Soil-sediment linkage and trace element contamination in forested/deforested areas of the Itacai�nas River Watershed, Brazil: To what extent land-use change plays a role?

dc.contributor.authorDall'Agnol, Roberto
dc.contributor.authorSahoo, Prafulla Kumar
dc.contributor.authorSalom�o, Gabriel Negreiros
dc.contributor.authorde Ara�jo, Alessandra Danieli Miranda
dc.contributor.authorda Silva, Marcio Sousa
dc.contributor.authorPowell, Mike A.
dc.contributor.authorJunior, Jair Ferreira
dc.contributor.authorRamos, Silvio Junio
dc.contributor.authorMartins, Gabriel Caixeta
dc.contributor.authorda Costa, Marlene Furtado
dc.contributor.authorGuilherme, Luiz Roberto Guimar�es
dc.date.accessioned2024-01-21T10:50:41Z
dc.date.accessioned2024-08-14T06:39:36Z
dc.date.available2024-01-21T10:50:41Z
dc.date.available2024-08-14T06:39:36Z
dc.date.issued2022-03-08T00:00:00
dc.description.abstractTrace elements (TE) contamination in forested areas of the Itacai�nas River Watershed (IRW), Brazilian Amazon, arouses growing interest owing to the rapid deforestation and mining activities. In this study, soils (surface, SS; bottom, BS) and stream sediments (SD) from forested/deforested areas of IRW were analyzed with the aim of (1) evaluating the major sources of TE (mainly As, Ba, Cd, Cu, Co, Cr, Hg, Mo, Mn, Ni, Pb, V, and Zn), and (2) examining the soil-sediment TE link related to land-use change and/or geologic factors. Compositional data analysis (CoDA) was used to eliminate data closure issues and the centred log-ratio (clr) transformation yielded better results in Principal Component Analysis (PCA). The TE distribution pattern was significantly different (p < 0.05) between forested and deforested areas, but in both areas the TE distribution pattern is significantly correlated between SS, BS, and SD, indicating a strong lithogenic control. PCA (clr-transformed) identified the major geochemical bedrock signature as Fe-Ti-V-Cu-Cr-Ni, which is nearly similar in soil and sediments. The more accentuated enrichment and the maximum number of anomalies of these elements were found in the Caraj�s Basin and are highly coincident with mineral deposits/local lithologies without clear indication of anthropogenic contamination from point sources. Besides geogenic factors, deforestation is also affecting TE distribution in the basin. In deforested areas, Mn was significantly enriched in the surface horizon. Furthermore, linear regression analysis shows stronger TE relationships between soils and sediments in deforested areas than in forested ones, reflecting higher erosion in the former. This could be the reason for the relatively higher enrichment of TE (e.g., Fe, Mn, Cu, Cr, Ni) in deforested sediments. The TE contamination using regional background values provides more accurate results than worldwide reference values. Thus, the former should be considered for a more realistic environmental risk assessment in IRW and other forest ecosystems in the Brazilian Amazon. � 2022 Elsevier B.V.en_US
dc.identifier.doi10.1016/j.scitotenv.2022.154327
dc.identifier.issn489697
dc.identifier.urihttps://kr.cup.edu.in/handle/32116/3982
dc.identifier.urlhttps://linkinghub.elsevier.com/retrieve/pii/S0048969722014206
dc.language.isoen_USen_US
dc.publisherElsevier B.V.en_US
dc.subjectBrazilian Amazon rainforesten_US
dc.subjectCompositional data analysisen_US
dc.subjectDeforestationen_US
dc.subjectForest soilsen_US
dc.subjectGeogenic enrichmenten_US
dc.subjectPotentially toxic elementsen_US
dc.titleSoil-sediment linkage and trace element contamination in forested/deforested areas of the Itacai�nas River Watershed, Brazil: To what extent land-use change plays a role?en_US
dc.title.journalScience of the Total Environmenten_US
dc.typeArticleen_US
dc.type.accesstypeClosed Accessen_US

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