CobaltMaghrebV1, PascalFrancis, Curation, bibRecord, 000263

Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)

Identifieur interne : 000263 ( PascalFrancis/Curation ); précédent : 000262; suivant : 000264

Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)

Auteurs : Ammar Mlayah [Tunisie] ; Eduardo Anselmo Ferreira Da Silva [Portugal] ; Fethi Lachaal [Tunisie] ; Samia Khadhar [Tunisie] ; Abdelkrim Charef [Tunisie] ; Fernando Noronha [Portugal]

Source :

Hydrological sciences journal [ 0262-6667 ] ; 2013.

RBID : Pascal:13-0194619

Descripteurs français

Pascal (Inist)
- Eau surface, Bassin versant, Oued, Pollution, Mine, Zinc, Strontium, Phosphate, Haldes, Aluminium, Arsenic, Bore, Baryum, Brome, Cadmium, Cobalt, Chrome, Cuivre, Mercure, Nickel, Uranium, Gestion ressource eau, Concentration, Contamination, Evaporite, Tunisie.
Wicri :
- geographic : Tunisie.
- topic : Pollution, Zinc, Phosphate, Aluminium, Brome, Cadmium, Cobalt, Chrome, Cuivre, Mercure, Nickel, Uranium.

English descriptors

KwdEn :
- Tunisia, aluminum, arsenic, barium, boron, bromine, cadmium, chromium, cobalt, concentration, contamination, copper, drainage basins, evaporites, mercury, mines, nickel, phosphates, pollution, strontium, surface water, tailings, uranium, wadis, water resource management, zinc.

Abstract

The northwest of Tunisia comprises more than 81% of surface waters and contains 95% of the country's mines and mineral deposits. The Mellègue catchment, located in this area, contains 10 mines extracting lead, zinc, iron, strontium, fluoride and phosphates. The impact of tailings from these mines on surface waters, was evaluated on the basis of several sampling campaigns. The results of ICP/MS analysis of the samples show that they are rich in Al, As, B, Ba, Br, Cd, Co, Cr, Cu, Hg, Mo, Ni, Sr, U and Zn. Tests for these elements in the waters of the Mellègue, its tributaries and in the Nebeur reservoir found that concentrations did not exceded the drinking water thresholds set by the WHO. The reduced water contamination with metals observed in this study may be due to: the presence of geological outcrops formed by limestone, clays and evaporite rocks, the absence of streams draining the tailings directly, and the formation of secondary minerals that strongly adsorb heavy metals and the extent of uncontaminated area in the catchment.

