Iron from a geochemical viewpoint. Understanding toxicity/pathogenicity mechanisms in iron-bearing minerals with a special attention to mineral fibers.
Diffraction
Iron
Mineral fibers
Oxidation state
Spectroscopy
Surface activity
Journal
Free radical biology & medicine
ISSN: 1873-4596
Titre abrégé: Free Radic Biol Med
Pays: United States
ID NLM: 8709159
Informations de publication
Date de publication:
03 2019
03 2019
Historique:
received:
14
06
2018
revised:
17
07
2018
accepted:
29
07
2018
pubmed:
3
8
2018
medline:
15
2
2020
entrez:
3
8
2018
Statut:
ppublish
Résumé
Iron and its role as soul of life on Earth is addressed in this review as iron is one of the most abundant elements of our universe, forms the core of our planet and that of telluric (i.e., Earth-like) planets, is a major element of the Earth's crust and is hosted in an endless number of mineral phases, both crystalline and amorphous. To study iron at an atomic level inside the bulk of mineral phases or at its surface, where it is more reactive, both spectroscopy and diffraction experimental methods can be used, taking advantage of nearly the whole spectrum of electromagnetic waves. These methods can be successfully combined to microscopy to simultaneously provide chemical (e.g. iron mapping) and morphological information on mineral particles, and shed light on the interaction of mineral surfaces with organic matter. This review describes the crystal chemistry of iron-bearing minerals of importance for the environment and human health, with special attention to iron in toxic minerals, and the experimental methods used for their study. Special attention is devoted to the Fenton-like chain reaction involving Fe
Identifiants
pubmed: 30071299
pii: S0891-5849(18)31299-1
doi: 10.1016/j.freeradbiomed.2018.07.023
pii:
doi:
Substances chimiques
Mineral Fibers
0
Minerals
0
Hydroxyl Radical
3352-57-6
Iron
E1UOL152H7
Types de publication
Journal Article
Research Support, Non-U.S. Gov't
Review
Langues
eng
Sous-ensembles de citation
IM
Pagination
21-37Informations de copyright
Copyright © 2018 Elsevier Inc. All rights reserved.