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 |
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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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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.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-023-10795-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>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</subject><ispartof>Environmental earth sciences, 2023-03, Vol.82 (6), p.145-145, Article 145</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. 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. 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.</description><subject>Biogeosciences</subject><subject>Carbon dioxide</subject><subject>China</subject><subject>Cluster analysis</subject><subject>Components</subject><subject>Confined groundwater</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Geochemistry</subject><subject>Geological processes</subject><subject>Geology</subject><subject>Geomorphology</subject><subject>Groundwater</subject><subject>humans</subject><subject>Hydrochemicals</subject><subject>hydrochemistry</subject><subject>Hydrogeology</subject><subject>Hydrology/Water Resources</subject><subject>Mineral springs</subject><subject>Mineral water</subject><subject>Minerals</subject><subject>Mountain regions</subject><subject>Mountains</subject><subject>Original Article</subject><subject>Salinity</subject><subject>springs (water)</subject><subject>Terrestrial Pollution</subject><subject>topographic slope</subject><subject>Water analysis</subject><subject>Water quality</subject><subject>Water sampling</subject><subject>Water springs</subject><subject>Water storage</subject><subject>Weathering</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kE1LxDAQhosouOj-AU8FL-uhmo_m6yhFXWFFBD2HbJrsZmmTNWkP---NVhQ8OJcZZt53mHmK4gKCawgAu0kQUUoqgHAFAROkIkfFDHJKK4qEOP6pOTgt5intQA4MsQB0VrwsD20Memt6p1VX2hB7Nbjgy97orfIu9WWwZe-8iXmc9tH5TSqdL5s83ayVK5_C6AeVO4tm67y6Oi9OrOqSmX_ns-Lt_u61WVar54fH5nZVKczIUCkCLdGgXmMmjKaAGdAqjCwANeB1rXJwzbQVUGAFtaEodyCwrUIQ2hbjs2Ix7d3H8D6aNMjeJW26TnkTxiQR50wIyCDP0ss_0l0Yo8_XScQ4qTnBFGYVmlQ6hpSisTJ_26t4kBDIT9ByAi0zaPkFWpJswpNpQmPi7-p_XB_DuYAZ</recordid><startdate>20230301</startdate><enddate>20230301</enddate><creator>Bian, Jianmin</creator><creator>Sun, Wenhao</creator><creator>Li, Jialin</creator><creator>Li, Yihan</creator><creator>Ma, Yuxi</creator><creator>Li, Yanmei</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7S9</scope><scope>L.6</scope></search><sort><creationdate>20230301</creationdate><title>Hydrochemical formation mechanism of mineral springs in Changbai Mountain (China)</title><author>Bian, Jianmin ; Sun, Wenhao ; Li, Jialin ; Li, Yihan ; Ma, Yuxi ; Li, Yanmei</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a375t-a51f5c04b379ec607e0da32f0040844aaaa8c7cf9193a1ce62aaa10fda211fd33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Biogeosciences</topic><topic>Carbon dioxide</topic><topic>China</topic><topic>Cluster analysis</topic><topic>Components</topic><topic>Confined groundwater</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Geochemistry</topic><topic>Geological processes</topic><topic>Geology</topic><topic>Geomorphology</topic><topic>Groundwater</topic><topic>humans</topic><topic>Hydrochemicals</topic><topic>hydrochemistry</topic><topic>Hydrogeology</topic><topic>Hydrology/Water Resources</topic><topic>Mineral springs</topic><topic>Mineral water</topic><topic>Minerals</topic><topic>Mountain regions</topic><topic>Mountains</topic><topic>Original Article</topic><topic>Salinity</topic><topic>springs (water)</topic><topic>Terrestrial Pollution</topic><topic>topographic slope</topic><topic>Water analysis</topic><topic>Water quality</topic><topic>Water sampling</topic><topic>Water springs</topic><topic>Water storage</topic><topic>Weathering</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bian, Jianmin</creatorcontrib><creatorcontrib>Sun, Wenhao</creatorcontrib><creatorcontrib>Li, Jialin</creatorcontrib><creatorcontrib>Li, Yihan</creatorcontrib><creatorcontrib>Ma, Yuxi</creatorcontrib><creatorcontrib>Li, Yanmei</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bian, Jianmin</au><au>Sun, Wenhao</au><au>Li, Jialin</au><au>Li, Yihan</au><au>Ma, Yuxi</au><au>Li, Yanmei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrochemical formation mechanism of mineral springs in Changbai Mountain (China)</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2023-03-01</date><risdate>2023</risdate><volume>82</volume><issue>6</issue><spage>145</spage><epage>145</epage><pages>145-145</pages><artnum>145</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>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.</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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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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