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汶川地震中甘肃清水田川黄土液化的试验研究
引用本文:王谦,王兰民,袁中夏,王平,丁风梅.汶川地震中甘肃清水田川黄土液化的试验研究[J].水文地质工程地质,2012,39(2):116-120.
作者姓名:王谦  王兰民  袁中夏  王平  丁风梅
作者单位:(1.中国地震局兰州地震研究所,兰州 730000;2.中国地震局地震预测研究所兰州科技创新基地,兰州 730000;3.中国地震局黄土地震工程开放实验室,兰州 730000)
基金项目:甘肃省地震局地震科技发展基金项目(2011S01);国家自然科学基金项目(50978239);中国地震局地震预测研究所基本科研业务经费项目(2010A76,2010A88-4);兰州地震研究所论著编号LC2011012
摘    要:2008年5·12特大地震中,位于甘肃省清水县郭川乡的田川村发生了饱和黄土的液化滑移灾害。本文首先在对田川场地进行考察的基础上,综合田川在汶川地震中的震害情况以及滑移区的地形条件,将该地区在汶川地震中的烈度进行了修正。其次对田川黄土进行了物性指标测试以及室内动三轴液化试验,根据试验结果,综合考虑产生液化所需的场地及土性条件、黄土的动强度和液化特性,对田川黄土液化灾害进行了分析,并采用反应分析的方法对其进行了液化判定。研究结果证明了田川黄土液化的事实存在性,为低烈度区黄土液化提供了新的震害依据。



关 键 词:黄土  地震液化  液化判别
收稿时间:2011-03-30
修稿时间:2011-07-06

A study of loess liquefaction induced by the Wenchuan Ms8.0 Earthquake in Tianchuan, Qingshui County, Gansu Province
WANG Qian , WANG Lan-min , YUAN Zhong-xia , WANG Ping , DING Feng-mei.A study of loess liquefaction induced by the Wenchuan Ms8.0 Earthquake in Tianchuan, Qingshui County, Gansu Province[J].Hydrogeology and Engineering Geology,2012,39(2):116-120.
Authors:WANG Qian  WANG Lan-min  YUAN Zhong-xia  WANG Ping  DING Feng-mei
Institution:(1. Lanzhou Institute of Seismology, CEA, Lanzhou, Gansu 730000,China; 2. Lanzhou Base of Institute of Earthquake Sciences, CEA, Lanzhou, Gansu 730000,China; 3. Open Laboratory of Loess Earthquake Engineering, CEA, Lanzhou, Gansu 730000, China )
Abstract:In the Wenchuan Ms8.0 Earthquake,the landslide damage due to liquefaction of saturated loess occurred in the Tianchuan,Qingshui County,Gansu Province.In this paper,based on the field and hazard investigation of the site,we amended the seismic intensity of the region in the Wenchuan earthquake by considering the geographic and geomorphic conditions and the seismic damage of structures of the village.Moreover,the tests on the physical property index and dynamic triaxial liquefaction of Tianchuan loess were carried out based on test results,the liquefaction of Tianchuan saturated loess was analyzed by considering the site conditions and soil characteristics,dynamic strength and liquefaction characteristics of the loess.Finally,the liquefaction discrimination of the loess was completed by using the response analysis method based on the result of dynamic triaxial liquefaction tests.The results show that the liquefaction of the loess is typical example of loess liquefaction,which provides a new example of loess liquefaction in low seismic intensity region.
Keywords:loess  seismic liquefaction  liquefaction evaluation
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