人民黄河Issue(3)：37-39,3.DOI:10.3969/j.issn.1000-1379.2014.03.013
分层包气带中铜离子迁移试验及模拟
Experiment and Simulation Prediction of Copper Migration in the Layered Vadose Zone
盛金昌 1徐力猛 1邵建明2
作者信息
- 1. 河海大学水利水电学院，江苏南京210098
- 2. 邹平县水务局，山东滨州256200
- 折叠
摘要
Abstract
It adopted the saturated-unsaturated layered soil column experiment and its numerical simulation to study the variation of copper migra-tion depth with time and the influence factors. The results show that early in the experiment,negative pressure in the vadose zone can lead to soil water redistribution:the moisture content of unsaturated soil increases in a small degree and that of upper unsaturated soil reduces obviously,but recovers soon. Water negative pressure has a little influence to the copper migration. Migration rate of copper will decrease with the increase of soil depth. Adsorption-precipitation effect is the main factor. That copper reaches the depth of 20 cm,35 cm,45 cm,52. 5 cm,66. 7 cm and 70 cm at the time of 60 d,110 d,160 d,1 y,3 y and 5 y,which can be used for dealing with copper polluting of soil and underground water.关键词
包气带/水势负压/吸附-沉淀作用/数值模拟/迁移深度Key words
vadose zone/water negative pressure/adsorption-precipitation/numerical simulation/migration depth分类
天文与地球科学引用本文复制引用
盛金昌,徐力猛,邵建明..分层包气带中铜离子迁移试验及模拟[J].人民黄河,2014,(3):37-39,3.
