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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.

    R.H.C. Wong et al. / International Journal of Rock Mechanics & Mining Sciences 38 (2001) 909924912

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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


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