CheneBelgiqueV2, PascalFrancis, Curation, bibRecord, 000116

Forest floor leachate fluxes under six different tree species on a metal contaminated site

Identifieur interne : 000116 ( PascalFrancis/Curation ); précédent : 000115; suivant : 000117

Forest floor leachate fluxes under six different tree species on a metal contaminated site

Auteurs : Lotte Van Nevel [Belgique] ; Jan Mertens [Belgique] ; An De Schrijver [Belgique] ; Lander Baeten [Belgique] ; Stefaan De Neve [Belgique] ; Filip M. G. Tack [Belgique] ; Erik Meers [Belgique] ; Kris Verheyen [Belgique]

Source :

Science of the total environment [ 0048-9697 ] ; 2013.

RBID : Pascal:13-0174250

Descripteurs français

Pascal (Inist)
- Sol forestier, Lessivat, Betula pendula, Métal lourd, Cadmium, Elément trace, Carbone organique dissous, Quercus robur, Phytostabilisation, Quercus petraea, Robinia pseudoacacia, Populus tremula, Pinus sylvestris, Pseudotsuga menziesii, Zinc, Phytoremédiation, Bioremédiation, Décontamination.
Wicri :
- topic : Métal lourd, Cadmium, Zinc.

English descriptors

KwdEn :
- Betula pendula, Bioremediation, Cadmium, Decontamination, Dissolved organic carbon, Forest soil, Heavy metal, Leachate, Phytoremediation, Phytostabilization, Pinus sylvestris, Populus tremula, Pseudotsuga menziesii, Quercus petraea, Quercus robur, Robinia pseudoacacia, Trace element, Zinc.

Abstract

Trees play an important role in the biogeochemical cycling of metals, although the influence of different tree species on the mobilization of metals is not yet clear. This study examined effects of six tree species on fluxes of Cd, Zn, DOC, H⁺ and base cations in forest floor leachates on a metal polluted site in Belgium. Forest floor leachates were sampled with zero-tension lysimeters in a 12-year-old post-agricultural forest on a sandy soil. The tree species included were silver birch (Betula pendula), oak (Quercus robur and Q. petraea), black locust (Robinia pseudoacacia), aspen (Populus tremula), Scots pine (Pinus sylvestris) and Douglas fir (Pseudotsuga menziesii). We show that total Cd fluxes in forest floor leachate under aspen were slightly higher than those in the other species' leachates, yet the relative differences between the species were considerably smaller when looking at dissolved Cd fluxes. The latter was probably caused by extremely low H⁺ amounts leaching from aspen's forest floor. No tree species effect was found for Zn leachate fluxes. We expected higher metal leachate fluxes under aspen as its leaf litter was significantly contaminated with Cd and Zn. We propose that the low amounts of Cd and Zn leaching under aspen's forest floor were possibly caused by high activity of soil biota, for example burrowing earthworms. Furthermore, our results reveal that Scots pine and oak were characterized by high H⁺ and DOC fluxes as well as low base cation fluxes in their forest floor leachates, implying that those species might enhance metal mobilization in the soil profile and thus bear a potential risk for belowground metal dispersion.

