Hydrogeochemical and isotopic evidences of unique groundwater recharge patterns in the Mongolian Plateau-Reference-Cited by-同舟云学术

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Hydrogeochemical and isotopic evidences of unique groundwater recharge patterns in the Mongolian Plateau

Published:2022-05 Issue:5 Volume:36 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Ma Fenyan¹,Chen Jiaqi²^ORCID,Chen Jiansheng³^ORCID,Wang Tao⁴

Affiliation:

1. College of Civil and Transportation Engineering Hohai University Nanjing China

2. College of Computer and Information Hohai University Nanjing China

3. School of Earth Sciences and Engineering Hohai University Nanjing China

4. College of Water Conservancy and Hydropower Engineering Hohai University Nanjing China

Funder

Central University Basic Research Fund of China

National Natural Science Foundation of China

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14554

Reference35 articles.

1. Strontium isotopic evidence on the chemical evolution of pore waters in the Milk River Aquifer, Alberta, Canada

2. Spatial distribution of δ18O in meteoric precipitation

3. Strontium isotopes as tracers of ecosystem processes: theory and methods

4. External Groundwater Alleviates the Degradation of Closed Lakes in Semi-Arid Regions of China

5. New lakes in the Taklamakan Desert;Geophysical Research Letters,2012

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