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A08	`01`	`1`	`FRE`	`@1 Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)`
A11	`01`	`1`		`@1 MLAYAH (Ammar)`
A11	`02`	`1`		`@1 FERREIRA DA SILVA (Eduardo Anselmo)`
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A11	`06`	`1`		`@1 NORONHA (Fernando)`
A14	`01`			`@1 Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020 @2 Soliman @3 TUN @Z 1 aut. @Z 3 aut. @Z 4 aut. @Z 5 aut.`
A14	`02`			`@1 GeoBioTec-Geobiosciences, Géotechnologies and Geoengineering Research Centre @2 3810-193 Aveiro @3 PRT @Z 2 aut.`
A14	`03`			`@1 Centro de Geologiada Universidade do Porto, Rua Campo Alegre @2 4769-007 Porto @3 PRT @Z 6 aut.`
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C01	`01`		`FRE`	@0 The northwest of Tunisia comprises more than 81% of surface waters and contains 95% of the country's mines and mineral deposits. The Mellègue catchment, located in this area, contains 10 mines extracting lead, zinc, iron, strontium, fluoride and phosphates. The impact of tailings from these mines on surface waters, was evaluated on the basis of several sampling campaigns. The results of ICP/MS analysis of the samples show that they are rich in Al, As, B, Ba, Br, Cd, Co, Cr, Cu, Hg, Mo, Ni, Sr, U and Zn. Tests for these elements in the waters of the Mellègue, its tributaries and in the Nebeur reservoir found that concentrations did not exceded the drinking water thresholds set by the WHO. The reduced water contamination with metals observed in this study may be due to: the presence of geological outcrops formed by limestone, clays and evaporite rocks, the absence of streams draining the tailings directly, and the formation of secondary minerals that strongly adsorb heavy metals and the extent of uncontaminated area in the catchment.
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C02	`05`	`2`		`@0 226B04`
C02	`06`	`2`		`@0 220B02`
C03	`01`	`2`	`FRE`	`@0 Eau surface @5 01`
C03	`01`	`2`	`ENG`	`@0 surface water @5 01`
C03	`01`	`2`	`SPA`	`@0 Agua superficie @5 01`
C03	`02`	`2`	`FRE`	`@0 Bassin versant @5 02`
C03	`02`	`2`	`ENG`	`@0 drainage basins @5 02`
C03	`02`	`2`	`SPA`	`@0 Cuenca @5 02`
C03	`03`	`2`	`FRE`	`@0 Oued @5 03`
C03	`03`	`2`	`ENG`	`@0 wadis @5 03`
C03	`04`	`2`	`FRE`	`@0 Pollution @5 04`
C03	`04`	`2`	`ENG`	`@0 pollution @5 04`
C03	`04`	`2`	`SPA`	`@0 Polución @5 04`
C03	`05`	`2`	`FRE`	`@0 Mine @5 05`
C03	`05`	`2`	`ENG`	`@0 mines @5 05`
C03	`05`	`2`	`SPA`	`@0 Mina @5 05`
C03	`06`	`2`	`FRE`	`@0 Zinc @5 06`
C03	`06`	`2`	`ENG`	`@0 zinc @5 06`
C03	`06`	`2`	`SPA`	`@0 Zinc @5 06`
C03	`07`	`2`	`FRE`	`@0 Strontium @5 07`
C03	`07`	`2`	`ENG`	`@0 strontium @5 07`
C03	`07`	`2`	`SPA`	`@0 Estroncio @5 07`
C03	`08`	`2`	`FRE`	`@0 Phosphate @2 NZ @5 08`
C03	`08`	`2`	`ENG`	`@0 phosphates @2 NZ @5 08`
