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Determination of soil-groundwater systems recharge mechanism in the middle Inner Mongolia Plateau by isotopic tracers

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Abstract

The steppe located in the middle Inner Mongolia Plateau (IMP) has scarce water resources and fragile ecosystems and has an arid-semiarid monsoon characterized by low and uneven seasonal precipitation and high evaporation. Until now, problems relating to the hydrologic processes in the area remain poorly understood, and thus strategies for the exploitation and utilization of the area’s local water resource remain limited. This study aimed to investigate the recharge and discharge processes of soil water and the source and circulation of groundwater through geochemical methods. The local meteoric water line (LMWI) of our study area in the middle IMP was first proposed and compared with the local meteoric water line of Baotou in Inner Mongolia and Ulan Bator. The δ18O and δD values of precipitation showed an increasing trend from June to August and decreasing trend from August to late October. The H and O isotopes of soil water varied with time, location, and soil profile depth. Besides the geographical and climatic factors, the Cl concentrations of soil water can be affected remarkably by land use type and land cover change. In our monitoring period, variations in the Cl concentrations and δ18O and δD values of shallow soil water indicated that the evaporation of soil water was in the sequence August > June > October. Furthermore, the detailed evaporation proportions of soil water were estimated. The isotope compositions of groundwater plotted on the LMWI and there could be a rapid recharge mechanism of the groundwater.

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References

  • Allison GB, Hughes MW (1978) The use of environmental chloride and tritium to estimate total recharge to an unconfined aquifer. Soil Res 16(2):181–195

    Article  Google Scholar 

  • Bao G (2015) Mongolian pines (Pinus sylvestris var. mongolica) in the Hulun Buir steppe, China, respond to climate in adjustment to the local water supply. Int J Biometeorol 59(1):1–10

    Article  Google Scholar 

  • Blasch KW, Bryson JR (2007) Distinguishing sources of ground water recharge by using δ2H and δ18O. Ground Water 45:294–308

    Article  Google Scholar 

  • Chen ZH, Xu HL (1996) Chloride tracer method for estimation natural groundwater recharge in arid and semiarid regions. Geol Sci Technol Inform 15(3):87–92

    Google Scholar 

  • Chen JS, Wang YC, Xie F, Xu Y, Chen YF, Zhan LC, Jiang QN (2016) Allogenic groundwater recharge to Erenhot Basin. Water Resour Protect 32:11–20

    Google Scholar 

  • Clark I, Fritz P (1997) Environmental isotopes in hydrogeology. CRC Press, Boca Raton, p P185

    Google Scholar 

  • Costa AM, Salis HHC, Viana JHM, Pacheco FAL (2019) Groundwater recharge potential for sustainable water use in urban areas of the Jequitiba River Basin, Brazil. Sustainability 11:2955

    Article  Google Scholar 

  • Craig H (1961) Isotopic variations in meteoric waters. Science 133:1702–1703

    Article  Google Scholar 

  • Dong Z, Qian G, Lv P, Hu G (2013) Investigation of the sand sea with the tallest dunes on Earth: China's Badain Jaran Sand Sea. Earth Sci Rev 120:20–39

    Article  Google Scholar 

  • Gammons CH, Poulson SR, Pellicori DA, Reed PJ, Roesler AJ, Petrescu E (2006) The hydrogen and oxygen isotopic composition of precipitation, evaporated mine water, and river water in Montana, USA. J Hydrol 328:319–330

    Article  Google Scholar 

  • Gao B, Zhang W, Sun ZX, Liu JH (2005) Study on hydrogeochemical properties of groundwater in Dongwu Banner, Inner Mongolia Autonomous Region. Arid Zone Res 22:431–435

    Google Scholar 

  • Gao H, Ryan M, Li C, Sun B (2017) Understanding the role of groundwater in a remote transboundary lake (Hulun Lake, China). Water 9(5):363

    Article  Google Scholar 

  • Gat JR (1996) Oxygen and hydrogen isotopes in the hydrologic cycle. Annu Rev Earth Planet Sci 24:225–262

    Article  Google Scholar 

  • Gates JB, Edmunds WM, Darling WG, Ma J, Pang Z, Young AA (2008) Conceptual model of recharge to southeastern Badain Jaran Desert groundwater and lakes from environmental tracers. Appl Geochem 23(12):3519–3534

    Article  Google Scholar 

  • Gazis C, Feng X (2004) A stable isotope study of soil water: evidence for mixing and preferential flow paths. Geoderma 119:97–111

    Article  Google Scholar 

  • Gonfiantini R (1986) Environmental isotopes in lake studies. In: Fritz P, Ch-Fontes J (eds) Handbook of Environmental Isotope geochemistry, vol 2, the terrestrial environment B. Elsevier, Amsterdam, New York, pp 113–163

    Google Scholar 

  • Liu J, Chen ZY, Wei W, Zhang YL, Li ZH, Liu FL, Guo HL (2014) Using chlorofluorocarbons (CFCs) and tritium (3H) to estimate groundwater age and flow velocity in Hohhot Basin, China. Hydrol Process 28:1372–1382

    Article  Google Scholar 

  • Liu J, Wang Y, Wei W, Zhang L, Liu FL (2017) Using stable isotope method to identify sources of groundwater recharge in Shetai Basin, Inner Monglia. J China Hydrol 37:51–55

    Google Scholar 

  • Pacheco FAL (2015) Regional groundwater flow in hard rocks. Sci Total Environ 506–507:182–195