A01	`01`	`1`		`@0 0048-9697`
A02	`01`			`@0 STENDL`
A03		`1`		`@0 Sci. total environ.`
A05				`@2 447`
A08	`01`	`1`	`ENG`	`@1 Forest floor leachate fluxes under six different tree species on a metal contaminated site`
A11	`01`	`1`		`@1 VAN NEVEL (Lotte)`
A11	`02`	`1`		`@1 MERTENS (Jan)`
A11	`03`	`1`		`@1 DE SCHRIJVER (An)`
A11	`04`	`1`		`@1 BAETEN (Lander)`
A11	`05`	`1`		`@1 DE NEVE (Stefaan)`
A11	`06`	`1`		`@1 TACK (Filip M. G.)`
A11	`07`	`1`		`@1 MEERS (Erik)`
A11	`08`	`1`		`@1 VERHEYEN (Kris)`
A14	`01`			`@1 Forest & Nature Lab, Department of Forest and Water Management, Ghent University, Geraardsbergsesteenweg 267 @2 9090 Melle @3 BEL @Z 1 aut. @Z 3 aut. @Z 4 aut. @Z 8 aut.`
A14	`02`			`@1 Faculty of Applied Bioscience Engineering, University College Ghent, Ghent University Association, Schoonmeersstraat 52 @2 9000 Ghent @3 BEL @Z 2 aut.`
A14	`03`			`@1 Department of Soil Management and Soil Care, Ghent University, Coupure Links 653 @2 9000 Ghent @3 BEL @Z 5 aut.`
A14	`04`			`@1 Laboratory for Analytical Chemistry and Applied Ecochemistry, Department of Applied Analytical and Physical Chemistry, Ghent University, Coupure Links 653 @2 9000 Ghent @3 BEL @Z 6 aut. @Z 7 aut.`
A20				`@1 99-107`
A21				`@1 2013`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 15662 @5 354000502474030120`
A44				`@0 0000 @1 © 2013 INIST-CNRS. All rights reserved.`
A45				`@0 3/4 p.`
A47	`01`	`1`		`@0 13-0174250`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Science of the total environment`
A66	`01`			`@0 GBR`
C01	`01`		`ENG`	@0 Trees play an important role in the biogeochemical cycling of metals, although the influence of different tree species on the mobilization of metals is not yet clear. This study examined effects of six tree species on fluxes of Cd, Zn, DOC, H⁺ and base cations in forest floor leachates on a metal polluted site in Belgium. Forest floor leachates were sampled with zero-tension lysimeters in a 12-year-old post-agricultural forest on a sandy soil. The tree species included were silver birch (Betula pendula), oak (Quercus robur and Q. petraea), black locust (Robinia pseudoacacia), aspen (Populus tremula), Scots pine (Pinus sylvestris) and Douglas fir (Pseudotsuga menziesii). We show that total Cd fluxes in forest floor leachate under aspen were slightly higher than those in the other species' leachates, yet the relative differences between the species were considerably smaller when looking at dissolved Cd fluxes. The latter was probably caused by extremely low H⁺ amounts leaching from aspen's forest floor. No tree species effect was found for Zn leachate fluxes. We expected higher metal leachate fluxes under aspen as its leaf litter was significantly contaminated with Cd and Zn. We propose that the low amounts of Cd and Zn leaching under aspen's forest floor were possibly caused by high activity of soil biota, for example burrowing earthworms. Furthermore, our results reveal that Scots pine and oak were characterized by high H⁺ and DOC fluxes as well as low base cation fluxes in their forest floor leachates, implying that those species might enhance metal mobilization in the soil profile and thus bear a potential risk for belowground metal dispersion.
C02	`01`	`X`		`@0 001D16D05`
C03	`01`	`X`	`FRE`	`@0 Sol forestier @2 NT @5 01`
C03	`01`	`X`	`ENG`	`@0 Forest soil @2 NT @5 01`
C03	`01`	`X`	`SPA`	`@0 Suelo forestal @2 NT @5 01`
C03	`02`	`X`	`FRE`	`@0 Lessivat @5 02`
C03	`02`	`X`	`ENG`	`@0 Leachate @5 02`
C03	`02`	`X`	`SPA`	`@0 Lixiviado @5 02`
C03	`03`	`X`	`FRE`	`@0 Betula pendula @2 NS @5 03`
C03	`03`	`X`	`ENG`	`@0 Betula pendula @2 NS @5 03`
