Rock Mechanics.pdf - Mining and Blasting

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METHODS OF IN SITU STRESS DETERMINATION The minimum tangential boundary stress is obtained by superimposing this stress on that given by equation 5.11, i.e. min = 3p2 − p1 − p0 and the minimum effective boundary stress is (5.12) ′ min = 3p2 − p1 − p0 − u (5.13) The crack re-opening pressure pr corresponds to the state of borehole pressure p0 where the minimum effective boundary stress is zero, i.e. introducing pr in equation 5.13 or 3p2 − p1 − pr − u = 0 p1 = 3p2 − pr − u (5.14) Because p2 = ps, equation 5.14 confirms that the magnitudes of the major and minor plane principal stresses p1 and p2 can be determined from measurements of shut-in pressure ps and crack re-opening pressure pr. The orientation of the principal stress axes may be deduced from the position of the boundary fractures, obtained using a device such as an impression packer. The azimuth of the major principal stress axis is defined by the hole diameter joining the trace of fractures on opposing boundaries of the hole. Although hydraulic fracturing is a simple and apparently attractive stress measurement technique, it is worth recalling the assumptions implicit in the method. First, it is assumed that the rock mass is continuous and elastic, at least in the zone of influence of the hole and the hydraulically induced fractures. Second, the hole axis is assumed to be parallel to a field principal stress axis. Third, the induced fracture plane is assumed to include the hole axis. If any of these assumptions is not satisfied, an invalid solution to the field stresses will be obtained. A further limitation is that it provides only plane principal stresses, and no information on the other components of the triaxial stress field. The usual assumption is that the vertical normal stress component is a principal stress, and that it is equal to the depth stress. 5.3.5 Other methods of estimating the in situ state of stress Compared with overcoring, flatjacks and hydraulic fracturing, some other methods of estimating the in situ state of stress are attractive by virtue of the relative ease with which the raw data for the stress determination can be recovered. Of particular interest in this regard are methods based on borehole breakouts, stress history gauging through the Kaiser effect, and differential strain curve analysis or deformation rate analysis. The borehole breakout method described by Zoback et al. (1985) relies on the state of stress around a borehole being sufficient to cause compressive fracture at preferred locations around the hole boundary. Assuming a principal stress direction is parallel to the borehole axis and that the principal stress field in the plane perpendicular to the hole axis is anisotropic, the Kirsch equations and a knowledge of the rock material 155
PRE-MINING STATE OF STRESS strength properties allow an estimate of the state of stress immediately outside the zone of influence of the borehole. Widely used in the petroleum industry for estimating the state of stress in deep reservoirs, the method is reviewed in detail by Zoback et al. (2003). An example of its application in hard rock is provided by Paillet and Kim (1987). Development and application of a method for in situ stress measurement based on the Kaiser effect is described by Villaescusa et al. (2002). The Kaiser effect is an expression of the immediately preceding maximum stress to which a specimen of rock has been subjected, and provides a method of estimating the recent stress history of a core sample recovered from a borehole. For a specimen containing microcracks, such as brittle rock, uniaxial loading is aseismic until a stress threshold is reached characteristic of the earlier stress magnitude it experienced. Application of the Kaiser effect in estimating the complete stress tensor relies on a capacity to determine reliably the magnitudes of the preceding normal stresses applied to the specimen in various directions. This is done by monitoring the emission of acoustic pulses during loading of small undercores recovered from the larger, oriented drill core taken from the ground. By Kaiser-effect gauging of preceding stresses in six undercores in six mutually independent orientations, it is possible to invert the normal stresses to recover the field stresses which the large core experienced in situ. The advantage of the method is the relative convenience and ease of application and the related low cost. Anelastic strain recovery (Voight, 1968) exploits the relaxation which a rock core experiences after it is isolated from the stressed host rock mass. The time-dependent strains are measured with strain gauges, the principal strains calculated, and the total strains are estimated by assuming direct proportionality between total strains and the anelastic strains. Differential strain curve analysis (Roegiers, 1989) or deformation rate analysis (Villaescusa et al., 2002) are similar in principle to Kaiser effect gauging of the recent stress history of a sample of rock. When a core is taken from the ground, relaxation of normal stress allows microcracks to open. In axial loading of undercores taken from a larger core, closure of open microcracks is indicated by a clear change in the slope of the axial stress-normal strain plot. The related value of the applied normal stress is taken to correspond to the normal stress existing in the ground immediately prior to recovery of the core. If closure stresses are determined for undercores taken in six mutually independent orientations, then as for Kaiser-effect gauging, it is possible to invert the stress data to recover the field principal stresses and their orientations. 5.4 Presentation of in situ stress measurement results The product of a stress measurement exercise is the set of six components of the field stress tensor, usually expressed relative to a set of local axes for the measurement hole. These yield the stress components expressed relative to the global axes by a simple transformation. The principal stress magnitudes and orientations are then determined from these quantities using the methods described in Chapter 2. If a single determination is made of the field stress tensor, the orientations of the principal stress axes can be plotted directly on to a stereonet overlay as shown in Figure 5.9. The value of this procedure is that the required mutual orthogonality of the principal 156
