Hydrochemical investigation of shallow groundwater in northwest margin of Lop Nur, northwest China
A hydrochemical investigation was conducted in northwest margin of Lop Nur to evaluate the groundwater chemical patterns and the main hydrological processes occurring in the groundwater system. Fourteen representative groundwater samples were collected from different springs and boreholes. Hydrochem...
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| Veröffentlicht in: | Environmental earth sciences 2016-02, Vol.75 (3), p.1, Article 214 |
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| creator | Zhao, Zhenhua Wu, Jichun Yuan, Gexin Chen, Jianjie Xu, Xiaofeng Yan, Changhong Bai, Youliang |
| description | A hydrochemical investigation was conducted in northwest margin of Lop Nur to evaluate the groundwater chemical patterns and the main hydrological processes occurring in the groundwater system. Fourteen representative groundwater samples were collected from different springs and boreholes. Hydrochemical data of the groundwater showed that SO
4
, Cl-Na and Cl, SO
4
-Na water types were dominant in this area, and the total dissolved solid (TDS) content rose along the flow path of the groundwater. Ionic relation analysis was used in conjunction with geochemical modeling to investigate the evolution of the chemical composition of groundwater. PHREEQC was used for inverse geochemical modeling. It is demonstrated that the groundwater, recharged mainly in the northern low mountains, acquired its mineralization properties principally from water–rock interactions, i.e., dissolution of evaporates and reverse cation exchange. The dissolution of halite, Glauber’s salt, dolomite and calcite determined the Na
+
, Cl
−
, Mg
2+
, Ca
2+
, SO
4
2−
and HCO
3
−
chemistry, but evaporation and precipitation also influenced the water composition. The shallow groundwater of Lop Nur was characterized by high salinity and slow circulation. |
| doi_str_mv | 10.1007/s12665-015-5060-9 |
| format | Article |
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4
, Cl-Na and Cl, SO
4
-Na water types were dominant in this area, and the total dissolved solid (TDS) content rose along the flow path of the groundwater. Ionic relation analysis was used in conjunction with geochemical modeling to investigate the evolution of the chemical composition of groundwater. PHREEQC was used for inverse geochemical modeling. It is demonstrated that the groundwater, recharged mainly in the northern low mountains, acquired its mineralization properties principally from water–rock interactions, i.e., dissolution of evaporates and reverse cation exchange. The dissolution of halite, Glauber’s salt, dolomite and calcite determined the Na
+
, Cl
−
, Mg
2+
, Ca
2+
, SO
4
2−
and HCO
3
−
chemistry, but evaporation and precipitation also influenced the water composition. The shallow groundwater of Lop Nur was characterized by high salinity and slow circulation.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-015-5060-9</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Biogeosciences ; Boreholes ; Calcite ; Cation exchange ; Dissolved solids ; Dolomite ; Earth and Environmental Science ; Earth Sciences ; Environmental Science and Engineering ; Evaporation ; Geochemistry ; Geology ; Groundwater ; Groundwater data ; Hydrology ; Hydrology/Water Resources ; Mathematical models ; Mineralization ; Mountains ; Original Article ; Terrestrial Pollution ; Water analysis ; Water sampling ; Water springs</subject><ispartof>Environmental earth sciences, 2016-02, Vol.75 (3), p.1, Article 214</ispartof><rights>Springer-Verlag Berlin Heidelberg 2015</rights><rights>Springer-Verlag Berlin Heidelberg 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-f528e655764bbd18b01d98ac4cdec6d74e760d6c44c88c386340fda34c9a1ad23</citedby><cites>FETCH-LOGICAL-a339t-f528e655764bbd18b01d98ac4cdec6d74e760d6c44c88c386340fda34c9a1ad23</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/s12665-015-5060-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-015-5060-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Zhao, Zhenhua</creatorcontrib><creatorcontrib>Wu, Jichun</creatorcontrib><creatorcontrib>Yuan, Gexin</creatorcontrib><creatorcontrib>Chen, Jianjie</creatorcontrib><creatorcontrib>Xu, Xiaofeng</creatorcontrib><creatorcontrib>Yan, Changhong</creatorcontrib><creatorcontrib>Bai, Youliang</creatorcontrib><title>Hydrochemical investigation of shallow groundwater in northwest margin of Lop Nur, northwest China</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>A hydrochemical investigation was conducted in northwest margin of Lop Nur to evaluate the groundwater chemical patterns and the main hydrological processes occurring in the groundwater system. Fourteen representative groundwater samples were collected from different springs and boreholes. Hydrochemical data of the groundwater showed that SO
4
, Cl-Na and Cl, SO
4
-Na water types were dominant in this area, and the total dissolved solid (TDS) content rose along the flow path of the groundwater. Ionic relation analysis was used in conjunction with geochemical modeling to investigate the evolution of the chemical composition of groundwater. PHREEQC was used for inverse geochemical modeling. It is demonstrated that the groundwater, recharged mainly in the northern low mountains, acquired its mineralization properties principally from water–rock interactions, i.e., dissolution of evaporates and reverse cation exchange. The dissolution of halite, Glauber’s salt, dolomite and calcite determined the Na
+
, Cl
−
, Mg
2+
, Ca
2+
, SO
4
2−
and HCO
3
−
