The configuration of the fresh–saline groundwater interface within the regional Judea Group carbonate aquifer in northern Israel between the Mediterranean and the Dead Sea base levels as delineated by deep geoelectromagnetic soundings
A combined high resolution short offset transient electromagnetic (SHOTEM) and deep sounding, long offset (LOTEM) survey has been carried out along two traverses between the Mediterranean Sea and the Jordan-Dead Sea Rift (DSR). The DSR is located in the study area some 200–250 m below sea level. The...
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| Veröffentlicht in: | Journal of hydrology (Amsterdam) 2007-09, Vol.344 (1), p.123-134 |
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| creator | Kafri, U. Goldman, M. Lyakhovsky, V. Scholl, C. Helwig, S. Tezkan, B. |
| description | A combined high resolution short offset transient electromagnetic (SHOTEM) and deep sounding, long offset (LOTEM) survey has been carried out along two traverses between the Mediterranean Sea and the Jordan-Dead Sea Rift (DSR). The DSR is located in the study area some 200–250
m below sea level. The measurements detected a deep conductor, the top of which exhibited a regular behavior along the both traverses, declining from the Mediterranean to the DSR base level. The geometry of this geoelectric boundary coincides fairly well with the configuration of a supposed fresh/saline groundwater interface as also obtained by both numerical and physical modeling for the known hydrogeological conditions in the study area. Therefore the detected geoelectric boundary is identified with the interface, supporting the hypothesis of current seawater intrusion into the deep regional aquifers between the Mediterranean and the DSR base levels. The intrusion causes the salination of fresh groundwater within the aquifers as well as the salination of the Sea of Galilee. |
| doi_str_mv | 10.1016/j.jhydrol.2007.07.003 |
| format | Article |
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m below sea level. The measurements detected a deep conductor, the top of which exhibited a regular behavior along the both traverses, declining from the Mediterranean to the DSR base level. The geometry of this geoelectric boundary coincides fairly well with the configuration of a supposed fresh/saline groundwater interface as also obtained by both numerical and physical modeling for the known hydrogeological conditions in the study area. Therefore the detected geoelectric boundary is identified with the interface, supporting the hypothesis of current seawater intrusion into the deep regional aquifers between the Mediterranean and the DSR base levels. The intrusion causes the salination of fresh groundwater within the aquifers as well as the salination of the Sea of Galilee.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2007.07.003</identifier><identifier>CODEN: JHYDA7</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>aquifers ; Base levels ; Dead Sea ; Earth sciences ; Earth, ocean, space ; electromagnetic induction techniques ; Exact sciences and technology ; freshwater ; Geochemistry ; geoelectric boundary ; Geoelectromagnetic methods ; Geophysics: general, magnetic, electric and thermic methods and properties ; Groundwater ; Hydrogeology ; Hydrology. Hydrogeology ; Internal geophysics ; Jordan Rift Valley ; Mineralogy ; Salination ; saline water ; saltwater intrusion ; Silicates ; Water geochemistry</subject><ispartof>Journal of hydrology (Amsterdam), 2007-09, Vol.344 (1), p.123-134</ispartof><rights>2007 Elsevier B.V.</rights><rights>2007 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a457t-cb2d6c68f124a0f1597bd9eb99c7f9c02a193808340f37cfb58e8ea6652200aa3</citedby><cites>FETCH-LOGICAL-a457t-cb2d6c68f124a0f1597bd9eb99c7f9c02a193808340f37cfb58e8ea6652200aa3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhydrol.2007.07.003$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>315,782,786,3552,27931,27932,46002</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=19074579$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Kafri, U.</creatorcontrib><creatorcontrib>Goldman, M.</creatorcontrib><creatorcontrib>Lyakhovsky, V.</creatorcontrib><creatorcontrib>Scholl, C.</creatorcontrib><creatorcontrib>Helwig, S.</creatorcontrib><creatorcontrib>Tezkan, B.</creatorcontrib><title>The configuration of the fresh–saline groundwater interface within the regional Judea Group carbonate aquifer in northern Israel between the Mediterranean and the Dead Sea base levels as delineated by deep geoelectromagnetic soundings</title><title>Journal of hydrology (Amsterdam)</title><description>A combined high resolution short offset transient electromagnetic (SHOTEM) and deep sounding, long offset (LOTEM) survey has been carried out along two traverses between the Mediterranean Sea and the Jordan-Dead Sea Rift (DSR). The DSR is located in the study area some 200–250
m below sea level. The measurements detected a deep conductor, the top of which exhibited a regular behavior along the both traverses, declining from the Mediterranean to the DSR base level. The geometry of this geoelectric boundary coincides fairly well with the configuration of a supposed fresh/saline groundwater interface as also obtained by both numerical and physical modeling for the known hydrogeological conditions in the study area. Therefore the detected geoelectric boundary is identified with the interface, supporting the hypothesis of current seawater intrusion into the deep regional aquifers between the Mediterranean and the DSR base levels. The intrusion causes the salination of fresh groundwater within the aquifers as well as the salination of the Sea of Galilee.