Mine Water Source Discrimination Based on Hydrogeochemical Characteristics in the Northern Ordos Basin, China
Sudden inrushes of mine water from coal roofs threaten the safe production of coal in China’s northern Ordos Basin. However, due to similar hydrochemical characteristics, routine hydrochemical analysis fails to discriminate the water sources. In this study, a new method, based on the characteristics...
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Veröffentlicht in: | Mine water and the environment 2021-06, Vol.40 (2), p.433-441 |
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description | Sudden inrushes of mine water from coal roofs threaten the safe production of coal in China’s northern Ordos Basin. However, due to similar hydrochemical characteristics, routine hydrochemical analysis fails to discriminate the water sources. In this study, a new method, based on the characteristics of dissolved organic matter (DOM), the major inorganic constituents, and environmental isotopes was used to discriminate mine water sources. It turns out that the total dissolved solids concentration is less than 560.0 mg/L in the shallow aquifer and surface water, but exceeds 1000 mg/L in the deep aquifers. The concentrations of deuterium (D) and oxygen isotope (
18
O) gradually decrease in the Quaternary, Cretaceous, and Jurassic aquifers, and with increased burial depth, the age of groundwater increases. The surface water and underground aquifers differ with respect to the concentration, type, fluorescence intensity, and fluorescence regional integral of DOM. The DOM concentration and the fluorescent parameter values both generally decrease with increased burial depth. Comprehensive analysis of DOM, inorganic constituents, and environmental isotopes in water samples can be used to distinguish water sources, which may help prevent and control mine water hazards in the study area. |
doi_str_mv | 10.1007/s10230-020-00723-5 |
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18
O) gradually decrease in the Quaternary, Cretaceous, and Jurassic aquifers, and with increased burial depth, the age of groundwater increases. The surface water and underground aquifers differ with respect to the concentration, type, fluorescence intensity, and fluorescence regional integral of DOM. The DOM concentration and the fluorescent parameter values both generally decrease with increased burial depth. Comprehensive analysis of DOM, inorganic constituents, and environmental isotopes in water samples can be used to distinguish water sources, which may help prevent and control mine water hazards in the study area.</description><identifier>ISSN: 1025-9112</identifier><identifier>EISSN: 1616-1068</identifier><identifier>DOI: 10.1007/s10230-020-00723-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Altitude ; Aquifers ; Coal ; Coal mines ; Coal mining ; Constituents ; Cretaceous ; Deuterium ; Dissolved organic matter ; Dissolved solids ; Earth and Environmental Science ; Earth Sciences ; Ecotoxicology ; Fault lines ; Fluorescence ; Geology ; Groundwater ; Hydrogeochemistry ; Hydrogeology ; Hydrology ; Industrial Pollution Prevention ; Isotopes ; Jurassic ; Mine drainage ; Mine waters ; Mineral Resources ; Oxygen isotopes ; Precipitation ; Quaternary ; Rain ; Rivers ; Runoff ; Surface water ; Surface-groundwater relations ; Technical Article ; Total dissolved solids ; Water analysis ; Water depth ; Water Quality/Water Pollution ; Water sampling</subject><ispartof>Mine water and the environment, 2021-06, Vol.40 (2), p.433-441</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-8df7d7726fecf6f0ba3e37395192b2a72089ab831656e12a5fd2d0b13e95b52e3</citedby><cites>FETCH-LOGICAL-c319t-8df7d7726fecf6f0ba3e37395192b2a72089ab831656e12a5fd2d0b13e95b52e3</cites><orcidid>0000-0002-3786-3278</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10230-020-00723-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10230-020-00723-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Yang, Jian</creatorcontrib><creatorcontrib>Dong, Shuning</creatorcontrib><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Li, Guoqing</creatorcontrib><creatorcontrib>Wang, Tiantian</creatorcontrib><creatorcontrib>Wang, Qiangmin</creatorcontrib><title>Mine Water Source Discrimination Based on Hydrogeochemical Characteristics in the