乾燥した岩石のダイラタンシーに関する理論的研究

書誌事項

タイトル別名
  • Theoretical Study on Dilatancy of Dry Rock.
  • カンソウシタ ガンセキ ノ ダイラタンシー ニ カンスル リロンテキ ケンキュ

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抄録

Dilatancy of rock is interpreted as the accumulation of microscopic failures induced by deviatric stress, based on a great number of experiment and observation. However, the ability to express the quantitative relationship between stress condition and dilatant strain caused by such micro-scopic failure requires more research. In this paper, on the assumption that open cracks grow in consequence of failures, the equations which describe the stress-strain relationship were derived by applying the fracture mechanics.<br>The conclusions are summarized as follows;<br>(1) Secondary cracks generated by deviatric stress grow almost in the direction of maximum compressive stress.<br>(2) Dilatant strain caused by the crack growth is in inverse proportion to minimum compressive stress.

収録刊行物

  • 材料

    材料 41 (466), 1068-1074, 1992

    公益社団法人 日本材料学会

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