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International Journal of Rock Mechanics & Mining Sciences 38 (2001) 909924
Analysis of crack coalescence in rock-like materials containingthree flawsFPart I: experimental approach
R.H.C. Wonga,*, K.T. Chaua, C.A. Tangb, P. Linb
aDepartment of Civil and Structural Engineering, The Hong Kong Polytechnic University, Hung Hom, Hong Kong, ChinabCentre for Rock Instability and Seismicity Research, Northeastern University, Shenyang, China
Accepted 6 September 2001
Abstract
Fractures in the forms of joints and microcracks are commonly found in natural rocks, and their failure mechanism strongly
depends on the crack coalescence pattern between pre-existing flaws. However, the crack coalescence pattern of rock specimens
containing three or more flaws has not been studied comprehensively. In this paper, we investigate experimentally crack coalescence
and peak strength of rock-like materials containing three parallel frictional flaws. Three flaws are arranged such that one pair of
flaws lines collinearly and the third flaw forms either a non-overlapping pattern or an overlapping pattern with the first flaw. It is
found that the mechanisms of crack coalescence depend on the flaw arrangement and the frictional coefficient m on the flaw surface.
Two rules of failure for the specimens containing three flaws are proposed. Rule No. 1: the pair of flaws with a lower value of
coalescence stress will dominate the process of coalescence. Rule No. 2: mixed and tensile modes of coalescence are always the dominant
modes if the coalescence stress of the two pairs of flaws is very close (say within 5%). In addition, it is found that the peak strength of
the specimens does not depend on the initial crack density but on the actual number of pre-existing flaws involved in the coalescence.
Comparisons of pattern of crack coalescence with the numerical approach are given in Part II of this study, and the two results agree
well. The research reported here provides increased understanding of the fundamental nature of rock failure in uniaxial
compression. r 2001 Elsevier Science Ltd. All rights reserved.
1. Introduction
When a brittle rock is loaded to failure, cracks
nucleate and propagate from pre-existing inhomogene-
ities, which can be in the form of pores, fractures,
inclusions or other defects. Crack initiation and
propagation in solids have been studied since the early
twenties [1,2]. Particular reference to fractures in rocks,
systematic, theoretical and experimental investigations
of crack initiation, propagation and interaction began at
about the middle of the last century and have continued
since [318]. It is recognized that under the compressive
loading, both tensile and shear stress concentrations can
develop at pre-existing inhomogeneities in rock. As the
compression applied to the rock further increases,
tensile cracks will be initiated. In the shear sliding crack
model, this tensile crack is called a wing crack, which
initiates from the tip of pre-existing fracture and grows
progressively parallel to the compression direction. At
the early stages, when the wing crack is short, the
growth is dominated by the stress field around the pre-
existing fracture from which it grows. As the crack
extends, it start to interact with neighbouring micro-
cracks, and this interaction ultimately leads to crack
coalescence and final failure of the sample [16].
Fracture propagation leading to rock failure is a very
important topic in rock mechanics research. A number
of studies have been done on two-dimensional (2-D)
model plates with through going pre-existing fractures
[329] and some of them have been done on 3-D
specimens [3033]. In reality, pre-existing fractures are
3-D in nature. The growth mechanisms of a 3-D crack
may be more complicated. Actually, according to the
observations by Germanovich et al. [3032] and
Germanovich and Dyskin [33], unlike in 2-D samples,
there are intrinsic limits on the growth of a crack in a
3-D model. However, the failure mechanism of rocks
containing 3-D cracks is out of the scope of the present
*Corresponding author. Tel.: +852-2766-6057; fax: +852-2334-
6389.
E-mail address: [email protected] (R.H.C. Wong).
1365-1609/01/$ - see front matter r 2001 Elsevier Science Ltd. All rights reserved.
PII: S 1 3 6 5 - 1 6 0 9 ( 0 1 ) 0 0 0 6 4 - 8
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coalescence observed by Bobet and Einstein [26] fall
within the classification of Wong and Chau [23]. Bobet
and Einstein [26] and Bobet [27] investigated the pattern
of crack coalescence under both uniaxial and biaxial
compression. They found that the patterns of crack
coalescence not only depend on the flaw geometry butalso on the stress conditions. Wing cracks initiate at the
flaw tips for uniaxial or low confinement biaxial
conditions, but the location of crack initiation moves
to the middle of the flaw and wing cracks disappear
completely for higher confining stresses. For the relation
between the strength and the pattern of crack coales-
cence of specimens, Wong [22] and Wong and Chau [24]
found that the compressive strength of the specimen for
wing crack coalescence is normally lower than that for
shear crack coalescence. Furthermore, Wong and Chau
[25] found that the strength of cracked solids does not
depend linearly on the number of pre-existing flaws
(density) once a threshold value of flaw density is
exceeded.
