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8/13/2019 Cracking in Clay
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Cracking in clay data report on
cracking of clay beams by 4-point
beam tests
N.I. Thusyanthan1, S.P.G. Madabhushi2,
A.W. Take3& M. D. Bolton4
CUED/D-SOILS/TR340 (2005)
1Research Fellow, Churchill college, University of Cambridge2Senior Lecturer, Engineering Department, University of Cambridge
3
Assistant Professor , Department of Civil Engineering Queen's University Kingston, CANADA4Professor of Soil Mechanics, Engineering Department, University of Cambridge
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
__________________________________________________________________________
CUED/D-SOILS/TR340 1
CONTENTS........................................................................................................................................................PG
1 INTRODUCTION........................................................ .............................................................. ................. 2
2 EXPERIMENTAL SETUP................................... ................................................................ ...................... 3
2.1.1 Specimen preparation ........................................................... .......................................................... 3
2.1.2 Installation of PPTTs into the clay beams..................................................... .................................. 4
3 TESTING PROCEDURE...................................................... .............................................................. ....... 5
3.1.1 PIV analysis ....................................................... ............................................................ ................. 9
4 RESULTS.................. ................................................................ ........................................................... ...... 11
4.1.1 Beam AL15.......................................................... ............................................................ .............. 12
4.1.2 AL45 ......................................................... ................................................................ ..................... 134.1.3 AL75 ......................................................... ................................................................ ..................... 14
4.1.4 AS45 ...................................................... ............................................................ ............................ 15
4.1.5 AS80 ...................................................... ............................................................ ............................ 16
4.1.6 AS62 ...................................................... ............................................................ ............................ 17
4.1.7 AS75 ...................................................... ............................................................ ............................ 18
4.1.8 AS80 ...................................................... ............................................................ ............................ 19
4.1.9 AS102 ................................................................ ............................................................. ............... 20
4.1.10 AS100 ........................................................... ............................................................... ............. 21
4.1.11 AS25 ........................................................... ........................................................... ................... 22
4.1.12 BS22 ........................................................... ........................................................... ................... 23
4.1.13 BS46 ........................................................... ........................................................... ................... 24
4.1.14 BS92 ........................................................... ........................................................... ................... 25
4.1.15 BS65 ........................................................... ........................................................... ................... 26
4.1.16 BS45 ........................................................... ........................................................... ................... 27
4.1.17 BS15 ........................................................... ........................................................... ................... 28
5 BEAM PICTURE AT THE START OF THE TEST AND AT THE INITIATION OF CRACK ..... 29
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CUED/D-SOILS/TR340 2
1 IntroductionLiner systems of a landfill perform the vital task of retaining the leachate produced by the
waste. A clay liner, with its characteristic very low permeability, has been the common form
of liner since the early days of landfill construction. Even though newer landfills have well
engineered composite liner systems with Geo-synthetic clay (GSC) liners, clay liners are still
commonly used in many countries of the world.
The low permeability of clay is the main property that makes it ideal for landfill liner
construction. The presence of cracks in clay impairs the main function of a clay liner.
Cracking in clay can be caused by many factors such as freezing and thawing, desiccation,
shrinkage and differential settlement (Fig. 1). The mass strength of the clay in liners,foundations, embankments and slopes can be adversely affected by cracks in the clay. Cracks
provide a preferential flow path to fluids, thus increasing the hydraulic conductivity many
fold. Understanding the criteria for tensile crack initiation would enable us to better design
and manage clay foundations, embankments, slopes, dams and liners.
Fig. 1 Clay liner cracking (Environment Agency, R&D Technical Report P1-385/TR1Source).
Differential settlement of the landfill foundation can induce tension cracks in the clay liner.
Fig. 1 shows such tension cracks in the clay liner in a schematic cross section of a landfill.
These tension cracks can be difficult to observe in a landfill as they are below the waste fills
and could cause leachate leakage and hence ground water pollution. Understanding the
cracking phenomenon in clay is essential not only for landfill liners but also for other
common facilities such as embankments and dams whose performs depend on the strength
and permeability of clay.
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
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CUED/D-SOILS/TR340 3
This chapter presents an investigation into the stress-strain criteria for cracking in clays by
performing 4-point bending tests on consolidated kaolin clay beams (Thusyanthan et al.
