DRAINED DEFORMATION-STRENGTH CHARACTERISTICS OF LOOSE SHIRASU (VOLCANIC SANDY SOIL) UNDER THREE DIMENSIONAL STRESSES
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概要
- 論文の詳細を見る
Pyroclastic flow deposits distributed in southern Kyushu, Japan, are called Shirasu. In order to investigate the drained deformation-strength behaviour of Shirasu in disturbed state, hydrostatic compression tests and radial shear tests using triaxial testing apparatus with independent stress-control systems were performed on cubical specimens of loose Shirasu under three dimensional stresses. The thirteen radial shear stress paths on the deviatoric plane classified into five groups were given to the specimens. The test results indicated that Shirasu specimens prepared by pluviation through water had an inherent cross-anisotropy. In the hydrostatic compression tests, the anisotropic behaviour occurred in compressive strains less than 10^<-2>. In the radial shear tests, deformation-strength behaviour was dependent on the relationship between the direction of the specimen-deposition and the directions of the major and minor principal stresses. The change of the shear behaviour was caused by the change of dilatancy, the strain increment ratio, with the radial shear stress path.
- 社団法人地盤工学会の論文
- 1985-03-15
著者
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春山 元寿
Department of Ocean Civil Engineering, Kagoshima University
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春山 元寿
Department Of Ocean Civil Engineering Kagoshima University
関連論文
- えびの・吉松地域に分布するシラスのセン断特性について
- 乱したシラスの排水セン断特性について
- ANISOTROPIC DEFORMATION-STRENGTH PROPERTIES OF SOFT SEDIMENTARY ROCK "SHIRASU" ORIGINATED FROM PYROCLASTIC FLOWS
- EFFECT OF DENSITY ON THE DRAINED DEFORMATION BEHAVIOR OF SHIRASU (VOLCANIC SANDY SOIL) UNDER THREE-DIMENSIONAL STRESSES
- DRAINED DEFORMATION-STRENGTH CHARACTERISTICS OF LOOSE SHIRASU (VOLCANIC SANDY SOIL) UNDER THREE DIMENSIONAL STRESSES
- ANISOTROPIC DEFORMATION-STRENGTH CHARACTERISTICS OF AN ASSEMBLY OF SPHERICAL PARTICLES UNDER THREE DIMENTIONAL STRESSES
- ANISOTROPIC DEFORMATION-STRENGTH CHARACTERISTICS OF AN ASSEMBLY OF SPHERICAL PARTICLES UNDER THREE DIMENSIONAL STRESSES
- A METHOD OF THE IDENTIFICATION AND CLASSIFICATION OF PYROCLASTIC FLOW DEPOSITS DUE TO HARDNESS
- DEFORMATION CHARACTERISTICS OF HIGHLY COMPRESSIBLE SAND "SHIRASU"