IMECH-IR  > 力学所知识产出(1956-2008)
冲击载荷下饱和砂土中超孔隙水压力的建立与消散过程
Alternative TitleBuild-up and dissipation of excess pore water pressure in saturated sand under impact loading
张均锋; 孟祥跃
Source Publication岩石力学与工程学报
2003
Volume22Issue:9Pages:1463-1468
ISSN1000-6915
Abstract对落锤冲击造成饱和砂土中的冲击压力进行了测量。通过测量得到了冲击时饱和砂土中超孔隙水压力的建立和消散过程,分析了多次冲击对超孔隙水压力建立的影响,得到了一次冲击就能使饱和砂土达到完全液化的冲击强度临界值。
Keyword土力学 冲击载荷 饱和砂土 超孔隙水压力 液化
Subject Area力学
Indexed ByEI ; CSCD
Language中文
CSCD IDCSCD:1168826
Citation statistics
Cited Times:6[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://dspace.imech.ac.cn/handle/311007/16996
Collection力学所知识产出(1956-2008)
Recommended Citation
GB/T 7714
张均锋,孟祥跃. 冲击载荷下饱和砂土中超孔隙水压力的建立与消散过程[J]. 岩石力学与工程学报,2003,22,9,:1463-1468.
APA 张均锋,&孟祥跃.(2003).冲击载荷下饱和砂土中超孔隙水压力的建立与消散过程.岩石力学与工程学报,22(9),1463-1468.
MLA 张均锋,et al."冲击载荷下饱和砂土中超孔隙水压力的建立与消散过程".岩石力学与工程学报 22.9(2003):1463-1468.
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