Northern Ordos Basin, China</title><title>Mine water and the environment</title><addtitle>Mine Water Environ</addtitle><description>Sudden inrushes of mine water from coal roofs threaten the safe production of coal in China’s northern Ordos Basin. However, due to similar hydrochemical characteristics, routine hydrochemical analysis fails to discriminate the water sources. In this study, a new method, based on the characteristics of dissolved organic matter (DOM), the major inorganic constituents, and environmental isotopes was used to discriminate mine water sources. It turns out that the total dissolved solids concentration is less than 560.0 mg/L in the shallow aquifer and surface water, but exceeds 1000 mg/L in the deep aquifers. The concentrations of deuterium (D) and oxygen isotope (
18
O) gradually decrease in the Quaternary, Cretaceous, and Jurassic aquifers, and with increased burial depth, the age of groundwater increases. The surface water and underground aquifers differ with respect to the concentration, type, fluorescence intensity, and fluorescence regional integral of DOM. The DOM concentration and the fluorescent parameter values both generally decrease with increased burial depth. Comprehensive analysis of DOM, inorganic constituents, and environmental isotopes in water samples can be used to distinguish water sources, which may help prevent and control mine water hazards in the study area.</description><subject>Altitude</subject><subject>Aquifers</subject><subject>Coal</subject><subject>Coal mines</subject><subject>Coal mining</subject><subject>Constituents</subject><subject>Cretaceous</subject><subject>Deuterium</subject><subject>Dissolved organic matter</subject><subject>Dissolved solids</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecotoxicology</subject><subject>Fault lines</subject><subject>Fluorescence</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Hydrogeochemistry</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Industrial Pollution Prevention</subject><subject>Isotopes</subject><subject>Jurassic</subject><subject>Mine drainage</subject><subject>Mine waters</subject><subject>Mineral Resources</subject><subject>Oxygen isotopes</subject><subject>Precipitation</subject><subject>Quaternary</subject><subject>Rain</subject><subject>Rivers</subject><subject>Runoff</subject><subject>Surface water</subject><subject>Surface-groundwater relations</subject><subject>Technical Article</subject><subject>Total dissolved solids</subject><subject>Water analysis</subject><subject>Water depth</subject><subject>Water Quality/Water Pollution</subject><subject>Water sampling</subject><issn>1025-9112</issn><issn>1616-1068</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kE9PAyEQxYnRxFr9Ap5IvLrKQIDlqPVvUu1BjUfCsmxL00KF7aHfXuqaePMwmTm835u8h9A5kCsgRF5nIJSRitAyRFJW8QM0AgGiAiLqw3ITyisFQI_RSc5LQkAKykdo_eKDw5-mdwm_xW2yDt_5bJNf-2B6HwO-Ndm1uBxPuzbFuYt24dbemhWeLEwytpA-995m7APuFw6_xlRWCniW2pj3vA-XRVwMT9FRZ1bZnf3uMfp4uH-fPFXT2ePz5GZaWQaqr-q2k62UVHTOdqIjjWGOSaY4KNpQIymplWlqBoILB9TwrqUtaYA5xRtOHRuji8F3k-LX1uVeL0u2UF5qqqAunKKyqOigsinmnFynNyW3STsNRO9r1UOtutSqf2rVvEBsgHIRh7lLf9b_UN8ycXrl</recordid><startdate>20210601</startdate><enddate>20210601</enddate><creator>Yang, Jian</creator><creator>Dong, Shuning</creator><creator>Wang, Hao</creator><creator>Li, Guoqing</creator><creator>Wang, Tiantian</creator><creator>Wang, Qiangmin</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7ST</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8C1</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>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</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><orcidid>https://orcid.org/0000-0002-3786-3278</orcidid></search><sort><creationdate>20210601</creationdate><title>Mine Water Source Discrimination Based on Hydrogeochemical Characteristics in the Northern Ordos Basin, China</title><author>Yang, Jian ; Dong, Shuning ; Wang, Hao ; Li, Guoqing ; Wang, Tiantian ; Wang, Qiangmin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-8df7d7726fecf6f0ba3e37395192b2a72089ab831656e12a5fd2d0b13e95b52e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Altitude</topic><topic>Aquifers</topic><topic>Coal</topic><topic>Coal mines</topic><topic>Coal mining</topic><topic>Constituents</topic><topic>Cretaceous</topic><topic>Deuterium</topic><topic>Dissolved