2005e). The clay beams were obtained from specimens of kaolin clay one dimensionally
normally consolidated to a stress of 500 kPa or 250 kPa. Load controlled and strain controlled
tests were performed on clay beams with varying initial suction to understand the stress-strain
criteria for crack initiation in clay. Tensile strain to cracking was measured by performing
PIV analysis (White et al. 2003) on the digital images of the beams being subjected to
bending, while the suction was measured by pore pressure and tension transducers (PPTTs)
installed at three different locations within the beams.
Clay beams could have been formed from compacted clay; however the variability present in
the compacted clay would make comparing the results of different beams difficult.
Furthermore, compacted clay beams would invariably have some weak layering which may
vary from beam to beam; hence the failure stress may be unique to each beam.
2 Experimental setup2.1.1 Specimen preparation
Load controlled and strain controlled 4-point bending tests were carried out on beams
trimmed from E-grade kaolin clay which had been one-dimensionally consolidated either to
500 kPa (type-A beams) or to 250 kPa (type-B beams).
E-grade kaolin clay powder was thoroughly mixed with an equal mass of water under vacuum
to produce a slurry. The kaolin slurry at 100% water content was then one-dimensionally
consolidated to an effective stress of 500 kPa or 250 kPa in a consolidation rig (Fig. 2(a)).
Beams 320 mm long (transverse to the consolidation loading) and of 80 mm cross-section,
weighing 4 kg, were cut from the consolidated clay specimens (Fig. 2(b)). All beams were
wrapped in polythene and stored in air-tight containers prior to testing. The E-grade kaolin
clay has a liquid limit of 51% a plastic limit of 30% and permeability of the order of 10 -9m/s
(Barker, 1998). The values of critical state parameters of E-grade kaolin clay from various
sources were summarised in section 3.5.2 in chapter 3- Thusyanthan 2005, Ph.D Thesis,
University of Cambridge.
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CUED/D-SOILS/TR340 4
(a) (b)
Fig. 2 Kaolin clay : (a) Consolidated clay specimen; (b) 320 mm 80 mm 80 mm clay beam.
2.1.2 Installation of PPTTs into the clay beamsPrior to testing a beam, it was removed from the air-tight container and three PPTTs (one near
the compression face, one near the tension face and the other in the middle of the beam) were
installed at the mid-length of the beam by slowly drilling from one end of the beam. The
PPTTs were saturated under vacuum prior to installation. The details of the saturation process
are described in Take and Bolton (2003). Fig. 3(a) shows the location of PPTTs in the clay
beam. A wooden framework and an aluminium guide were used to ensure that the drilling
alignment and depth were correct (Fig. 3(b)) with the beam protected against evaporation by a
polythene cover. The PPTTs were installed on a diagonal of the cross section of the beam in
an attempt to mitigate their tendency to weaken the cross-section. The PPTTs were inserted
into the drilled holes, back filled with clay slurry and allowed to set (Fig. 3(c)). After the
installation of PPTTs, the pore pressure was monitored to ensure that it was uniform before
the polythene cover was removed. The elevation face of the beam which would face the
digital camera was dusted with dyed fine sand. This gives the surface some texture which is
required for good PIV analysis of the beam images.
K0'v
K0'v
'v
320 mm80 mm
80 mm
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CUED/D-SOILS/TR340 5
20mm
20mm
40mm
160 mm
320 mm
80 mm
30 mm
80 mm
240 mm
80d
80
20 mm
b
(a)
(b) (c)
Fig. 3 Preparation of clay beams: (a) PPT location; (b) Drilling into clay beam; (c) PPTs installed and
allowed to set.
3 Testing procedureAll the beams initially registered suction in the range 15 kPa to 30 kPa after the equilibration
of PPTTs. This suction increased slowly as the beams were allowed to air dry for different
periods to obtain various values of initial suction. An air fan was used to speed up the drying
process for beams requiring high suction for testing. Beams were rotated at regular intervals
to facilitate uniform drying from all sides. This was confirmed by the uniform readings of the
PPTTs. Fig. 4 shows the PPTT readings during installation, setting of back filled clay and
drying. The spikes in the PPTT readings during installation were caused when the PPTT
reached the end of the drilled hole and got pressed again the clay while the spikes during
setting and drying was caused when rotating the beam. Load-controlled and strain-controlled
bending tests were performed on the beams with various initial suctions. 30 mm diameter
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CUED/D-SOILS/TR340 7
Load-controlled tests were carried out on 3 beams of type-A using the set up shown in Fig.