    Article  Google Scholar 

  • Pacheco FAL, Van der Weijden CH (2014a) Modeling rock weathering in small watersheds. J Hydrol 513C:13–27

    Article  Google Scholar 

  • Pacheco FAL, Van der Weijden CH (2014b) Role of hydraulic diffusivity in the decrease of weathering rates over time. J Hydrol 512:87–106

    Article  Google Scholar 

  • Shao YS (1989) Environmental isotope geochemistry of the groundwater in Hohhot basin, Inner Mongolia. Geotech Investig Surv 4:41–43

    Google Scholar 

  • Tan HB, Zhang YF, Zhang WJ, Kong N, Zhang Q, Huang JZ (2014) Understanding the circulation of geothermal waters in the Tibetan Plateau using oxygen and hydrogen stable isotopes. Appl Geochem 51:23–32

    Article  Google Scholar 

  • Tan HB, Wen XW, Rao WB, Bradd J, Huang JZ (2016) Temporal variation of stable isotopes in a precipitation–groundwater system: implications for determining the mechanism of groundwater recharge in high mountain–hills of the Loess Plateau, China. Hydrol Process 30:1491–1505

    Article  Google Scholar 

  • Tan HB, Liu ZH, Rao WB, Jin B, Zhang Y (2017a) Understanding recharge in soil-groundwater systems in high loess hills on the Loess Plateau using isotopic data. CATENA 156:18–29

    Article  Google Scholar 

  • Tan HB, Liu ZH, Rao WB, Wei HZ, Zhang YD, Jin B (2017b) Stable isotopes of soil water: implications for soil water and shallow groundwater recharge in hill and gully regions of the Loess Plateau China. Agr Ecosyst Environ 243:1–9

    Article  Google Scholar 

  • Tang XW, Wu JK, Xue LY, Zhang MQ, Frauke B, Lutz B, Hans-Georg F (2014) Maior ion chemistry of surface water in the Xilin River Basin and the possible controls. Environ Sci 35(1):131–142

    Google Scholar 

  • Tenenwurcel MA, Moura MS, Costa AM, Mota PK, Viana JHM, Sanches Fernandes LF, Pacheco FAL (2020) An improved model for the evaluation of groundwater recharge based on the Concept of Conservative Use Potential: a study in the River Pandeiros Watershed, Minas Gerais, Brazil. Water 12:1001

    Article  Google Scholar 

  • Vogel JC, Urk VH (1975) Isotopic composition of groundwater in semi-arid regions of southern Africa. J Hydrol 25:23–36

    Article  Google Scholar 

  • Wang R (2014) The Sanshui Transformation Mechanism Analysis of Luanhe River Basin Based on environmental isotope data. Master Thesis, Inner Mongolia Agricultural University

  • Wang P, Yu J, Zhang Y, Liu C (2013) Groundwater recharge and hydrogeochemical evolution in the Ejina Basin, northwest China. J Hydrol 476:72–86

    Article  Google Scholar 

  • Wang ZY, Hou J, Qu ZQ, Guo JY, Li JR (2017) Root distribution of 430 plants in temperate grassland of northern China. Appl Ecol Env Res 15:1625–1651

    Article  Google Scholar 

  • Wang Y, Chen M, Yan L, Hu Y, Deng W, Zhou F (2019) Critical depth of groundwater recharge for vegetation in semi-arid areas. In: IOP Conference Series: Earth and Environmental Science (Vol. 237, No. 3,). IOP Publishing, p 032091

  • Wassenaar LI, Athanasopoulos P, Hendry MJ (2011) Isotope hydrology of precipitation, surface and ground waters in the Okanagan Valley, British Columbia, Canada. J Hydrol 411:37–48

    Article  Google Scholar 

  • Xi H, Feng Q, Liu W, Si J, Chang Z, Su Y (2010) The research of groundwater flow model in Ejina Basin, Northwestern China. Environ Earth Sciences 60(5):953–963

    Article  Google Scholar 

  • Yang QY, Wu JK, Ding YJ, Ye BS, Zhang MQ (2009) A study of isotope hydrology in shallow groundwater and stream water in the Xinlin River Basin. J Glaciol Geocryol 31(5):850–856

    Google Scholar 

  • Zhao L, Xiao H, Dong Z, Xiao S, Zhou M, Cheng G, Yin Z (2012) Origins of groundwater inferred from isotopic patterns of the Badain Jaran Desert Northwestern China. Groundwater 50(5):715–725

    Article  Google Scholar 

Download references

Acknowledgements

This study was financially supported by National Natural Science Foundation of China (41807215 and 51609153), the Fundamental Research Fund of the China Institute of Water Resources and Hydropower Research (MK2019J12 and MK2017J01).

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Authors and Affiliations

  1. Institute of Water Resource for Pastoral Area, Ministry of Water Resources of the People’s Republic of China, Hohhot, China

    Yanfei Zhang, Yongfu Wei, Zilong Liao, Xiaomin Xu, Zhenhua Han, Wentao Liang, Yinhui Long & Jianying Guo

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  1. Yanfei Zhang
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  2. Yongfu Wei
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  3. Zilong Liao
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  4. Xiaomin Xu
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Correspondence to Yanfei Zhang.

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Zhang, Y., Wei, Y., Liao, Z. et al. Determination of soil-groundwater systems recharge mechanism in the middle Inner Mongolia Plateau by isotopic tracers. Environ Earth Sci 79, 473 (2020). https://doi.org/10.1007/s12665-020-09226-6

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