Although previous studies provide a general under-
standing of the coalescence pattern between two flaws,
when specimens contain three or more flaws, the crack
interaction between the flaws has not been studiedcomprehensively. This is important because rock con-
tain many flaws. Thus, Wong et al. [28,29] reported very
briefly the results of specimens containing two flaws to
multiple flaws under both uniaxial and biaxial compres-
sion. The number of flaws in the specimens was from 3
to 42. To report the results more comprehensively, we
present in this paper only the results of crack
coalescence and peak stress of rock-like materials
containing three flaws. The research of this paper is of
fundamental importance to understand the mechanism
controlling crack coalescence in the multiple flawed
specimens.
In this study, the flaw angle a; bridge angle b and thefrictional coefficient m are varied under a fixed flaw
length 2c and bridge length 2b, which have been
defined in Fig. 1. Our main interest is to investigate the
dominant factors controlling the failure patterns in
specimens containing three flaws. A further objective of
the present paper is to investigate the failure mechanism
of rock bridges in brittle materials containing multiple
flaws in order to represent fully the failure of intact rock.
The numerical study of the same problem is presented in
Part II [34].
There are two general areas where a study of this type
could prove useful: in problems of stability of rock incivil engineering, such as the excavated underground
openings or slopes, and in fracture mechanics involving
multiple flaws. The relevant observations in the first case
are that the collapse of a rock structure containing non-
persistent joints may be preceded by several stages of
crack propagation, interaction and coalescence. Our
investigation should provide the fundamental under-
standing of crack propagation, interaction and coales-
cence in rock under uniaxial compression. With respect
to the contribution to fracture mechanics, the coales-
cence of multiple non-persistent joints is involved in the
fracture of all brittle materials.
2. Experimental studies
In order to have a good comparison between our
present study and the previous study, the mixture of the
modelling material is the same as that used by of Wong
and Chau [23], which is a mixture of barite, sand, plaster
and water with a mass ratio of 2 : 4 : 1 : 1.5. The average
values of unit weight, uniaxial compressive strength,
tensile strength and frictional coefficient of the model-
ling material are gm 17:68 kN/m3, scm 2:09 MPa,
Fig. 2. Classifications of coalescence of a 2-flaw specimen with
different combinations of flaw angle a; bridge angle b and frictionalcoefficient m: (a) is the classification for m 0:6 and (b) is the
classification for m 0:7: Triangles, rhombuses and squares were thedata points of the 2-flaw specimens for shear, mixed and wing tensile
modes, respectively. The S-regime is the regime in which the shear
mode of crack coalescence is expected to occur. The M-regime is the
regime in which the mixed shear/tensile mode of crack coalescence is
likely to occur, and the W-regime is the regime in which wing crack
failures are expected (after Wong and Chau [23]).
R.H.C. Wong et al. / International Journal of Rock Mechanics & Mining Sciences 38 (2001) 909924 911
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stm 0:35 MPa and mm 0:62; respectively. The aver-age value of the tangent Youngs modulus (Em) at 50%
of peak strength is 0.33 GPa and the Poissons ratio (nm)
is 0.19. The fracture toughness KIC of the modelling
material is 0.0443 MPam1/2. The p factors of dimen-
sional analysis of this artificial material have been found
comparable to the physical ranges of the p factors forsandstone; therefore, Wong and Chau [23] concluded
that the material is appropriate as a sandstone-like
modelling material. The overall dimensions of specimens
containing three flaws are 60mm wide 120 mm
long25 mm thick. To simplify the present analysis,
the bridge length 2b (distance between two flaws) and
the flaw length 2c are fixed at 20 and 12 mm,
respectively.
Flaws were created by inserting steel shims into three
slots in the mould template and removing them during
curing (Fig. 3). Different degrees of the roughness of the
flaw surface are created by applying different numbers
of punch marks to the smooth steel shims (Fig. 4). Thefrictional coefficients on the flaw surfaces are measured
by the titling test on specimens with a through going
flaw. The mean frictional coefficient on flaw surfaces
simulated by inserting plain steel shim is 0.6, while
that simulated by steel shim with punched-indentations
is 0.7.
Two different flaw angles a were used to investigate
the effect of flaw geometry on the pattern of crack
coalescence. The chosen flaw angles are 451 and 651,
where 651 is the preferred orientation for the frictional
flaws (m 0:620:7) of the specimen to slide under
uniaxial compression [23]. The layout of specimenscontaining three flaws is shown in Fig. 5. For sake of
later discussions, the three flaws are labelled as , and
, respectively.
As shown in Fig. 5, there are two bridge angles b1 and
b2 for the three-flaw model. In the experiments, b1(between flaws and ) is fixed at 451, and b2 (between
flaws and ) varies from 751 to 1201 with increments
of 151. Thus, there are two different bridge angles
between the three flaws. As is illustrated in Fig. 2, the
flaw settings of b 451 result in a shear coalescence
pattern, and the other settings of b 751 to 1201 result
in mixed and tensile coalescence modes. Therefore, we
can investigate whether coalescence occurs along therock bridge of b1 (i.e. shear crack coalescence), along
that rock bridge of b2 (i.e. tensile and mixed crack
coalescence), or along the rock bridge of both b1 and b2:Then the possible relevance of the coalescence in the 2-
flaw-specimens to the 3-flaw-specimens can also be
examined.