5(a). A step load of 20 N was applied to the beam at intervals of 180s by allowing 2 kg of
water to flow into the bucket attached to the framework. Fig. 5(b) shows the set-up used in
strain-controlled tests. A motorised actuator was used to apply the load on the beam at a
uniform displacement rate of 0.23 mm/min. Pore pressure readings from all 3 PPTTs were
recorded throughout the tests.
Two digital cameras were mounted facing the beams, one to capture the central region of the
beam and the other to capture the entire beam, as the beam was subjected to bending. The
digital images were captured every 10 s during the test. These images were used in particle
image velocimetry (PIV) analysis (White et al. 2003) to obtain the displacement vectors in the
beam. A thin glass sheet, with a grid of black markers at known locations, was positioned
very close to the beam. These markers acted as control targets to normalise the PIV analysis.
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CUED/D-SOILS/TR340 8
80mm
Base Plate
320 mm
Clay Beam
30
mm
240 mm
40 mm
80 mm
Load Cell
Water container
(a)
Fig. 5 (a) Setup for load controlled test; (b) setup for stain controlled test.
Digital
camera 1
glass sheet
80 mm
Motorised
actuator
Load cell
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CUED/D-SOILS/TR340 9
3.1.1 PIV analysisThe experimental investigation of cracking described in this paper concentrates on the stress-
strain behaviour of the mid-span of the beam where the bending moment was uniform at its
maximum value. The evolution of the magnitude and distribution of the longitudinal bendingstrain, zz, at this location was precisely measured using the non-contact digital image
correlation technique of Particle Image Velocimetry (PIV). This technique is described by
White et al. (2003) and Take (2003) and allows the precise determination of soil
displacements though a series of digital images without resorting to predefined target markers,
instead operating on the visual image texture of the soil (colour, grain orientation, etc.) In this
application, the grain size of the soil, E-grade Kaolin, ensured that the natural texture of the
material could only be seen at the microscopic level. Thus, using the technique described byTake (2003), an artificial texture was applied to the elevation face of the beam using with
dyed fine sand. As shown in Fig. 6(a), the resulting image texture is a high contrast black and
white random pattern ideal for PIV analysis.
As PIV operates on image texture rather than pre-defined target markers, the displacement of
any location throughout the beam could be measured. In this application, 33 pairs of 32x32
pixel measurement patches were defined in the digital image on either side of the mid-span ofthe beam throughout the full height (Fig. 6(a)). Thus, these pairs of displacement nodes can be
thought of as thirty-three virtual strain gauges and can be used to calculate the longitudinal
strains throughout the depth of the beam by dividing the horizontal movement of the two
patches making up each pair by the original distance between the patches (Fig. 6(b)).
Digital images of the beams were captured every 10s during flexural testing by two 4
Megapixel digital cameras: one focussed on a wide field of view to observe the behaviour of
the entire beam (Fig. 7)and the other zoomed to capture the detailed behaviour of the mid-
span (Fig. 6(a)). As shown in Fig. 6(a), a thin glass sheet containing a grid of black control
makers at known locations was placed in front of the beam to provide a reference coordinate
system visible in both cameras. This coordinate system was then used to improve the
precision of the measured strains using photogrammetric camera calibration to remove camera
errors such as the variation in scale factor due to imperfect camera positioning, radial and
tangential lens distortion, and refraction (White et al., 2003).
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CUED/D-SOILS/TR340 10
200 400 600 800 1000 1200 1400 1600 1800 2000 2200
200
400
600
800
1000
1200
1400
Pixels
Pixels
(a)
(b)
Fig. 6 (a) View from camera 1 and 32 32 pixel size patches used in PIV analysis; (b) strain calculation
from the patch movement
Fig. 7 Images from camera 2
Zo
Z1 Z2
Strain = (Z1+Z2)/(Zo)
Patch in image 1
Patch in image 2
z
y
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CUED/D-SOILS/TR340 11
4 ResultsAll the beams failed by tension cracking near the mid-span of the beam. The load and hence
the bending moment experienced by the beams increased up to the onset of cracking. After
the initiation of a tension crack the load decreased and the crack grew through the beams.
