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不同降雨条件下成都黏土基坑边坡入渗深度研究

梁树 谢强 郭永春 李朝阳

水文地质工程地质2017,Vol.44Issue(5):107-111,130,6.
水文地质工程地质2017,Vol.44Issue(5):107-111,130,6.DOI:10.16030/j.cnki.issn.1000-3665.2017.05.17

不同降雨条件下成都黏土基坑边坡入渗深度研究

Infiltration depth of Chengdu clay foundation pit slope under different rainfall conditions

梁树 1谢强 1郭永春 1李朝阳1

作者信息

  • 1. 西南交通大学地球科学与环境工程学院,四川成都610031
  • 折叠

摘要

Abstract

Rainfall humidification causes large deformation or damage to Chengdu clay pit slope.Methods of model test,field test and numerical simulation are used to analysis infiltration depth under different rainfall conditions.Infiltration law and infiltration depth empirical formula are obtained by comparing the results of the analysis.The results show that model test is difficult to simulate really due to Chengdu clay swelling,soil structure and microcracks having a big influence on seepage.The results need a correction through field test.The main factor which influences the rainfall duration is the depth of infiltration.With the increase of rainfall time and rainfall intensity,the increasing speed of infiltration depth gradually slows down.It is good to use piecewise linear fitting.The infiltration depth of single rainfall in Chengdu clay slope is less than 1 m.

关键词

成都黏土/基坑边坡/入渗深度/模型试验/现场试验

Key words

Chengdu clay/foundation pit slope/infiltration depth/model test/field test

分类

天文与地球科学

引用本文复制引用

梁树,谢强,郭永春,李朝阳..不同降雨条件下成都黏土基坑边坡入渗深度研究[J].水文地质工程地质,2017,44(5):107-111,130,6.

基金项目

《岩土工程系列问题研究——膨胀土与软弱地基专题研究》资助项目(CSCEC-2008-Z-30-4) (CSCEC-2008-Z-30-4)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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