Source of salinity in the groundwater of Lenjanat Plain, Isfahan, Iran
The present study aimed at identifying the salinity source in the groundwater of Lenjanat Plain. To do so, non-isotopic geochemical methods were employed: groundwater samples were collected seasonally from 33 wells widespread in the area, and physicochemical parameters as well as major and minor ele...
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| Veröffentlicht in: | Environmental earth sciences 2013, Vol.68 (2), p.413-427 |
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| description | The present study aimed at identifying the salinity source in the groundwater of Lenjanat Plain. To do so, non-isotopic geochemical methods were employed: groundwater samples were collected seasonally from 33 wells widespread in the area, and physicochemical parameters as well as major and minor elements were measured in the 132 samples. The data collected from the field and laboratory measurements were interpreted through statistical and hydrogeochemical graphs, mass ratios and saturation indexes obtained from modeling. The results revealed that hydrogeochemical properties of the study aquifer were controlled by rock/water interactions including ion exchange, dissolution of evaporation deposits (halite and gypsum) and precipitation/dissolution of carbonates. Based on the values of Cl/Br ratio in Lenjanat groundwater (329–4,492), dissolution of evaporation deposits in aquifer was the main cause for groundwater salinity. Considering the Lenjanat groundwater geochemical properties, the data confirm the reported Cl/Br ratios for groundwater affected by the dissolution of evaporation deposits (Cl/Br > 300) and overlaps with the range of Cl/Br ratios for domestic sewage effluent groundwater. Selecting the best chemical components and their ratios in non-isotopic geochemical methods provides an accurate distinction between sources of groundwater salinity. |
| doi_str_mv | 10.1007/s12665-012-1746-4 |
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To do so, non-isotopic geochemical methods were employed: groundwater samples were collected seasonally from 33 wells widespread in the area, and physicochemical parameters as well as major and minor elements were measured in the 132 samples. The data collected from the field and laboratory measurements were interpreted through statistical and hydrogeochemical graphs, mass ratios and saturation indexes obtained from modeling. The results revealed that hydrogeochemical properties of the study aquifer were controlled by rock/water interactions including ion exchange, dissolution of evaporation deposits (halite and gypsum) and precipitation/dissolution of carbonates. Based on the values of Cl/Br ratio in Lenjanat groundwater (329–4,492), dissolution of evaporation deposits in aquifer was the main cause for groundwater salinity. Considering the Lenjanat groundwater geochemical properties, the data confirm the reported Cl/Br ratios for groundwater affected by the dissolution of evaporation deposits (Cl/Br > 300) and overlaps with the range of Cl/Br ratios for domestic sewage effluent groundwater. Selecting the best chemical components and their ratios in non-isotopic geochemical methods provides an accurate distinction between sources of groundwater salinity.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-012-1746-4</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Aquifers ; Biogeosciences ; bromine ; Carbonates ; Deposition ; Dissolution ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental science ; Environmental Science and Engineering ; Evaporation ; Exact sciences and technology ; Geochemistry ; Geology ; Groundwater ; Groundwater data ; Gypsum ; Household wastes ; Hydrogeology ; Hydrology. Hydrogeology ; Hydrology/Water Resources ; ion exchange ; Original Article ; Physicochemical properties ; Pollution, environment geology ; Salinity ; Samples ; Saturation index ; Sewage ; sewage effluent ; Statistical methods ; Terrestrial Pollution ; Water analysis ; Water sampling ; wells</subject><ispartof>Environmental earth sciences, 2013, Vol.68 (2), p.413-427</ispartof><rights>Springer-Verlag 2012</rights><rights>2014 INIST-CNRS</rights><rights>Springer-Verlag Berlin Heidelberg 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a426t-51fb6f19326b235b9ce5f79176f48fa59c5c16b6d4ff0094f8478f0493f050313</citedby><cites>FETCH-LOGICAL-a426t-51fb6f19326b235b9ce5f79176f48fa59c5c16b6d4ff0094f8478f0493f050313</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/s12665-012-1746-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-012-1746-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,4023,27922,27923,27924,41487,42556,51318</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27637439$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Nassery, Hamid Reza</creatorcontrib><creatorcontrib>Kayhomayoon, Zahra</creatorcontrib><title>Source of salinity in the groundwater of Lenjanat Plain, Isfahan, Iran</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>The present study aimed at identifying the salinity source in the groundwater of Lenjanat Plain. To do so, non-isotopic geochemical methods were employed: groundwater samples were collected seasonally from 33 wells widespread in the area, and physicochemical parameters as well as major and minor elements were measured in the 132 samples. The data collected from the field and laboratory measurements were interpreted through statistical and hydrogeochemical graphs, mass ratios and saturation indexes obtained from modeling. The results revealed that hydrogeochemical properties of the study aquifer were controlled by rock/water interactions including ion exchange, dissolution of evaporation deposits (halite and gypsum) and precipitation/dissolution of carbonates. Based on the values of Cl/Br ratio in Lenjanat groundwater (329–4,492), dissolution of evaporation deposits in aquifer was the main cause for groundwater salinity. Considering the Lenjanat groundwater geochemical properties, the data confirm the reported Cl/Br ratios for groundwater affected by the dissolution of evaporation deposits (Cl/Br > 300) and overlaps with the range of Cl/Br ratios for domestic sewage effluent groundwater. Selecting the best chemical components and their ratios in non-isotopic geochemical methods provides an accurate distinction between sources of groundwater salinity.