C03	`08`	`2`	`SPA`	`@0 Fosfato @2 NZ @5 08`
C03	`09`	`2`	`FRE`	`@0 Haldes @5 09`
C03	`09`	`2`	`ENG`	`@0 tailings @5 09`
C03	`09`	`2`	`SPA`	`@0 Esteril @5 09`
C03	`10`	`2`	`FRE`	`@0 Aluminium @5 10`
C03	`10`	`2`	`ENG`	`@0 aluminum @5 10`
C03	`10`	`2`	`SPA`	`@0 Aluminio @5 10`
C03	`11`	`2`	`FRE`	`@0 Arsenic @5 11`
C03	`11`	`2`	`ENG`	`@0 arsenic @5 11`
C03	`11`	`2`	`SPA`	`@0 Arsénico @5 11`
C03	`12`	`2`	`FRE`	`@0 Bore @5 12`
C03	`12`	`2`	`ENG`	`@0 boron @5 12`
C03	`12`	`2`	`SPA`	`@0 Boro @5 12`
C03	`13`	`2`	`FRE`	`@0 Baryum @5 13`
C03	`13`	`2`	`ENG`	`@0 barium @5 13`
C03	`13`	`2`	`SPA`	`@0 Bario @5 13`
C03	`14`	`2`	`FRE`	`@0 Brome @5 14`
C03	`14`	`2`	`ENG`	`@0 bromine @5 14`
C03	`14`	`2`	`SPA`	`@0 Bromo @5 14`
C03	`15`	`2`	`FRE`	`@0 Cadmium @5 15`
C03	`15`	`2`	`ENG`	`@0 cadmium @5 15`
C03	`15`	`2`	`SPA`	`@0 Cadmio @5 15`
C03	`16`	`2`	`FRE`	`@0 Cobalt @5 16`
C03	`16`	`2`	`ENG`	`@0 cobalt @5 16`
C03	`16`	`2`	`SPA`	`@0 Cobalto @5 16`
C03	`17`	`2`	`FRE`	`@0 Chrome @5 17`
C03	`17`	`2`	`ENG`	`@0 chromium @5 17`
C03	`17`	`2`	`SPA`	`@0 Cromo @5 17`
C03	`18`	`2`	`FRE`	`@0 Cuivre @5 18`
C03	`18`	`2`	`ENG`	`@0 copper @5 18`
C03	`18`	`2`	`SPA`	`@0 Cobre @5 18`
C03	`19`	`2`	`FRE`	`@0 Mercure @5 19`
C03	`19`	`2`	`ENG`	`@0 mercury @5 19`
C03	`19`	`2`	`SPA`	`@0 Mercurio @5 19`
C03	`20`	`2`	`FRE`	`@0 Nickel @5 20`
C03	`20`	`2`	`ENG`	`@0 nickel @5 20`
C03	`20`	`2`	`SPA`	`@0 Niquel @5 20`
C03	`21`	`2`	`FRE`	`@0 Uranium @5 21`
C03	`21`	`2`	`ENG`	`@0 uranium @5 21`
C03	`21`	`2`	`SPA`	`@0 Uranio @5 21`
C03	`22`	`2`	`FRE`	`@0 Gestion ressource eau @5 22`
C03	`22`	`2`	`ENG`	`@0 water resource management @5 22`
C03	`22`	`2`	`SPA`	`@0 Gestión recurso agua @5 22`
C03	`23`	`2`	`FRE`	`@0 Concentration @5 23`
C03	`23`	`2`	`ENG`	`@0 concentration @5 23`
C03	`23`	`2`	`SPA`	`@0 Concentración @5 23`
C03	`24`	`2`	`FRE`	`@0 Contamination @5 24`
C03	`24`	`2`	`ENG`	`@0 contamination @5 24`
C03	`24`	`2`	`SPA`	`@0 Contaminación @5 24`
C03	`25`	`2`	`FRE`	`@0 Evaporite @2 NV @5 25`
C03	`25`	`2`	`ENG`	`@0 evaporites @2 NV @5 25`
C03	`25`	`2`	`SPA`	`@0 Evaporito @2 NV @5 25`
C03	`26`	`2`	`FRE`	`@0 Tunisie @2 NG @5 61`
C03	`26`	`2`	`ENG`	`@0 Tunisia @2 NG @5 61`
C03	`26`	`2`	`SPA`	`@0 Tunez @2 NG @5 61`
C07	`01`	`2`	`FRE`	`@0 Roche chimique @2 NV`
C07	`01`	`2`	`ENG`	`@0 chemically precipitated rocks @2 NV`
C07	`01`	`2`	`SPA`	`@0 Roca química @2 NV`
C07	`02`	`2`	`FRE`	`@0 Roche sédimentaire @2 NV`
C07	`02`	`2`	`ENG`	`@0 sedimentary rocks @2 NV`
C07	`02`	`2`	`SPA`	`@0 Roca sedimentaria @2 NV`
C07	`03`	`2`	`FRE`	`@0 Afrique du Nord @2 NG`
C07	`03`	`2`	`ENG`	`@0 North Africa @2 NG`
C07	`03`	`2`	`SPA`	`@0 Africa del norte @2 NG`
C07	`04`	`2`	`FRE`	`@0 Afrique @2 564`
C07	`04`	`2`	`ENG`	`@0 Africa @2 564`
C07	`04`	`2`	`SPA`	`@0 Africa @2 564`
N21				`@1 175`