To obtain reliable results in the experiment, the
sample preparation procedures were under well control.
The modelling materials were weighed by using the
electronic weighting balance to a 70.01. Each mixing
procedure was under time control where for the mixture
of barium sulphate and sand it was 4 min. Then cold
water was added evenly and mixed until all particles had
been wetted (4 min). Finally, plaster was added and
mixed evenly until the mixture became a churn-like
paste (7 min). The mixture was then poured into a
mould under vibration (4 min).
To prevent the boundary condition of specimen
affecting the results of experiments, the positions of
three pre-existing flaws were designed as far away as
possible from the side boundaries of specimen. Other-
wise, local failure may be observed instead of crack
coalescence between the pre-existing flaws during the
testing.Fig. 3. Flaws are created in the specimen by inserting stainless steel
shims into three slots in the mould template.
Fig. 4. The stainless steel shims with different roughness used in
creating the flaws in the modelling material. The top and lower shims
give a frictional coefficient of 0.6 and 0.7 on the surfaces of the flaws,
respectively.
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In this study, two specimens with the same parameters
have been cast and tested. If the pattern of crack
coalescence for both specimens is the same, the mean
value of the peak strength is taken. If only one fails by
crack coalescence and the other fails but without crack
coalescence, one more specimen with the same para-
meters was prepared and tested. If both specimens failed
with no crack coalescence, two more specimens with the
same parameters were prepared and tested. If, again, no
crack coalescence was observed for these additional
specimens, the mean peak strength of these specimens is
recorded for comparison purposes only.
The uniaxial compression tests of the specimens were
performed in a Wykeham Farrance WF-5562s loading
machine. This is a load control machine available in our
rock mechanics laboratory. The average loading rate is
about 0.002 kN/s, and it takes about 2530 min to load
one specimen to failure. Two LVDTs were installed in
the front and behind the specimen for measuring the
vertical deformation of the specimen. Only three of
specimens fail suddenly after peak applied stress;
otherwise, the recorded displacement rate is rather
steady up to peak applied stress and even after.
Therefore, there should be no appreciable differencebetween the displacement and load control in our
particular case. Thus, the loading process can be
considered as displacement-controlled approximately.
The setting of the apparatus is shown in Fig. 6 where a
load cell of 5 kN is placed below the lower loading
platen to measure the applied load. To reduce the
friction between the specimen and the loading platens,
two pieces of polythene sheet were inserted. All speci-
mens were loaded until either the flaws coalesced or the
specimen failed, which is identified by the drop in the
applied load. All the loading and displacement records
are transferred to and stored in an IBM PC through a
KYOWA UCAM-5B Data Logger.In all the reported experiments, no local failure was
observed, thus no sample boundaries affect to the results
of our experiment.
3. The coalescence of cracks
3.1. Comparisons of the patterns of crack coalescence
between specimens containing two and three flaws
Wong and Chau [23] concluded that there are three
modes of coalescence in the bridge area, wing tensile,shear and mixed (tensile and shear), for specimens
containing two flaws. To compare the patterns of crack
coalescence between specimens containing two and three
flaws, Figs. 7 and 8 report all the failure patterns
for various values of flaw angle (a 451 and 651),
bridge angle (b 451; 7511201) and frictional co-efficient (m 0:6 and 0.7) for 2- and 3-flaw-specimens,respectively.
The notations S (shear mode crack coalescence), MI,
MII (mixed shear/tensile mode crack coalescence), WI,
WII, WIII and WII/III (wing tensile mode crack
coalescence) are the same as those used in Fig. 6 of
Wong and Chau [23] which is also given in Fig. 9 here.
For the S-type coalescence, crack links between the tip
of two flaws along the direction roughly parallel to the
flaw. For the MI-type coalescence, the growing wing
cracks, which initiated from the two tips of the flaws, are
coalesced by a shear crack in the middle of bridge area.
For the MII-type of coalescence, a growing wing crack
is coalesced by a shear crack that appeared at the other
tip of a flaw. The WI-type of coalescence is a simple
coalescence between two wing cracks. The WII-type of
coalescence is resulted as a growing wing crack coalesces
with the other flaw. The WIII-type of coalescence is a
1
2
Outer Flaw Tip
Outer Flaw Tip
Inner Flaw Tip
Inner Flaw Tip
1
3
2
Fig. 5. The layout of specimens containing three flaws. The inclina-
tions of the pre-existing flaws a used in this study are 451 and 651. The
bridge angle ofb1 is fixed at 451, while b2 vary from 751 to 1201. The
length of flaw 2c is fixed at 12mm. The bridge distance between the
two flaws 2b is fixed at 20 mm. The inner and outer flaw tips are also
shown.
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growing wing crack joining the outer tip of the other
flaw. From comparisons of Figs. 7 and 8, for the same
a=b it is observed that the type of failure patterns in the3-flaw specimens are the same as those for the 2-flaw
specimens. Coalescence in the 3-flaw specimens can
again be identified as either shear S, wing tensile WI or
mixed (tensile and shear) MI and MII depending on the
values ofa; m and the coalescence angle bc; defined as thebridge angle along which the crack coalescence occurs
(i.e. either b1 or b2). Unlike the studies on 2-flaw models(Fig. 7), coalescence with a bridge angle b of 1201 was
not observed in all specimens with three flaws (Fig. 8).
