Authors
Abstract
A literature review revealed that most of the empirical equations introduced for determination of the uniaxial 
  compressive strength (UCS) of rocks based on the Schmidt hammer rebound number (N) are not sufficiently 
  reliable mostly due to the relatively low coefficient of correlations. This is attributed to the fact that in most 
  cases one formula is used for all types of rocks, although the density of rocks is introduced to the formulae in 
  some cases. On the other hand, if one specific relationship between N and UCS is introduced for one rock 
  type, the equation will yield a much higher coefficient of correlation. During a research program supported 
  by the Shahrood University of Technology, Iran, a third type of approach was considered. The study aimed 
  to establish a relationship between N and UCS of a rock mass under particular geological circumstances. As 
  an example, in this study, the immediate roof rock of coal seams in North-Eastern coal fields of Iran was 
  selected. In order to determine the N and UCS, a significant number of samples were selected and tested, 
  both in-situ and in the laboratory, and a new equation was established. The equation can be used to predict 
  UCS   of   the roof  rock  in   coal extracting  areas in this  zone   by  performing  simple   in-situ  Schmidt   hammer 
  tests. It is predicted that such a procedure will be feasible for other geological conditions.
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