Complete collapse of the beams was observed once the crack had propagated through about
two thirds of the beam thickness.
References
1. Take, W. A. & Bolton, M. D. (2003). Tensiometer saturation and reliablemeasurement of soil suction, Gotechnique 53, No. 2, 159-172.
2. White D.J., Take W.A. & Bolton M.D. (2003). Soil deformation measurementusing particle image velocimetry (PIV) and photogrammetry. Gotechnique 53, No.
7, pp. 619-631.
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CUED/D-SOILS/TR340 12
4.1.1 Beam AL15
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
100
200
300
400
500
600
700
800
900
Strain (%)
Time(s)
Tension face
Compression face
300 400 500 600 700 800
-2
-1
0
1
2
3
4
Time(s)
Strain(%)
Bendingmoment(N/m)
100 200 300 400 500 600 700 800
-0.1
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
Time(s)
Curvature(1/m)
0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.81
1.5
2
2.5
3
3.5
4
Curvature(1/m)
Bendingmoment(N/m)
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CUED/D-SOILS/TR340 13
4.1.2 AL45
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
1400
1600
1800
Strain (%)
Time(s)
Tension faceCompression face
400 600 800 1000 1200 1400 1600
-2
0
2
4
6
8
Time(s)
Strain(%)
Bendingmoment(N/m)
200 400 600 800 1000 1200 1400 1600
-0.1
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
Time(s)
Curvature(1/m)
0 0.1 0.2 0.3 0.4 0.5 0.6
2
3
4
5
6
7
Curvature(1/m)
Bendingmoment(N/m)
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4.1.3 AL75
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
1400
1600
1800
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000 1200 1400 1600
-2
-1
0
1
2
3
4
5
6
7
Time(s)
Strain(%)
Bendingmoment(N/m)
0 0.1 0.2 0.3 0.4 0.5
2
3
4
5
6
7
8
Curvature(1/m)
Bendingmoment(N/m)
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CUED/D-SOILS/TR340 15
4.1.4 AS45Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
Strain (%)
Time(s)
Tension face
Compression face
0 200 400 600 800 1000 1200-4
-2
0
2
4
6
8
Time(s)
S
train(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 1
0
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
Curvature(1/m)
E(MPa)
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CUED/D-SOILS/TR340 17
4.1.6 AS62Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000 1200-6
-4
-2
0
2
4
6
8
10
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 1-5
0
5
10
15
20
25
Curvature(1/m)
E(MPa)
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4.1.7 AS75Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000-2
0
2
4
6
8
10
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
910
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
5
10
15
20
25
30
Curvature(1/m)
E(MPa)
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CUED/D-SOILS/TR340 19
4.1.8 AS80Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
1400
1600
Strain (%)
Time(s)
Tension face
Compression face
400 600 800 1000 1200 1400 1600
-4
-2
0
2
4
6
8
10
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 1
0
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
E(MPa)
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4.1.9 AS102Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
1200
1400
Strain (%)
Time(s)
Tension faceCompression face
400 600 800 1000 1200 1400-2
0
2
4
6
8
10
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
2
4
6
8
10
12
14
16
Curvature(1/m)
E(MPa)
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4.1.10AS100Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
Strain (%)
Time(s)
Tension face
Compression face
100 200 300 400 500 600 700 800 900-2
0
2
4
6
8
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
2
4
6
8
10
12
14
16
18
Curvature(1/m)
E(MPa)
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4.1.11AS25Every 50 s
-4 -3 -2 -1 0 1 2 3 4
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-4 -3 -2 -1 0 1 2 3 40
200
400
600
800
1000
1200
1400
Strain (%)
Time(s)
Tension face
Compression face
0 200 400 600 800 1000 1200 1400-4
-3
-2
-1
0
1
2
3
4
5
6
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 1-2
0
2
4
6
8
10
12
Curvature(1/m)
E(MPa)
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4.1.12BS22Every 50 s
-4 -2 0 2