organic matter</topic><topic>Dissolved solids</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecotoxicology</topic><topic>Fault lines</topic><topic>Fluorescence</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Hydrogeochemistry</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Industrial Pollution Prevention</topic><topic>Isotopes</topic><topic>Jurassic</topic><topic>Mine drainage</topic><topic>Mine waters</topic><topic>Mineral Resources</topic><topic>Oxygen isotopes</topic><topic>Precipitation</topic><topic>Quaternary</topic><topic>Rain</topic><topic>Rivers</topic><topic>Runoff</topic><topic>Surface water</topic><topic>Surface-groundwater relations</topic><topic>Technical Article</topic><topic>Total dissolved solids</topic><topic>Water analysis</topic><topic>Water depth</topic><topic>Water Quality/Water Pollution</topic><topic>Water sampling</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Jian</creatorcontrib><creatorcontrib>Dong, Shuning</creatorcontrib><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Li, Guoqing</creatorcontrib><creatorcontrib>Wang, Tiantian</creatorcontrib><creatorcontrib>Wang, Qiangmin</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Public Health Database</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>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>SciTech Premium Collection</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><jtitle>Mine water and the environment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yang, Jian</au><au>Dong, Shuning</au><au>Wang, Hao</au><au>Li, Guoqing</au><au>Wang, Tiantian</au><au>Wang, Qiangmin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mine Water Source Discrimination Based on Hydrogeochemical Characteristics in the Northern Ordos Basin, China</atitle><jtitle>Mine water and the environment</jtitle><stitle>Mine Water Environ</stitle><date>2021-06-01</date><risdate>2021</risdate><volume>40</volume><issue>2</issue><spage>433</spage><epage>441</epage><pages>433-441</pages><issn>1025-9112</issn><eissn>1616-1068</eissn><abstract>Sudden inrushes of mine water from coal roofs threaten the safe production of coal in China’s northern Ordos Basin. However, due to similar hydrochemical characteristics, routine hydrochemical analysis fails to discriminate the water sources. In this study, a new method, based on the characteristics of dissolved organic matter (DOM), the major inorganic constituents, and environmental isotopes was used to discriminate mine water sources. It turns out that the total dissolved solids concentration is less than 560.0 mg/L in the shallow aquifer and surface water, but exceeds 1000 mg/L in the deep aquifers. The concentrations of deuterium (D) and oxygen isotope (
18
O) gradually decrease in the Quaternary, Cretaceous, and Jurassic aquifers, and with increased burial depth, the age of groundwater increases. The surface water and underground aquifers differ with respect to the concentration, type, fluorescence intensity, and fluorescence regional integral of DOM. The DOM concentration and the fluorescent parameter values both generally decrease with increased burial depth. Comprehensive analysis of DOM, inorganic constituents, and environmental isotopes in water samples can be used to distinguish water sources, which may help prevent and control mine water hazards in the study area.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10230-020-00723-5</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0002-3786-3278</orcidid></addata></record> |
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subjects | Altitude Aquifers Coal Coal mines Coal mining Constituents Cretaceous Deuterium Dissolved organic matter Dissolved solids Earth and Environmental Science Earth Sciences Ecotoxicology Fault lines Fluorescence Geology Groundwater Hydrogeochemistry Hydrogeology Hydrology Industrial Pollution Prevention Isotopes Jurassic Mine drainage Mine waters Mineral Resources Oxygen isotopes Precipitation Quaternary Rain Rivers Runoff Surface water Surface-groundwater relations Technical Article Total dissolved solids Water analysis Water depth Water Quality/Water Pollution Water sampling |
title | Mine Water Source Discrimination Based on Hydrogeochemical Characteristics in the Northern Ordos Basin, China |
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