| 注册
首页|期刊导航|华东师范大学学报(自然科学版)|地下淡水驱替咸水过程中水文地球化学作用的试验研究

地下淡水驱替咸水过程中水文地球化学作用的试验研究

邢立亭 王立艳 李常锁 徐天

华东师范大学学报(自然科学版)Issue(4):132-143,12.
华东师范大学学报(自然科学版)Issue(4):132-143,12.DOI:10.3969/j.issn.1000-5641.2015.04.014

地下淡水驱替咸水过程中水文地球化学作用的试验研究

Experimental study on hydrogeochemistry action in the process of freshwater displacing saltwater

邢立亭 1王立艳 2李常锁 3徐天1

作者信息

  • 1. 济南大学 资源与环境学院,济南 250022
  • 2. 山东正元建设工程有限责任公司,济南 250100
  • 3. 山东省地矿工程勘察院,济南 250014
  • 折叠

摘要

Abstract

Based on test materials,including of silt,shallow salt groundwater and atmospheric precipitation which were got in northwestern Shandong geochemistry action in the process of freshwater displacing saltwater were studied.The results indicated that (1)When content of clay was high in aquifer medium,and specific conductivity of exudate was less than or equal to 0.83 ms/cm in the process of freshwater displacing saltwater,clay played a role of film effect in con-centrating ion components.(2)Dolomite still kept precipitation with water,and halite still kept dissolution in the process of freshwater displacing saltwater.Calite precipitated when specific conductivity of exudate was more than 1 .00 ms/cm;Gypsum balanced with water when specific conductivity of exudate was more than or equal to 6.22 ms/cm.Mg/Ca-Na exchange interaction was remarkable with critical ion strength being in 0.20~0.25 mol/L.Adsorption was remarka-ble while specific conductivity of exudate was more then 12.00 ms/cm.Displacement experiment showed that hydrogeochemistry actions were happened in the process of freshwater displacing saltwater with adsorption,exchange interaction,lixiviation,dolomitization and mixing action.

关键词

浅层咸水/水化学特征/水文地球化学作用/驱替试验/内陆地区

Key words

shallow salt groundwater/water chemical characteristics/hydrogeochemistry action/displacement experiment/inland region

分类

建筑与水利

引用本文复制引用

邢立亭,王立艳,李常锁,徐天..地下淡水驱替咸水过程中水文地球化学作用的试验研究[J].华东师范大学学报(自然科学版),2015,(4):132-143,12.

基金项目

国家自然科学基金 ()

华东师范大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1000-5641

访问量0
|
下载量0
段落导航相关论文