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These large-scale groundwater salinization problems tend to be sourced from two major means natural and anthropogenic. The normal sources tend to be diversified from connate saline groundwater, seawater intrusion, evaporation, dissolution of soluble salts, membrane filtration procedure to geothermal beginning. The anthropogenic resources include irrigation return flow, roadway deicing salts, manufacturing and agricultural wastewater, and gas and oil production activities. The built-in strategy of