</description><subject>aquifers</subject><subject>Base levels</subject><subject>Dead Sea</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>electromagnetic induction techniques</subject><subject>Exact sciences and technology</subject><subject>freshwater</subject><subject>Geochemistry</subject><subject>geoelectric boundary</subject><subject>Geoelectromagnetic methods</subject><subject>Geophysics: general, magnetic, electric and thermic methods and properties</subject><subject>Groundwater</subject><subject>Hydrogeology</subject><subject>Hydrology. Hydrogeology</subject><subject>Internal geophysics</subject><subject>Jordan Rift Valley</subject><subject>Mineralogy</subject><subject>Salination</subject><subject>saline water</subject><subject>saltwater intrusion</subject><subject>Silicates</subject><subject>Water geochemistry</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNqFkc9uEzEQxlcIJELgERC-wC3B3n9enxAqUIqKOLQ9W7Pe8cbRxk7t3Ua58Q68IWcegtmkEkeskS2PfvN5PF-WvRZ8Lbio32_X282xi2FY55zL9Ry8eJItRCPVKpdcPs0WnOf5StSqfJ69SGnLaRVFucj-3G6QmeCt66cIowueBctGStqIafP7568Eg_PI-hgm3x1gxMicp92CQXZw48b5Ex-xp2oY2LepQ2CXxO-ZgdhSckQG95Ozp1rmQ6SC6NlVioADa3E8IJ5VvmPnSDyCR_AMfHfKfkLo2A2ptpCQDfiAQ2KQWIdzbyTfsfZIN9yzHgMOaMYYdtB7HJ1hae7c-T69zJ5ZGBK-ejyX2d2Xz7cXX1fXPy6vLj5er6Cs5Lgybd7Vpm6syEvgVlRKtp3CVikjrTI8B6GKhjdFyW0hjW2rBhuEuq5yMgCgWGbvzrr7GO4nTKPeuWRwGOhXYUo6F2SHqiSB1Rk0MaQU0ep9dDuIRy24nr3VW_3orZ691XOQccvs7eMDkAwMlsZlXPpXrLiknyji3pw5C0FDH4m5u8m5KDhvykaeiA9ngiaKDw6jTsahN2RDpCnqLrj_9PIXG6zONw</recordid><startdate>20070930</startdate><enddate>20070930</enddate><creator>Kafri, U.</creator><creator>Goldman, M.</creator><creator>Lyakhovsky, V.</creator><creator>Scholl, C.</creator><creator>Helwig, S.</creator><creator>Tezkan, B.</creator><general>Elsevier B.V</general><general>Elsevier Science</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20070930</creationdate><title>The configuration of the fresh–saline groundwater interface within the regional Judea Group carbonate aquifer in northern Israel between the Mediterranean and the Dead Sea base levels as delineated by deep geoelectromagnetic soundings</title><author>Kafri, U. ; Goldman, M. ; Lyakhovsky, V. ; Scholl, C. ; Helwig, S. ; Tezkan, B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a457t-cb2d6c68f124a0f1597bd9eb99c7f9c02a193808340f37cfb58e8ea6652200aa3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>aquifers</topic><topic>Base levels</topic><topic>Dead Sea</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>electromagnetic induction techniques</topic><topic>Exact sciences and technology</topic><topic>freshwater</topic><topic>Geochemistry</topic><topic>geoelectric boundary</topic><topic>Geoelectromagnetic methods</topic><topic>Geophysics: general, magnetic, electric and thermic methods and properties</topic><topic>Groundwater</topic><topic>Hydrogeology</topic><topic>Hydrology. Hydrogeology</topic><topic>Internal geophysics</topic><topic>Jordan Rift Valley</topic><topic>Mineralogy</topic><topic>Salination</topic><topic>saline water</topic><topic>saltwater intrusion</topic><topic>Silicates</topic><topic>Water geochemistry</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kafri, U.</creatorcontrib><creatorcontrib>Goldman, M.</creatorcontrib><creatorcontrib>Lyakhovsky, V.</creatorcontrib><creatorcontrib>Scholl, C.</creatorcontrib><creatorcontrib>Helwig, S.</creatorcontrib><creatorcontrib>Tezkan, B.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kafri, U.</au><au>Goldman, M.</au><au>Lyakhovsky, V.</au><au>Scholl, C.</au><au>Helwig, S.</au><au>Tezkan, B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The configuration of the fresh–saline groundwater interface within the regional Judea Group carbonate aquifer in northern Israel between the Mediterranean and the Dead Sea base levels as delineated by deep geoelectromagnetic soundings</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2007-09-30</date><risdate>2007</risdate><volume>344</volume><issue>1</issue><spage>123</spage><epage>134</epage><pages>123-134</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><abstract>A combined high resolution short offset transient electromagnetic (SHOTEM) and deep sounding, long offset (LOTEM) survey has been carried out along two traverses between the Mediterranean Sea and the Jordan-Dead Sea Rift (DSR). The DSR is located in the study area some 200–250
m below sea level. The measurements detected a deep conductor, the top of which exhibited a regular behavior along the both traverses, declining from the Mediterranean to the DSR base level. The geometry of this geoelectric boundary coincides fairly well with the configuration of a supposed fresh/saline groundwater interface as also obtained by both numerical and physical modeling for the known hydrogeological conditions in the study area. Therefore the detected geoelectric boundary is identified with the interface, supporting the hypothesis of current seawater intrusion into the deep regional aquifers between the Mediterranean and the DSR base levels. The intrusion causes the salination of fresh groundwater within the aquifers as well as the salination of the Sea of Galilee.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2007.07.003</doi><tpages>12</tpages></addata></record> |
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| subjects | aquifers Base levels Dead Sea Earth sciences Earth, ocean, space electromagnetic induction techniques Exact sciences and technology freshwater Geochemistry geoelectric boundary Geoelectromagnetic methods Geophysics: general, magnetic, electric and thermic methods and properties Groundwater Hydrogeology Hydrology. Hydrogeology Internal geophysics Jordan Rift Valley Mineralogy Salination saline water saltwater intrusion Silicates Water geochemistry |
| title | The configuration of the fresh–saline groundwater interface within the regional Judea Group carbonate aquifer in northern Israel between the Mediterranean and the Dead Sea base levels as delineated by deep geoelectromagnetic soundings |
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