Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)
Water in the fissured limestone and dolomite of the Turonian aquifer of Tunisia has been investigated using geochemical (major ions) and isotopic (δ¹⁸O, δ²H, ¹⁴C) data. To carry out a characterization of aquifer behaviour, 48 representative samples were collected at the end of the humid season. The...
Gespeichert in:
| Veröffentlicht in: | Hydrogeology journal 2011-03, Vol.19 (2), p.415-427 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 427 |
|---|---|
| container_issue | 2 |
| container_start_page | 415 |
| container_title | Hydrogeology journal |
| container_volume | 19 |
| creator | Abid, Kamel Zouari, Kamel Dulinski, Marek Chkir, Najiba Abidi, Brahim |
| description | Water in the fissured limestone and dolomite of the Turonian aquifer of Tunisia has been investigated using geochemical (major ions) and isotopic (δ¹⁸O, δ²H, ¹⁴C) data. To carry out a characterization of aquifer behaviour, 48 representative samples were collected at the end of the humid season. The evolution of chemical composition of groundwater from recharge areas to discharge areas is characterized by increasing sodium, chloride and sulphate contents as a result of leaching of evaporite rock. In the study, three distinct chemical trends in groundwater were identified. The major reactions responsible for the chemical evolution of groundwater in the investigated area fall into three categories: (1) calcite precipitation, (2) gypsum and halite dissolution, and (3) ion exchange. The stable isotope composition of water samples indicates large-scale interaction between the Continental Intercalaire and the Turonian aquifer and the presence of a young local component which probably enters the system via faults and/or fractures. |
| doi_str_mv | 10.1007/s10040-010-0668-z |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_876242548</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>876242548</sourcerecordid><originalsourceid>FETCH-LOGICAL-a394t-18bf5f3f80e1d6f30ddf343ac55f5a4f7b62d0a982e6786648454dcdc8ded4713</originalsourceid><addsrcrecordid>eNp9kUtLxDAUhYMoOD5-gCuLG3VRzW2SNrOUwRcMuHBmHWIeNUNNNGmRmV9vxgqCCxdJ7s39zuXAQegE8BVg3FynfFNcYsinrnm52UEToITlH9bsftdQVtDQfXSQ0gpnGhoyQeFhrWPoQutUIb0uWvPTWKn6EFOhgu8z0DnfFm0Mg9efsjdxC6pX8-ZSH9eF80X_aorFEIN30hfyY3A2QxcpDHkQfR55l5y8PEJ7VnbJHP-8h2h5d7uYPZTzp_vH2c28lGRK-xL4i2WWWI4N6NoSrLUllEjFmGWS2ualrjSWU16ZuuF1TTllVCutuDaaNkAO0fm49z2Gj8GkXmSrynSd9CYMSfCmrmjFKM_k2R9yFYbosznBGaGAAViGYIRUDClFY8V7dG8yrgVgsQ1AjAGIHIDYBiA2WVONmpRZ35r4u_g_0ekosjII2UaXxPK5wkAwTCkDSskXq1GUSA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>853410115</pqid></control><display><type>article</type><title>Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)</title><source>SpringerLink Journals - AutoHoldings</source><creator>Abid, Kamel ; Zouari, Kamel ; Dulinski, Marek ; Chkir, Najiba ; Abidi, Brahim</creator><creatorcontrib>Abid, Kamel ; Zouari, Kamel ; Dulinski, Marek ; Chkir, Najiba ; Abidi, Brahim</creatorcontrib><description>Water in the fissured limestone and dolomite of the Turonian aquifer of Tunisia has been investigated using geochemical (major ions) and isotopic (δ¹⁸O, δ²H, ¹⁴C) data. To carry out a characterization of aquifer behaviour, 48 representative samples were collected at the end of the humid season. The evolution of chemical composition of groundwater from recharge areas to discharge areas is characterized by increasing sodium, chloride and sulphate contents as a result of leaching of evaporite rock. In the study, three distinct chemical trends in groundwater were identified. The major reactions responsible for the chemical evolution of groundwater in the investigated area fall into three categories: (1) calcite precipitation, (2) gypsum and halite dissolution, and (3) ion exchange. The stable isotope composition of water samples indicates large-scale interaction between the Continental Intercalaire and the Turonian aquifer and the presence of a young local component which probably enters the system via faults and/or fractures.