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Rock Mechanics
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Rock Mechanics for underground mini
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Contents Preface to the third editi
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CONTENTS 9 Excavation design in blo
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CONTENTS ix Appendix A Basic constr
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PREFACE TO THE THIRD EDITION Mining
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PREFACE TO THE SECOND EDITION In th
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PREFACE TO THE FIRST EDITION design
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ACKNOWLEDGEMENTS Safety in Mines Re
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Figure 1.1 (a) Pre-mining condition
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ROCK MECHANICS AND MINING ENGINEERI
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Figure 1.4 Principal features of a
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10 Figure 1.5 Definition of activit
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Figure 1.7 Components and logic of
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Figure 2.1 (a) A finite body subjec
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Figure 2.2 Free-body diagram for es
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STRESS AND INFINITESIMAL STRAIN As
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STRESS AND INFINITESIMAL STRAIN In
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Figure 2.3 Free-body diagram for de
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Figure 2.5 Problem geometry for det
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Figure 2.7 Rigid-body rotation of a
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STRESS AND INFINITESIMAL STRAIN the
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STRESS AND INFINITESIMAL STRAIN str
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⎡ ⎢ ⎣ xx yy zz xy yz zx STRES
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Figure 2.11 Cylindrical polar coord
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STRESS AND INFINITESIMAL STRAIN fre
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Figure 2.13 Construction of a Mohr
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STRESS AND INFINITESIMAL STRAIN fun
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3 Rock Figure 3.1 Sidewall failure
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Figure 3.2 Jointing in a folded str
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Figure 3.5 Diagrammatic longitudina
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Figure 3.7 Discontinuity spacing hi
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Figure 3.9 Illustration of persiste
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Figure 3.11 Typical roughness profi
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ROCK MASS STRUCTURE AND CHARACTERIS
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Figure 3.17 Sample number vs. preci
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Figure 3.19 Diagrammatic illustrati
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Figure 3.20 Computerised depiction
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Figure 3.23 Stereographic projectio
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Figure 3.26 Polar stereographic net
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Figure 3.28 Contours of pole concen
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Figure 3.30 Geological Strength Ind
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Figure 4.1 Idealised illustration o
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ROCK STRENGTH AND DEFORMABILITY wit
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Figure 4.4 Influence of end restrai
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ROCK STRENGTH AND DEFORMABILITY whe
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Figure 4.8 Principle of closed-loop
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Figure 4.12 Two classes of stress-
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Figure 4.14 Point load test apparat
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Figure 4.15 Biaxial compression tes
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Figure 4.18 Results of triaxial com
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Page 123 and 124: Figure 4.23 Coulomb strength envelo
Page 125 and 126: Figure 4.25 Extension of a preexist
Page 127 and 128: Figure 4.29 The three basic modes o
Page 129 and 130: Figure 4.30 Normalised peak strengt
Page 131 and 132: ROCK STRENGTH AND DEFORMABILITY Tab
Page 133 and 134: Figure 4.32 The normality condition
Page 135 and 136: Figure 4.33 Variation of peak princ
Page 137 and 138: Figure 4.35 Direct shear test confi
Page 139 and 140: Figure 4.37 Shear stress-shear disp
Page 141 and 142: Figure 4.40 Peak and residual effec
Page 143 and 144: Figure 4.43 Effect of shearing dire
Page 145 and 146: Figure 4.45 Relations between norma
Page 147 and 148: Figure 4.47 Coulomb friction, linea
Page 149 and 150: ROCK STRENGTH AND DEFORMABILITY whe
Page 151 and 152: Figure 4.49 Composite peak strength
Page 153 and 154: Figure 4.50 Hoek-Brown peak strengt
Page 155 and 156: Figure 4.52 Determination of the Yo
Page 157 and 158: ROCK STRENGTH AND DEFORMABILITY 4 A
Page 159 and 160: 5 Pre-mining Figure 5.1 Method of s
Page 161 and 162: Figure 5.2 The effect of irregular
