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Rock Mechanics.pdf - Mining and Blasting

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ROCK MASS STRUCTURE AND CHARACTERISATION<br />

be carried out in two orthogonal directions, usually horizontal <strong>and</strong> vertical. Ideally,<br />

equal total horizontal <strong>and</strong> vertical scanline lengths should be used, but this is often<br />

difficult to achieve in practice.<br />

The value xi0 given by equation 3.6 will be the true normal spacing of the discontinuities<br />

only when the face is normal to the discontinuities. If the scanline intersects<br />

N sets of discontinuities, the discontinuity frequency measured along the scanline is<br />

given by<br />

=<br />

N<br />

i=1<br />

i0 cos i<br />

(3.7)<br />

where i0 is the frequency of set i measured along the normal to the discontinuities<br />

<strong>and</strong> i is the acute angle between the normal <strong>and</strong> the scanline.<br />

Hudson <strong>and</strong> Priest (1983) showed that if i, i are the trend (the azimuth of the<br />

vertical plane containing the line) <strong>and</strong> plunge (the acute angle measured in a vertical<br />

plane between the downward directed end of the line <strong>and</strong> the horizontal) of the normal<br />

to the ith discontinuity set <strong>and</strong> s, s are the trend <strong>and</strong> plunge of the scanline, the<br />

discontinuity frequency measured along the scanline is<br />

where<br />

= A sin s cos s + B cos s cos s + C sin s<br />

A =<br />

B =<br />

C =<br />

N<br />

i=1<br />

N<br />

i=1<br />

N<br />

i=1<br />

i0 sin i cos i<br />

i0 cos i cos i<br />

i0 sin i<br />

(3.8)<br />

Priest <strong>and</strong> Hudson (1981) have pointed out that there is also a natural variability in<br />

the mean discontinuity spacing ¯x computed as<br />

¯x =<br />

n<br />

xi<br />

i=1<br />

n<br />

(3.9)<br />

where xi is the ith discontinuity spacing measurement along a scanline of length L<br />

yielding n values. The question arises as to what value n should take in order that<br />

the value of ¯x can be estimated with acceptable precision. In theory, a plot of the<br />

frequency of occurrence of values of ¯x determined from several scanline surveys in<br />

the one direction with different values of n, should have a normal distribution (Figure<br />

3.16a). It is known that, in this case, a proportion (z) of the different scanlines<br />

will yield a mean value within ± z/ √ n of the population mean (Figure 3.16b)<br />

where z is the st<strong>and</strong>ard normal variable associated with a certain confidence level<br />

<strong>and</strong> is the st<strong>and</strong>ard deviation of the population of values. Tabulations of values of<br />

62

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