Origin of Salinity in Groundwater of Neighboring Villages of the Cerro Prieto Geothermal Field
The residual brine of the Cerro Prieto Geothermal Field (CPGF) is disposed in an evaporation pond. The seepage of this pond has contaminated the water and agricultural soil around it. The contamination of the groundwater towards the southwest by the evaporation pond, in the direction of the regional...
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| Veröffentlicht in: | Water, air, and soil pollution air, and soil pollution, 2010-11, Vol.213 (1-4), p.389-400 |
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| creator | Moncada-Aguilar, Andrés M Ramírez-Hernández, Jorge Quintero-Núñez, Margarito Avendaño-Reyes, Leonel |
| description | The residual brine of the Cerro Prieto Geothermal Field (CPGF) is disposed in an evaporation pond. The seepage of this pond has contaminated the water and agricultural soil around it. The contamination of the groundwater towards the southwest by the evaporation pond, in the direction of the regional flow, has been shown before. Hydrogeochemical modeling (PHREEQCI) and Schoeller and Piper diagrams have been used in this work to show that the chemical composition of the groundwater in villages neighboring CPGF is the product of mixing between irrigation water from the Colorado River and brine from the evaporation pond. The high potassium concentration in the water and the relative increase in concentration of sodium and chlorides along the flow path as well as the hydrogeochemical models for this system explain this mixing process. This work will allow proposing new managing techniques to avoid the presence of the residual brine in the groundwater of agricultural lands. |
| doi_str_mv | 10.1007/s11270-010-0393-1 |
| format | Article |
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The seepage of this pond has contaminated the water and agricultural soil around it. The contamination of the groundwater towards the southwest by the evaporation pond, in the direction of the regional flow, has been shown before. Hydrogeochemical modeling (PHREEQCI) and Schoeller and Piper diagrams have been used in this work to show that the chemical composition of the groundwater in villages neighboring CPGF is the product of mixing between irrigation water from the Colorado River and brine from the evaporation pond. The high potassium concentration in the water and the relative increase in concentration of sodium and chlorides along the flow path as well as the hydrogeochemical models for this system explain this mixing process. This work will allow proposing new managing techniques to avoid the presence of the residual brine in the groundwater of agricultural lands.</description><identifier>ISSN: 0049-6979</identifier><identifier>EISSN: 1573-2932</identifier><identifier>DOI: 10.1007/s11270-010-0393-1</identifier><identifier>CODEN: WAPLAC</identifier><language>eng</language><publisher>Dordrecht: Dordrecht : Springer Netherlands</publisher><subject>Agricultural land ; Applied sciences ; Aquifers ; Atmospheric Protection/Air Quality Control/Air Pollution ; Brines ; chemical composition ; chlorides ; Climate Change/Climate Change Impacts ; Concentration (composition) ; Contamination ; Earth and Environmental Science ; Electric power plants ; Environment ; Environmental monitoring ; Evaporation ; Exact sciences and technology ; Geothermal ; Geothermal power ; Groundwater ; groundwater contamination ; Groundwater pollution ; Hydrogeology ; Irrigation water ; new methods ; Pollution ; Ponds ; potassium ; river water ; Salinity ; Salt water ; Sediments ; sodium ; Soil pollution ; Soil Science & Conservation ; soil water ; Studies ; Valleys ; Villages ; Water pollution ; Water Quality/Water Pollution ; Water, Underground</subject><ispartof>Water, air, and soil pollution, 2010-11, Vol.213 (1-4), p.389-400</ispartof><rights>Springer Science+Business Media B.V. 2010</rights><rights>2015 INIST-CNRS</rights><rights>COPYRIGHT 2010 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a496t-14f098e0e03bbac7c2060233443bed5e3bd332104f7881dffe18e985f55d6a253</citedby><cites>FETCH-LOGICAL-a496t-14f098e0e03bbac7c2060233443bed5e3bd332104f7881dffe18e985f55d6a253</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/s11270-010-0393-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11270-010-0393-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>315,781,785,27929,27930,41493,42562,51324</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23320768$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Moncada-Aguilar, Andrés