Page 163 and 164: PRE-MINING STATE OF STRESS surround
Page 165 and 166: PRE-MINING STATE OF STRESS induced
Page 167 and 168: Figure 5.5 (a) Definition of hole l
Page 169 and 170: Figure 5.6 (a) Core drilling a slot
Page 171: Figure 5.7 Principles of stress mea
Page 175 and 176: PRE-MINING STATE OF STRESS A second
Page 177 and 178: PRE-MINING STATE OF STRESS by the e
Page 179 and 180: PRE-MINING STATE OF STRESS extend i
Page 181 and 182: PRE-MINING STATE OF STRESS (d) Dete
Page 183 and 184: METHODS OF STRESS ANALYSIS quantita
Page 185 and 186: METHODS OF STRESS ANALYSIS It is in
Page 187 and 188: Figure 6.2 A thick-walled cylinder
Page 189 and 190: METHODS OF STRESS ANALYSIS For the
Page 191 and 192: Figure 6.3 Problem geometry, coordi
Page 193 and 194: Figure 6.4 Problem geometry, coordi
Page 195 and 196: METHODS OF STRESS ANALYSIS When the
Page 197 and 198: Figure 6.5 Superposition scheme dem
Page 199 and 200: METHODS OF STRESS ANALYSIS The disc
Page 201 and 202: Figure 6.7 Development of a finite
Page 203 and 204: METHODS OF STRESS ANALYSIS Solution
Page 205 and 206: Figure 6.8 A simple finite element
Page 207 and 208: Figure 6.9 A schematic representati
Page 209 and 210: METHODS OF STRESS ANALYSIS block ce
Page 211 and 212: METHODS OF STRESS ANALYSIS where ˚
Page 213 and 214: METHODS OF STRESS ANALYSIS The prin
Page 215 and 216: EXCAVATION DESIGN IN MASSIVE ELASTI
Page 217 and 218: Figure 7.2 A logical framework for
Page 219 and 220: Figure 7.3 (a) Axisymmetric stress
Page 221 and 222: Figure 7.6 A plane of weakness, ori
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Figure 7.8 A flat-lying plane of we
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Figure 7.10 Shear stress/normal str
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Figure 7.12 Ovaloidal opening in a
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Figure 7.15 States of stress at sel
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Figure 7.16 Prediction of the exten
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Figure 7.18 Contour plots of princi
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Figure 7.19 Problem geometry for de
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EXCAVATION DESIGN IN MASSIVE ELASTI
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EXCAVATION DESIGN IN MASSIVE ELASTI
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8 Excavation Figure 8.1 An excavati
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EXCAVATION DESIGN IN STRATIFIED ROC
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Figure 8.4 Experimental apparatus f
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Figure 8.7 Free body diagrams and n
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Figure 8.8 Assumed distributions of
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Figure 8.9 Flow chart for the deter
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Figure 8.10 Normalised arch thickne
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EXCAVATION DESIGN IN STRATIFIED ROC
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Figure 8.11 Normalised deflection a
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9 Excavation Figure 9.1 Generation
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Figure 9.3 (a) A finite, non-tapere
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(a) (b) Figure 9.4 (a) Vertical cro
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(a) (b) (c) EP EP Reference circle
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Figure 9.10 JP 100 is the only JP w
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Figure 9.12 Traces of the views of
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EXCAVATION DESIGN IN BLOCKY ROCK In
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Figure 9.14 Free-body diagrams of a
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EXCAVATION DESIGN IN BLOCKY ROCK di
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Figure 9.16 Symmetrical wedge in th
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Figure 9.17 (a) Geometry for determ
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Figure 9.18 Problem geometry demons
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Figure 9.20 Cut-and-fill stope mine
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Figure 9.22 Chart to determine fact
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EXCAVATION DESIGN IN BLOCKY ROCK Th
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Figure 10.1 (a) Pre-mining state of
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Figure 10.3 (a) Dynamic loading of
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Figure 10.5 (a) Pre-mining and (b)
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Figure 10.6 Problem definition and
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ENERGY, MINE STABILITY, MINE SEISMI
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Figure 10.9 Force and stress compon
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Figure 10.12 Distribution of radial
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Figure 10.15 Problem geometry for d
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Figure 10.17 (a) Schematic represen
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Figure 10.20 Elastic/post-peak stif
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Figure 10.24 Relation between frequ
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Figure 10.28 Six possible ways that
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Figure 10.29 First motions for P an
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11Rock support and reinforcement 11
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Figure 11.1 (a) Hypothetical exampl
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Figure 11.4 Non-linear support reac
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Figure 11.5 Idealised elastic-britt
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Figure 11.6 Calculated required sup
