Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1002/hyp.13243 |
Insights into groundwater salinization from hydrogeochemical and isotopic evidence in an arid inland basin | |
Liu, Yalei1,2,3; Jin, Menggui1,2,3; Wang, Jianjun1,2,3 | |
通讯作者 | Jin, Menggui |
来源期刊 | HYDROLOGICAL PROCESSES
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ISSN | 0885-6087 |
EISSN | 1099-1085 |
出版年 | 2018 |
卷号 | 32期号:20页码:3108-3127 |
英文摘要 | In the Manas River basin (MRB), groundwater salinization has become a major concern, impeding groundwater use considerably. Isotopic and hydrogeochemical characteristics of 73 groundwater and 11 surface water samples from the basin were analysed to determine the salinization process and potential sources of salinity. Groundwater salinity ranged from 0.2 to 11.91g/L, and high salinities were generally located in the discharge area, arable land irrigated by groundwater, and depression cone area. The quantitative contributions of the evaporation effect were calculated, and the various groundwater contributions of transpiration, mineral dissolution, and agricultural irrigation were identified using hydrogeochemical diagrams and D and O-18 compositions of the groundwater and surface water samples. The average evaporation contribution ratios to salinity were 5.87% and 32.7% in groundwater and surface water, respectively. From the piedmont plain to the desert plain, the average groundwater loss by evaporation increased from 7% to 29%. However, the increases in salinity by evaporation were small according to the deuterium excess signals. Mineral dissolution, transpiration, and agricultural irrigation activities were the major causes of groundwater salinization. Isotopic information revealed that river leakage quickly infiltrated into aquifers in the piedmont area with weak evaporation effects. The recharge water interacted with the sediments and dissolved minerals and subsequently increased the salinity along the flow path. In the irrigation land, shallow groundwater salinity and Cl- concentrations increased but not O-18, suggesting that both the leaching of soil salts due to irrigation and transpiration effect dominated in controlling the hydrogeochemistry. Depleted O-18 and high Cl- concentrations in the middle and deep groundwater revealed the combined effects of mixing with paleo-water and mineral dissolution with a long residence time. These results could contribute to the management of groundwater sources and future utilization programs in the MRB and similar areas. |
英文关键词 | deuterium excess groundwater salinization Northwest China Manas River basin stable isotopes |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000444948700003 |
WOS关键词 | MULCHED DRIP IRRIGATION ; ENVIRONMENTAL TRACERS ; NORTHERN CHINA ; DATONG BASIN ; GEOCHEMICAL PROCESSES ; SALINE GROUNDWATER ; NORTHWESTERN CHINA ; COASTAL AQUIFERS ; SOIL-SALINITY ; CL/BR RATIOS |
WOS类目 | Water Resources |
WOS研究方向 | Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/209904 |
作者单位 | 1.China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Hubei, Peoples R China; 2.China Univ Geosci, Lab Basin Hydrol & Wetland Ecorestorat, Wuhan, Hubei, Peoples R China; 3.China Univ Geosci, Sch Environm Studies, Wuhan, Hubei, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, Yalei,Jin, Menggui,Wang, Jianjun. Insights into groundwater salinization from hydrogeochemical and isotopic evidence in an arid inland basin[J],2018,32(20):3108-3127. |
APA | Liu, Yalei,Jin, Menggui,&Wang, Jianjun.(2018).Insights into groundwater salinization from hydrogeochemical and isotopic evidence in an arid inland basin.HYDROLOGICAL PROCESSES,32(20),3108-3127. |
MLA | Liu, Yalei,et al."Insights into groundwater salinization from hydrogeochemical and isotopic evidence in an arid inland basin".HYDROLOGICAL PROCESSES 32.20(2018):3108-3127. |
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