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

Author:

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

Funder

National Natural Science Foundation of China

Fundamental Research Fund of the China Institute of Water Resources and Hydropower Research

Young Scientists Fund

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Reference37 articles.

1. 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

2. 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

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

4. 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

5. 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

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