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非饱和黄土震陷物理力学机制与主导影响因素

孙军杰 王强 王兰民

西北地震学报2011,Vol.33Issue(z1):71-76,6.
西北地震学报2011,Vol.33Issue(z1):71-76,6.

非饱和黄土震陷物理力学机制与主导影响因素

Study on the Physical-mechanical Mechanism and Dominant Influence Factors of Unsaturated Loess Subsidence under Seismic Loading

孙军杰 1王强 2王兰民3

作者信息

  • 1. 中国地震局兰州地震研究所,甘肃兰州730000
  • 2. 中国地震局黄土地震工程开放实验室,甘肃兰州730000
  • 3. 甘肃省岩土防灾工程技术研究中心,甘肃兰州730000
  • 折叠

摘要

Abstract

Based on the comprehensive analysis of physical process and mechanical mechanism of loess seismic subsidence, the seismic subsidence of unsaturated loess could be described as a consolidation response of generalized solid-phase-media of soil mass under external dynamic loading. The dominant influence factors of loess seismic subsidence should include two aspects, which are the strength and volume characteristics of generalized solid-phase-media of soil mass and external dynamic loading features. The strength characteristic of the media could be figured by the cohesion and internal friction angle, both obtained expediently through laboratory geotechnical tests, while the volume feature of the media could be described by the void ratio. By the view of the macro physical-mechanical mechanism of seismic subsidence in unsaturated loess, the factors of cohesion and internal friction angle briefly represent the characteristics of soil structure strength, and the factor of void ratio influences the final seismic subsidence magnitude of soil mass. In fact, the strength feature of loess shows the endurance capacity of soil mass to resist the external dynamic loading meanwhile, the subsidence magnitude characteristic of loess describes the settlement capacity of soil mass under the external dynamic loading.

关键词

非饱和黄土/广义固相介质/动荷载/震陷/物理力学机制/影响因素

Key words

Unsaturated loess/Generalized solid-phase-media/Dynamic loading/Seismic subsidence/Physical-mechanical mechanism/Influence factor

分类

建筑与水利

引用本文复制引用

孙军杰,王强,王兰民..非饱和黄土震陷物理力学机制与主导影响因素[J].西北地震学报,2011,33(z1):71-76,6.

基金项目

中国地震局兰州地震研究所论著编号:LC2011038 ()

西北地震学报

OA北大核心CSCDCSTPCD

1000-0844

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