The Control of Groundwater Flow Systems and Geochemical Processes on Groundwater Chemistry: A Case Study in Wushenzhao Basin, NW China

• Published in: Water (Basel) Vol. 11; no. 4; p. 790
• Main Authors: Lyu, Min, Pang, Zhonghe, Yin, Lihe, Zhang, Jun, Huang, Tianming, Yang, Shuo, Li, Zhenbin, Wang, Xiaoyong, Gulbostan, Tursun
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.04.2019
• Subjects: Age composition; anthropogenic contamination; Aquifers; Basins; Chemical composition; Chemical evolution; Chemistry; Cretaceous; Dissolution; Flow system; Geochemistry; Geology; Groundwater; Groundwater chemistry; Groundwater flow; Groundwater management; Gypsum; hydrochemical evolution; Hydrogeology; Ion exchange; Isotopes; Laboratories; Lakes; nested groundwater flow systems; Precipitation; radiocarbon; Spatial distribution; Stable isotopes; Sustainability management; Sustainable development; Topography; Travel; Travel time; Water flow; Water resources; Water sampling; United States > US; China
• ISSN: 2073-4441; 2073-4441
• DOI: 10.3390/w11040790

The lowest reaches of a large-scale basin could be the discharge areas of local, intermediate and regional groundwater flow systems with significantly distinct travel distances and travel times. This study aims to delineate the groundwater chemical characteristics and the mechanism controlling the chemical evolution in the lowest reaches of the Wushenzhao Cretaceous basin, NW China. A total of 38 groundwater samples were collected and were chemically classified into five distinct water types by means of a Piper Plot. According to the hydrogeological setting and groundwater age, the spatial distribution of these water types is found to be associated with hierarchically nested groundwater flow systems (local and regional system): Types 1, 2, 3 and 4 belong to the local groundwater flow system, while type 5 belongs to the regional flow system. Graphical plots, stable isotopes and geochemical modeling techniques were used to interpret the observed compositions. The results show the dominance of carbonate and gypsum dissolution in type 1 waters; ion exchange in types 2, 3 and 4; and evaporite dissolution in type 5. In addition, human activities in the form of extensive irrigation also affect the chemical compositions of type 1 water. These findings are important for the sustainable management of groundwater resources in the study area.