CHANGES IN IN SITU ULTRASONIC PROPERTIES OF ROCK ON STRAIN RELAXATION

In situ and laboratory measurements of ultrasonic velocity have been compared to test for the effect of strain relaxation on rock properties. For granites, the larger changes in compressional-wave velocity (vp) correlate with higher in situ stresses, the maximum vp being parallel to the directory of maximum compressive stress. For sedimentary rocks, the relation between changes in vp and in situ stress is dependent on lithology. In sandstone, the direction associated with the maximum decrease in vp accompanying strain relaxation is parallel to the maximum compressive stress. Limestone is virtually isotropic with little decrease in vp on strain relaxation. (Author/TRRL)

  • Availability:
  • Corporate Authors:

    Pergamon Press, Incorporated

    Headington Hill Hall
    Oxford OX30BW,    
  • Authors:
    • Engelder, T
    • Plumb, R
  • Publication Date: 1984-4

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Filing Info

  • Accession Number: 00386614
  • Record Type: Publication
  • Source Agency: Transport Research Laboratory
  • Files: ITRD, TRIS
  • Created Date: Jul 30 1984 12:00AM