</description><identifier>ISSN: 1431-2174</identifier><identifier>EISSN: 1435-0157</identifier><identifier>DOI: 10.1007/s10040-010-0668-z</identifier><language>eng</language><publisher>Berlin/Heidelberg: Berlin/Heidelberg : Springer-Verlag</publisher><subject>Aquatic Pollution ; Aquifers ; Calcite ; Categories ; Chemical evolution ; Chlorides ; Dissolution ; Dolomite ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geology ; Geophysics/Geodesy ; Groundwater ; Groundwater recharge ; Gypsum ; Hydrogeology ; Hydrology ; Hydrology/Water Resources ; ion exchange ; Ions ; Leaching ; Limestone ; Mixing process ; precipitation ; Rock ; Sodium ; Stable isotopes ; Waste Water Technology ; Water analysis ; Water Management ; Water Pollution Control ; Water Quality/Water Pollution ; Water sampling</subject><ispartof>Hydrogeology journal, 2011-03, Vol.19 (2), p.415-427</ispartof><rights>Springer-Verlag 2010</rights><rights>Springer-Verlag 2011</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a394t-18bf5f3f80e1d6f30ddf343ac55f5a4f7b62d0a982e6786648454dcdc8ded4713</citedby><cites>FETCH-LOGICAL-a394t-18bf5f3f80e1d6f30ddf343ac55f5a4f7b62d0a982e6786648454dcdc8ded4713</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/s10040-010-0668-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10040-010-0668-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Abid, Kamel</creatorcontrib><creatorcontrib>Zouari, Kamel</creatorcontrib><creatorcontrib>Dulinski, Marek</creatorcontrib><creatorcontrib>Chkir, Najiba</creatorcontrib><creatorcontrib>Abidi, Brahim</creatorcontrib><title>Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)</title><title>Hydrogeology journal</title><addtitle>Hydrogeol J</addtitle><description>Water in the fissured limestone and dolomite of the Turonian aquifer of Tunisia has been investigated using geochemical (major ions) and isotopic (δ¹⁸O, δ²H, ¹⁴C) data. To carry out a characterization of aquifer behaviour, 48 representative samples were collected at the end of the humid season. The evolution of chemical composition of groundwater from recharge areas to discharge areas is characterized by increasing sodium, chloride and sulphate contents as a result of leaching of evaporite rock. In the study, three distinct chemical trends in groundwater were identified. The major reactions responsible for the chemical evolution of groundwater in the investigated area fall into three categories: (1) calcite precipitation, (2) gypsum and halite dissolution, and (3) ion exchange. The stable isotope composition of water samples indicates large-scale interaction between the Continental Intercalaire and the Turonian aquifer and the presence of a young local component which probably enters the system via faults and/or fractures.</description><subject>Aquatic Pollution</subject><subject>Aquifers</subject><subject>Calcite</subject><subject>Categories</subject><subject>Chemical evolution</subject><subject>Chlorides</subject><subject>Dissolution</subject><subject>Dolomite</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Groundwater</subject><subject>Groundwater recharge</subject><subject>Gypsum</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology/Water Resources</subject><subject>ion exchange</subject><subject>Ions</subject><subject>Leaching</subject><subject>Limestone</subject><subject>Mixing process</subject><subject>precipitation</subject><subject>Rock</subject><subject>Sodium</subject><subject>Stable isotopes</subject><subject>Waste Water Technology</subject><subject>Water analysis</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>Water Quality/Water Pollution</subject><subject>Water sampling</subject><issn>1431-2174</issn><issn>1435-0157</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kUtLxDAUhYMoOD5-gCuLG3VRzW2SNrOUwRcMuHBmHWIeNUNNNGmRmV9vxgqCCxdJ7s39zuXAQegE8BVg3FynfFNcYsinrnm52UEToITlH9bsftdQVtDQfXSQ0gpnGhoyQeFhrWPoQutUIb0uWvPTWKn6EFOhgu8z0DnfFm0Mg9efsjdxC6pX8-ZSH9eF80X_aorFEIN30hfyY3A2QxcpDHkQfR55l5y8PEJ7VnbJHP-8h2h5d7uYPZTzp_vH2c28lGRK-xL4i2WWWI4N6NoSrLUllEjFmGWS2ualrjSWU16ZuuF1TTllVCutuDaaNkAO0fm49z2Gj8GkXmSrynSd9CYMSfCmrmjFKM_k2R9yFYbosznBGaGAAViGYIRUDClFY8V7dG8yrgVgsQ1AjAGIHIDYBiA2WVONmpRZ35r4u_g_0ekosjII2UaXxPK5wkAwTCkDSskXq1GUSA</recordid><startdate>20110301</startdate><enddate>20110301</enddate><creator>Abid, Kamel</creator><creator>Zouari, Kamel</creator><creator>Dulinski, Marek</creator><creator>Chkir, Najiba</creator><creator>Abidi, Brahim</creator><general>Berlin/Heidelberg : Springer-Verlag</general><general>Springer-Verlag</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20110301</creationdate><title>Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)</title><author>Abid, Kamel ; Zouari, Kamel ; Dulinski, Marek ; Chkir, Najiba ; Abidi, Brahim</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a394t-18bf5f3f80e1d6f30ddf343ac55f5a4f7b62d0a982e6786648454dcdc8ded4713</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Aquatic Pollution</topic><topic>Aquifers</topic><topic>Calcite</topic><topic>Categories</topic><topic>Chemical