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饱和兰州黄土液化过程中孔压和应变发展的试验研究
引用本文:孙海妹,王兰民,王平,刘红玫.饱和兰州黄土液化过程中孔压和应变发展的试验研究[J].岩土力学,2010,31(11):3464-3468.
作者姓名:孙海妹  王兰民  王平  刘红玫
作者单位:1. 中国地震局地震预测研究所兰州基地,兰州 730000;2. 中国地震局兰州地震研究所,兰州 730000
基金项目:中国地震局地震预测研究所基本科研业务费专项(No. 2009A22)资助。
摘    要:采用WF12440型空心圆柱扭剪仪,用反压饱和法对初始饱和度较低的原状黄土进行饱和,进行室内原状黄土饱和液化试验研究,探讨了饱和兰州黄土液化过程中孔隙水压力、轴向应变、应力-应变滞回圈的发展规律。结果表明,对初始饱和度较低的原状黄土,反压饱和法使孔压系数B值达到0.95以上,即土样完全饱和;兰州黄土在均压固结条件下液化的孔压发展,开始时上升速率较缓慢,循环数一定后会出现孔压迅速增高的现象直至达到有效围压;应力-应变滞回特性随着振动次数的增加发生变化,塑性逐步增大;当轴向应变小于2%时,孔压增长缓慢;此后,孔压上升速率加大,3%应变可以出现在初始液化前;接近液化时偏应力为负值时的有效应力大于正值时的有效应力。

关 键 词:黄土  液化  孔压  应变  试验研究  
收稿时间:2009-08-12

Experimental study of development of strain and pore water pressure during liquefaction of saturated Lanzhou loess
SUN Hai-mei,WANG Lan-ming,WANG Ping,LIU Hong-mei.Experimental study of development of strain and pore water pressure during liquefaction of saturated Lanzhou loess[J].Rock and Soil Mechanics,2010,31(11):3464-3468.
Authors:SUN Hai-mei  WANG Lan-ming  WANG Ping  LIU Hong-mei
Institution:1. Lanzhou Research Base of Earthquake Sciences, China Earthquake Administration, Lanzhou 730000, China; 2. Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China
Abstract:Using a dynamic hollow cylinder apparatus WF12440 as the test platform, this paper firstly studied the loess saturation by the back pressure method. The developments of pore water pressure, axial strain, deviatoric stress-axial strain curve during liquefaction are then investigated. Testing results indicate that the back pressure method can be successfully used for loess saturation; and the pore water pressure coefficient could achieve 0.95 and more. Under the condition of isotropic consolidation, pore water pressure increased slowly at the beginning; after several cycles the pore water pressure increased rapidly until it reached the effective consolidation pressure. The deviatoric stress-axial strain curve developed with the increase of cycles; and plastic strain increased step by step. When the axial strain was less than 2%, the pore water pressure increased slowly; afterwards, its increase ratio was much larger, and a strain of 3% could appear at the initial liquefaction process. Before liquefaction of the loess, the mean effective stress under negative deviatoric stress is larger than that under the positive deviatoric stress.
Keywords:loess  liquefaction  pore water pressure  strain  experimental study
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