Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s10040-017-1659-0 |
Groundwater mixing and mineralization processes in a mountain-oasis-desert basin, northwest China: hydrogeochemistry and environmental tracer indicators | |
Ma, Bin1,2; Jin, Menggui1,2; Liang, Xing2,3; Li, Jing2 | |
通讯作者 | Jin, Menggui |
来源期刊 | HYDROGEOLOGY JOURNAL
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ISSN | 1431-2174 |
EISSN | 1435-0157 |
出版年 | 2018 |
卷号 | 26期号:1页码:233-250 |
英文摘要 | Hydrogeochemistry and environmental tracers (H-2, O-18, Sr-87/Sr-86) in precipitation, river and reservoir water, and groundwater have been used to determine groundwater recharge sources, and to identify mixing characteristics and mineralization processes in the Manas River Basin (MRB), which is a typical mountain-oasis-desert ecosystem in arid northwest China. The oasis component is artificial (irrigation). Groundwater with enriched stable isotope content originates from local precipitation and surface-water leakage in the piedmont alluvial-oasis plain. Groundwater with more depleted isotopes in the north oasis plain and desert is recharged by lateral flow from the adjacent mountains, for which recharge is associated with high altitude and/or paleo-water infiltrating during a period of much colder climate. Little evaporation and isotope exchange between groundwater and rock and soil minerals occurred in the mountain, piedmont and oasis plain. Groundwater delta H-2 and delta O-18 values show more homogeneous values along the groundwater flow direction and with well depths, indicating inter-aquifer mixing processes. A regional contrast of groundwater allows the Sr-87/Sr-86 ratios and delta O-18 values to be useful in a combination with Cl, Na, Mg, Ca and Sr concentrations to distinguish the groundwater mixing characteristics. Two main processes are identified: groundwater lateral-flow mixing and river leakage in the piedmont alluvial-oasis plain, and vertical mixing in the north oasis plain and the desert. The Sr-87/Sr-86 ratios and selected ion ratios reveal that carbonate dissolution and mixing with silicate from the southern mountain area are primarily controlling the strontium isotope hydrogeochemistry. |
英文关键词 | Stable isotopes Groundwater flow Mineralization processes Arid regions China |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000423051600016 |
WOS关键词 | MAJOR ION GEOCHEMISTRY ; WORLD WATER CHEMISTRY ; MANAS RIVER-BASIN ; ISOTOPE COMPOSITION ; FLOW PATHS ; NORTHERN CHINA ; STRONTIUM ISOTOPES ; DATONG BASIN ; MURRAY BASIN ; TRANS-PECOS |
WOS类目 | Geosciences, Multidisciplinary ; Water Resources |
WOS研究方向 | Geology ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/209864 |
作者单位 | 1.China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China; 2.China Univ Geosci, Sch Environm Studies, Wuhan 430074, Peoples R China; 3.China Univ Geosci, Hubei Key Lab Wetland Evolut & Ecol Restorat, Wuhan 430074, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, Bin,Jin, Menggui,Liang, Xing,et al. Groundwater mixing and mineralization processes in a mountain-oasis-desert basin, northwest China: hydrogeochemistry and environmental tracer indicators[J],2018,26(1):233-250. |
APA | Ma, Bin,Jin, Menggui,Liang, Xing,&Li, Jing.(2018).Groundwater mixing and mineralization processes in a mountain-oasis-desert basin, northwest China: hydrogeochemistry and environmental tracer indicators.HYDROGEOLOGY JOURNAL,26(1),233-250. |
MLA | Ma, Bin,et al."Groundwater mixing and mineralization processes in a mountain-oasis-desert basin, northwest China: hydrogeochemistry and environmental tracer indicators".HYDROGEOLOGY JOURNAL 26.1(2018):233-250. |
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