摘要
本文进行了基于内时理论的动荷载下饱和黄土孔压增长模型的试验研究,结果表明:饱和黄土液化过程中其孔压的增长与土的干密度、饱和度以及动应力有着一定的相关关系。
Based on the endochronic theory, the experiment and study on the model of pore water pressure of saturated loess increasing under dynamic load are done. The results show that the increase of pore water pressure of saturated loess has correlate relationship with the dry density, saturation degree of soil samples as well as the dynamic load.
出处
《西北地震学报》
CSCD
北大核心
2004年第4期371-373,共3页
Northwestern Seismological Journal
基金
地震联合基金资助(批准号:604016)
中国地震局兰州地震研究所青年基金资助(批准号:A0133)
中国地震局兰州地震研究所论著编号:LC20040014.
关键词
黄土
液化
孔压
Loess
Liquefaction
Pore water pressure.