RECURSIVE BIFURCATION AS SOURCES OF COMPLEXITY IN SOIL SHEARING BEHAVIOR
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概要
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This paper identifies recursive symmetry-breaking bifurcation phenomena as major sources of complexity in soil shearing behavior. By means of the group-theoretic bifurcation theory, a complete rule for bifurcation is presented for a cylindrical domain made up of uniform geotechnical materials, such as soil, sand, and rock. The bifurcation behavior of soil has two major phases : i) the formation of diamond, oblique stripe and echelon modes with high spatial frequencies at an earlier stage, and ii) the deformation pattern change and shear-band formation at a later stage. This behavior is indeed a recursive loss of symmetry that enlarges and changes deformation patterns. The mathematical knowledge of recursive bifurcation provides an overall view of the soil behavior.
- 社団法人地盤工学会の論文
- 1997-09-15
著者
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室田 一雄
Research Institute for Mathematical Sciences, Kyoto University
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池田 清宏
Dept. of Civ. Engrg., Tohoku Univ.
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- RECURSIVE BIFURCATION AS SOURCES OF COMPLEXITY IN SOIL SHEARING BEHAVIOR
- BIFURCATION AS SOURCES OF UNCERTAINTY IN SOIL SHEARING BEHAVIOR