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-5 -4 -3 -2 -1 0 1 2 3 4 50
200
400
600
800
1000
1200
1400
1600
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000 1200 1400 1600-6
-4
-2
0
2
4
Time(s)
S
train(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(N/m)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
Curvature(1/m)
E(MPa)
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4.1.13BS46Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000-3
-2
-1
0
1
2
3
4
Time(s)
Strain(%)
Bendingmoment(Nm)
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
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CUED/D-SOILS/TR340 25
4.1.14BS92Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
-3 -2 -1 0 1 2 30
200
400
600
800
1000
Strain (%)
Time(s)
Tension faceCompression face
200 400 600 800 1000-4
-2
0
2
4
6
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(N/m)
0 0.2 0.4 0.6 0.8 10
2
4
6
8
10
12
Curvature(1/m)
E(MPa)
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4.1.15BS65Every 50 s
-3 -2 -1 0 1 2 3
20
30
40
50
60
70
80
90
100
Strain (%)
mm
PIVbeam15cam1
00001
beam15cam1
00002.txt
200 400 600 800 1000 1200 1400 1600 1800 2000 2200
200
400
600
800
1000
1200
1400
1600
-3 -2 -1 0 1 2 30
200
400
600
800
1000
Strain (%)
Time(s)
Tension faceCompression face
0 200 400 600 800 1000-3
-2
-1
0
1
2
3
4
5
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmoment(N/m)
0 0.2 0.4 0.6 0.8 10
5
10
15
20
Curvature(1/m)
E(MPa)
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
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4.1.16BS45Every 50 s
-5 -4 -3 -2 -1 0 1 2 3 4 5
20
30
40
50
60
70
80
90
100
Strain (%)
mm
PIVbeam16cam1
00001
beam16cam1
00002.txt
200 400 600 800 1000 1200 1400 1600 1800 2000 2200
200
400
600
800
1000
1200
1400
1600
-5 -4 -3 -2 -1 0 1 2 3 4 50
100
200
300
400
500
600
Strain (%)
Time(s)
Tension faceCompression face
0 100 200 300 400 500 600-6
-4
-2
0
2
4
6
Time(s)
Strain
(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Ben
dingmoment(N/m)
0 0.2 0.4 0.6 0.8 1-1
0
1
2
3
4
5
Curvature(1/m)
E(MPa)
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4.1.17BS15Every 50 s
-5 -4 -3 -2 -1 0 1 2 3 4 5
20
30
40
50
60
70
80
90
100
Strain (%)
mm
PIVbeam17cam1
00001
beam17cam1
00002.txt
200 400 600 800 1000 1200 1400 1600 1800 2000 2200
200
400
600
800
1000
1200
1400
1600
-5 -4 -3 -2 -1 0 1 2 3 4 50
500
1000
1500
2000
Strain (%)
Time(s)
Tension faceCompression face
0 500 1000 1500 2000-5
-4
-3
-2
-1
0
1
2
3
Time(s)
Strain(%)
Bendingmoment(Nm)
0 0.2 0.4 0.6 0.8 10
1
2
3
4
5
6
7
8
9
10
Curvature(1/m)
Bendingmo
ment(N/m)
0 0.2 0.4 0.6 0.8 10
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
Curvature(1/m)
E(MP
a)
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29
5 Beam picture at the start of the test and at the initiation of crackAL15
At the start of the test At initiation of crack
AL45
At the start of the test At initiation of crack
AL75
At the start of the test At initiation of crack
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AS45
At the start of the test At initiation of crack
AS82
At the start of the test At initiation of crack
AS62
At the start of the test At initiation of crack
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
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AS75
At the start of the test At initiation of crack
AS80
At the start of the test At initiation of crack
AS102
At the start of the test At initiation of crack
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CUED/D-SOILS/TR340 32
AS100
At the start of the test At initiation of crack
AS25
At the start of the test At initiation of crack
BS22
At the start of the test At initiation of crack
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Cracking in clay data report on cracking of clay beams by 4-point beam tests
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CUED/D-SOILS/TR340 33
BS46
At the start of the test At initiation of crack
BS92
At the start of the test At initiation of crack
BS65
At the start of the test At initiation of crack
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CUED/D-SOILS/TR336
BS16
At the start of the test At initiation of crack
BS15
At the start of the test At initiation of crack