Evaluation of groundwater recharge sources based on environmental tracers in an arid alluvial fan, NW China

被引：7
|
作者：
Xu, Wei [1 ]
Zhu, Pucheng [2 ]
Yang, Fengtian [3 ]
机构：
[1] Shenyang Agr Univ, Coll Water Conservancy, Shenyang 110866, Liaoning, Peoples R China
[2] Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Hebei, Peoples R China
[3] Jilin Univ, Inst Water Resources & Environm, Changchun 130021, Jilin, Peoples R China
来源：
JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY | 2019年 / 319卷 / 01期
基金：
中国国家自然科学基金;
关键词：
Groundwater recharge; Stable isotope; Chloride; Arid area; Northwest China; HEIHE RIVER; HYDROGEOCHEMICAL EVOLUTION; UNSATURATED ZONE; STABLE-ISOTOPES; MINQIN BASIN; GOBI DESERT; NORTHWEST; WATER; CHLORIDE; CHEMISTRY;
D O I：
10.1007/s10967-018-6272-8
中图分类号：
O65 [分析化学];
学科分类号：
070302 ; 081704 ;
摘要：
Environmental tracers include stable isotopes and chloride in natural water were used to recognize the recharge sources of groundwater in Nalenggele alluvial fan, NW China. There is little effective recharge from local precipitation, the original resources of groundwater are glacier melting water and precipitation in high Kunlun mountain, groundwater is directly recharged by river infiltration along the river stretch and lateral groundwater flow from the high mountain area. In this study the effects of the depth infiltrated of river water on the mixing ratio was investigated. Results show that the mixing ratio decreases with the infiltrated river water depth.
引用
收藏
页码：123 / 133
页数：11
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