Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau
Thermokarst lakes are a ubiquitous landscape feature that impact the thermal state, hydrological process, ecological environment, and engineering stability of the permafrost. This study established the hydrochemistry and stable isotope (δ 18 O and δD) variations of lake water and groundwater in a ty...
Published in: | Water |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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MDPI AG
2020
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Online Access: | https://doi.org/10.3390/w12082269 https://doaj.org/article/806c4d73e9524c839400d8f61568916c |
_version_ | 1821682191613034496 |
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author | Jinlong Li Wei Wang Dahao Wang Jiaqi Li Jie Dong |
author_facet | Jinlong Li Wei Wang Dahao Wang Jiaqi Li Jie Dong |
author_sort | Jinlong Li |
collection | Directory of Open Access Journals: DOAJ Articles |
container_issue | 8 |
container_start_page | 2269 |
container_title | Water |
container_volume | 12 |
description | Thermokarst lakes are a ubiquitous landscape feature that impact the thermal state, hydrological process, ecological environment, and engineering stability of the permafrost. This study established the hydrochemistry and stable isotope (δ 18 O and δD) variations of lake water and groundwater in a typical basin located in the central Qinghai–Tibet Plateau (QTP) of China. The results showed that most water samples could be classified as slightly alkaline, with high levels of salinity and hardness, while the dominant water types were HCO 3 -CO 3 and Cl types. Natural hydrochemical processes, such as mineral dissolution, cation exchange, and groundwater evaporation, had strong impacts on the groundwater chemistry in this region. Dissolution of halite and carbonate minerals causes the major reactions controlling water chemistry in this basin. Additionally, the calculation of the saturation index (SI) values suggested that aragonite, calcite, and dolomite are saturated, while halite is not. Based on the analysis of the stable isotope characteristics, atmospheric precipitation, groundwater, and meltwater from the permafrost are the major sources of thermokarst lakes. Moreover, the evaporation-to-inflow ratio (E/I) indicated that all of the lakes continuously expanded and rapidly developed. Overall, groundwater is an crucial source of lake recharge and its hydrochemical characteristics also have a certain impact on lake water quality. |
format | Article in Journal/Newspaper |
genre | permafrost Thermokarst |
genre_facet | permafrost Thermokarst |
id | ftdoajarticles:oai:doaj.org/article:806c4d73e9524c839400d8f61568916c |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_doi | https://doi.org/10.3390/w12082269 |
op_relation | https://www.mdpi.com/2073-4441/12/8/2269 https://doaj.org/toc/2073-4441 doi:10.3390/w12082269 2073-4441 https://doaj.org/article/806c4d73e9524c839400d8f61568916c |
op_source | Water, Vol 12, Iss 2269, p 2269 (2020) |
publishDate | 2020 |
publisher | MDPI AG |
record_format | openpolar |
spelling | ftdoajarticles:oai:doaj.org/article:806c4d73e9524c839400d8f61568916c 2025-01-17T00:16:02+00:00 Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau Jinlong Li Wei Wang Dahao Wang Jiaqi Li Jie Dong 2020-08-01T00:00:00Z https://doi.org/10.3390/w12082269 https://doaj.org/article/806c4d73e9524c839400d8f61568916c EN eng MDPI AG https://www.mdpi.com/2073-4441/12/8/2269 https://doaj.org/toc/2073-4441 doi:10.3390/w12082269 2073-4441 https://doaj.org/article/806c4d73e9524c839400d8f61568916c Water, Vol 12, Iss 2269, p 2269 (2020) groundwater thermokarst lake hydrochemical characteristics stable isotopic Qinghai–Tibet Plateau Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 article 2020 ftdoajarticles https://doi.org/10.3390/w12082269 2022-12-30T21:19:22Z Thermokarst lakes are a ubiquitous landscape feature that impact the thermal state, hydrological process, ecological environment, and engineering stability of the permafrost. This study established the hydrochemistry and stable isotope (δ 18 O and δD) variations of lake water and groundwater in a typical basin located in the central Qinghai–Tibet Plateau (QTP) of China. The results showed that most water samples could be classified as slightly alkaline, with high levels of salinity and hardness, while the dominant water types were HCO 3 -CO 3 and Cl types. Natural hydrochemical processes, such as mineral dissolution, cation exchange, and groundwater evaporation, had strong impacts on the groundwater chemistry in this region. Dissolution of halite and carbonate minerals causes the major reactions controlling water chemistry in this basin. Additionally, the calculation of the saturation index (SI) values suggested that aragonite, calcite, and dolomite are saturated, while halite is not. Based on the analysis of the stable isotope characteristics, atmospheric precipitation, groundwater, and meltwater from the permafrost are the major sources of thermokarst lakes. Moreover, the evaporation-to-inflow ratio (E/I) indicated that all of the lakes continuously expanded and rapidly developed. Overall, groundwater is an crucial source of lake recharge and its hydrochemical characteristics also have a certain impact on lake water quality. Article in Journal/Newspaper permafrost Thermokarst Directory of Open Access Journals: DOAJ Articles Water 12 8 2269 |
spellingShingle | groundwater thermokarst lake hydrochemical characteristics stable isotopic Qinghai–Tibet Plateau Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 Jinlong Li Wei Wang Dahao Wang Jiaqi Li Jie Dong Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title | Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title_full | Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title_fullStr | Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title_full_unstemmed | Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title_short | Hydrochemical and Stable Isotope Characteristics of Lake Water and Groundwater in the Beiluhe Basin, Qinghai–Tibet Plateau |
title_sort | hydrochemical and stable isotope characteristics of lake water and groundwater in the beiluhe basin, qinghai–tibet plateau |
topic | groundwater thermokarst lake hydrochemical characteristics stable isotopic Qinghai–Tibet Plateau Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
topic_facet | groundwater thermokarst lake hydrochemical characteristics stable isotopic Qinghai–Tibet Plateau Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
url | https://doi.org/10.3390/w12082269 https://doaj.org/article/806c4d73e9524c839400d8f61568916c |