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水-土作用对土体渗透系数的影响研究

伍艳 王玮屏 任海平 史粉英

水文地质工程地质2011,Vol.38Issue(6):39-43,5.
水文地质工程地质2011,Vol.38Issue(6):39-43,5.

水-土作用对土体渗透系数的影响研究

Experimental studies of coefficient of permeability of soil affected by water-soil interactions

伍艳 1王玮屏 1任海平 2史粉英1

作者信息

  • 1. 黄河水利科学研究院,郑州 450003
  • 2. 黄河勘测规划设计有限公司,郑州450003
  • 折叠

摘要

Abstract

In order to examine the influence of water-soil interactions on coefficient of permeability of soil, soil samples have been tested in laboratory with different chemical solutions, including deionized water, solution with different Ph, and Na2SO4, NaHCO3, CaCl2, TP, TN solutions with different concentrations. The results indicate that the coefficient of permeability are changed, and there exist both positive and negative effects on the specimens in this test. The SEM photos show that dissolution and deposition of water on soil composition and ion-exchange adsorption of water with soil can affect the soil microstructure and pore characteristics, and change the permeability of soil.

关键词

水-土作用/渗透系数/微观结构/机理

Key words

water-soil interaction/coefficient of permeability/microstructure/mechanism

分类

天文与地球科学

引用本文复制引用

伍艳,王玮屏,任海平,史粉英..水-土作用对土体渗透系数的影响研究[J].水文地质工程地质,2011,38(6):39-43,5.

基金项目

水利部堤防安全与病害防治工程技术研究中心开放课题基金项目(200904) (200904)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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