CREEP OF ROCK BASED ON LONG-TERM EXPERIMENTS

Nabarro pointed out theoretically that any polycrystalline solid yields to an applied shear stress to change its shape due to self-diffusion within crystal grains. Since 1957 Kumagai and Ito have carried out the long-term creep experiment on granite beams. Their experimental results over 24 years show that granite flows viscously without a yield stress. It may be essential that a solid has no yield stress. Long-term creep experiments on rock are described, and the theory on creep by Nabarro and Herring is discussed. The number of the covering abstract of the congress is TRIS no. 385148. (TRRL)

  • Availability:
  • Supplemental Notes:
    • This paper was presented at the Fifth International Congress on Rock Mechanics, Melbourne, Australia, 1983, Volume 1, Theme A.
  • Corporate Authors:

    AA Balkema

    P.O. Box 1675
    Rotterdam,   Netherlands  BR-3000

    Australasian Institute of Mining and Metallurgy

    204 Lygon Street
    Carlton, Victoria  Australia  3053
  • Authors:
    • Ito, H
  • Publication Date: 1983

Media Info

Subject/Index Terms

Filing Info

  • Accession Number: 00385160
  • Record Type: Publication
  • Source Agency: ARRB
  • ISBN: 90 6191 237 7
  • Report/Paper Numbers: BOOK
  • Files: ITRD, TRIS, ATRI
  • Created Date: May 30 1984 12:00AM