Experimental Measures of Affine and Nonaffine Deformation in Granular Shear
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岩土力学英文版
Introduction
Geotechnical Engineering, also known as Soil Mechanics
or Rock Mechanics, is a branch of civil engineering
that deals with the behavior of soil and rock materials
under various conditions. It is an important field of
study as it helps engineers understand the properties
and characteristics of these materials, which in turn
enables them to design and construct safe and stable
structures.
Soil Mechanics
Soil Mechanics is the study of the behavior of soil
materials, including its formation, classification, and
properties. Various aspects of soil mechanics are
essential in geotechnical engineering, such as soil
compaction, permeability, and soil stability.
Soil formation is a complex process that involves the
weathering and erosion of existing rocks, resulting in
the formation of different soil types. The composition
J.Cent.South Univ.(2013)20:2275—2284 DoI:10.1007/sl1771.013。1734.1 垒Springer
Anisotropic characteristics of granular materials under simple shear
QIAN Jian—gu(钱建固) 一,YOU Zi—pei(由子沛) 一,HUANG Map.song(黄茂松) ,。
1.Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education(Tongji University),
Shanghai 200092,China;
2.Department of Geotechnical Engineering,Tongji University,Shanghai 200092,China
◎Central South University Press and Springer-Verlag Berlin Heidelberg 20 1 3
Abstraet:The discrete element method was used to investigate the microscopic characteristics of granular materials under simple shear 1oading conditions.A series of simple tests on photo—elastic materials were used as a benchmark.With respect to the origina1 experimental observations.average micro—variables such as the shear stress shear strain and the volumetric dilatancy were ex仃acted to illustrate the performance of the DEM simulation.The change of anisotropic density distributions of contact normals and contact forces was demonstrated during the course of simple shear.On the basis of microscopic characteristics.an analytical approach was further used to explore the macroscopic behaviors involving anisotropic shear strength and anisotropic stress—dilatancy.This results show that under simple shear loading.anisotropic shear strength arises primarily due to the difference between principal directions of the stress and the Nbric.In addition.non—coaxiality.refen'ing to the difierence bet、veen principa1 directions of the strain rate and the stress.generates Iess stress—dilatancy.In particular,the anisotropic hardening and anisotropic stress—dilatancy will reduce to the isotropic hardening and the classical Taylor’s stress—dilatancy under proportional1oading.
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曹新文1,2,3 孙知明1 黄宝春2 曹勇1 裴军令1 叶小舟1 刘思琪2
CAOXinWen1,2,3,SUNZhingMing1,HUANGBaoChun2,CAOYong1,PEIJunLing1,YEXiaoZhou1andLIUSiQi2
1自然资源部古地磁与古构造重建重点实验室,中国地质科学院地质力学研究所,北京 100081
2北京大学地球与空间科学学院,教育部造山带与构造演化重点实验室,北京 100871
3自然资源部深地动力学实验室,中国地质科学院地质研究所,北京 100037
1MNRKeyLaboratoryofPaleomagnetismandTectonicReconstruction,InstituteofGeomechanics,ChineseAcademyofGeologicalSciences,Beijing
100081,China
2MOEKeyLaboratoryofOrogenicBeltsandCrustalEvolution,SchoolofEarthandSpaceSciences,PekingUniversity,Beijing100871,China
3MNRKeyLaboratoryofDeepEarthDynamics,InstituteofGeology,ChineseAcademyofGeologicalSciences,Beijing100037,China
20210730收稿,20210929改回
CaoXW,SunZM,HuangBC,CaoY,PeiJL,YeXZandLiuSQ2021Theinvestigationsofthedeformationofthe