The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria
A study of the hydrogeochemical processes in the Morsott-El Aouinet aquifer was carried out with the objective of identifying the geochemical processes and their relation with groundwater quality as well as to get an insight into the hydrochemical evaluation of groundwater. The high salinity coupled...
Gespeichert in:
| Veröffentlicht in: | Environmental Geology 2009-10, Vol.58 (7), p.1611-1620, Article 1611 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1620 |
|---|---|
| container_issue | 7 |
| container_start_page | 1611 |
| container_title | Environmental Geology |
| container_volume | 58 |
| creator | Fehdi, Ch Rouabhia, Aek Baali, F. Boudoukha, A. |
| description | A study of the hydrogeochemical processes in the Morsott-El Aouinet aquifer was carried out with the objective of identifying the geochemical processes and their relation with groundwater quality as well as to get an insight into the hydrochemical evaluation of groundwater. The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as future exploitation. A combined hydrogeologic and isotopic investigation have been carried out using chemical and isotopic data to deduce a hydrochemical evaluation of the aquifer system based on the ionic constituents, water types, hydrochemical facies and factors controlling groundwater quality. The ionic speciation and mineral dissolution/precipitation was calculated by WATEQF package software. The increase in salinity is related to the dissolution and/or precipitation processes during the water–rock interaction and to the cationic exchange reactions between groundwater and clay minerals. The isotopic analysis of some groundwater samples shows a similarity with the meteoric waters reflect their short residence time and a lowest evaporation phenomenon of infiltrated groundwater. |
| doi_str_mv | 10.1007/s00254-008-1667-4 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_21259705</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>21259705</sourcerecordid><originalsourceid>FETCH-LOGICAL-a399t-d7830c0e5cd35ac79df9dedf2f7ffa8ae0aef0fe07b01130f0476996c5a9c3d93</originalsourceid><addsrcrecordid>eNp1kEFP3DAQha0KpC7QH9BbhAQnXMaOHa-PK7S0lShc4NCTNXXGJCgbg50c4Nfj1SKQkHqaw3zv6elj7LuAHwLAnGcAqRUHWHLRNIarL2whVC05KKv32AKsqjkI0F_ZQc4PAGClsQv297ajqntuU7yn6Dva9B6HyneY0E-U-hec-jhWMVR_Yspxmvh6qFZx7keaKnya-0DprLqOaeoIc0mM1Wq4L0E8YvsBh0zf3u4hu7tc31784lc3P39frK441tZOvDXLGjyQ9m2t0RvbBttSG2QwIeASCZACBALzD4SoIYAyjbWN12h93dr6kJ3ueh9TfJopT27TZ0_DgCPFOTsppLYGdAGPP4EPcU5j2VYYWCqp5BYSO8inmHOi4B5Tv8H07AS4rWm3M-2Kabc17VTJnLwVYy72QsLR9_k9KIWVVjfbbrnjcnmNRdLHgP-XvwKH648F</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>210842425</pqid></control><display><type>article</type><title>The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria</title><source>Springer Nature - Complete Springer Journals</source><creator>Fehdi, Ch ; Rouabhia, Aek ; Baali, F. ; Boudoukha, A.</creator><creatorcontrib>Fehdi, Ch ; Rouabhia, Aek ; Baali, F. ; Boudoukha, A.</creatorcontrib><description>A study of the hydrogeochemical processes in the Morsott-El Aouinet aquifer was carried out with the objective of identifying the geochemical processes and their relation with groundwater quality as well as to get an insight into the hydrochemical evaluation of groundwater. The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as future exploitation. A combined hydrogeologic and isotopic investigation have been carried out using chemical and isotopic data to deduce a hydrochemical evaluation of the aquifer system based on the ionic constituents, water types, hydrochemical facies and factors controlling groundwater quality. The ionic speciation and mineral dissolution/precipitation was calculated by WATEQF package software. The increase in salinity is related to the dissolution and/or precipitation processes during the water–rock interaction and to the cationic exchange reactions between groundwater and clay minerals. The isotopic analysis of some groundwater samples shows a similarity with the meteoric waters reflect their short residence time and a lowest evaporation phenomenon of infiltrated groundwater.