现代地质Issue(2)：238-244,7.
新疆玛纳斯河流域平原区地下水水文地球化学特征研究
Groundwater Hydro-geochemistry in Plain of Manasi River Basin,Xinjiang
摘要
Abstract
Groundwater is main source of water supply in Manasi River Basin.In order to understand groundwa-ter hydrology characteristics and main process of groundwater formed,hydro-geochemistry in Plain of Manasi River Basin is studied according to the analysis of constant chemistry component,Gibbs graph,ion ratio and i-sotopic characteristics of groundwater in typical profile using the method of Shukaliefu classification,mathemati-cal statistics method,Gibbs graph and ion ratio.It is found that unconfined water and confined water have a close hydraulic relationship.The values ofδ18 O and δD are increase from upstream to downstream.Hydrolysis process occurring in groundwater systems which decided the chemical characteristics of research area,includes evaporation concentration,precipitation and lixiviation of carbonate rock and sulfate rock.关键词
玛纳斯河流域/水化学类型/离子比/同位素Key words
Manasi River Basin/hydrochemistry type/ion ratio/isotope分类
天文与地球科学引用本文复制引用
李巧,周金龙,高业新,杜明亮,程凡,李丰,孟奇..新疆玛纳斯河流域平原区地下水水文地球化学特征研究[J].现代地质,2015,(2):238-244,7.基金项目
新疆农业大学博士后经费；国家自然科学基金项目（51069016；U1403283）；新疆维吾尔自治区水文学及水资源重点学科基金项目（XJSWSZYZDXK20101202）；新疆维吾尔自治区地方公派出国留学成组配套项目（XJDF201307）；中国地质调查局项目“西北地区主要城市地下水污染调查评价”（1212011220982）。 （）
