Abstract
To investigate the chemical characteristics, spatial distribution and evolution of groundwater in the middle reaches of the Heihe River, 100 shallow groundwater samples were collected and tested. The results of this assessment indicate that the shallow groundwater in the study area is weakly alkaline and brackish. Concentrations of K+, Cl− and NO3− are highly variable in groundwater and are the highest in areas with intensive human land use activities. The TDS content of groundwater gradually increases from the recharge area to the discharge area, and the chemical composition gradually changes from SO42−–HCO3−–Na+·Mg2+ to SO42−–Na+–Mg2+. Overall, the chemical composition and groundwater types in the study area are primarily affected by water–rock reactions, and certain areas are more affected by human activities. Isotopic evidence indicates that the main source of shallow groundwater in the study area is snowmelt.












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Acknowledgements
This work was supported by Center for Hydrogeology and Environmental Geology Survey, China Geological Survey. Funded projects are “A 1:50,000 hydrogeological survey of the Heihe river basin in the hexi corridor (DD20160292)”and “Major research project of the national natural science foundation of China: observation and mechanism research on the mutual transformation of surface water and groundwater in Heihe river basin (91025019)”.
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Gao, Z., Wang, Z., Wang, S. et al. Factors that influence the chemical composition and evolution of shallow groundwater in an arid region: a case study from the middle reaches of the Heihe River, China. Environ Earth Sci 78, 390 (2019). https://doi.org/10.1007/s12665-019-8391-0
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DOI: https://doi.org/10.1007/s12665-019-8391-0