C03	`03`	`X`	`SPA`	`@0 Betula pendula @2 NS @5 03`
C03	`04`	`X`	`FRE`	`@0 Métal lourd @5 04`
C03	`04`	`X`	`ENG`	`@0 Heavy metal @5 04`
C03	`04`	`X`	`SPA`	`@0 Metal pesado @5 04`
C03	`05`	`X`	`FRE`	`@0 Cadmium @2 NC @2 FX @5 05`
C03	`05`	`X`	`ENG`	`@0 Cadmium @2 NC @2 FX @5 05`
C03	`05`	`X`	`SPA`	`@0 Cadmio @2 NC @2 FX @5 05`
C03	`06`	`X`	`FRE`	`@0 Elément trace @5 06`
C03	`06`	`X`	`ENG`	`@0 Trace element @5 06`
C03	`06`	`X`	`SPA`	`@0 Elemento traza @5 06`
C03	`07`	`X`	`FRE`	`@0 Carbone organique dissous @5 07`
C03	`07`	`X`	`ENG`	`@0 Dissolved organic carbon @5 07`
C03	`07`	`X`	`SPA`	`@0 Carbono orgánico disuelto @5 07`
C03	`08`	`X`	`FRE`	`@0 Quercus robur @2 NS @5 08`
C03	`08`	`X`	`ENG`	`@0 Quercus robur @2 NS @5 08`
C03	`08`	`X`	`SPA`	`@0 Quercus robur @2 NS @5 08`
C03	`09`	`X`	`FRE`	`@0 Phytostabilisation @5 09`
C03	`09`	`X`	`ENG`	`@0 Phytostabilization @5 09`
C03	`09`	`X`	`SPA`	`@0 Fitoestabilización @5 09`
C03	`10`	`X`	`FRE`	`@0 Quercus petraea @2 NS @5 10`
C03	`10`	`X`	`ENG`	`@0 Quercus petraea @2 NS @5 10`
C03	`10`	`X`	`SPA`	`@0 Quercus petraea @2 NS @5 10`
C03	`11`	`X`	`FRE`	`@0 Robinia pseudoacacia @2 NS @5 11`
C03	`11`	`X`	`ENG`	`@0 Robinia pseudoacacia @2 NS @5 11`
C03	`11`	`X`	`SPA`	`@0 Robinia pseudoacacia @2 NS @5 11`
C03	`12`	`X`	`FRE`	`@0 Populus tremula @2 NS @5 12`
C03	`12`	`X`	`ENG`	`@0 Populus tremula @2 NS @5 12`
C03	`12`	`X`	`SPA`	`@0 Populus tremula @2 NS @5 12`
C03	`13`	`X`	`FRE`	`@0 Pinus sylvestris @2 NS @5 13`
C03	`13`	`X`	`ENG`	`@0 Pinus sylvestris @2 NS @5 13`
C03	`13`	`X`	`SPA`	`@0 Pinus sylvestris @2 NS @5 13`
C03	`14`	`X`	`FRE`	`@0 Pseudotsuga menziesii @2 NS @5 14`
C03	`14`	`X`	`ENG`	`@0 Pseudotsuga menziesii @2 NS @5 14`
C03	`14`	`X`	`SPA`	`@0 Pseudotsuga menziesii @2 NS @5 14`
C03	`15`	`X`	`FRE`	`@0 Zinc @2 NC @5 15`
C03	`15`	`X`	`ENG`	`@0 Zinc @2 NC @5 15`
C03	`15`	`X`	`SPA`	`@0 Zinc @2 NC @5 15`
C03	`16`	`X`	`FRE`	`@0 Phytoremédiation @5 32`
C03	`16`	`X`	`ENG`	`@0 Phytoremediation @5 32`
C03	`16`	`X`	`SPA`	`@0 Fitorremediación @5 32`
C03	`17`	`X`	`FRE`	`@0 Bioremédiation @5 33`
C03	`17`	`X`	`ENG`	`@0 Bioremediation @5 33`
C03	`17`	`X`	`SPA`	`@0 Biorremediación @5 33`
C03	`18`	`X`	`FRE`	`@0 Décontamination @5 34`
C03	`18`	`X`	`ENG`	`@0 Decontamination @5 34`
C03	`18`	`X`	`SPA`	`@0 Descontaminación @5 34`
C07	`01`	`X`	`FRE`	`@0 Betulaceae @2 NS`
C07	`01`	`X`	`ENG`	`@0 Betulaceae @2 NS`
C07	`01`	`X`	`SPA`	`@0 Betulaceae @2 NS`
C07	`02`	`X`	`FRE`	`@0 Dicotyledones @2 NS`
C07	`02`	`X`	`ENG`	`@0 Dicotyledones @2 NS`
C07	`02`	`X`	`SPA`	`@0 Dicotyledones @2 NS`
C07	`03`	`X`	`FRE`	`@0 Angiospermae @2 NS`
C07	`03`	`X`	`ENG`	`@0 Angiospermae @2 NS`
C07	`03`	`X`	`SPA`	`@0 Angiospermae @2 NS`
C07	`04`	`X`	`FRE`	`@0 Spermatophyta @2 NS`
C07	`04`	`X`	`ENG`	`@0 Spermatophyta @2 NS`
C07	`04`	`X`	`SPA`	`@0 Spermatophyta @2 NS`
C07	`05`	`X`	`FRE`	`@0 Fagaceae @2 NS`
C07	`05`	`X`	`ENG`	`@0 Fagaceae @2 NS`
C07	`05`	`X`	`SPA`	`@0 Fagaceae @2 NS`
C07	`06`	`X`	`FRE`	`@0 Leguminosae @2 NS`
C07	`06`	`X`	`ENG`	`@0 Leguminosae @2 NS`
C07	`06`	`X`	`SPA`	`@0 Leguminosae @2 NS`
C07	`07`	`X`	`FRE`	`@0 Salicaceae @2 NS`
C07	`07`	`X`	`ENG`	`@0 Salicaceae @2 NS`
C07	`07`	`X`	`SPA`	`@0 Salicaceae @2 NS`
C07	`08`	`X`	`FRE`	`@0 Coniferales @2 NS`
C07	`08`	`X`	`ENG`	`@0 Coniferales @2 NS`
C07	`08`	`X`	`SPA`	`@0 Coniferales @2 NS`
C07	`09`	`X`	`FRE`	`@0 Gymnospermae @2 NS`
C07	`09`	`X`	`ENG`	`@0 Gymnospermae @2 NS`
C07	`09`	`X`	`SPA`	`@0 Gymnospermae @2 NS`
C07	`10`	`X`	`FRE`	`@0 Métal transition @2 NC @5 53`
C07	`10`	`X`	`ENG`	`@0 Transition metal @2 NC @5 53`
C07	`10`	`X`	`SPA`	`@0 Metal transición @2 NC @5 53`
N21				`@1 154`