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Pascal:13-0194619

Le document en format XML

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<author><name sortKey="Mlayah, Ammar" sort="Mlayah, Ammar" uniqKey="Mlayah A" first="Ammar" last="Mlayah">Ammar Mlayah</name>
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<author><name sortKey="Ferreira Da Silva, Eduardo Anselmo" sort="Ferreira Da Silva, Eduardo Anselmo" uniqKey="Ferreira Da Silva E" first="Eduardo Anselmo" last="Ferreira Da Silva">Eduardo Anselmo Ferreira Da Silva</name>
<affiliation wicri:level="1"><inist:fA14 i1="02"><s1>GeoBioTec-Geobiosciences, Géotechnologies and Geoengineering Research Centre</s1>
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<author><name sortKey="Charef, Abdelkrim" sort="Charef, Abdelkrim" uniqKey="Charef A" first="Abdelkrim" last="Charef">Abdelkrim Charef</name>
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<author><name sortKey="Noronha, Fernando" sort="Noronha, Fernando" uniqKey="Noronha F" first="Fernando" last="Noronha">Fernando Noronha</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="fr" level="a">Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)</title>
<author><name sortKey="Mlayah, Ammar" sort="Mlayah, Ammar" uniqKey="Mlayah A" first="Ammar" last="Mlayah">Ammar Mlayah</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020</s1>
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<author><name sortKey="Ferreira Da Silva, Eduardo Anselmo" sort="Ferreira Da Silva, Eduardo Anselmo" uniqKey="Ferreira Da Silva E" first="Eduardo Anselmo" last="Ferreira Da Silva">Eduardo Anselmo Ferreira Da Silva</name>
<affiliation wicri:level="1"><inist:fA14 i1="02"><s1>GeoBioTec-Geobiosciences, Géotechnologies and Geoengineering Research Centre</s1>
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</author>
<author><name sortKey="Lachaal, Fethi" sort="Lachaal, Fethi" uniqKey="Lachaal F" first="Fethi" last="Lachaal">Fethi Lachaal</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020</s1>
<s2>Soliman</s2>
<s3>TUN</s3>
<sZ>1 aut.</sZ>
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<country>Tunisie</country>
</affiliation>
</author>
<author><name sortKey="Khadhar, Samia" sort="Khadhar, Samia" uniqKey="Khadhar S" first="Samia" last="Khadhar">Samia Khadhar</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020</s1>
<s2>Soliman</s2>
<s3>TUN</s3>
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<country>Tunisie</country>
</affiliation>
</author>
<author><name sortKey="Charef, Abdelkrim" sort="Charef, Abdelkrim" uniqKey="Charef A" first="Abdelkrim" last="Charef">Abdelkrim Charef</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020</s1>
<s2>Soliman</s2>
<s3>TUN</s3>
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<author><name sortKey="Noronha, Fernando" sort="Noronha, Fernando" uniqKey="Noronha F" first="Fernando" last="Noronha">Fernando Noronha</name>
<affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Centro de Geologiada Universidade do Porto, Rua Campo Alegre</s1>
<s2>4769-007 Porto</s2>
<s3>PRT</s3>
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<country>Portugal</country>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Hydrological sciences journal</title>
<title level="j" type="abbreviated">Hydrol. sci. j.</title>
<idno type="ISSN">0262-6667</idno>
<imprint><date when="2013">2013</date>
</imprint>
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</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Hydrological sciences journal</title>
<title level="j" type="abbreviated">Hydrol. sci. j.</title>
<idno type="ISSN">0262-6667</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Tunisia</term>
<term>aluminum</term>
<term>arsenic</term>
<term>barium</term>
<term>boron</term>
<term>bromine</term>
<term>cadmium</term>
<term>chromium</term>
<term>cobalt</term>
<term>concentration</term>
<term>contamination</term>
<term>copper</term>
<term>drainage basins</term>
<term>evaporites</term>
<term>mercury</term>
<term>mines</term>
<term>nickel</term>
<term>phosphates</term>
<term>pollution</term>
<term>strontium</term>
<term>surface water</term>
<term>tailings</term>
<term>uranium</term>
<term>wadis</term>
<term>water resource management</term>
<term>zinc</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Eau surface</term>
<term>Bassin versant</term>
<term>Oued</term>
<term>Pollution</term>
<term>Mine</term>
<term>Zinc</term>
<term>Strontium</term>
<term>Phosphate</term>
<term>Haldes</term>
<term>Aluminium</term>
<term>Arsenic</term>
<term>Bore</term>
<term>Baryum</term>
<term>Brome</term>
<term>Cadmium</term>
<term>Cobalt</term>
<term>Chrome</term>
<term>Cuivre</term>
<term>Mercure</term>
<term>Nickel</term>
<term>Uranium</term>
<term>Gestion ressource eau</term>
<term>Concentration</term>
<term>Contamination</term>
<term>Evaporite</term>
<term>Tunisie</term>
</keywords>
<keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Tunisie</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Pollution</term>
<term>Zinc</term>
<term>Phosphate</term>
<term>Aluminium</term>
<term>Brome</term>
<term>Cadmium</term>
<term>Cobalt</term>
<term>Chrome</term>
<term>Cuivre</term>
<term>Mercure</term>
<term>Nickel</term>