For 3-flaw specimens with bridge angles ofb1; b2 451;1201, coalescence occurs only for b1 451 but not for
b2 1201 (Fig. 8).
The classification given in Fig. 2 of this study suggests
that the appearance of these modes of coalescence
depends on the values of a; b and m: The patterns ofcrack coalescence for 3-flaw specimens in the a bcspace for m 0:6 and 0.7 were superimposed onto theregime classification given in Fig. 2; and the results are
plotted on Fig. 10. The triangles, rhombuses and
squares in circles are used to denote the data points
for shear, mixed and wing tensile modes observed in the
3-flaw specimens, respectively. Except for one specimen
with a=bc=m 451=1051=0:6 (see Fig. 10a), it is foundthat all of the experimental results for 3-flaw specimens
fall within the same regimes classification of 2-flaw
specimens.
3.2. General observation for 3-flaw specimens
Experimental observations (see Fig. 8) show that
crack coalescence occurred in 14 out of the 16 geometric
settings. There are three possible scenarios in the process
of crack growth. (1) In about 27% of the specimens,
tensile cracks (wing cracks) initiate first at the tips of the
two flaws (either the flaw , or ) followed by wing
crack initiation from a third flaw at a later stage.
However, no matter which wing crack initiates first,
crack coalescence occurs only between two flaws (flaws
and ) at failure. (2) In about 60% of the specimens,
wing cracks initiate from only two flaws (either between
flaws and or flaws and ), with no wing cracknucleating from the third flaw during the whole loading
process and the final coalescence also does not involve
the third crack. (3) In the remaining 13% of specimens,
wing cracks initiate from all three flaws at the same time,
but no crack coalescence is observed at failure.
The process of coalescence between the growing wing
cracks is normally slow enough to be captured by eye
observation. It is observed that crack initiates first at
either inner tip or outer tip of the flaws, followed by
crack growth at the other tip of the same flaw (see the
definitions of inner and outer tips in Fig. 5). In general,
the growth of cracks at the outer tips is faster than that
observed at the inner tips. The growth rate of each inner
crack is not the same. When an inner crack grows
rapidly, the other inner tip of flaw normally grows much
slower and even seems to stop growing. This is because
of the higher stress concentration around the growing
inner crack tip and causing the crack to grow further.
With a nearby propagating inner crack, a high stress
concentration at the neighbouring inner crack tip will be
affected. A further discussion of stress distribution
within the bridge area will be presented in Part II of
this study [34]. The types of cracking in the bridge area
between the three flaws can be wing tensile, shear, or a
Fig. 6. The layout of the loading system with the displacement recording system.
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mix of these. Furthermore, it is observed that if the
growth rate of the inner cracks is the same, no
coalescence occurs even when the applied stress drops.
In general, when an inner crack coalesces with the
neighbouring inner crack, the applied stress will
decrease. The test is stopped until the axial stress drops
to 70% of the peak stress.
Fig. 8 illustrates the very important feature that crack
coalescence occurs only between two flaws either
between flaws and or between and , and never
between flaws and . What makes the flaw to
coalesce with the flaw but why not the or the
reverse order? Why crack coalescence does not occur
between flaws and under uniaxial compression?
Fig. 7. The mode of crack coalescence for specimens containing two flaws. The angles b represent the bridge angle with m 0:6 and 0.7. The
notations S (shear mode crack coalescence), MI, MII (mixed mode crack coalescence), WI, WII, WIII and WII/III (wing tensile mode crack
coalescence) are the same as those proposed in Fig. 6 of Wong and Chau [23] or Fig. 9 of this paper.
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To demonstrate the above rules, the observed data ofthe 3-flaw specimens are summarised in Table 1. The
peak strength results (or coalescence stress, in general,
crack coalescence was observed at about the peak
strength of specimen) for the 2-flaw specimens are
tabulated in Table 1 together with the results for the 3-
flaw specimens with the same a; m and bc (coalescenceangle). For example, for the 3-flaw specimens with the
parameter set a=b1; b2=m 451=451; 751=0:6; thereare two possible angles of coalescence bc 451 (coales-
cence between flaw and ) or bc 751 (coalescence
between flaw and ). The coalescence stress for 2-flaw
specimen with a=bc 451=451 is 1.67 MPa, comparedwith 1.59 MPa for specimen with a=bc 451=751 (thiscoalescence stress is smaller than 1.67 MPa). Fig. 11
shows the peak strength and crack coalescence of 2-flaw
specimens of b 451 and 751 and 3-flaw specimen of
b1=b2 451=751 with the same m (0.6) and the same atogether. The mode of coalescence for the 3-flaw
specimens is clearly the same as that for the 2-flaw
specimen with a=bc 451=751 (between flaws andin Fig. 11a). Therefore, Rule 1 applies in this case.
That is, a bc value that corresponds to the smaller
coalescence stress seems to prevail in the process of
crack coalescence. In the lower part of Table 1, all data
that comply with Rule 1 are marked with super-script 1.