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Le document en format XML

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<author><name sortKey="Van Nevel, Lotte" sort="Van Nevel, Lotte" uniqKey="Van Nevel L" first="Lotte" last="Van Nevel">Lotte Van Nevel</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Forest floor leachate fluxes under six different tree species on a metal contaminated site</title>
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<author><name sortKey="Baeten, Lander" sort="Baeten, Lander" uniqKey="Baeten L" first="Lander" last="Baeten">Lander Baeten</name>
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<author><name sortKey="De Neve, Stefaan" sort="De Neve, Stefaan" uniqKey="De Neve S" first="Stefaan" last="De Neve">Stefaan De Neve</name>
<affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Department of Soil Management and Soil Care, Ghent University, Coupure Links 653</s1>
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<author><name sortKey="Tack, Filip M G" sort="Tack, Filip M G" uniqKey="Tack F" first="Filip M. G." last="Tack">Filip M. G. Tack</name>
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<s2>9000 Ghent</s2>
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</inist:fA14>
<country>Belgique</country>
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<author><name sortKey="Meers, Erik" sort="Meers, Erik" uniqKey="Meers E" first="Erik" last="Meers">Erik Meers</name>
<affiliation wicri:level="1"><inist:fA14 i1="04"><s1>Laboratory for Analytical Chemistry and Applied Ecochemistry, Department of Applied Analytical and Physical Chemistry, Ghent University, Coupure Links 653</s1>
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<author><name sortKey="Verheyen, Kris" sort="Verheyen, Kris" uniqKey="Verheyen K" first="Kris" last="Verheyen">Kris Verheyen</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Forest & Nature Lab, Department of Forest and Water Management, Ghent University, Geraardsbergsesteenweg 267</s1>
<s2>9090 Melle</s2>
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</analytic>
<series><title level="j" type="main">Science of the total environment</title>
<title level="j" type="abbreviated">Sci. total environ.</title>
<idno type="ISSN">0048-9697</idno>
<imprint><date when="2013">2013</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Science of the total environment</title>
<title level="j" type="abbreviated">Sci. total environ.</title>
<idno type="ISSN">0048-9697</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Betula pendula</term>
<term>Bioremediation</term>
<term>Cadmium</term>
<term>Decontamination</term>
<term>Dissolved organic carbon</term>
<term>Forest soil</term>
<term>Heavy metal</term>
<term>Leachate</term>
<term>Phytoremediation</term>
<term>Phytostabilization</term>
<term>Pinus sylvestris</term>
<term>Populus tremula</term>
<term>Pseudotsuga menziesii</term>
<term>Quercus petraea</term>
<term>Quercus robur</term>
<term>Robinia pseudoacacia</term>
<term>Trace element</term>
<term>Zinc</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Sol forestier</term>
<term>Lessivat</term>
<term>Betula pendula</term>
<term>Métal lourd</term>
<term>Cadmium</term>
<term>Elément trace</term>
<term>Carbone organique dissous</term>
<term>Quercus robur</term>
<term>Phytostabilisation</term>
<term>Quercus petraea</term>
<term>Robinia pseudoacacia</term>
<term>Populus tremula</term>
<term>Pinus sylvestris</term>
<term>Pseudotsuga menziesii</term>
<term>Zinc</term>
<term>Phytoremédiation</term>
<term>Bioremédiation</term>
<term>Décontamination</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Métal lourd</term>
<term>Cadmium</term>
<term>Zinc</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Trees play an important role in the biogeochemical cycling of metals, although the influence of different tree species on the mobilization of metals is not yet clear. This study examined effects of six tree species on fluxes of Cd, Zn, DOC, H<sup>+</sup>
 and base cations in forest floor leachates on a metal polluted site in Belgium. Forest floor leachates were sampled with zero-tension lysimeters in a 12-year-old post-agricultural forest on a sandy soil. The tree species included were silver birch (Betula pendula), oak (Quercus robur and Q. petraea), black locust (Robinia pseudoacacia), aspen (Populus tremula), Scots pine (Pinus sylvestris) and Douglas fir (Pseudotsuga menziesii). We show that total Cd fluxes in forest floor leachate under aspen were slightly higher than those in the other species' leachates, yet the relative differences between the species were considerably smaller when looking at dissolved Cd fluxes. The latter was probably caused by extremely low H<sup>+</sup>
 amounts leaching from aspen's forest floor. No tree species effect was found for Zn leachate fluxes. We expected higher metal leachate fluxes under aspen as its leaf litter was significantly contaminated with Cd and Zn. We propose that the low amounts of Cd and Zn leaching under aspen's forest floor were possibly caused by high activity of soil biota, for example burrowing earthworms. Furthermore, our results reveal that Scots pine and oak were characterized by high H<sup>+</sup>