</description><identifier>ISSN: 0943-0105</identifier><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1432-0495</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s00254-008-1667-4</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aquifer systems ; Aquifers ; Clay minerals ; Domestic water ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Environmental geology ; Evaporation ; Exact sciences and technology ; Geochemistry ; Geology ; Groundwater ; Groundwater levels ; Hydrogeology ; Hydrology. Hydrogeology ; Irrigation water ; Isotope geochemistry ; Isotope geochemistry. Geochronology ; Isotopes ; Meteoric water ; Mineralogy ; Original Article ; Salinity ; Silicates ; Speciation ; Water analysis ; Water geochemistry ; Water quality ; Water sampling ; Water supply</subject><ispartof>Environmental Geology, 2009-10, Vol.58 (7), p.1611-1620, Article 1611</ispartof><rights>Springer-Verlag 2008</rights><rights>2015 INIST-CNRS</rights><rights>Springer-Verlag 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a399t-d7830c0e5cd35ac79df9dedf2f7ffa8ae0aef0fe07b01130f0476996c5a9c3d93</citedby><cites>FETCH-LOGICAL-a399t-d7830c0e5cd35ac79df9dedf2f7ffa8ae0aef0fe07b01130f0476996c5a9c3d93</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/s00254-008-1667-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00254-008-1667-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,778,782,27911,27912,41475,42544,51306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21929565$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Fehdi, Ch</creatorcontrib><creatorcontrib>Rouabhia, Aek</creatorcontrib><creatorcontrib>Baali, F.</creatorcontrib><creatorcontrib>Boudoukha, A.</creatorcontrib><title>The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria</title><title>Environmental Geology</title><addtitle>Environ Geol</addtitle><description>A study of the hydrogeochemical processes in the Morsott-El Aouinet aquifer was carried out with the objective of identifying the geochemical processes and their relation with groundwater quality as well as to get an insight into the hydrochemical evaluation of groundwater. The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as future exploitation. A combined hydrogeologic and isotopic investigation have been carried out using chemical and isotopic data to deduce a hydrochemical evaluation of the aquifer system based on the ionic constituents, water types, hydrochemical facies and factors controlling groundwater quality. The ionic speciation and mineral dissolution/precipitation was calculated by WATEQF package software. The increase in salinity is related to the dissolution and/or precipitation processes during the water–rock interaction and to the cationic exchange reactions between groundwater and clay minerals. The isotopic analysis of some groundwater samples shows a similarity with the meteoric waters reflect their short residence time and a lowest evaporation phenomenon of infiltrated groundwater.</description><subject>Aquifer systems</subject><subject>Aquifers</subject><subject>Clay minerals</subject><subject>Domestic water</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Environmental geology</subject><subject>Evaporation</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater levels</subject><subject>Hydrogeology</subject><subject>Hydrology. Hydrogeology</subject><subject>Irrigation water</subject><subject>Isotope geochemistry</subject><subject>Isotope geochemistry. Geochronology</subject><subject>Isotopes</subject><subject>Meteoric water</subject><subject>Mineralogy</subject><subject>Original Article</subject><subject>Salinity</subject><subject>Silicates</subject><subject>Speciation</subject><subject>Water analysis</subject><subject>Water geochemistry</subject><subject>Water quality</subject><subject>Water sampling</subject><subject>Water supply</subject><issn>0943-0105</issn><issn>1866-6280</issn><issn>1432-0495</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</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>eNp1kEFP3DAQha0KpC7QH9BbhAQnXMaOHa-PK7S0lShc4NCTNXXGJCgbg50c4Nfj1SKQkHqaw3zv6elj7LuAHwLAnGcAqRUHWHLRNIarL2whVC05KKv32AKsqjkI0F_ZQc4PAGClsQv297ajqntuU7yn6Dva9B6HyneY0E-U-hec-jhWMVR_Yspxmvh6qFZx7keaKnya-0DprLqOaeoIc0mM1Wq4L0E8YvsBh0zf3u4hu7tc31784lc3P39frK441tZOvDXLGjyQ9m2t0RvbBttSG2QwIeASCZACBALzD4SoIYAyjbWN12h93dr6kJ3ueh9TfJopT27TZ0_DgCPFOTsppLYGdAGPP4EPcU5j2VYYWCqp5BYSO8inmHOi4B5Tv8H07AS4rWm3M-2Kabc17VTJnLwVYy72QsLR9_k9KIWVVjfbbrnjcnmNRdLHgP-XvwKH648F</recordid><startdate>20091001</startdate><enddate>20091001</enddate><creator>Fehdi, Ch</creator><creator>Rouabhia, Aek</creator><creator>Baali, F.</creator><creator>Boudoukha, A.