<term>Uranium</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="fr">The northwest of Tunisia comprises more than 81% of surface waters and contains 95% of the country's mines and mineral deposits. The Mellègue catchment, located in this area, contains 10 mines extracting lead, zinc, iron, strontium, fluoride and phosphates. The impact of tailings from these mines on surface waters, was evaluated on the basis of several sampling campaigns. The results of ICP/MS analysis of the samples show that they are rich in Al, As, B, Ba, Br, Cd, Co, Cr, Cu, Hg, Mo, Ni, Sr, U and Zn. Tests for these elements in the waters of the Mellègue, its tributaries and in the Nebeur reservoir found that concentrations did not exceded the drinking water thresholds set by the WHO. The reduced water contamination with metals observed in this study may be due to: the presence of geological outcrops formed by limestone, clays and evaporite rocks, the absence of streams draining the tailings directly, and the formation of secondary minerals that strongly adsorb heavy metals and the extent of uncontaminated area in the catchment.</div>
</front>
</TEI>
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<fA02 i1="01"><s0>HSJODN</s0>
</fA02>
<fA03 i2="1"><s0>Hydrol. sci. j.</s0>
</fA03>
<fA05><s2>58</s2>
</fA05>
<fA06><s2>3</s2>
</fA06>
<fA08 i1="01" i2="1" l="FRE"><s1>Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>MLAYAH (Ammar)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>FERREIRA DA SILVA (Eduardo Anselmo)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>LACHAAL (Fethi)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>KHADHAR (Samia)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>CHAREF (Abdelkrim)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>NORONHA (Fernando)</s1>
</fA11>
<fA14 i1="01"><s1>Laboratoire Géoressources, Centre de Recherches et des Technologies des Eaux (CERTE), Université Tunis Carthage, Route touristique de Soliman 8020</s1>
<s2>Soliman</s2>
<s3>TUN</s3>
<sZ>1 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>GeoBioTec-Geobiosciences, Géotechnologies and Geoengineering Research Centre</s1>
<s2>3810-193 Aveiro</s2>
<s3>PRT</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Centro de Geologiada Universidade do Porto, Rua Campo Alegre</s1>
<s2>4769-007 Porto</s2>
<s3>PRT</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA20><s1>686-705</s1>
</fA20>
<fA21><s1>2013</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA24 i1="01"><s0>fre</s0>
</fA24>
<fA43 i1="01"><s1>INIST</s1>
<s2>8967B</s2>
<s5>354000503796850130</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2013 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>13-0194619</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Hydrological sciences journal</s0>
</fA64>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="FRE"><s0>The northwest of Tunisia comprises more than 81% of surface waters and contains 95% of the country's mines and mineral deposits. The Mellègue catchment, located in this area, contains 10 mines extracting lead, zinc, iron, strontium, fluoride and phosphates. The impact of tailings from these mines on surface waters, was evaluated on the basis of several sampling campaigns. The results of ICP/MS analysis of the samples show that they are rich in Al, As, B, Ba, Br, Cd, Co, Cr, Cu, Hg, Mo, Ni, Sr, U and Zn. Tests for these elements in the waters of the Mellègue, its tributaries and in the Nebeur reservoir found that concentrations did not exceded the drinking water thresholds set by the WHO. The reduced water contamination with metals observed in this study may be due to: the presence of geological outcrops formed by limestone, clays and evaporite rocks, the absence of streams draining the tailings directly, and the formation of secondary minerals that strongly adsorb heavy metals and the extent of uncontaminated area in the catchment.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E01N01</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01O04</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01B02</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>226A01</s0>
</fC02>
<fC02 i1="05" i2="2"><s0>226B04</s0>
</fC02>
<fC02 i1="06" i2="2"><s0>220B02</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Eau surface</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>surface water</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Agua superficie</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Bassin versant</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>drainage basins</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Cuenca</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Oued</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>wadis</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Pollution</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>pollution</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Polución</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Mine</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>mines</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Mina</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Zinc</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>zinc</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Zinc</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Strontium</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>strontium</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Estroncio</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Phosphate</s0>