 and DOC fluxes as well as low base cation fluxes in their forest floor leachates, implying that those species might enhance metal mobilization in the soil profile and thus bear a potential risk for belowground metal dispersion.</div>
</front>
</TEI>
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<fA05><s2>447</s2>
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<fA08 i1="01" i2="1" l="ENG"><s1>Forest floor leachate fluxes under six different tree species on a metal contaminated site</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>VAN NEVEL (Lotte)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>MERTENS (Jan)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>DE SCHRIJVER (An)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>BAETEN (Lander)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>DE NEVE (Stefaan)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>TACK (Filip M. G.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>MEERS (Erik)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>VERHEYEN (Kris)</s1>
</fA11>
<fA14 i1="01"><s1>Forest & Nature Lab, Department of Forest and Water Management, Ghent University, Geraardsbergsesteenweg 267</s1>
<s2>9090 Melle</s2>
<s3>BEL</s3>
<sZ>1 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Faculty of Applied Bioscience Engineering, University College Ghent, Ghent University Association, Schoonmeersstraat 52</s1>
<s2>9000 Ghent</s2>
<s3>BEL</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Department of Soil Management and Soil Care, Ghent University, Coupure Links 653</s1>
<s2>9000 Ghent</s2>
<s3>BEL</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Laboratory for Analytical Chemistry and Applied Ecochemistry, Department of Applied Analytical and Physical Chemistry, Ghent University, Coupure Links 653</s1>
<s2>9000 Ghent</s2>
<s3>BEL</s3>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA20><s1>99-107</s1>
</fA20>
<fA21><s1>2013</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>15662</s2>
<s5>354000502474030120</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2013 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3/4 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>13-0174250</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Science of the total environment</s0>
</fA64>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Trees play an important role in the biogeochemical cycling of metals, although the influence of different tree species on the mobilization of metals is not yet clear. This study examined effects of six tree species on fluxes of Cd, Zn, DOC, H<sup>+</sup>
 and base cations in forest floor leachates on a metal polluted site in Belgium. Forest floor leachates were sampled with zero-tension lysimeters in a 12-year-old post-agricultural forest on a sandy soil. The tree species included were silver birch (Betula pendula), oak (Quercus robur and Q. petraea), black locust (Robinia pseudoacacia), aspen (Populus tremula), Scots pine (Pinus sylvestris) and Douglas fir (Pseudotsuga menziesii). We show that total Cd fluxes in forest floor leachate under aspen were slightly higher than those in the other species' leachates, yet the relative differences between the species were considerably smaller when looking at dissolved Cd fluxes. The latter was probably caused by extremely low H<sup>+</sup>
 amounts leaching from aspen's forest floor. No tree species effect was found for Zn leachate fluxes. We expected higher metal leachate fluxes under aspen as its leaf litter was significantly contaminated with Cd and Zn. We propose that the low amounts of Cd and Zn leaching under aspen's forest floor were possibly caused by high activity of soil biota, for example burrowing earthworms. Furthermore, our results reveal that Scots pine and oak were characterized by high H<sup>+</sup>
 and DOC fluxes as well as low base cation fluxes in their forest floor leachates, implying that those species might enhance metal mobilization in the soil profile and thus bear a potential risk for belowground metal dispersion.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001D16D05</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Sol forestier</s0>
<s2>NT</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Forest soil</s0>
<s2>NT</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Suelo forestal</s0>
<s2>NT</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Lessivat</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Leachate</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Lixiviado</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Betula pendula</s0>
<s2>NS</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Betula pendula</s0>
<s2>NS</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Betula pendula</s0>
<s2>NS</s2>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Métal lourd</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Heavy metal</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Metal pesado</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Cadmium</s0>
<s2>NC</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Cadmium</s0>
<s2>NC</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Cadmio</s0>
