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10: EVALUATION TECHNIQUES  245


                 or  in situ. Subjective data helps with the  10.5.1  Quantitative assessment of rock
                 decision making fairly early in a project, but
                 these data will always need quantification. It  There are numerous good textbooks which
                 is therefore necessary to study and record the  cover the properties of rocks from an engineer-
                 direction and properties of joints, cleavage,  ing point of view (Krynine & Judd 1957,
                 cleats, bedding fissures, and faults, and to study  Goodman 1976, 1989, Farmer 1983, Brady &
                 and record the mechanical properties (mechan-  Brown 1985), the latter reference being particu-
                 ics of deformation and fracture under load),  larly relevant to underground mining. The
                 petrology, and fabric of the rock between the  main properties which are used in the engineer-
                 discontinuities.                             ing classification of rocks for their quantitative
                   It is clear from the above that structural  assessment are porosity, permeability, specific
                 information is extremely important in mine   gravity (bulk density), durability and slakabil-
                 planning. In the initial phases of a program  ity, sonic velocity, and rock strength.
                 most of the structural data come from core.    Porosity and permeability are important in
                 The geologist can log fracture spacing, attitude,  the assessment of subsurface water. Specific
                 and fracture infill at the rig site. A subjective  gravity is required to determine the mass of
                 description of the quality of the core can be  the rock. Durability and slakability tests reveal
                 given using Rock Quality Designation (RQD)   what affect alternate wetting and drying will
                 (Table 10.8). Pieces of core greater than 10 cm  have on surface or near-surface exposures.
                 are measured and their length summed. This is  Under conditions of seasonal humidity some
                 divided by the total length of the core run and  rocks have been known to disaggregate com-
                 expressed as a percentage. A low percentage  pletely (Obert & Duval 1967). Sonic velocity
                 means a poor rock while a high percentage    tests give an indication of the fracture intensity
                 means a good quality rock.                   of the rock. Probably the most important prop-
                   Bieniawski (1976) developed a geomechan-   erty of rock is its strength.
                 ical classification scheme using five criteria:
                 strength of the intact rock, RQD, joint spacing,  Rock strength
                 conditions of the joints, and ground water con-
                 ditions. He assigned a rating value to each of  The fundamental parameters that define rock
                 these variables, and by summing the values   strength are stress and strain, and the rela-
                 of the ratings determined for the individual  tionship between stress and strain. Stress (σ)
                 properties he obtained an overall rock mass  is a force acting on a unit area. It may be hydro-
                 rating (RMR). Determination of the RMR of an  static when the force is equal in all direc-
                 unsupported excavation, for example, can be  tions, compressional when the force is directed
                 used to determine the stand up time of that  towards a plane, tensional when directed away
                 excavation.                                  from a plane, torsional (twisting), or shear
                   In order to provide information that will  stress (τ) when the forces are directed towards
                 assist the geotechnical and mining engineers it  each other but not necessarily in line. Strain
                 is necessary to understand the stress–strain  (ε) is the response of a material to stress by pro-
                 characteristics of the rocks. This is especially  ducing a deformation, i.e. a change in shape,
                 important in relation to the mining method   length, or volume. The linear relationship
                 that is proposed for the rocks, the way in which  between stress and strain is known as Hooke’s
                 the rocks will respond in the long term to sup-  law and the constant (E) connecting them is
                 port (in underground mining), or in deep open  Young’s modulus. It is also called the modulus
                 pits how deformation characteristics affect the  of elasticity, and gives a measure of stiffness.
                 stability of a slope. As these rock properties  The strength of a rock sample can be tested
                 become better understood, it is possible for the  (usually in the laboratory) in several ways.
                 geotechnical and mining engineers to improve  Unconfined (uniaxial) compressive strength
                 the design of underground mines, the way in  is measured when a cylinder (usually core) of
                 which excavations are supported, the effici-  rock is loaded to a point of failure. The load im-
                 ency of mining machinery, and the safety of the  mediately prior to failure indicates the rock’s
                 mine environment.                            strength. Tensile strength is measured by
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