However, some data in Table 1 do not comply with
Rule 1. For example (see Table 1), for the 3-flaw
specimen with the parameter set a=b1;b2=m 65=45; 75=0:6; the coalescence stress for 2-flaw speci-men with a=bc 651=451 is 1.42 MPa, for specimenwith a=bc 651=751 is 1.45MPa. If Rule 1 is theonly rule for coalescence, the angle of coalescence bc for
data set a=b1;b2=m 65=45; 75=0:6 should be 451(coalescence between flaws and ) instead of 751
(coalescence between flaws and ). However, the
coalescence in 3-flaw specimen is between flaws and
(Table 1 and Fig. 11b). Consequently, Rule 2 is
formulated for crack coalescence for 3-flaw models as:
when the coalescence stress of the two pairs of flaw is
very close (say within 5%), mixed and tensile modes of
crack coalescence always dominate. All data that
comply with Rule 2 are indicated by the superscript
2 in Table 1.
Table 1 shows that 12 of the 14 coalescence sets of 3-
flaw data conform to these rules of coalescence, a
conformity of 86%. If b2 equals to 751 or 901, the
conformity is 100%. Since these rules of crack coales-
cence are rather preliminary based on limited tests,
Shear
Crack
S
Shear
Crack
WingCrack
M I
Shear
Crack
WingCrack
M II
Wing
Crack
W I
WingCrack
W II
Wing
Crack
W III
Fig. 9. Six different patterns of crack coalescence observed in the 2-flaw specimens. The notations S, M and W indicate the shear, mixed (shear/
tensile) and wing tensile mode crack coalescence, respectively (after Wong and Chau [23]).
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numerical simulation studies were conducted and will be
presented in Part II of this study [34].
Up to this stage, it cannot be explained why crack
coalescence does not occur between flaws and . The
following section attempts to address this question by
comparison with Nemat-Nasser and Horii [12].
3.4. Comparison with Nemat-Nasser and Horii (1982)
It is instructive to compare the observations of this
study to those by Nemat-Nasser and Horii [12], who
used Columbia resin CR39 as the modelling material.
The specimens were 6 mm thick, flaw lengths about
12 mm, flaw widths or openings about 0.4 mm, and each
crack was lined with two 0.2 mm thick brass shims in
order to reduce friction between the two flaw faces. The
flaw distance (bridge length) was 12 mm and a was 451.
The specimens contained two rows of two parallel
collinear flaws with b1 of 451 and b2 of 901 (estimated by
direct measurements on Figs. 17(ac) and 18(ab) of
Nemat-Nasser and Horii [12]). In order to give a clear
discussion and illustration, Fig. 12 reproduces the
experimental observation given in Fig. 18(b) of Nemat-
Nasser and Horii [12]. Three of the flaws are named
similar to the 3-flaw specimens of , and . Under
uniaxial compression, wing cracks initiate and propa-
gate (the solid line) from the tips of the flaws. The wing
cracks from the lower row flaw tips (e.g. flaw )
propagate upward to the upper one (e.g. flaw ), and
those wing cracks from the upper row flaw tips grow
downward to the lower one. However, the specimens
failed by axial splitting rather than localized coalescence
failure. In contrast, coalescence failures were formed in
the specimens for this study (see Fig. 8) under uniaxial
compression for the same values of a and b: Thisdiscrepancy between the present study and that by
Nemat-Nasser and Horii [12] may have resulted from:
(i) their material and the one used in this study are
conducive to different modes of failure even though
both are brittle; and (ii) their frictional coefficient m
Fig. 10. (a,b) Modes of crack coalescence for specimens containing three flaws superimposed onto the classifications given in Fig. 2. Symbols ,
and indicate the shear, mixed shear/tensile and wing tensile modes of coalescence observed in the 3-flaw specimens, respectively.
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(which is actually not given) may be very small
comparing to that of the present study. As illustrated
in Wong and Chau [23], deviation of the orientation of
wing cracks from the line of flaw decreases with increase
of m: To further illustrate the second possible reason,Fig. 8 from Wong and Chau [23] is redrawn in Fig. 12
(the small figure at the left lower corner) together with
the reproduction of Nemat-Nasser and Horii [12]. As
shown in the figure, if a higher value ofm had been used
on the surfaces of the flaws, the path for the growth of
wing cracks would have been more likely to follow a
path linking the flaw tips (between flaws and ,
indicated by the dotted line in Fig. 12). Therefore, it is
clear from the small figure of Fig. 12 that specimens with
a higher value of the frictional coefficient m on the flaw
surfaces are more conducive to wing crack coalescence
compared to cases of small m values (as in the
experiment of Nemat-Nasser & Horii [12]). If zero m
value has been used on the surfaces of the flaws, the path
for the growth of wing cracks would have been more
likely to follow a path linking the flaw tips between
and (indicated by the dotted line in Fig. 12). However,
a higher value ofm had been used in our study, therefore
no crack coalescence is observed between flaws and
in our 3-flaws study. As reviewed from Fig. 8, for those
cracks initiated from flaws and , the growth of inner
tip of flaw propagates towards flaw , while the
growth of outer tip of flaw grows towards the edge of
specimen under uniaxial compression. For the same flaw
arrangement under a biaxial compression [28], second-
ary crack can initiate at the outer tip of flaw ,
propagate towards flaw and coalesce. In this case,
failure involves three flaws.
