table 6. Number of tests for each stone type, breaking load and
mean spall angle values and coefficient of variation with M6 thread
cone bolt anchors
7.
Ku ~
smax
stm
10.
In Figure 13, the area of the projected cone failure surface, Acf,
is represented and may be given by:
8.
h
i
Acf ^p ðhv : cot azðwu =2ÞÞ2 {ðwu =2Þ2
~p h2 : cot2 azhv :wu : cot a
Ku ~
st : 2 : 2
p hv cot azhv :wu :cota
Fu
The chart in Figure 15 shows, for each stone type, the
concentration factor value obtained from Equation 10 with the
average values for Fu, a and hv taken from Table 6 and the
diameter of the undercut wu from Table 5. The tensile strength
values from Table 4 were substituted in Equation 10, respectively.
v
The breaking load Fu value may then be expressed as follows:
9.
Fu ~
st :
Acf
Ku
where hv is the maximum spall thickness equal to (du2z), see
(Figures 3 and 13); st is the tensile strength of the stone; Acf is
the area of the projected cone failure surface; and Ku is the
stress concentration factor for the undercut.
By substituting Equation 8 into Equation 9 and expressing the
result for Ku, we obtain:
Table 8 reveals that the same stone type showed no relevant
differences in the concentration factor values, which leads to
the conclusion that the thread size of the cone bolt anchors and
the dimensions of the drilled hole do not affect the said values.
The medium to gross grain granite (A.R.) shows a higher stress
concentration factor and a smaller spall angle when compared
with the other granites, namely the C.A. and P.S. granites.
Similarly, but obviously for other reasons, the Estremoz
marble, E.T., which has a large degree of recrystallisation
has a smaller spall angle and a higher concentration factor in
comparison with the noncrystalline stones such as M.L. and
S.R. limestone.
Breaking load
Stone
identification
C.A.
P.S.
A.R.
M.L.
S.R.
Spall angle
Number
of tests
F: kN
c.v.: %
a: ˚
c.v.: %
t: mm
wt: mm
du: mm
12
25
25
9
10
10?53
9?14
4?42
5?41
2?45
7?22
12?63
10?17
13?85
18?69
18?76
19?23
15?92
19?22
19?93
22?5
16?8
10?8
21?7
9?7
31?7
31?0
32?9
29?3
28?5
13?0
13?0
13?1
12?9
13?0
13?0
13?0
13?1
12?9
13?0
Table 7. Number of tests for each stone type, breaking load and
medium spall angle values and coefficient of variation with M8
thread cone bolt anchors
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Volume 166 Issue CM3
Undercut anchorage in
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Camposinhos
12.00
11.00
(C.A. 10.45 kN)
10.00
9.00
(P.S. 8.90 kN)
8.00
kN
7.00
6.00
(M.L. 5.52 kN)
(E.T. 4.92 kN)
5.00
(A.R. 4.30 kN)
4.00
3.00
(S.R. 2.41 kN)
2.00
1.00
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
0.00
Figure 9. Mean anchorage breaking load values per stone type
with Fischerß cone bolt anchors
4.3
Finite-element stress calculation method
A finite-element stress analysis was carried out to investigate
stress distribution near the undercut and along the observed
spall surface. The material properties used in the model were
assumed to be linear-elastic, isotropic and homogeneous in
behaviour, even though dimension stone, as a naturally
occurring material, is often heterogeneous and anisotropic.
However, the model was used to verify the induced stress state,
namely the maximum principal stress for the observed pull-out
loads.
A three-dimensional computer model was generated using
solid elements to investigate the stress distribution present in
Figure 10. Testing rig and arrangement for breaking load at the
dowel hole
Figure 11. Specimen edge after the test according to EN 13364
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Undercut anchorage in
dimension stone cladding
Camposinhos
12.00
10.00
kN
8.00
6.00
4.00
2.00
0.00
Undercut anchorage
dowell hole
C.A.
P.S.
10.45
3.03
8.90
2.67
A.R.
4.30
M.L.
5.52
1.36
1.76
S.R.
E.T.
