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Rock Mechanics.pdf - Mining and Blasting

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AN INFINITE LINE LOAD<br />

B.2 An infinite line load<br />

For a line load, of intensity px per unit length, applied at the xy co-ordinate origin,<br />

in the x direction, <strong>and</strong> tensile normal stresses reckoned positive, etc.<br />

px x<br />

xx =−<br />

4(1 − ) r 2<br />

<br />

2 2x<br />

(1 − 2) +<br />

r 2<br />

<br />

px x<br />

yy =−<br />

4(1 − ) r 2<br />

<br />

−(1 − 2) + 2y2<br />

r 2<br />

<br />

px y<br />

xy =−<br />

4(1 − ) r 2<br />

<br />

2 2x<br />

(1 − 2) +<br />

r 2<br />

<br />

2<br />

<br />

px x<br />

ux =<br />

− (3 − 4) ℓn r<br />

8G(1 − ) r 2<br />

px xy<br />

u y =<br />

8 G(1 − ) R2 where r 2 = x 2 + y 2 .<br />

Appendix C Calculation sequences for<br />

rock–support interaction analysis<br />

C.1 Scope<br />

The stepwise calculation sequences presented in this appendix permit rock–support<br />

interaction analyses to be carried out for the axisymmetric problem defined in Figure<br />

A.6. Further details of these analyses are given by Daemen (1975), Hoek <strong>and</strong> Brown<br />

(1980), <strong>and</strong> Brown et al. (1983).<br />

C.2 Required support line calculations<br />

Solution using the elastic-brittle rock mass behaviour model of Figure 11.5<br />

Input data<br />

c = uniaxial compressive strength of intact rock pieces;<br />

m, s = material constants for the original rock mass;<br />

E, = Young’s modulus <strong>and</strong> Poisson’s ratio of the original rock mass;<br />

mr, sr = material constants for the broken rock mass;<br />

f = gradient of −ε p<br />

3 vs. εp<br />

1 line (Figure 11.5);<br />

p = hydrostatic field stress;<br />

ri = internal tunnel radius.<br />

575

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