4. Peak strength of flawed specimens
Table 1 shows that the peak strength for specimens
with the same a; b and m are basically the same,regardless of whether they contain two or three flaws.
In other words, peak strength appears not to decrease
proportionally with the initial flaw density.
These observations not only appear in 3-flaw specimens,
but also were observed in the modelling specimens
Table 1
A comparison of the experimental peak strength for specimens containing two flaws and three flaws
Two flaws
a (1) b1 (1) m 0:6 m 0:7
bc (1) Peak strength (MPa) bc (1) Peak strength (MPa)
45 45 45 1.67 45 1.8875 75 1.59 75 1.80
90 90 1.59 90 1.57
105 105 1.88 105 1.84
120 120 1.64 120 1.73
65 45 45 1.42 45 1.44
75 75 1.45 75 1.49
90 90 1.49 90 1.48
105 105 1.51 105 1.52
120 Nob 1.46 120 1.48
Three flaws
a (1) b1; b2 m 0:6 m 0:7
bc (
1) Peak strength (MPa)
bc (
1) Peak strength (MPa)
45 45, 75 751 1.59 751 1.73
45, 90 901 1.57 901 1.73
45, 105 105a 1.60 1051 1.61
45, 120 Nob 1.69 45a 1.70
65 45, 75 752 1.43 752 1.58
45, 90 902 1.42 902 1.52
45, 105 451 1.51 451 1.62
45, 120 451 1.51 Nob 1.58
aThese results do not comply with the rule of failure.bNo crack coalescence occurs at failure.
751 Data comply with Rule 1.
902 Data comply with Rule 2.
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containing multiple flaws (18 and 42 with the specimen
size of 400 mm 400 mm 25 mm [24]). This is also
precisely what was observed for the Hong Kong granite
by Wong and Chau [25], and Yuen Long marble by
Wong et al. [35] that peak strength does not decrease
with initial flaw density once a threshold value of flaw
density is exceeded. We speculate that the peak strength
for a specimen is not proportional to the number of
flaws, and the following hypothesis is thus proposed.
The peak strength for flawed specimens does not depend
on the total number of pre-existing flaws, but only on the
number of flaws actually involved in the formation of the
failure pattern. (Note, the above conclusion is from
specimens with fixed flaw spacing of 20 mm [24], and
from Yuen Long marble with varying flaw spacing from
53 to 106mm [35]).
To examine this hypothesis, the model by Ashby and
Hallam [16] is employed. Ashby and Hallam [16] derived
the following total stress intensity factor KI for the
growth of wing cracks:
KI
s1
ffiffiffiffiffipc
psin 2c m m cos 2c
1 L3=20:23L
1
ffiffiffi3
p1 L1=2
" #
2e0L cos cp
1=2; 1
where s1 is the uniaxial compression, c is the angle
measured from the s1-direction to the direction along
the flaw surface (i.e. c 901 a), 2c is the length of the
pre-existing flaw, L c=c is the normalized length of thewing cracks (c is the length of the growing wing crack),
m is the frictional coefficient along the shear or frictional
flaw, and the flaw density e0 is defined as Nc2=A (N is the
number of flaw per area A). Although strictly speaking
(1) is for the case of multiple initial flaws, it was found
that it can also be applied to the specimen containing
Fig. 11. (a,b) The mode of crack coalescence and the peak stress of specimens containing two flaws and three flaws with the same a; b and mpresented here for discussion on the two rules of coalescence for solids containing three flaws.
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two flaws (see Table 2 of [23] which is also given in
Table 2 of present study). Therefore, the peak uni-
axial compressive strength smax1 of a flawed solid can be
estimated as Wong and Chau [23]:
smax1
KICffiffiffiffiffipc
p sin 2c m m cos 2c1 Lcr
3=2
(
0:23Lcr 1ffiffiffi
3p
1 Lcr1=2
" #
2e0Lcr cos c
p
1=2)1; 2
where KIC is the fracture toughness (0.0443 MPaOm forour modelling material), Lcr cmax=ccmax 2b sin b isthe maximum possible value for the length of the
coalesced wing cracks, and 2b is the distance between
the two flaws). In this study, the initial flaw density of
specimens containing three flaws is e0 0:015(e0 Nc
2=A note that N 3; A 0:06 m 0.12 m andc 0:006 m). Predictions of the normalized peakstrength (smax1 Opc=KIC) by using Eq. (2) and the
experimental observations are tabulated in Table 3. Todemonstrate the above hypothesis, the peak strength of
the specimens containing 18 and 42 flaws [24] are
tabulated in Table 3 together with the results for the 3-
flaw specimens with the same flaw length 2c, bridge
length 2b, a; b and m: For the specimen containing 18flaws, 3 rows of 6 collinear flaws are placed at the central
region. For the specimen containing 42 flaws, the flaw
arrangement is 9 rows of 4 collinear flaws at the central
region and 2 rows of 3 parallel flaws at the upper and
lower ends of specimen. The density of the multiple
flawed specimens for 18 and 42 flaws are e0 0:016 and0.038, respectively (Table 3). It is found that if initial
flaw density e0 is used in the calculation, the prediction ismuch lower than the experimental observations. The
hypothesis was then tested by using the number of flaws
involved in the formation of the failure pattern in
calculating flaw density ef: For the 3-flaw specimen, ef
0:01 is used, because the observations presented in thisstudy show that final crack coalescence involves only
two flaws but not three. For 18- and 42-flaws specimens,
the number of flaws involved in the failure pattern are 15
and 5. Thus the values of the adjusted crack density are
ef 0:0135 and 0.0045, respectively. It is found that thepredicted peak strength based on flaw density ef agrees
well with the experiments, as shown in Table 3.
