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- W2359158805 abstract "Jinghuiqu irrigation district is located in semi-arid regions of northwestern China,where groundwater is the most important source for industry,agriculture and local people.The present work is conducted in the Jinghuiqu irrigation district to identify the geochemical characteristics and the hydrogeochemical evolutionary processes of sulfate in groundwater.Hydrochemical compositions combined with geological and hydrogeological data of sulfate,irrigation test and Hydrus-1D were used for this purpose.The result show that groundwater types changed from 3 HCO in 1982 to 2 SO 4water types in 2009.Elevated 2 SO 4was initially derived from sulfate mineral dissolution,but from 1990 to 2009,the increased 2 SO 4mainly came from the irrigated groundwater which contained higher 2 SO 4concentrations." @default.
- W2359158805 created "2016-06-24" @default.
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- W2359158805 date "2012-01-01" @default.
- W2359158805 modified "2023-09-26" @default.
- W2359158805 title "Sulfate hydrochemical characteristics and evolution processes in shallow groundwater of Jinghuiqu irrigation district" @default.
- W2359158805 hasPublicationYear "2012" @default.
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