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砂土液化动稳态强度分析
引用本文:王星华,周海林.砂土液化动稳态强度分析[J].岩石力学与工程学报,2003,22(1):96-102.
作者姓名:王星华  周海林
作者单位:中南大学铁道校区,长沙,410075
基金项目:国家自然科学基金(59979001)资助项目。
摘    要:根据动三轴实验数据,砂土的应力路径最终达到一个稳定的阶段,此时,在不同的振动周期,砂土的孔隙水压幅值不再增加,应力路径相互重叠,但是应变幅值却以恒定的速率不断增加,这种相对稳定状态中的极限强度是评估砂土抗液化能力的重要指标,并结合饱和砂土的孔隙水压力发展和应力路径,使砂土液化强度更加明了。

关 键 词:砂土液化  土力学  动强度  动稳态
文章编号:1000-6915(2003)01-0096-07
收稿时间:2001-2-13
修稿时间:2001-4-28

STUDY ON DYNAMIC STEADY STATE STRENGTH OF SAND SOIL LIQUEFACTION
Wang Xinghua,Zhou Hailin.STUDY ON DYNAMIC STEADY STATE STRENGTH OF SAND SOIL LIQUEFACTION[J].Chinese Journal of Rock Mechanics and Engineering,2003,22(1):96-102.
Authors:Wang Xinghua  Zhou Hailin
Abstract:According to the dynamic triaxial test of sand, there is a steady state at the last phase of the development of strain and stress path. In different cycle of this phase, the stress paths superpose with each other, but the axial strain tends to a steady rate. The strength of the sand in this phase is studied because it is an important parameter to evaluate the stability of sand soil liquefaction. Considering the strength developed with stress path, the mechanism of saturated sand liquefaction seems more clear.
Keywords:soil mechanics  sand soil liquefaction  dynamic strength  dynamic steady state
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