<s2>NZ</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>phosphates</s0>
<s2>NZ</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Fosfato</s0>
<s2>NZ</s2>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Haldes</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>tailings</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Esteril</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Aluminium</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>aluminum</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Aluminio</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Arsenic</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>arsenic</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Arsénico</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Bore</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>boron</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Boro</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Baryum</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>barium</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Bario</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Brome</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>bromine</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Bromo</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Cadmium</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>cadmium</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Cadmio</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Cobalt</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>cobalt</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Cobalto</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Chrome</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>chromium</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Cromo</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Cuivre</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>copper</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Cobre</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Mercure</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>mercury</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Mercurio</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Nickel</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>nickel</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Niquel</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Uranium</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>uranium</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Uranio</s0>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Gestion ressource eau</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>water resource management</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Gestión recurso agua</s0>
<s5>22</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Concentration</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>concentration</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Concentración</s0>
<s5>23</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Contamination</s0>
<s5>24</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>contamination</s0>
<s5>24</s5>
</fC03>
<fC03 i1="24" i2="2" l="SPA"><s0>Contaminación</s0>
<s5>24</s5>
</fC03>
<fC03 i1="25" i2="2" l="FRE"><s0>Evaporite</s0>
<s2>NV</s2>
<s5>25</s5>
</fC03>
<fC03 i1="25" i2="2" l="ENG"><s0>evaporites</s0>
<s2>NV</s2>
<s5>25</s5>
</fC03>
<fC03 i1="25" i2="2" l="SPA"><s0>Evaporito</s0>
<s2>NV</s2>
<s5>25</s5>
</fC03>
<fC03 i1="26" i2="2" l="FRE"><s0>Tunisie</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="ENG"><s0>Tunisia</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="SPA"><s0>Tunez</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Roche chimique</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>chemically precipitated rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Roca química</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Roche sédimentaire</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>sedimentary rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Roca sedimentaria</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Afrique du Nord</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>North Africa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Africa del norte</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Afrique</s0>
<s2>564</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Africa</s0>
<s2>564</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Africa</s0>
<s2>564</s2>
</fC07>
<fN21><s1>175</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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	Serveur d'exploration sur le cobalt au Maghreb
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Serveur d'exploration sur le cobalt au Maghreb

Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)

Effet auto-épurateur de la lithologie des affleurements géologiques dans un climat semi-aride: cas du bassin versant de l'Oued Mellègue (Nord-Ouest de la Tunisie)

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