</creator><general>Springer Berlin Heidelberg</general><general>Springer</general><general>Springer Nature B.V</general><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></search><sort><creationdate>20091001</creationdate><title>The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria</title><author>Fehdi, Ch ; Rouabhia, Aek ; Baali, F. ; Boudoukha, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a399t-d7830c0e5cd35ac79df9dedf2f7ffa8ae0aef0fe07b01130f0476996c5a9c3d93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Aquifer systems</topic><topic>Aquifers</topic><topic>Clay minerals</topic><topic>Domestic water</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Environmental geology</topic><topic>Evaporation</topic><topic>Exact sciences and technology</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Groundwater levels</topic><topic>Hydrogeology</topic><topic>Hydrology. Hydrogeology</topic><topic>Irrigation water</topic><topic>Isotope geochemistry</topic><topic>Isotope geochemistry. Geochronology</topic><topic>Isotopes</topic><topic>Meteoric water</topic><topic>Mineralogy</topic><topic>Original Article</topic><topic>Salinity</topic><topic>Silicates</topic><topic>Speciation</topic><topic>Water analysis</topic><topic>Water geochemistry</topic><topic>Water quality</topic><topic>Water sampling</topic><topic>Water supply</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fehdi, Ch</creatorcontrib><creatorcontrib>Rouabhia, Aek</creatorcontrib><creatorcontrib>Baali, F.</creatorcontrib><creatorcontrib>Boudoukha, A.</creatorcontrib><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 (ProQuest)</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 (ProQuest)</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 Geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fehdi, Ch</au><au>Rouabhia, Aek</au><au>Baali, F.</au><au>Boudoukha, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria</atitle><jtitle>Environmental Geology</jtitle><stitle>Environ Geol</stitle><date>2009-10-01</date><risdate>2009</risdate><volume>58</volume><issue>7</issue><spage>1611</spage><epage>1620</epage><pages>1611-1620</pages><artnum>1611</artnum><issn>0943-0105</issn><issn>1866-6280</issn><eissn>1432-0495</eissn><eissn>1866-6299</eissn><abstract>A study of the hydrogeochemical processes in the Morsott-El Aouinet aquifer was carried out with the objective of identifying the geochemical processes and their relation with groundwater quality as well as to get an insight into the hydrochemical evaluation of groundwater. The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as future exploitation. A combined hydrogeologic and isotopic investigation have been carried out using chemical and isotopic data to deduce a hydrochemical evaluation of the aquifer system based on the ionic constituents, water types, hydrochemical facies and factors controlling groundwater quality. The ionic speciation and mineral dissolution/precipitation was calculated by WATEQF package software. The increase in salinity is related to the dissolution and/or precipitation processes during the water–rock interaction and to the cationic exchange reactions between groundwater and clay minerals. The isotopic analysis of some groundwater samples shows a similarity with the meteoric waters reflect their short residence time and a lowest evaporation phenomenon of infiltrated groundwater.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00254-008-1667-4</doi><tpages>10</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0943-0105 |
| ispartof | Environmental Geology, 2009-10, Vol.58 (7), p.1611-1620, Article 1611 |
| issn | 0943-0105 1866-6280 1432-0495 1866-6299 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_21259705 |
| source | Springer Nature - Complete Springer Journals |
| subjects | Aquifer systems Aquifers Clay minerals Domestic water Earth and Environmental Science Earth Sciences Earth, ocean, space Environmental geology Evaporation Exact sciences and technology Geochemistry Geology Groundwater Groundwater levels Hydrogeology Hydrology. Hydrogeology Irrigation water Isotope geochemistry Isotope geochemistry. Geochronology Isotopes Meteoric water Mineralogy Original Article Salinity Silicates Speciation Water analysis Water geochemistry Water quality Water sampling Water supply |
| title | The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-15T15%3A28%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20hydrogeochemical%20characterization%20of%20Morsott-El%20Aouinet%20aquifer,%20Northeastern%20Algeria&rft.jtitle=Environmental%20Geology&rft.au=Fehdi,%20Ch&rft.date=2009-10-01&rft.volume=58&rft.issue=7&rft.spage=1611&rft.epage=1620&rft.pages=1611-1620&rft.artnum=1611&rft.issn=0943-0105&rft.eissn=1432-0495&rft_id=info:doi/10.1007/s00254-008-1667-4&rft_dat=%3Cproquest_cross%3E21259705%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=210842425&rft_id=info:pmid/&rfr_iscdi=true |