Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China

Abstract The Jiangcang Basin is an important mining area of the former Qilian Mountain large coal base in Qinghai Province, and understanding the groundwater circulation mechanism is the basis for studying the hydrological effects of permafrost degradation in alpine regions. In this study, hydrogeoc...

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Published in:Groundwater
Main Authors: Zhao, Chongqin, Li, Xiangquan, Wang, Zhenxing, Hou, Xinwei, Ma, Jianfei
Other Authors: National Key Research and Development Program of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1111/gwat.13363
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spelling crwiley:10.1111/gwat.13363 2024-06-02T08:13:07+00:00 Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China Zhao, Chongqin Li, Xiangquan Wang, Zhenxing Hou, Xinwei Ma, Jianfei National Key Research and Development Program of China 2023 http://dx.doi.org/10.1111/gwat.13363 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Groundwater volume 62, issue 3, page 427-438 ISSN 0017-467X 1745-6584 journal-article 2023 crwiley https://doi.org/10.1111/gwat.13363 2024-05-03T10:34:09Z Abstract The Jiangcang Basin is an important mining area of the former Qilian Mountain large coal base in Qinghai Province, and understanding the groundwater circulation mechanism is the basis for studying the hydrological effects of permafrost degradation in alpine regions. In this study, hydrogeochemical and multiple isotope tracer analysis methods are used to understand the chemical evolution and circulation mechanisms of the groundwater in the typical alpine region of the Jiangcang Basin. The diversity of the groundwater hydrochemistry in the study area reflects the complexity of the hydrogeochemical environment in which it is located. The suprapermafrost water and intrapermafrost water are recharged by modern meteoric water. The groundwater is closely hydraulically connected to the surface water with weak evaporation overall. The high δ 34 S value of deep groundwater is due to SO 4 reduction, and SO 4 2− ‐rich snow recharge with lixiviated sulfate minerals are the main controlling factor for the high SO 4 2− concentration in groundwater. According to the multivariate water conversion relationships, it reveals that the river receives more groundwater recharge, suprapermafrost water is recharged by the proportion of meteoric water, which is closely related to the mountainous area at the edge of the basin, while intrapermafrost water is mainly recharged by the shallow groundwater. This study provides a data‐driven approach to understanding groundwater recharge and evolution in alpine regions, in addition to having significant implications for water resource management and ecological environmental protection in coal bases of the Tibetan Plateau. Article in Journal/Newspaper permafrost Wiley Online Library Groundwater
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The Jiangcang Basin is an important mining area of the former Qilian Mountain large coal base in Qinghai Province, and understanding the groundwater circulation mechanism is the basis for studying the hydrological effects of permafrost degradation in alpine regions. In this study, hydrogeochemical and multiple isotope tracer analysis methods are used to understand the chemical evolution and circulation mechanisms of the groundwater in the typical alpine region of the Jiangcang Basin. The diversity of the groundwater hydrochemistry in the study area reflects the complexity of the hydrogeochemical environment in which it is located. The suprapermafrost water and intrapermafrost water are recharged by modern meteoric water. The groundwater is closely hydraulically connected to the surface water with weak evaporation overall. The high δ 34 S value of deep groundwater is due to SO 4 reduction, and SO 4 2− ‐rich snow recharge with lixiviated sulfate minerals are the main controlling factor for the high SO 4 2− concentration in groundwater. According to the multivariate water conversion relationships, it reveals that the river receives more groundwater recharge, suprapermafrost water is recharged by the proportion of meteoric water, which is closely related to the mountainous area at the edge of the basin, while intrapermafrost water is mainly recharged by the shallow groundwater. This study provides a data‐driven approach to understanding groundwater recharge and evolution in alpine regions, in addition to having significant implications for water resource management and ecological environmental protection in coal bases of the Tibetan Plateau.
author2 National Key Research and Development Program of China
format Article in Journal/Newspaper
author Zhao, Chongqin
Li, Xiangquan
Wang, Zhenxing
Hou, Xinwei
Ma, Jianfei
spellingShingle Zhao, Chongqin
Li, Xiangquan
Wang, Zhenxing
Hou, Xinwei
Ma, Jianfei
Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
author_facet Zhao, Chongqin
Li, Xiangquan
Wang, Zhenxing
Hou, Xinwei
Ma, Jianfei
author_sort Zhao, Chongqin
title Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
title_short Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
title_full Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
title_fullStr Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
title_full_unstemmed Use of Hydrogeochemistry and Isotopes for Evaluation of Groundwater in Qilian Coal Base of China
title_sort use of hydrogeochemistry and isotopes for evaluation of groundwater in qilian coal base of china
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1111/gwat.13363
genre permafrost
genre_facet permafrost
op_source Groundwater
volume 62, issue 3, page 427-438
ISSN 0017-467X 1745-6584
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/gwat.13363
container_title Groundwater
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