5. Conclusions
In this study, experimental results on the mechanism
of crack coalescence and on the peak strength of rock-
like materials containing three flaws under uniaxial
compression loading were presented. The specimens
used in this study are made of a sandstone-like material
and contain three parallel frictional flaws. Various
values of inclination of these flaw angles a; the bridge
angle b and the frictional coefficient m were used in ourparametric studies. For specimens containing three
flaws, it was found that:
* Crack coalescence occurs between only two flaws (not
three).* The mechanisms of crack coalescence depend on the
coalescence stress of the pair of flaws. The lower
value of coalescence stress between the pair of flaws
will dominate the process of coalescence.* Mixed and wing tensile modes of coalescence are
more likely to occur than shear mode, if the
Wing Crack
= 0.90.7
0.6
0.0
Pre-existing
Flaw
From Fig.8 of Wong
and Chau [23]1 in
Possible path for crack
growth if is higher
Possible path for
crack growth ifis zero
2
1
3
2
1
Fig. 12. Shows the effect ofm on the path of wing crack propagation.
The specimen with two parallel rows of collinear pre-existing cracks is
adopted from Fig. 18 of Nemat-Nasser and Horii [12]. For a higher m;the possible path for crack growth may occur between flaws and .
For a lower mE0; the possible path for crack growth may appearbetween flaws and . The small figure showing the effect ofm on the
path of wing crack from Fig. 8 of Wong and Chau [23] is redrawn here
for comparison.
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coalescence stress between the pair of flaws is very
close (within 5% of each other).* The frictional coefficient m of flaw surface can affect
the pattern of coalescence of the cracked solids.* The uniaxial peak strength for cracked specimens
does not depend on the total number of flaws but
only on the number of flaws actually involved in theformation of the shear zone of the failure pattern.
Our observation provides a better understanding on
the failure behaviour of crack coalescence between three
flaws. In addition, to further examine the reason of
crack coalescence occurring between only two flaws, a
comprehensive numerical study will be presented in
Part II of the paper [34]. In particular, we focus on the
stress distribution within the bridge area.
Acknowledgements
The study was supported by the Research Project No.
A-PA42 of the Hong Kong Polytechnic University to
RHCW. The laboratory assistance by C.Y. Chim is
appreciated.
References
[1] Griffith AA. The phenomena of rupture and flow in solids. Phil
Trans Royal Soc London, Ser, 1921;A221:16398.
[2] Griffith AA. The theory of rupture. Proceeding of First
International Congress Applied Mechanics, 1st Delft, 1924,
p. 5563.[3] Hoek E, Bieniawski ZT. Brittle fracture propagation in rock
under compression. Int J Fract Mech 1965;1:13755.
[4] Peng S, Johnson AM. Crack growth and faulting in cylindrical
specimens of Chelmsford granite. Int J Rock Mech Min Sci
Geomech Abstr 1972;9:3786.
[5] Hallbauer DK, Wagner H, Cook NGW. Some observations
concerning the microscopic and mechanical behaviour of quart-
zite specimens in stiff triaxial compression tests. Int J Rock Mech
Min Sci Geomech Abstr 1973;10:71326.
[6] Tapponnier P, Brace WF. Development of stress-induced micro-
cracks in Westerly granite. Int J Rock Mech Min Sci Geomech
Abstr 1976;13:10312.
[7] Olsson WA, Peng SS. Microcrack nucleation in marble. Int J
Rock Mech Min Sci Geomech Abstr 1976;13:539.
[8] Kranz RL. Crackcrack and crackpore interactions in stressedgranite. Int J Rock Mech Min Sci Geomech Abstr 1979;16:3747.
[9] Batzle ML, Simmons G, Siegfried RW. Microcrack closure in
rocks under stress: direct observation. J Geophys Res
1980;85:707290.
[10] Dey TN, Wang CY. Some mechanisms of microcrack growth and
interaction in compressive rock failure. Int J Rock Mech Min Sci
Geomech Abstr 1981;18:199209.
[11] Wong TF. Micromechanics of faulting in westerly granite. Int J
Rock Mech Min Sci, Geomech Abstr 1982;19:4964.
