EFFECT OF DENSITY ON THE DRAINED DEFORMATION BEHAVIOR OF SHIRASU (VOLCANIC SANDY SOIL) UNDER THREE-DIMENSIONAL STRESSES
スポンサーリンク
概要
- 論文の詳細を見る
The effect of density on the drained deformation properties of pyroclastic flow deposits, so called Shirasu, distributed in the Southern Kyushu, Japan, was investigated by using a triaxial testing apparatus with independent stress-control systems. Hydrostatic compression tests and radial shear tests maintaining a constant mean principal stress were performed on Shirasu specimens prepared by pluviation through water. The test results indicate that the reconstituted specimens of Shirasu were characterized by an inherent cross-anisotropy and a density-dependence of their deformation properties. In general, the specimens had a low compressibility and a high expansibility in the direction of specimen-deposition compared with the direction along the bedding plane. The maximum shear strength in the identical stress state having different stress-path occurred when the major principal stress was applied to the direction of the specimen-deposition. The change of the deformation-strength properties was caused by the change of strain increment ratio which depends on the dilatancy occurring under the different stress path.
- 社団法人地盤工学会の論文
- 1987-03-15
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
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- 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"