Detangling past and modern zinc anthropogenic source contributions in an urbanized coastal river by combining elemental, isotope and speciation approaches.

Gadolinium Metal pollution Zn XAS Zn isotope Zn speciation domestic sewage tidal dynamic

Journal

Journal of hazardous materials
ISSN: 1873-3336
Titre abrégé: J Hazard Mater
Pays: Netherlands
ID NLM: 9422688

Informations de publication

Date de publication:
14 Sep 2024
Historique:
received: 04 07 2024
revised: 30 08 2024
accepted: 30 08 2024
medline: 20 9 2024
pubmed: 20 9 2024
entrez: 19 9 2024
Statut: aheadofprint

Résumé

The accumulation of trace metals in the environmental compartments of coastal rivers is a global and complex environmental issue, requiring multiple tools to constrain the various anthropogenic sources and biogeochemical processes affecting the water quality of these environments. The Valao fluvio-estuarine system (Rio de Janeiro, Brazil) presents a challenging case of a coastal river contaminated by both modern and historical anthropogenic metal sources, located in the land and in the intra-estuary, continuously mixed by tidal cycles. This study employed a combination of spatial distribution analysis of trace metals including gadolinium (Gd), zinc (Zn) isotopic analyses, and X-ray absorption spectroscopy (XAS) to distinguish between these sources. The concentrations of metals in both dissolved (water samples) and surficial sediment compartments (Suspended Particulate Matter and sediment samples) display an overall enrichment trend from upstream to downstream. Multivariate statistical analysis allows to discriminate geogenic elements derived from watershed geology (Ti, K, and Mg) vs anthropogenic contaminants from urban runoff and domestic sewage discharges (Cu, Cr, Pb, Zn, and Gd); and legacy metal contaminants (Zn and Cd) remobilized from ancient metallurgical wastes and transported upstream in the estuary during tidal cycles. The anthropogenic Gd concentration in the dissolved compartment increases along the watercourse, highlighting continuous ongoing sewage discharge. Zinc solid speciation also indicates that Zn contribution from legacy metallurgy waste is primarily associated with sulfide-Zn and Zn-phyllosilicate in the outlet estuary, while in upstream sediments of fluvio-estuarine system, Zn is found bound to organic matter. Zinc isotope systematically reveals a progressive downstream shift to heavier isotope compositions. Upstream, the relatively pristine site and the urbanized section of the river exhibit a relatively uniform δ

Identifiants

pubmed: 39298958
pii: S0304-3894(24)02293-3
doi: 10.1016/j.jhazmat.2024.135714
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

135714

Informations de copyright

Copyright © 2024 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of Competing Interest The authors declare the following financial interests/personal relationships which may be considered as potential competing interests. Jeremie garnier reports financial support was provided by National Council for Scientific and Technological Development. Jeremie garnier reports was provided by Coordination of Higher Education Personnel Improvement. Jeremie garnier reports a relationship with National Council for Scientific and Technological Development that includes: funding grants. If there are other authors, they declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

J Garnier (J)

University of Brasilia, Institute of Geosciences, Graduate Program in Geology, Asa Norte, 70910-900 Brasilia, DF, Brazil. Electronic address: garnier@unb.br.

M Tonha (M)

University of Brasilia, Institute of Geosciences, Graduate Program in Geology, Asa Norte, 70910-900 Brasilia, DF, Brazil.

D F Araujo (DF)

Ifremer, CCEM, Unité Contamination Chimique des Ecosystèmes Marins, F-F-44300 Nantes, France.

G Landrot (G)

Synchrotron SOLEIL, 91190 Saint Aubin, France.

B Cunha (B)

University of Brasilia, Institute of Geosciences, Graduate Program in Geology, Asa Norte, 70910-900 Brasilia, DF, Brazil; Center of Geochronological Research, Geoscience Institute, University of São Paulo, São Paulo, SP, Brazil.

W Machado (W)

Geochemistry Department, Federal University of Fluminense, Campus do Valonguinho, Niterói, Rio de Janeiro, Brazil.

E Resongles (E)

Hydrosciences Montpellier, Univ. Montpellier, CNRS, IRD, Montpellier, France.

R Freydier (R)

Hydrosciences Montpellier, Univ. Montpellier, CNRS, IRD, Montpellier, France.

P Seyler (P)

University of Brasilia, Institute of Geosciences, Graduate Program in Geology, Asa Norte, 70910-900 Brasilia, DF, Brazil; Hydrosciences Montpellier, Univ. Montpellier, CNRS, IRD, Montpellier, France.

G Ratié (G)

Nantes Université, Univ. Angers, Le Mans Université, CNRS, Laboratoire de Planétologie et Géosciences LPG UMR 6112, F-44000 Nantes, France.

Classifications MeSH