Hydrochemical formation mechanism of mineral springs in Changbai Mountain (China)

Changbai Mountain area is an important mineral water storage and development area in China. The hydrochemical composition of mineral water is the decisive factor for mineral–water quality. Based on the hydrochemical data of 74 mineral water samples collected from 2018 to 2020, the characteristics an...

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Veröffentlicht in:Environmental earth sciences 2023-03, Vol.82 (6), p.145-145, Article 145
Hauptverfasser: Bian, Jianmin, Sun, Wenhao, Li, Jialin, Li, Yihan, Ma, Yuxi, Li, Yanmei
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container_issue 6
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container_title Environmental earth sciences
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creator Bian, Jianmin
Sun, Wenhao
Li, Jialin
Li, Yihan
Ma, Yuxi
Li, Yanmei
description Changbai Mountain area is an important mineral water storage and development area in China. The hydrochemical composition of mineral water is the decisive factor for mineral–water quality. Based on the hydrochemical data of 74 mineral water samples collected from 2018 to 2020, the characteristics and formation mechanism of the hydrochemical components of the mineral water were analyzed. The results show that the formation of single-type mineral springs (metasilicate mineral water) is controlled by rock weathering; compound mineral springs (metasilicate mineral water with high CO 2 content) are the product of CO 2 -rich, weakly acidic, confined hot groundwater with high salinity, which are mixed with shallow groundwater as rising along the fracture. The volcanic geological process greatly influences the formation of the hydrochemical components of mineral springs on the North slope of Changbai Mountain. The mineral springs on the Longgang Mountain are greatly affected by human activities. The results of cluster analysis only consider that hydrochemical components are consistent with the classification of the areas which concentrated distributions of mineral as determined by hydrogeological and geomorphological studies. The results of this study are useful for understanding the distribution, hydrochemical characteristics, and formation mechanism of mineral springs in the Changbai Mountain area of China and provide the theoretical basis for the protection and development of mineral spring.
doi_str_mv 10.1007/s12665-023-10795-5
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The hydrochemical composition of mineral water is the decisive factor for mineral–water quality. Based on the hydrochemical data of 74 mineral water samples collected from 2018 to 2020, the characteristics and formation mechanism of the hydrochemical components of the mineral water were analyzed. The results show that the formation of single-type mineral springs (metasilicate mineral water) is controlled by rock weathering; compound mineral springs (metasilicate mineral water with high CO 2 content) are the product of CO 2 -rich, weakly acidic, confined hot groundwater with high salinity, which are mixed with shallow groundwater as rising along the fracture. The volcanic geological process greatly influences the formation of the hydrochemical components of mineral springs on the North slope of Changbai Mountain. The mineral springs on the Longgang Mountain are greatly affected by human activities. The results of cluster analysis only consider that hydrochemical components are consistent with the classification of the areas which concentrated distributions of mineral as determined by hydrogeological and geomorphological studies. 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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a375t-a51f5c04b379ec607e0da32f0040844aaaa8c7cf9193a1ce62aaa10fda211fd33</citedby><cites>FETCH-LOGICAL-a375t-a51f5c04b379ec607e0da32f0040844aaaa8c7cf9193a1ce62aaa10fda211fd33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-023-10795-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-023-10795-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Bian, Jianmin</creatorcontrib><creatorcontrib>Sun, Wenhao</creatorcontrib><creatorcontrib>Li, Jialin</creatorcontrib><creatorcontrib>Li, Yihan</creatorcontrib><creatorcontrib>Ma, Yuxi</creatorcontrib><creatorcontrib>Li, Yanmei</creatorcontrib><title>Hydrochemical formation mechanism of mineral springs in Changbai Mountain (China)</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>Changbai Mountain area is an important mineral water storage and development area in China. The hydrochemical composition of mineral water is the decisive factor for mineral–water quality. Based on the hydrochemical data of 74 mineral water samples collected from 2018 to 2020, the characteristics and formation mechanism of the hydrochemical components of the mineral water were analyzed. The results show that the formation of single-type mineral springs (metasilicate mineral water) is controlled by rock weathering; compound mineral springs (metasilicate mineral water with high CO 2 content) are the product of CO 2 -rich, weakly acidic, confined hot groundwater with high salinity, which are mixed with shallow groundwater as rising along the fracture. The volcanic geological process greatly influences the formation of the hydrochemical components of mineral springs on the North slope of Changbai Mountain. The mineral springs on the Longgang Mountain are greatly affected by human activities. 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The hydrochemical composition of mineral water is the decisive factor for mineral–water quality. Based on the hydrochemical data of 74 mineral water samples collected from 2018 to 2020, the characteristics and formation mechanism of the hydrochemical components of the mineral water were analyzed. The results show that the formation of single-type mineral springs (metasilicate mineral water) is controlled by rock weathering; compound mineral springs (metasilicate mineral water with high CO 2 content) are the product of CO 2 -rich, weakly acidic, confined hot groundwater with high salinity, which are mixed with shallow groundwater as rising along the fracture. The volcanic geological process greatly influences the formation of the hydrochemical components of mineral springs on the North slope of Changbai Mountain. The mineral springs on the Longgang Mountain are greatly affected by human activities. The results of cluster analysis only consider that hydrochemical components are consistent with the classification of the areas which concentrated distributions of mineral as determined by hydrogeological and geomorphological studies. The results of this study are useful for understanding the distribution, hydrochemical characteristics, and formation mechanism of mineral springs in the Changbai Mountain area of China and provide the theoretical basis for the protection and development of mineral spring.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-023-10795-5</doi><tpages>1</tpages></addata></record>
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source Springer Nature - Complete Springer Journals
subjects Biogeosciences
Carbon dioxide
China
Cluster analysis
Components
Confined groundwater
Earth and Environmental Science
Earth Sciences
Environmental Science and Engineering
Geochemistry
Geological processes
Geology
Geomorphology
Groundwater
humans
Hydrochemicals
hydrochemistry
Hydrogeology
Hydrology/Water Resources
Mineral springs
Mineral water
Minerals
Mountain regions
Mountains
Original Article
Salinity
springs (water)
Terrestrial Pollution
topographic slope
Water analysis
Water quality
Water sampling
Water springs
Water storage
Weathering
title Hydrochemical formation mechanism of mineral springs in Changbai Mountain (China)
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