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ROCK SUPPORT AND REINFORCEMENT The
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Figure 11.9 Ground reaction curves
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Figure 11.12 Use of grouted reinfor
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ROCK SUPPORT AND REINFORCEMENT If,
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Figure 11.16 Local reinforcement ac
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Figure 11.18 Typical working sketch
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Figure 11.19 Permanent support and
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Figure 11.22 Basis of natural coord
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Figure 11.24 Distributions of (a) s
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Figure 11.26 Resin grouted rockbolt
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Figure 11.28 Alternative methods of
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ROCK SUPPORT AND REINFORCEMENT Tabl
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Figure 11.31 Toussaint-Heintzmann y
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MINING METHODS AND METHOD SELECTION
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Figure 12.2 Elements of a supported
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Figure 12.6 Schematic layout for bi
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Figure 12.8 Layout for shrink stopi
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Figure 12.9 Schematic layout for VC
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Figure 12.11 Key elements of longwa
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Figure 12.13 Mining layout for tran
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13 Figure 13.1 Schematic illustrati
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Figure 13.3 Layout of barrier pilla
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Figure 13.5 Principal modes of defo
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Figure 13.8 Geometry for tributary
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PILLAR SUPPORTED MINING METHODS str
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Figure 13.10 Distribution of vertic
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Figure 13.12 Pillar behaviour domai
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PILLAR SUPPORTED MINING METHODS Lun
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Figure 13.15 Options in the design
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Figure 13.17 Relation between yield
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Figure 13.19 Model of yield of coun
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Figure 13.20 North-south vertical c
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Figure 13.23 Stope-and-pillar layou
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Figure 13.25 Calibrated stability c
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PILLAR SUPPORTED MINING METHODS wor
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Figure 13.28 Pillar performance, de
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Figure 13.29 (a) Stope and pillar l
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Figure 13.31 (a) Plane strain analy
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PILLAR SUPPORTED MINING METHODS Pan
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14 Artificially supported mining me
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ARTIFICIALLY SUPPORTED MINING METHO
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Figure 14.2 Simplified view of stru
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Figure 14.5 Confined block model fo
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Figure 14.7 Crown and sidewall stre
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Figure 14.10 Sublevel open stoping
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Figure 14.12 Some applications of c
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15 Longwall and caving mining metho
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Figure 15.2 Shear stress drop in th
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LONGWALL AND CAVING MINING METHODS
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Figure 15.6 Hydraulic prop reaction
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Figure 15.7 Development and extract
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Figure 15.8 Vertical stress redistr
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Figure 15.11 Distribution of observ
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Figure 15.13 Plan view of microseis
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Figure 15.16 Ground-support interac
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Figure 15.18 Roadway support and re
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Figure 15.25 Comparison of isolated
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Figure 15.26 Geometry of a sublevel
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Figure 15.28 Theoretical determinat
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Figure 15.31 Deterioration of a cro
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Figure 15.32 Distinct element simul
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Figure 15.34 Extended Mathews stabi
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Figure 15.36 Comparison of postand
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Figure 15.39 Idealised plan illustr
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Figure 15.41 Idealised vertical sec
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Figure 15.42 Vertical slice through
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16 Figure 16.1 Trough subsidence ov
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MINING-INDUCED SURFACE SUBSIDENCE c
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Figure 16.4 North-south section, At
