Iron isotope fractionation of redox and geochemical cycling in the typical Gleysols in Mun River Basin, Northeast Thailand.
Fe isotope fractionation
Geochemical cycling
Redox
Soil profile
Thailand
Journal
The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500
Informations de publication
Date de publication:
15 Dec 2023
15 Dec 2023
Historique:
received:
11
04
2023
revised:
26
08
2023
accepted:
27
08
2023
medline:
3
9
2023
pubmed:
3
9
2023
entrez:
2
9
2023
Statut:
ppublish
Résumé
Iron (Fe) isotope is a potential tool for tracking redox process and geochemical cycling in terrestrial environment. In this study, Fe concentration and its isotopic composition (δ
Identifiants
pubmed: 37659557
pii: S0048-9697(23)05289-0
doi: 10.1016/j.scitotenv.2023.166664
pii:
doi:
Types de publication
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
166664Informations de copyright
Copyright © 2023 Elsevier B.V. All rights reserved.
Déclaration de conflit d'intérêts
Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.