南水北调与水利科技Issue(1)：143-148,135,7.DOI:10.13476/j.cnki.nsbdqk.2016.01.024
潮白河地下水调蓄区水岩作用过程模拟
Simulation of the water-rock reaction in Chaobai River ground-water storage area
摘要
Abstract
In the process of The South-to-North Water Transfers, some of the water will be used to supplement the groundwater of Chaobai River basin. Due to the differences of Danjiangkou reservoir water and Beijing groundwater, water-rock interaction may occur. Taking the example of Chaobai River basin, we analyzed the water-rock interaction and changes of water during re-charge by batch experiments and hydrogeochemist ry simulation. The results showed that: during the recharge, the water was af-fected by nitrification, cat ion exchange and solution of minerals. With the increase of proport ion of southern water, calcite and dolomite dissolve and concentrations of calcium and magnesium were elevated coupled with cation exchange which mainly is so-dium with calcium and/ or magnesium. The higher proportion of south water, the stronger of nitrification is found. Affect ed by nitrif ication and carbonate balance, pH of groundwater was reduced at early stage then elevated at late stage.关键词
南水北调/水-岩相互作用/硝化作用/阳离子交换/水文地球化学模拟/饱和指数/矿物溶解Key words
The South-to-North Water Transfers/water-rock interaction/nitrification/cat ionexchange/hydrogeochemistry simu-lation/saturation index/dissolution of minerals分类
资源环境引用本文复制引用
贾文飞,杨洋,赵阳,李娟,吕宁磬,席北斗,李鸣晓,杨津津,郭艳菲..潮白河地下水调蓄区水岩作用过程模拟[J].南水北调与水利科技,2016,(1):143-148,135,7.基金项目
国家水体污染控制与治理科技重大专项(2014ZX07203010)Fund：Major Science and Technology Program for Water Pollution C ontr ol and Treatment of China(2014ZX07203010) （2014ZX07203010）
