Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria

Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sour...
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Autor*in:	Maoui, Ammar [verfasserIn] Kherici, N. Derradji, F.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	Hydrochemistry Ain oussera Sandstone Thermodynamic Algeria

Anmerkung:	© Springer-Verlag 2009

Übergeordnetes Werk:	Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 60(2009), 4 vom: 30. Juni, Seite 689-701
Übergeordnetes Werk:	volume:60 ; year:2009 ; number:4 ; day:30 ; month:06 ; pages:689-701

Links:	Volltext

DOI / URN:	10.1007/s12665-009-0207-1

Katalog-ID:	SPR026665972

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publishDate	2009
allfields	10.1007/s12665-009-0207-1 doi (DE-627)SPR026665972 (SPR)s12665-009-0207-1-e DE-627 ger DE-627 rakwb eng Maoui, Ammar verfasserin aut Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2009 Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213 Kherici, N. aut Derradji, F. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 60(2009), 4 vom: 30. Juni, Seite 689-701 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:60 year:2009 number:4 day:30 month:06 pages:689-701 https://dx.doi.org/10.1007/s12665-009-0207-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 60 2009 4 30 06 689-701
spelling	10.1007/s12665-009-0207-1 doi (DE-627)SPR026665972 (SPR)s12665-009-0207-1-e DE-627 ger DE-627 rakwb eng Maoui, Ammar verfasserin aut Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2009 Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213 Kherici, N. aut Derradji, F. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 60(2009), 4 vom: 30. Juni, Seite 689-701 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:60 year:2009 number:4 day:30 month:06 pages:689-701 https://dx.doi.org/10.1007/s12665-009-0207-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 60 2009 4 30 06 689-701
allfields_unstemmed	10.1007/s12665-009-0207-1 doi (DE-627)SPR026665972 (SPR)s12665-009-0207-1-e DE-627 ger DE-627 rakwb eng Maoui, Ammar verfasserin aut Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2009 Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213 Kherici, N. aut Derradji, F. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 60(2009), 4 vom: 30. Juni, Seite 689-701 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:60 year:2009 number:4 day:30 month:06 pages:689-701 https://dx.doi.org/10.1007/s12665-009-0207-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 60 2009 4 30 06 689-701
allfieldsGer	10.1007/s12665-009-0207-1 doi (DE-627)SPR026665972 (SPR)s12665-009-0207-1-e DE-627 ger DE-627 rakwb eng Maoui, Ammar verfasserin aut Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2009 Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213 Kherici, N. aut Derradji, F. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 60(2009), 4 vom: 30. Juni, Seite 689-701 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:60 year:2009 number:4 day:30 month:06 pages:689-701 https://dx.doi.org/10.1007/s12665-009-0207-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 60 2009 4 30 06 689-701
allfieldsSound	10.1007/s12665-009-0207-1 doi (DE-627)SPR026665972 (SPR)s12665-009-0207-1-e DE-627 ger DE-627 rakwb eng Maoui, Ammar verfasserin aut Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2009 Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213 Kherici, N. aut Derradji, F. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 60(2009), 4 vom: 30. Juni, Seite 689-701 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:60 year:2009 number:4 day:30 month:06 pages:689-701 https://dx.doi.org/10.1007/s12665-009-0207-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 60 2009 4 30 06 689-701
language	English
source	Enthalten in Environmental earth sciences 60(2009), 4 vom: 30. Juni, Seite 689-701 volume:60 year:2009 number:4 day:30 month:06 pages:689-701
sourceStr	Enthalten in Environmental earth sciences 60(2009), 4 vom: 30. Juni, Seite 689-701 volume:60 year:2009 number:4 day:30 month:06 pages:689-701
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Hydrochemistry Ain oussera Sandstone Thermodynamic Algeria
isfreeaccess_bool	false
container_title	Environmental earth sciences
authorswithroles_txt_mv	Maoui, Ammar @@aut@@ Kherici, N. @@aut@@ Derradji, F. @@aut@@
publishDateDaySort_date	2009-06-30T00:00:00Z
hierarchy_top_id	599673451
id	SPR026665972
language_de	englisch
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author	Maoui, Ammar
spellingShingle	Maoui, Ammar misc Hydrochemistry misc Ain oussera misc Sandstone misc Thermodynamic misc Algeria Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria
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topic_title	Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria Hydrochemistry (dpeaa)DE-He213 Ain oussera (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Thermodynamic (dpeaa)DE-He213 Algeria (dpeaa)DE-He213
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title	Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria
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title_full	Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria
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title_sort	hydrochemistry of an albian sandstone aquifer in a semi arid region, ain oussera, algeria
title_auth	Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria
abstract	Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. © Springer-Verlag 2009
abstractGer	Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. © Springer-Verlag 2009
abstract_unstemmed	Abstract The studied area is in the south of Algeria. Chemical data are used to determine the status of water quality in the Albian sandstone aquifer of Ain oussera, as well as to clarify the hydrological regime in the study area, to identify spatial and temporal variations of water quality and sources of contamination (natural and anthropogenic). Waters in sandstone are dominated by a magnesium chloride type and sodium chloride type. Interpretation of chemical data with thermodynamic calculation suggests that the chemical evolution of groundwater is primarily controlled by water–rock interactions. Piezometric map suggests that water is moving from the south toward north. The agricultural irrigation effluent and domestic effluents have largely contributed to contamination of groundwater. © Springer-Verlag 2009
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title_short	Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria
url	https://dx.doi.org/10.1007/s12665-009-0207-1
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Hydrochemistry of an Albian sandstone aquifer in a semi arid region, Ain oussera, Algeria

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