Abstract
We investigated major ions, stable isotopes, and radiocarbon dates in a Quaternary aquifer in semi-arid northwestern China to gain insights into groundwater recharge and evolution. Most deep and shallow groundwater in the Helan Mountains was fresh, with total dissolved solids <1,000 mg L−1 and Cl− <250 mg L−1. The relationships of major ions with Cl− suggest strong dissolution of evaporites. However, dissolution of carbonates, albite weathering, and ion exchange are also the major groundwater process in Jilantai basin. The shallow desert groundwater is enriched in δ18O and intercepts the local meteoric water line at δ18O = −13.4 ‰, indicating that direct infiltration is a minor recharge source. The isotope compositions in intermediate confined aquifers resemble those of shallow unconfined groundwater, revealing that upward recharge from intermediate formations is a major source of shallow groundwater in the plains and desert. The estimated residence time of 10.0 kyr at one desert site, indicating that some replenishment of desert aquifers occurred in the late Pleistocene and early Holocene with a wetter and colder climate than at present.
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Acknowledgments
This research was supported by the National Natural Science Foundation of China (Nos. 41271039 and 41172163), the Fundamental Research Funds for the Central Universities, and the Key grant Project of the Chinese Ministry of Education (No. 310005). This work also forms part of the 111 project (No. B06026), the wider UK-China research collaboration, the program for New Century Excellent Talents in University (No. NCET-12-0251), and the Fundamental Research Funds for the Central Universities (Grant No. lzujbky-2013-k17). We thank Xifen Zhu, Jianhua He, Xiang Xu, Can Ma and Jingfang Wang for their assistance with our field work and laboratory analysis.
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Wei, G., Chen, F., Ma, J. et al. Groundwater recharge and evolution of water quality in China’s Jilantai Basin based on hydrogeochemical and isotopic evidence. Environ Earth Sci 72, 3491–3506 (2014). https://doi.org/10.1007/s12665-014-3257-y
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DOI: https://doi.org/10.1007/s12665-014-3257-y