2.41
1.36
1.98
4.92
Figure 12. Breaking load values comparison – undercut cone bolt
anchorage and at dowel hole
the typical undercut anchorage configuration load tested by
the author, as described above.
Fu
hv
t
hv cot
u
For this analysis, the eight-noded hexahedron element type
was chosen. Although not relevant for this study, different
values of the modulus of elasticity ranging from 40 000 to
60 000 MPa were used for each type of rock studied. A
constant value of 0?3 for the Poisson ratio was considered
adequate for all rock types.
max
tm
Acf
Figure 13. Spall configuration and detachment angle in slab
Figure 14. Stress concentration factor as the relation between the
actual maximum stress, smax and the medium stress stm
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Undercut anchorage in
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Camposinhos
10.00
9.00
8.00
7.00
Ku
6.00
5.00
4.00
3.00
2.00
1.00
0.00
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
6 mm
4.92
4.69
7.16
6.75
5.62
8.96
8 mm
4.82
4.44
6.32
6.96
5.27
Figure 15. Stress concentration factor, Ku, for the six stone types
studied with M6 and M8 cone bolt undercut anchorages
For simplicity, the load was applied directly to the solid element
nodes at the nodes in contact with the expansion ring of the cone
bolt thread assuming full contact along the stone surface.
In the finite-element model (FEM), the advantages of the
symmetry are put to use. The computational model is taken as
a volumetric structure modelled using isoparametric volumetric finite elements, of the eight-node brick type (Figure 16).
Rigid supports were defined at all nodes according to the test
setup. At the nodes belonging to the symmetry face, the
degrees of freedom were blocked accordingly.
Stone identification
Fine to medium grain size granite
Fine to medium grain size granite
Medium to gross grain size granite
Limestone
Limestone
Marble
Concentration
factor
Spall angle a: ˚
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
M6 cone bolts
M8 cone bolts
Mean
Ku
17?79
19?94
15?44
18?62
19?12
15?14
18?76
19?23
15?92
19?22
19?93
–
18?28
19?59
15?68
18?92
19?53
15?14
4?87
4?56
6?74
6?85
5?45
8?96
Table 8. Spall angles and stress concentration factors, mean values
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4 mm
30 mm
11 mm
Construction Materials
Volume 166 Issue CM3
mm
7. 3
60
Y
mm
Z
X
Figure 16. Finite-element mesh for a quarter-sample of the studied
slab area
Stress contour maps
Fu = 10 454 N
Figure 17. Three-dimensional stress maps for the C.A. granite
breaking load equal to 10?45 kN and FEM calculated maximum
tensile stress equal to 10?20 MPa
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Undercut anchorage in
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Camposinhos
Nodal stresses were averaged from the stresses evaluated at the
standard 2 6 2 6 2 Gauss integration points.
is desirable to compare the values obtained through both
methods, such that the stress value found in this manner may
be compared with the semi-empirical formulation derived from
Equation 10 as follows:
Figures 16 and 17 show, respectively, a three-dimensional view of
the geometry and a stress map, Figure 18 shows a two-dimensional
section cut according to the calculated stone’s maximum principal
tensile stresses. Stress concentrations are present in the vicinity of
the hole and dissipate quickly, suggesting that anchorage failures
are influenced by a non-uniform stress distribution over the failure
surface. The direction of the maximum principal stresses located
adjacent to the hole are approximately perpendicular to the failure
surface observed in tests, meaning that failure initiates at this
location, as was expected.
One run for each breaking load value was performed with the
corresponding value for the six different stone types as
reported in Figure 9.
5.
Discussion
The universal availability of powerful, effective computational
capabilities, usually based on the FEM, has altered the need
for and the use of stress concentration factors. Nevertheless, it
11.
st ~
:
p
Fu Ku
h2v :cot2 azhv :wu :cota
A comparison between the maximum calculated tensile stress
using the FEM method and the stone’s indirect tensile strength
obtained via flexural tests is shown in Table 9. The stress
values for both cases are also plotted in Figure 19.