chemistry, but evaporation and precipitation also influenced the water composition. The shallow groundwater of Lop Nur was characterized by high salinity and slow circulation.</description><subject>Biogeosciences</subject><subject>Boreholes</subject><subject>Calcite</subject><subject>Cation exchange</subject><subject>Dissolved solids</subject><subject>Dolomite</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Evaporation</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater data</subject><subject>Hydrology</subject><subject>Hydrology/Water Resources</subject><subject>Mathematical models</subject><subject>Mineralization</subject><subject>Mountains</subject><subject>Original Article</subject><subject>Terrestrial Pollution</subject><subject>Water analysis</subject><subject>Water sampling</subject><subject>Water springs</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE1LAzEQhoMoWGp_gLeAV1eTzccmRylqhaIXPYdskv0o201Ndi3996auSC_OZQbmeedlXgCuMbrDCBX3EeecswxhljHEUSbPwAwLzjOeS3n-Nwt0CRYxblAqgolEfAbK1cEGbxq3bY3uYNt_uTi0tR5a30NfwdjorvN7WAc_9navBxcSBHsfhmafULjVoW5_0LXfwdcx3J4sl03b6ytwUekuusVvn4OPp8f35Spbvz2_LB_WmSZEDlnFcuE4YwWnZWmxKBG2UmhDjXWG24K6giPLDaVGCEMEJxRVVhNqpMba5mQObqa7u-A_x2SvNn4MfbJUuGBSIkIESxSeKBN8jMFVahfa9MRBYaSOaaopTZXSVMc0lUyafNLExPa1CyeX_xV9A79OeME</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Zhao, Zhenhua</creator><creator>Wu, Jichun</creator><creator>Yuan, Gexin</creator><creator>Chen, Jianjie</creator><creator>Xu, Xiaofeng</creator><creator>Yan, Changhong</creator><creator>Bai, Youliang</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>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></search><sort><creationdate>20160201</creationdate><title>Hydrochemical investigation of shallow groundwater in northwest margin of Lop Nur, northwest China</title><author>Zhao, Zhenhua ; Wu, Jichun ; Yuan, Gexin ; Chen, Jianjie ; Xu, Xiaofeng ; Yan, Changhong ; Bai, Youliang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-f528e655764bbd18b01d98ac4cdec6d74e760d6c44c88c386340fda34c9a1ad23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Biogeosciences</topic><topic>Boreholes</topic><topic>Calcite</topic><topic>Cation exchange</topic><topic>Dissolved solids</topic><topic>Dolomite</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Evaporation</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Groundwater data</topic><topic>Hydrology</topic><topic>Hydrology/Water Resources</topic><topic>Mathematical models</topic><topic>Mineralization</topic><topic>Mountains</topic><topic>Original Article</topic><topic>Terrestrial Pollution</topic><topic>Water analysis</topic><topic>Water sampling</topic><topic>Water springs</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhao, Zhenhua</creatorcontrib><creatorcontrib>Wu, Jichun</creatorcontrib><creatorcontrib>Yuan, Gexin</creatorcontrib><creatorcontrib>Chen, Jianjie</creatorcontrib><creatorcontrib>Xu, Xiaofeng</creatorcontrib><creatorcontrib>Yan, Changhong</creatorcontrib><creatorcontrib>Bai, Youliang</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 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><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhao, Zhenhua</au><au>Wu, Jichun</au><au>Yuan, Gexin</au><au>Chen, Jianjie</au><au>Xu, Xiaofeng</au><au>Yan, Changhong</au><au>Bai, Youliang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrochemical investigation of shallow groundwater in northwest margin of Lop Nur, northwest China</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2016-02-01</date><risdate>2016</risdate><volume>75</volume><issue>3</issue><spage>1</spage><pages>1-</pages><artnum>214</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>A hydrochemical investigation was conducted in northwest margin of Lop Nur to evaluate the groundwater chemical patterns and the main hydrological processes occurring in the groundwater system. Fourteen representative groundwater samples were collected from different springs and boreholes. Hydrochemical data of the groundwater showed that SO
4
, Cl-Na and Cl, SO
4
-Na water types were dominant in this area, and the total dissolved solid (TDS) content rose along the flow path of the groundwater. Ionic relation analysis was used in conjunction with geochemical modeling to investigate the evolution of the chemical composition of groundwater. PHREEQC was used for inverse geochemical modeling. It is demonstrated that the groundwater, recharged mainly in the northern low mountains, acquired its mineralization properties principally from water–rock interactions, i.e., dissolution of evaporates and reverse cation exchange. The dissolution of halite, Glauber’s salt, dolomite and calcite determined the Na
+
, Cl
−
, Mg
2+
, Ca
2+
, SO
4
2−
and HCO
3
−
chemistry, but evaporation and precipitation also influenced the water composition. The shallow groundwater of Lop Nur was characterized by high salinity and slow circulation.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-015-5060-9</doi></addata></record> |
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| ispartof | Environmental earth sciences, 2016-02, Vol.75 (3), p.1, Article 214 |
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| language | eng |
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| source | SpringerNature Journals |
| subjects | Biogeosciences Boreholes Calcite Cation exchange Dissolved solids Dolomite Earth and Environmental Science Earth Sciences Environmental Science and Engineering Evaporation Geochemistry Geology Groundwater Groundwater data Hydrology Hydrology/Water Resources Mathematical models Mineralization Mountains Original Article Terrestrial Pollution Water analysis Water sampling Water springs |
| title | Hydrochemical investigation of shallow groundwater in northwest margin of Lop Nur, northwest China |
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