Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet
Groundwater is undoubtedly important for water security and eco-environmental protection, especially in areas that experience earthquakes. Analyzing the characteristics and variation of groundwater after an earthquake is significant to obtain a better understanding of the seismic risk and rational m...
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2021
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oai:doaj.org-article:255a481d4c034e129bcd016ce46c78f12021-11-11T19:57:36ZHydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet10.3390/w132131112073-4441https://doaj.org/article/255a481d4c034e129bcd016ce46c78f12021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3111https://doaj.org/toc/2073-4441Groundwater is undoubtedly important for water security and eco-environmental protection, especially in areas that experience earthquakes. Analyzing the characteristics and variation of groundwater after an earthquake is significant to obtain a better understanding of the seismic risk and rational management of groundwater resources. This study investigated the hydrogeochemical characteristics of groundwater at the epicenter of the 2021 Biru M6.1 earthquake in central Tibet, southwest China, using 23 water samples. The results showed that: (1) the hydrochemical type, hydrogen and oxygen isotope ratios, and SiO<sub>2</sub> concentrations of three hot spring water samples in the study area were significantly different from those of samples taken elsewhere, indicating that the hot spring water originates from deeper geothermal reservoirs and has undergone more distant migration and longer fractionation processes; (2) the geochemical characteristics of groundwater from some sampling sites in the epicentral area were apparently distinct from those of other shallow groundwater or surface water samples, suggesting that the groundwater environment in the epicentral area has been affected by the earthquake. Along with the macroscopic groundwater responses in the epicentral area after the earthquake, we investigated the influencing mechanisms of the earthquake on the regional groundwater environment. We conclude that a shorter distance from the epicenter to the seismogenic fault leads to a greater possibility of the generation of new fractures, which then induce macroscopic responses and chemical characteristic variations for groundwater.Pengtao YangXiaolong SunDongying LiuZhongtai HeYongsheng LiMDPI AGarticleBiru M6.1 earthquakehydrochemical characteristicshydrogen and oxygen isotopesgroundwater responseHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3111, p 3111 (2021) |
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Biru M6.1 earthquake hydrochemical characteristics hydrogen and oxygen isotopes groundwater response Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
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Biru M6.1 earthquake hydrochemical characteristics hydrogen and oxygen isotopes groundwater response Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 Pengtao Yang Xiaolong Sun Dongying Liu Zhongtai He Yongsheng Li Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
description |
Groundwater is undoubtedly important for water security and eco-environmental protection, especially in areas that experience earthquakes. Analyzing the characteristics and variation of groundwater after an earthquake is significant to obtain a better understanding of the seismic risk and rational management of groundwater resources. This study investigated the hydrogeochemical characteristics of groundwater at the epicenter of the 2021 Biru M6.1 earthquake in central Tibet, southwest China, using 23 water samples. The results showed that: (1) the hydrochemical type, hydrogen and oxygen isotope ratios, and SiO<sub>2</sub> concentrations of three hot spring water samples in the study area were significantly different from those of samples taken elsewhere, indicating that the hot spring water originates from deeper geothermal reservoirs and has undergone more distant migration and longer fractionation processes; (2) the geochemical characteristics of groundwater from some sampling sites in the epicentral area were apparently distinct from those of other shallow groundwater or surface water samples, suggesting that the groundwater environment in the epicentral area has been affected by the earthquake. Along with the macroscopic groundwater responses in the epicentral area after the earthquake, we investigated the influencing mechanisms of the earthquake on the regional groundwater environment. We conclude that a shorter distance from the epicenter to the seismogenic fault leads to a greater possibility of the generation of new fractures, which then induce macroscopic responses and chemical characteristic variations for groundwater. |
format |
article |
author |
Pengtao Yang Xiaolong Sun Dongying Liu Zhongtai He Yongsheng Li |
author_facet |
Pengtao Yang Xiaolong Sun Dongying Liu Zhongtai He Yongsheng Li |
author_sort |
Pengtao Yang |
title |
Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
title_short |
Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
title_full |
Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
title_fullStr |
Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
title_full_unstemmed |
Hydrochemical Characteristics of Groundwater at the Epicenter of the 2021 Biru M6.1 Earthquake in Central Tibet |
title_sort |
hydrochemical characteristics of groundwater at the epicenter of the 2021 biru m6.1 earthquake in central tibet |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doaj.org/article/255a481d4c034e129bcd016ce46c78f1 |
work_keys_str_mv |
AT pengtaoyang hydrochemicalcharacteristicsofgroundwaterattheepicenterofthe2021birum61earthquakeincentraltibet AT xiaolongsun hydrochemicalcharacteristicsofgroundwaterattheepicenterofthe2021birum61earthquakeincentraltibet AT dongyingliu hydrochemicalcharacteristicsofgroundwaterattheepicenterofthe2021birum61earthquakeincentraltibet AT zhongtaihe hydrochemicalcharacteristicsofgroundwaterattheepicenterofthe2021birum61earthquakeincentraltibet AT yongshengli hydrochemicalcharacteristicsofgroundwaterattheepicenterofthe2021birum61earthquakeincentraltibet |
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1718431337347547136 |