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dc.contributor.authorSungur, Ali
dc.contributor.authorVural, Alaaddin
dc.contributor.authorGundogdu, Ali
dc.contributor.authorSoylak, Mustafa
dc.date.accessioned2021-11-09T19:49:20Z
dc.date.available2021-11-09T19:49:20Z
dc.date.issued2020
dc.identifier.issn0341-8162
dc.identifier.issn1872-6887
dc.identifier.urihttps://doi.org/10.1016/j.catena.2019.104255
dc.identifier.urihttps://hdl.handle.net/20.500.12440/4009
dc.description.abstractIn this study, the possible impacts of an antimonite mineralization area on agricultural lands with regard to heavy metal concentrations were examined. In this scope, surface soil samples (0-20 cm) were taken from a total of 27 locations including eleven from the Avliyana antimonite mineralization area (Torul, Gumushane-NW Turkey) and its surroundings, eleven from agricultural areas and five from the control area. We digestion method was used with aqua regia procedure for determining the total heavy metal (Cd, Cr, Cu, Ni, Pb, Zn) concentrations of the soil samples. The geochemical fractions of heavy metals in soil samples were determined by way of a sequential extraction procedure. The total heavy metal contents of the soils were determined as: Ni > Cr > Zn > Cu > Pb > Cd for control soils, Cr > Ni > Zn > Cu > Pb > Cd for agricultural soils and Zn > Cu > Ni > Cr > Pb > Cd for mining area soils. It was determined that especially the values of Zn (57.6 +/- 6.2 mu g/g) and Cu (52.4 +/- 5.8 mu g/g) were high at the mineralization area due to hydrothermal alterations that are effective in the formation of mineralization. It was put forth as a result of sequential extraction that the heavy metals examined excluding Pb were observed dominantly in the residual fraction for all data set. On the other hand, it was determined that the non-residual mobile fractions reached from 11% Cr to 78% Pb in control soils, from 20% Cd to 88% Pb in agricultural soils and from 24% Cd to 87% Pb in mineralization area soils. Contamination signals due to mineralization area were monitored by way of the metal content in mobile fractions. Even though the metal concentrations determined in short term are not alarming for agricultural production, signals were observed especially for Cd, Pb, Cu, Ni and Zn elements to be more mobile in mineralization area soils in the long term due to the impact of environmental factors thereby being carried over to and accumulating in agricultural soils. In conclusion, while it is expected that the metal inputs due to mineralization areas may increase in the future, it is suggested to include plant analyses in future studies for determining the impact of the amount of bioavailable metal.en_US
dc.language.isoengen_US
dc.publisherElsevieren_US
dc.relation.ispartofCatenaen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectMineralization areaen_US
dc.subjectAgricultural areaen_US
dc.subjectMetalen_US
dc.subjectSequential extractionen_US
dc.subjectContaminationen_US
dc.titleEffect of antimonite mineralization area on heavy metal contents and geochemical fractions of agricultural soils in Gumushane Province, Turkeyen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.description.wospublicationidWOS:000525323800016en_US
dc.description.scopuspublicationid2-s2.0-85072982039en_US
dc.departmentGümüşhane Üniversitesien_US
dc.authoridSoylak, Mustafa / 0000-0002-1017-0244
dc.authoridGundogdu, Ali / 0000-0002-9594-4121
dc.authoridVURAL, Alaaddin / 0000-0002-0446-828X
dc.identifier.volume184en_US
dc.identifier.doi10.1016/j.catena.2019.104255
dc.authorwosidGUNDOGDU, Ali / AAT-3635-2020
dc.authorwosidSoylak, Mustafa / K-7956-2012
dc.authorscopusid25224170800
dc.authorscopusid55970654700
dc.authorscopusid16042269000
dc.authorscopusid7006488616


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