<s2>NC</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Elément trace</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Trace element</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Elemento traza</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Carbone organique dissous</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Dissolved organic carbon</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Carbono orgánico disuelto</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Quercus robur</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Quercus robur</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Quercus robur</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Phytostabilisation</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Phytostabilization</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Fitoestabilización</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Quercus petraea</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Quercus petraea</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Quercus petraea</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Robinia pseudoacacia</s0>
<s2>NS</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Robinia pseudoacacia</s0>
<s2>NS</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Robinia pseudoacacia</s0>
<s2>NS</s2>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Populus tremula</s0>
<s2>NS</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Populus tremula</s0>
<s2>NS</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Populus tremula</s0>
<s2>NS</s2>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Pinus sylvestris</s0>
<s2>NS</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Pinus sylvestris</s0>
<s2>NS</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Pinus sylvestris</s0>
<s2>NS</s2>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Pseudotsuga menziesii</s0>
<s2>NS</s2>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Pseudotsuga menziesii</s0>
<s2>NS</s2>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Pseudotsuga menziesii</s0>
<s2>NS</s2>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Zinc</s0>
<s2>NC</s2>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Zinc</s0>
<s2>NC</s2>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Zinc</s0>
<s2>NC</s2>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="X" l="FRE"><s0>Phytoremédiation</s0>
<s5>32</s5>
</fC03>
<fC03 i1="16" i2="X" l="ENG"><s0>Phytoremediation</s0>
<s5>32</s5>
</fC03>
<fC03 i1="16" i2="X" l="SPA"><s0>Fitorremediación</s0>
<s5>32</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE"><s0>Bioremédiation</s0>
<s5>33</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG"><s0>Bioremediation</s0>
<s5>33</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA"><s0>Biorremediación</s0>
<s5>33</s5>
</fC03>
<fC03 i1="18" i2="X" l="FRE"><s0>Décontamination</s0>
<s5>34</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG"><s0>Decontamination</s0>
<s5>34</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA"><s0>Descontaminación</s0>
<s5>34</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Betulaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Betulaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Betulaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="FRE"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="ENG"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="SPA"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="FRE"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="ENG"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="SPA"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="FRE"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="ENG"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="SPA"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="FRE"><s0>Leguminosae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="ENG"><s0>Leguminosae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="SPA"><s0>Leguminosae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="FRE"><s0>Salicaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="ENG"><s0>Salicaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="SPA"><s0>Salicaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="FRE"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="ENG"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="SPA"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="09" i2="X" l="FRE"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="09" i2="X" l="ENG"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="09" i2="X" l="SPA"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="10" i2="X" l="FRE"><s0>Métal transition</s0>
<s2>NC</s2>
<s5>53</s5>
</fC07>
<fC07 i1="10" i2="X" l="ENG"><s0>Transition metal</s0>
<s2>NC</s2>
<s5>53</s5>
</fC07>
<fC07 i1="10" i2="X" l="SPA"><s0>Metal transición</s0>
<s2>NC</s2>
<s5>53</s5>
</fC07>
<fN21><s1>154</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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Forest floor leachate fluxes under six different tree species on a metal contaminated site

Forest floor leachate fluxes under six different tree species on a metal contaminated site

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