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Rock Mechanics.pdf - Mining and Blasting

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BEHAVIOUR OF DISCONTINUOUS ROCK MASSES<br />

illustrate the criterion’s application in practice. A further update was given by Hoek<br />

et al. (2002). The summary of the criterion given here is based on these accounts <strong>and</strong><br />

those of Marinos <strong>and</strong> Hoek (2000) <strong>and</strong> Brown (2003).<br />

In effective stress terms, the generalised Hoek-Brown peak strength criterion for<br />

jointed rock masses is given by:<br />

′ 1 = ′ 3 + mbc ′ 3 + s 2a c<br />

(4.37)<br />

where mb is the reduced value of the material constant mi (see equation 4.25) for the<br />

rock mass, <strong>and</strong> s <strong>and</strong> a are parameters which depend on the characteristics or quality<br />

of the rock mass. The values of mb <strong>and</strong> s are related to the GSI for the rock mass (see<br />

section 3.7.4) by the relations<br />

<strong>and</strong><br />

mb = mi exp{(GSI − 100)/(28 − 14D)} (4.38)<br />

s = exp{(GSI − 100)/(9 − 3D)} (4.39)<br />

where D is a factor which depends on the degree to which the rock mass has been<br />

disturbed by blasting or stress relaxation. D varies from 0 for undisturbed in situ rock<br />

masses to 1.0 for very disturbed rock masses. For good quality blasting, it might be<br />

expected that D ≈ 0.7.<br />

In the initial version of the Hoek-Brown criterion, the index a took the value 0.5 as<br />

shown in equation 4.25. After a number of other changes, Hoek et al. (2002) expressed<br />

the value of a which applies over the full range of GSI values as the function:<br />

a = 0.5 + (exp −GSI/15 − exp −20/3 )/6 (4.40)<br />

Note that for GSI > 50, a ≈ 0.5, the original value. For very low values of GSI, a →<br />

0.65.<br />

The uniaxial compressive strength of the rock mass is obtained by setting ′ 3 to<br />

zero in equation 4.37 giving<br />

cm = cs a<br />

(4.41)<br />

Assuming that the uniaxial <strong>and</strong> biaxial tensile strengths of brittle rocks are approximately<br />

equal, the tensile strength of the rock mass may be estimated by putting<br />

′ 1 = ′ 3 = tm in equation 4.37 to obtain<br />

tm =−s c/mb<br />

(4.42)<br />

The resulting peak strength envelope for the rock mass is as illustrated in Figure 4.50.<br />

Because analytical solutions <strong>and</strong> numerical analyses of a number of mining rock<br />

mechanics problems use Coulomb shear strength parameters rather than principal<br />

stress criteria, the Hoek-Brown criterion has also been represented in shear stresseffective<br />

normal stress terms. The resulting shear strength envelopes are non-linear<br />

<strong>and</strong> so equivalent shear strength parameters have to be determined for a given normal<br />

stress or effective normal stress, or for a small range of those stresses (Figure 4.50).<br />

135

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