Partition of Cd, Cu, Pb and Zn among mineral particles during their sorption in soils

Purpose Heterogeneity of soil mineral particles may lead to the misinterpretation of bulk sorption data on their role in metal sorption, which may be resolved through the direct observation of metal distribution among the soil particles after the sorption. Materials and methods Analytical transmissi...

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Veröffentlicht in:Journal of soils and sediments 2019-04, Vol.19 (4), p.1775-1787
Hauptverfasser: Sipos, Péter, Tóth, Adrienn, Kis, Viktória Kovács, Balázs, Réka, Kovács, Ivett, Németh, Tibor
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container_end_page 1787
container_issue 4
container_start_page 1775
container_title Journal of soils and sediments
container_volume 19
creator Sipos, Péter
Tóth, Adrienn
Kis, Viktória Kovács
Balázs, Réka
Kovács, Ivett
Németh, Tibor
description Purpose Heterogeneity of soil mineral particles may lead to the misinterpretation of bulk sorption data on their role in metal sorption, which may be resolved through the direct observation of metal distribution among the soil particles after the sorption. Materials and methods Analytical transmission electron microscopy was used to study metal (Cd, Cu, Pb, Zn) sorption characteristics of clay minerals, Fe-oxyhydroxides and their natural assemblages in soils with contrasting pH under single element and competitive situations. Results and discussion Iron-oxyhydroxides sorbed higher metal amounts than clay mineral particles mostly, and the sorption capacity of the latter phases were more affected by competition. Iron-oxyhydroxide particles acted as effective metal sorbents in soils not only as individual particles but also as coatings on other mineral particles, and the structural Fe in clay minerals may also resulted in higher metal sorption in some cases. Besides the direct observation of metal sorption onto soil mineral particles, metal precipitates could be identified directly, and the role of organic surfaces in metal sorption could be inferred indirectly in certain cases. Conclusions Comparison of metal affinity sequences and their partition characteristics between the bulk soil and different mineral particles were found to be an effective tool to specify the most active mineral components in metal sorption at given soil and sorption condition.
doi_str_mv 10.1007/s11368-018-2184-z
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Materials and methods Analytical transmission electron microscopy was used to study metal (Cd, Cu, Pb, Zn) sorption characteristics of clay minerals, Fe-oxyhydroxides and their natural assemblages in soils with contrasting pH under single element and competitive situations. Results and discussion Iron-oxyhydroxides sorbed higher metal amounts than clay mineral particles mostly, and the sorption capacity of the latter phases were more affected by competition. Iron-oxyhydroxide particles acted as effective metal sorbents in soils not only as individual particles but also as coatings on other mineral particles, and the structural Fe in clay minerals may also resulted in higher metal sorption in some cases. Besides the direct observation of metal sorption onto soil mineral particles, metal precipitates could be identified directly, and the role of organic surfaces in metal sorption could be inferred indirectly in certain cases. Conclusions Comparison of metal affinity sequences and their partition characteristics between the bulk soil and different mineral particles were found to be an effective tool to specify the most active mineral components in metal sorption at given soil and sorption condition.</description><identifier>ISSN: 1439-0108</identifier><identifier>EISSN: 1614-7480</identifier><identifier>DOI: 10.1007/s11368-018-2184-z</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Cadmium ; Clay ; Clay minerals ; Copper ; Dust ; Earth and Environmental Science ; Electron microscopy ; Environment ; Environmental Physics ; Heavy metals ; Heterogeneity ; Iron ; Lead ; Metals ; Minerals ; Partitions ; Precipitates ; Sec 3 • Remediation and Management of Contaminated or Degraded Lands • Research Article ; Soil ; Soil conditions ; Soil Science &amp; Conservation ; Soils ; Sorbents ; Sorption ; Transmission electron microscopy ; Zinc</subject><ispartof>Journal of soils and sediments, 2019-04, Vol.19 (4), p.1775-1787</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2018</rights><rights>Journal of Soils and Sediments is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c359t-cc8c686d08d2124c1cc34df63e96617f3f9ca1b2148b24e4e4a3f63b4cafbda3</citedby><cites>FETCH-LOGICAL-c359t-cc8c686d08d2124c1cc34df63e96617f3f9ca1b2148b24e4e4a3f63b4cafbda3</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/s11368-018-2184-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11368-018-2184-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Sipos, Péter</creatorcontrib><creatorcontrib>Tóth, Adrienn</creatorcontrib><creatorcontrib>Kis, Viktória Kovács</creatorcontrib><creatorcontrib>Balázs, Réka</creatorcontrib><creatorcontrib>Kovács, Ivett</creatorcontrib><creatorcontrib>Németh, Tibor</creatorcontrib><title>Partition of Cd, Cu, Pb and Zn among mineral particles during their sorption in soils</title><title>Journal of soils and sediments</title><addtitle>J Soils Sediments</addtitle><description>Purpose Heterogeneity of soil mineral particles may lead to the misinterpretation of bulk sorption data on their role in metal sorption, which may be resolved through the direct observation of metal distribution among the soil particles after the sorption. Materials and methods Analytical transmission electron microscopy was used to study metal (Cd, Cu, Pb, Zn) sorption characteristics of clay minerals, Fe-oxyhydroxides and their natural assemblages in soils with contrasting pH under single element and competitive situations. Results and discussion Iron-oxyhydroxides sorbed higher metal amounts than clay mineral particles mostly, and the sorption capacity of the latter phases were more affected by competition. Iron-oxyhydroxide particles acted as effective metal sorbents in soils not only as individual particles but also as coatings on other mineral particles, and the structural Fe in clay minerals may also resulted in higher metal sorption in some cases. Besides the direct observation of metal sorption onto soil mineral particles, metal precipitates could be identified directly, and the role of organic surfaces in metal sorption could be inferred indirectly in certain cases. 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Materials and methods Analytical transmission electron microscopy was used to study metal (Cd, Cu, Pb, Zn) sorption characteristics of clay minerals, Fe-oxyhydroxides and their natural assemblages in soils with contrasting pH under single element and competitive situations. Results and discussion Iron-oxyhydroxides sorbed higher metal amounts than clay mineral particles mostly, and the sorption capacity of the latter phases were more affected by competition. Iron-oxyhydroxide particles acted as effective metal sorbents in soils not only as individual particles but also as coatings on other mineral particles, and the structural Fe in clay minerals may also resulted in higher metal sorption in some cases. Besides the direct observation of metal sorption onto soil mineral particles, metal precipitates could be identified directly, and the role of organic surfaces in metal sorption could be inferred indirectly in certain cases. Conclusions Comparison of metal affinity sequences and their partition characteristics between the bulk soil and different mineral particles were found to be an effective tool to specify the most active mineral components in metal sorption at given soil and sorption condition.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11368-018-2184-z</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record>
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ispartof Journal of soils and sediments, 2019-04, Vol.19 (4), p.1775-1787
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1614-7480
language eng
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source SpringerLink Journals
subjects Cadmium
Clay
Clay minerals
Copper
Dust
Earth and Environmental Science
Electron microscopy
Environment
Environmental Physics
Heavy metals
Heterogeneity
Iron
Lead
Metals
Minerals
Partitions
Precipitates
Sec 3 • Remediation and Management of Contaminated or Degraded Lands • Research Article
Soil
Soil conditions
Soil Science & Conservation
Soils
Sorbents
Sorption
Transmission electron microscopy
Zinc
title Partition of Cd, Cu, Pb and Zn among mineral particles during their sorption in soils
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