ON STRESS-DILATANCY RELATION OF SAND IN SIMPLE SHEAR TEST
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概要
- 論文の詳細を見る
rights: 社団法人地盤工学会rights: 本文データは学協会の許諾に基づきCiNiiから複製したものであるrelation: IsVersionOf: http://ci.nii.ac.jp/naid/110003913497/A stress-dilatancy relation of sand is proposed on the basis of the experimental fact that the principal stress axes and the principal strain increment axes rotate without complete coincidence with each other during monotonous increace of horizontal shear stress acting on a sample in a simple shear test. The inclination angle ψ of the major principal stress axis to the vertical direction is deduced from a simple relationship ; τ/σ_N=κtan ψ, which is derived from theoretical consideration (Oda and Konishi, 1974) and verified by Cole's experimental results. The value of κ is a material constant for a given sand which is dependent only on the interparticle friction angle. By using this relation, the principal stress parameters such as mean stress (σ_1+σ_3)/2 and maximum shear stress (σ_1-σ_3)/2 are easily deduced from the shear stress τ and the normal stress σ_N acting on the horizontal shear plane in a simple shear test or even in a direct shear test.
- 社団法人地盤工学会の論文
- 1975-06-15
著者
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小田 匡寛
Dept. Of Foundation Engineering Faculty Of Engineering Saitama University
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小田 匡寛
Department Of Foundation Engineering Saitama University
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- 粒状体としての砂の構造および力学的性質と構造との関係について
- INITIAL FABRICS AND THEIR RELATIONS TO MECHANICAL PROPERTIES OF GRANULAR MATERIAL
- A MECHANICAL AND STATISTICAL MODEL OF GRANULAR MATERIAL
- DEFORMATION MECHANISM OF SAND IN TRIAXIAL COMPRESSION TESTS
- THE MECHANISM OF FABRIC CHANGES DURING COMPRESSIONAL DEFORMATION OF SAND
- EFFECT OF STRENGTH ANISOTROPY ON BEARING CAPACITY OF SHALLOW FOOTING IN A DENSE SAND
- EXPERIMENTAL STUDY OF ANISOTROPIC SHEAR STRENGTH OF SAND BY PLANE STRAIN TEST
- STRESS-INDUCED ANISOTROPY IN GRANULAR MASSES
- ROTATION OF PRINCIPAL STRESSES IN GRANULAR MATERIAL DURING SIMPLE SHEAR
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- SHEAR STRENGTH OF UNDISTURBED SAMPLE OF DECOMPOSED GRANITE SOIL
- マサ土の乱さない試料のセン断強度(『土質工学会論文報告集』Vol.16,No.1(1976年3月発行)掲載論文の概要)
- SHEAR STRENGTH OF UNDISTURBED SAMPLE OF DECOMPOSED GRANITE SOIL
- THE EFFECT OF CRACK GEOMETRY ON HYDRODYNAMIC DISPERSION IN CRACKED MEDIA
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