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Figure 16.6 (a) Rectangular block g
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MINING-INDUCED SURFACE SUBSIDENCE f
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Figure 16.8 Relation between stope
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MINING-INDUCED SURFACE SUBSIDENCE M
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MINING-INDUCED SURFACE SUBSIDENCE
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Figure 16.14 Chart developed to est
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Figure 16.16 Progressive hangingwal
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Figure 16.19 Idealised model used i
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Figure 16.21 Longitudinal section,
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MINING-INDUCED SURFACE SUBSIDENCE t
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MINING-INDUCED SURFACE SUBSIDENCE w
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MINING-INDUCED SURFACE SUBSIDENCE F
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Figure 16.25 Subsidence troughs pre
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Figure 16.28 Predicted and measured
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17 Blasting mechanics 17.1 Blasting
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Figure 17.1 An empirical matching o
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Figure 17.2 A finite difference mod
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Figure 17.4 Reflection of a cylindr
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BLASTING MECHANICS means that no ci
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Figure 17.8 Layout of blast holes i
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Figure 17.9 Influence of field stat
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Figure 17.11 Generation of surface
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BLASTING MECHANICS The components o
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BLASTING MECHANICS amplitudes of th
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BLASTING MECHANICS 17.9 Evaluation
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Figure 17.15 (a) Schematic cross se
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BLASTING MECHANICS in Figure 17.17,
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MONITORING ROCK MASS PERFORMANCE (a
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MONITORING ROCK MASS PERFORMANCE su
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MONITORING ROCK MASS PERFORMANCE Ta
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Figure 18.2 The Distometer ISETH, a
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Figure 18.5 Self-inductance multipl
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MONITORING ROCK MASS PERFORMANCE is
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Figure 18.9 Biaxial vibrating wire
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MONITORING ROCK MASS PERFORMANCE me
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Figure 18.12 Cross section at 6650N
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Figure 18.13 Examples of convergenc
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Figure 18.15 Longitudinal section l
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Figure 18.16 (Cont.) MONITORING ROC
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Appendix A Basic constructions usin
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Figure A.3 Determining the angle be
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APPENDIX A USE OF HEMISPHERICAL PRO
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APPENDIX B STRESSES AND DISPLACEMEN
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Figure A.6 Axisymmetric tunnel prob
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Figure A.9 Bolt load-extension curv
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APPENDIX D LIMITING EQUILIBRIUM ANA
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ANSWERS TO PROBLEMS 2 (a) 0.087 - 0
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ANSWERS TO PROBLEMS 3 wp = 38.6 m,
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REFERENCES Symp. & 17th Tunn. Assn
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REFERENCES Brady, B. H. G. and Bray
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REFERENCES Collier, P. A. (1993) De
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REFERENCES Drescher, A. and Vardoul
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REFERENCES Gustafsson, P. (1998) Wa
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REFERENCES Hood, M. and Brown, E. T
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REFERENCES Kaiser, P. K. and Tannan
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REFERENCES Lorig, L. J. and Brady,
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REFERENCES Ortlepp, W. D. (1994) Gr
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REFERENCES Rojas, E., Molina, R. an
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REFERENCES Spottiswoode, S. M. and
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REFERENCES Villaescusa, E., Windsor
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Index Page numbers appearing in bol
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INDEX Coulomb (cont.) parameters 96
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INDEX Excavation (cont.) support ra
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INDEX Jaeger’s plane of weakness
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INDEX Panel caving 470-2, 473, 474,
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INDEX Seismic (cont.) moment 306, 3
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INDEX Strength (cont.) residual 86,
Page 645:
INDEX United States (USA) 395, 396,
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