It must be emphasised that the difference in the stress values
were 12?6% superior for granites and 12?0% inferior for the
limestone and marble stone types. These stress value differences may be considered acceptable, considering the variations
in the breaking load test results (Tables 6 and 7) and the
stone’s flexural strength or its indirect tensile strength
(Table 4). Nevertheless, note the unavoidable shortcomings
of the finite-element modelling, in particular the geometry
discretisation and material constitutive law.
Fu = 4924 N
Max stress contours
Radial section cut
Figure 18. Stress maps, two-dimensional view of a radial section
cut of the drilled region for the E.T. marble’s breaking load equal to
4?92 kN and FEM calculated maximum tensile stress equal to
5?04 MPa
171
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Rock type
Granite
Limestone
Marble
Undercut anchorage in
dimension stone cladding
Camposinhos
Stone identification
Average breaking load values
(Figure 9): kN
Indirect tensile strength
(Table 4): MPa
FEM stress values: MPa
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
10?45
8?90
4?30
5?52
2?41
4?92
9?16
8?05
3?88
6?88
2?71
5?81
10?20
9?10
4?40
5?64
2?58
5?04
Table 9. Breaking loads, tensile strength and stress values from the
FEM calculation of tested stone
Finite-element method
Tensile strength
Semi-empirical (Equation 11)
Cinzento Alpalhão (C.A.)
10.000
8.000
Estremoz (E.T.)
6.000
Pedras Salgadas (P.S.)
4.000
2.000
0.000
Amarelo Real (A.R.)
Semi Rijo (S.R.)
Moleanos (M.L.)
Figure 19. Calculated stress with the FEM method and Equation
11 compared with tensile strength for the studied stone types
(values in MPa)
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Volume 166 Issue CM3
Rock type
Undercut anchorage in
dimension stone cladding
Camposinhos
Stone identification
Indirect tensile strength
(Table 4): MPa
Finite-element method
stress calculated values: MPa
Stress calculated values
Equation 11: MPa
C.A.
P.S.
A.R.
M.L.
S.R.
E.T.
9?16
8?05
3?88
6?88
2?71
5?81
10?20
9?10
4?40
5?64
2?58
5?04
9?72
8?80
4?18
7?70
2?83
5?97
Granite
Limestone
Marble
Table 10. Comparison between maximum stress from the FEM and
Equation 11 with indirect tensile strength
For the geometry of the undercut drill hole, hv, was regarded as
equal to 11?3 mm and an average value of 14?5 mm was
applied for wu.
Using the FEM with linear-elastic material properties, together
with the maximum principal stress failure criteria, has proven to be
an appropriate design procedure for estimating the breaking load.
To make use of Equation 11, the medium spall angles and
stress concentration factors were taken from Table 8.
Observation of the test results allows for some further
conclusions.
Table 10 shows the comparison between stresses calculated (i)
using the FEM (ii), Equation 11 and (iii) the indirect tensile
strength.
(a)
As for the semi-empirical approach in Equation 11, the
calculated values appear to be conservative. On average they
are 7?8% superior for the granites and 6?4% superior for the
limestone and marble stone types, when compared with the
indirect tensile strength.
(b)
(c)
(d)
(e)
A plot of the three groups of stress values from Table 10 and
per stone type is shown in Figure 19.
6.
Conclusion
This paper examined the relationships between material
strength, anchorage strength and induced stress states for the
undercut anchorage. The findings are based on a significant
number of tests performed on six stone types, three granites,
two limestones and one marble.
The breaking load does not vary with the thread size for
the same stone type.
Anchorage embedment depth is directly related to the
anchor’s tensile capacity.
Based on the semi-empirical formulation for the same
tensile strength, it can be shown that the greater the
embedment depth the higher the load bearing capacity.
Spall angle measurements made it possible to define a
minimum space between anchors and distance to edges.
For the studied specimens, it was found that the medium
anchorage capacity of the undercut anchors is three times
greater than that of the dowel anchorage type.
Acknowledgements
The author wishes to thank Dr Roland Unterweger for his
support and the back-up provided by the Fischerwerke GmbH
& Co. KG in supplying the hardware and the specimen
undercutting drills.
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