M</creatorcontrib><creatorcontrib>Ramírez-Hernández, Jorge</creatorcontrib><creatorcontrib>Quintero-Núñez, Margarito</creatorcontrib><creatorcontrib>Avendaño-Reyes, Leonel</creatorcontrib><title>Origin of Salinity in Groundwater of Neighboring Villages of the Cerro Prieto Geothermal Field</title><title>Water, air, and soil pollution</title><addtitle>Water Air Soil Pollut</addtitle><description>The residual brine of the Cerro Prieto Geothermal Field (CPGF) is disposed in an evaporation pond. The seepage of this pond has contaminated the water and agricultural soil around it. The contamination of the groundwater towards the southwest by the evaporation pond, in the direction of the regional flow, has been shown before. Hydrogeochemical modeling (PHREEQCI) and Schoeller and Piper diagrams have been used in this work to show that the chemical composition of the groundwater in villages neighboring CPGF is the product of mixing between irrigation water from the Colorado River and brine from the evaporation pond. The high potassium concentration in the water and the relative increase in concentration of sodium and chlorides along the flow path as well as the hydrogeochemical models for this system explain this mixing process. This work will allow proposing new managing techniques to avoid the presence of the residual brine in the groundwater of agricultural lands.</description><subject>Agricultural land</subject><subject>Applied sciences</subject><subject>Aquifers</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Brines</subject><subject>chemical composition</subject><subject>chlorides</subject><subject>Climate Change/Climate Change Impacts</subject><subject>Concentration (composition)</subject><subject>Contamination</subject><subject>Earth and Environmental Science</subject><subject>Electric power plants</subject><subject>Environment</subject><subject>Environmental monitoring</subject><subject>Evaporation</subject><subject>Exact sciences and technology</subject><subject>Geothermal</subject><subject>Geothermal power</subject><subject>Groundwater</subject><subject>groundwater contamination</subject><subject>Groundwater 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Pollut</stitle><date>2010-11-01</date><risdate>2010</risdate><volume>213</volume><issue>1-4</issue><spage>389</spage><epage>400</epage><pages>389-400</pages><issn>0049-6979</issn><eissn>1573-2932</eissn><coden>WAPLAC</coden><abstract>The residual brine of the Cerro Prieto Geothermal Field (CPGF) is disposed in an evaporation pond. The seepage of this pond has contaminated the water and agricultural soil around it. The contamination of the groundwater towards the southwest by the evaporation pond, in the direction of the regional flow, has been shown before. Hydrogeochemical modeling (PHREEQCI) and Schoeller and Piper diagrams have been used in this work to show that the chemical composition of the groundwater in villages neighboring CPGF is the product of mixing between irrigation water from the Colorado River and brine from the evaporation pond. The high potassium concentration in the water and the relative increase in concentration of sodium and chlorides along the flow path as well as the hydrogeochemical models for this system explain this mixing process. This work will allow proposing new managing techniques to avoid the presence of the residual brine in the groundwater of agricultural lands.</abstract><cop>Dordrecht</cop><pub>Dordrecht : Springer Netherlands</pub><doi>10.1007/s11270-010-0393-1</doi><tpages>12</tpages></addata></record> |
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| ispartof | Water, air, and soil pollution, 2010-11, Vol.213 (1-4), p.389-400 |
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| source | SpringerNature Journals |
| subjects | Agricultural land Applied sciences Aquifers Atmospheric Protection/Air Quality Control/Air Pollution Brines chemical composition chlorides Climate Change/Climate Change Impacts Concentration (composition) Contamination Earth and Environmental Science Electric power plants Environment Environmental monitoring Evaporation Exact sciences and technology Geothermal Geothermal power Groundwater groundwater contamination Groundwater pollution Hydrogeology Irrigation water new methods Pollution Ponds potassium river water Salinity Salt water Sediments sodium Soil pollution Soil Science & Conservation soil water Studies Valleys Villages Water pollution Water Quality/Water Pollution Water, Underground |
| title | Origin of Salinity in Groundwater of Neighboring Villages of the Cerro Prieto Geothermal Field |
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