evolution</topic><topic>Chlorides</topic><topic>Dissolution</topic><topic>Dolomite</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Groundwater</topic><topic>Groundwater recharge</topic><topic>Gypsum</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Hydrology/Water Resources</topic><topic>ion exchange</topic><topic>Ions</topic><topic>Leaching</topic><topic>Limestone</topic><topic>Mixing process</topic><topic>precipitation</topic><topic>Rock</topic><topic>Sodium</topic><topic>Stable isotopes</topic><topic>Waste Water Technology</topic><topic>Water analysis</topic><topic>Water Management</topic><topic>Water Pollution Control</topic><topic>Water Quality/Water Pollution</topic><topic>Water sampling</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Abid, Kamel</creatorcontrib><creatorcontrib>Zouari, Kamel</creatorcontrib><creatorcontrib>Dulinski, Marek</creatorcontrib><creatorcontrib>Chkir, Najiba</creatorcontrib><creatorcontrib>Abidi, Brahim</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</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>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</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>Technology Collection</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>Engineering Research Database</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>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering 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>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Hydrogeology journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Abid, Kamel</au><au>Zouari, Kamel</au><au>Dulinski, Marek</au><au>Chkir, Najiba</au><au>Abidi, Brahim</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)</atitle><jtitle>Hydrogeology journal</jtitle><stitle>Hydrogeol J</stitle><date>2011-03-01</date><risdate>2011</risdate><volume>19</volume><issue>2</issue><spage>415</spage><epage>427</epage><pages>415-427</pages><issn>1431-2174</issn><eissn>1435-0157</eissn><abstract>Water in the fissured limestone and dolomite of the Turonian aquifer of Tunisia has been investigated using geochemical (major ions) and isotopic (δ¹⁸O, δ²H, ¹⁴C) data. To carry out a characterization of aquifer behaviour, 48 representative samples were collected at the end of the humid season. The evolution of chemical composition of groundwater from recharge areas to discharge areas is characterized by increasing sodium, chloride and sulphate contents as a result of leaching of evaporite rock. In the study, three distinct chemical trends in groundwater were identified. The major reactions responsible for the chemical evolution of groundwater in the investigated area fall into three categories: (1) calcite precipitation, (2) gypsum and halite dissolution, and (3) ion exchange. The stable isotope composition of water samples indicates large-scale interaction between the Continental Intercalaire and the Turonian aquifer and the presence of a young local component which probably enters the system via faults and/or fractures.</abstract><cop>Berlin/Heidelberg</cop><pub>Berlin/Heidelberg : Springer-Verlag</pub><doi>10.1007/s10040-010-0668-z</doi><tpages>13</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1431-2174 |
| ispartof | Hydrogeology journal, 2011-03, Vol.19 (2), p.415-427 |
| issn | 1431-2174 1435-0157 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_876242548 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Aquatic Pollution Aquifers Calcite Categories Chemical evolution Chlorides Dissolution Dolomite Earth and Environmental Science Earth Sciences Geochemistry Geology Geophysics/Geodesy Groundwater Groundwater recharge Gypsum Hydrogeology Hydrology Hydrology/Water Resources ion exchange Ions Leaching Limestone Mixing process precipitation Rock Sodium Stable isotopes Waste Water Technology Water analysis Water Management Water Pollution Control Water Quality/Water Pollution Water sampling |
| title | Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-27T21%3A14%3A23IST&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=Hydrologic%20and%20geologic%20factors%20controlling%20groundwater%20geochemistry%20in%20the%20Turonian%20aquifer%20(southern%20Tunisia)&rft.jtitle=Hydrogeology%20journal&rft.au=Abid,%20Kamel&rft.date=2011-03-01&rft.volume=19&rft.issue=2&rft.spage=415&rft.epage=427&rft.pages=415-427&rft.issn=1431-2174&rft.eissn=1435-0157&rft_id=info:doi/10.1007/s10040-010-0668-z&rft_dat=%3Cproquest_cross%3E876242548%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=853410115&rft_id=info:pmid/&rfr_iscdi=true |