Engineering Rock Mechanics

(Jacob Rumans) #1

340 Underground excavation instability mechanisms


in terms of kinematics may be conveniently conducted through the use of
hemispherical projection techniques. Initially the analysis will be limited
to horizontal roofs (so that the plane of the projection is parallel to the
excavation surface); later the projection will be inclined to account for any
orientation of the excavation periphery.
Given that a tetrahedral block exists, there are three kinematic
possibilities to be examined: the block falls from the roof; the block slides
(either along the line of maximum dip of a discontinuity, or along the line
of intersection of two discontinuities); or the block is stable.


Falling. Falling occurs when a block detaches from the roof of an
excavation without sliding on any of the bounding discontinuity planes.
In the case of gravitational loading, the direction of movement is vertically
downwards. This is represented on the projection as a line with a dip of
90°, i.e. at the centre of the projection. Thus, if this point falls within the
spherical triangle formed by the bounding discontinuities, falling is
kinematically feasible, as illustrated in Fig. 19.1.


Sliding. In Sections 18.1.1 and 18.1.2, plane and wedge instability analyses
for a surface slope were discussed. A similar method is used here to
consider blocks sliding from the roof, either on one discontinuity plane (as
plane failure) or on a line of intersection (as wedge failure), as illustrated
in Fig. 19.2 by consideration of the spherical triangle and whether any part
of it has a dip greater than the angle of friction.
Assuming that both discontinuity planes have the same friction angle,
there are only two candidates for the sliding direction: either the line of
maximum dip of one plane, or the line of intersection of two planes. No
other part of the spherical triangle represents a line of steeper dip than
these candidates.
Not all lines of maximum dip can be candidates for the sliding direction.
An example is afforded by the line of maximum dip, A, of plane 3 in


Figure 19.1


Perimeter of projection

movement due to gra

Kinematic identification of a falling block.
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