[12] Nemat-Nasser S, Horii H. Compression-induced nonlinear crack
extension with application to splitting, exfoliation, and rockburst.
J Geophys Res 1982;87(B8):680521.
[13] Steif PS. Crack extension under compressive loading. Eng Fract
Mech 1984;20(3):46373.
[14] Horii H, Nemat-Nasser S. Compression-induced microcrack
growth in brittle solids: axial splitting and shear failure. J
Geophys Res 1985;90(B4):310525.
[15] Horii H, Nemat-Nasser S. Brittle failure in compression: splitting,
faulting and brittle-ductile transition. Phil Trans Roy Soc London
1986;A319:16398.
[16] Ashby MF, Hallam SD. The failure of brittle solids containing
small cracks under compressive stress states. Acta Metall
1986;34(3):497510.
[17] Sammis CG, Ashby MF. The failure of brittle porous solids under
compressive stress states. Acta Metall 1986;34(3):51126.
[18] Kemeny JM, Cook NGW. Crack models for the failure of rock
under compression. Proceedings of the Second International
Conference on Constitutive Laws for Engineering Materials,
vol. 2, 1987. p. 87987.
[19] Reyes O. Experimental study, analytic modeling of compressive
fracture in brittle materials. Ph.D.Thesis, Massachusetts Institute
of Technology, Cambridge, 1991.
[20] Reyes O, Einstein HH. Fracture mechanism of fractured
rockFa fracture coalescence model. Proceeding of the Seventh
International Conference On Rock Mechanics,vol. 1, 1991.
p. 33340.
[21] Shen B, Stephansson O, Einstein HH, Ghahreman B. Coalescenceof fractures under shear stress experiments. J Geophys Res
1995;100(6):597590.
[22] Wong RHC.Failure mechanisms, peak strength of natural rocks
and rock-like solids containing frictional cracks. Ph.D.Thesis, The
Hong Kong Polytechnic University, Hong Kong, 1997.
[23] Wong RHC, Chau KT. Crack coalescence in a rock-like material
containing two cracks. Int J Rock Mech Min Sci 1998;35(2):
14764.
[24] Wong RHC, Chau KT. The coalescence of frictional cracks and
the shear zone formation in brittle solids under compressive
stresses. Int J of Rock Mech Min Sci 1997;34(3/4):366, paper
No. 335.
[25] Wong RHC, Chau KT. Peak strength of replicated and real rocks
containing cracks. Key Eng Mater 1998;145149:9538.
[26] Bobet A, Einstein HH. Fracture coalescence in rock-type
materials under uniaxial and biaxial compression. Int J Rock
Mech Min Sci 1998;35(7):86388.
[27] Bobet A. Modelling of crack initiation, propagation and
coalescence in uniaxial compression. Rock mech Rock Eng
2000;33(2):11939.
[28] Lin P, Wong RHC, Chau KT, Tang CA. Multi-crack coalescence
in rock-like material under uniaxial and biaxial loading. Key Eng
Mater 2000;183187:80914.
[29] Wong RHC, Lin P, Chau KT, Tang CA. The effects of confining
compression on fracture coalescence in rock-like material. Key
Eng Mater 2000;183187:85762.
[30] Germanovich LN, Salganik RL, Dyskin AV, Lee KK. Mechan-
isms of brittle fracture of rocks with multiple pre-existing cracks
in compression. Pure Appl Geophys 1994;143 (1/2/3) 11749.[31] Germanovich LN, Ring LM, Carter BJ, Ingraffea AR, Dyskin
AV, Ustinov KB. Simulation of crack growth and interaction in
compression, Proceedings of the Eighth International Conference
on Rock Mechanics, vol. 1. Rotterdam and Brookfield: Balkema,
1995. p. 21926.
[32] Germanovich LN, Carter BJ, Dyskin AV, Ingraffea AR, Lee KK.
Mechanics of 3-D crack growth under compressive loads, In:
Aubertin M, Hassani F, Mitri H, editors. Rock mechanics tools
and techniques. Proceedings of the Second North American Rock
Mechanics Symposium: NARMS96. Rotterdam and Brookfield:
Balkema, 1996, p. 1151160.
[33] Germanovich LN, Dyskin AV. Fracture mechanisms and
instability of openings in compression. Int J Rock Mech Min
Sci 2000;37:26384.
R.H.C. Wong et al. / International Journal of Rock Mechanics & Mining Sciences 38 (2001) 909924 923
8/7/2019 Analysis of Crack Coalescence in Rock-like Materials
16/16
[34] Tang CA, Wong RHC, Chau KT, Lin P. Analysis of crack
coalescence in rock-like materials containing three flawsFPart II:
numerical approach. Int J Rock Mech Min Sci 2001;38(7):
92539.
[35] Wong RHC, Chau KT, Wang P. Microcracking and grain size
effect in Yuen Long marbles. Int J Rock Mech Min Sci Geomech
Abstr 1996;33(5):47985.
R.H.C. Wong et al. / International Journal of Rock Mechanics & Mining Sciences 38 (2001) 909924924