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不排水条件下全风化花岗岩残积土工程特性与本构模型
引用本文:栾茂田,罗锦添,李焯芬,翟阳.不排水条件下全风化花岗岩残积土工程特性与本构模型[J].大连理工大学学报,2000,40(Z1):S83-S89.
作者姓名:栾茂田  罗锦添  李焯芬  翟阳
作者单位:大连理工大学土木工程系!辽宁大连116024大连理工大学海岸与近海工程国家重点实验室,辽宁大连116024,加拿大Carleton大学土木与环境工程系!加拿大渥太华香港大学土木及结构工程系,中国香港特别行政区,大连理工大学土木工程系!辽宁大连116024香港大学土木及结构工程系!中国香港
基金项目:香港特别行政区土木工程署土力工程处资助项目
摘    要:通过土工试验对不排水剪切条件下的饱和松散砂质土的工程特性进行了探讨 ,发现其在剪切时的应力 -应变关系呈现出加工软化特性 ,土体超过峰值强度后最终达到了变形的稳定状态 .基于稳定状态概念 ,将临界土力学理论与非线性应力 -应变关系相结合 ,建立了非线性应力 -应变 -临界状态本构模型 .采用香港钻石山地区全风化花岗岩残积土的不排水三轴试验结果 ,确定了有关模型参数 ,验证了所建议本构模型的合理性

关 键 词:本构模型  稳定状态  峰值强度/应变软化  不排水剪切  全风化花岗岩  松散填土边坡
修稿时间::

Fundamental behavior and constitutive modeling of a CDG residual soil under undrained shear
LUAN Mao tian ,LAW K T ,LEE C F ,ZHAI Yang.Fundamental behavior and constitutive modeling of a CDG residual soil under undrained shear[J].Journal of Dalian University of Technology,2000,40(Z1):S83-S89.
Authors:LUAN Mao tian    LAW K T    LEE C F    ZHAI Yang
Institution:LUAN Mao tian 1,2,LAW K T 3,4,LEE C F 1,4,ZHAI Yang 4
Abstract:The stress strain relationships of saturated loose sandy soils under undrained shear show strain softening behaviour and soils will reach the steady state of deformation after beyond the peak shear stress. In this paper, on the basis of the concept of steady state, the fundamental theory of the critical soil mechanics and nonlinear stress strain relationship are combined together to establish the constitutive model for describing nonlinear type stress strain curves and critical states. The experimental data of undrained triaxial compression tests for a loose completely decomposed granite (CDG) residual soil from Diamond Hill Development Site Formation in Hong Kong is used to define the model parameters. The proposed constitutive model is verified by comparing the predicted results and experimental data.
Keywords:constitutive relation  steady state  peak strength/strain softening  undrained shear  completely  decomposed granite (CDG)  loose fill soil slope
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