</description><subject>Aquifers</subject><subject>Biogeosciences</subject><subject>bromine</subject><subject>Carbonates</subject><subject>Deposition</subject><subject>Dissolution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental science</subject><subject>Environmental Science and Engineering</subject><subject>Evaporation</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater data</subject><subject>Gypsum</subject><subject>Household wastes</subject><subject>Hydrogeology</subject><subject>Hydrology. Hydrogeology</subject><subject>Hydrology/Water Resources</subject><subject>ion exchange</subject><subject>Original Article</subject><subject>Physicochemical properties</subject><subject>Pollution, environment geology</subject><subject>Salinity</subject><subject>Samples</subject><subject>Saturation index</subject><subject>Sewage</subject><subject>sewage effluent</subject><subject>Statistical methods</subject><subject>Terrestrial Pollution</subject><subject>Water analysis</subject><subject>Water sampling</subject><subject>wells</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</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>eNp9kE9LxDAQxYsoKLofwJMFETxYzeRvcxRxVVhQWPccpjVZu9RUky6y397ULiIenMsMzG8eb16WHQO5BELUVQQqpSgI0AIUlwXfyQ6glLKQVOvdn7kk-9kkxhVJxYBpIg-y6bxbh9rmncsjto1v-k3e-Lx_tfkydGv_8om9DcN6Zv0KPfb5U4uNv8gfosNXHIaA_ijbc9hGO9n2w2wxvX2-uS9mj3cPN9ezAjmVfSHAVdKBZlRWlIlK11Y4pUFJx0uHQteiBlnJF-4cIZq7kqvSEa6ZI2LwfJidj7rvoftY29ibtybWtm3R224dDTAQEhQVPKGnf9BVetUnd-Y7LiWAqUTBSNWhizFYZ95D84ZhY4CYIVwzhmtSuGYI1wzKZ1tljDW2Lv1fN_HnkCrJFGc6cXTkYlr5pQ2_HPwjfjIeOewMLkMSXswpAU4IEK4YZV-r_o8W</recordid><startdate>2013</startdate><enddate>2013</enddate><creator>Nassery, Hamid Reza</creator><creator>Kayhomayoon, Zahra</creator><general>Springer-Verlag</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><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>7SU</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>2013</creationdate><title>Source of salinity in the groundwater of Lenjanat Plain, Isfahan, Iran</title><author>Nassery, Hamid Reza ; Kayhomayoon, Zahra</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a426t-51fb6f19326b235b9ce5f79176f48fa59c5c16b6d4ff0094f8478f0493f050313</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Aquifers</topic><topic>Biogeosciences</topic><topic>bromine</topic><topic>Carbonates</topic><topic>Deposition</topic><topic>Dissolution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Environmental science</topic><topic>Environmental Science and Engineering</topic><topic>Evaporation</topic><topic>Exact sciences and technology</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Groundwater data</topic><topic>Gypsum</topic><topic>Household wastes</topic><topic>Hydrogeology</topic><topic>Hydrology. Hydrogeology</topic><topic>Hydrology/Water Resources</topic><topic>ion exchange</topic><topic>Original Article</topic><topic>Physicochemical properties</topic><topic>Pollution, environment geology</topic><topic>Salinity</topic><topic>Samples</topic><topic>Saturation index</topic><topic>Sewage</topic><topic>sewage effluent</topic><topic>Statistical methods</topic><topic>Terrestrial Pollution</topic><topic>Water analysis</topic><topic>Water sampling</topic><topic>wells</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Nassery, Hamid Reza</creatorcontrib><creatorcontrib>Kayhomayoon, Zahra</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><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>Environmental Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Nassery, Hamid Reza</au><au>Kayhomayoon, Zahra</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Source of salinity in the groundwater of Lenjanat Plain, Isfahan, Iran</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2013</date><risdate>2013</risdate><volume>68</volume><issue>2</issue><spage>413</spage><epage>427</epage><pages>413-427</pages><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>The present study aimed at identifying the salinity source in the groundwater of Lenjanat Plain. To do so, non-isotopic geochemical methods were employed: groundwater samples were collected seasonally from 33 wells widespread in the area, and physicochemical parameters as well as major and minor elements were measured in the 132 samples. The data collected from the field and laboratory measurements were interpreted through statistical and hydrogeochemical graphs, mass ratios and saturation indexes obtained from modeling. The results revealed that hydrogeochemical properties of the study aquifer were controlled by rock/water interactions including ion exchange, dissolution of evaporation deposits (halite and gypsum) and precipitation/dissolution of carbonates. Based on the values of Cl/Br ratio in Lenjanat groundwater (329–4,492), dissolution of evaporation deposits in aquifer was the main cause for groundwater salinity. Considering the Lenjanat groundwater geochemical properties, the data confirm the reported Cl/Br ratios for groundwater affected by the dissolution of evaporation deposits (Cl/Br > 300) and overlaps with the range of Cl/Br ratios for domestic sewage effluent groundwater. Selecting the best chemical components and their ratios in non-isotopic geochemical methods provides an accurate distinction between sources of groundwater salinity.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s12665-012-1746-4</doi><tpages>15</tpages></addata></record> |
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| subjects | Aquifers Biogeosciences bromine Carbonates Deposition Dissolution Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental science Environmental Science and Engineering Evaporation Exact sciences and technology Geochemistry Geology Groundwater Groundwater data Gypsum Household wastes Hydrogeology Hydrology. Hydrogeology Hydrology/Water Resources ion exchange Original Article Physicochemical properties Pollution, environment geology Salinity Samples Saturation index Sewage sewage effluent Statistical methods Terrestrial Pollution Water analysis Water sampling wells |
| title | Source of salinity in the groundwater of Lenjanat Plain, Isfahan, Iran |
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