Multi O- and S-isotopes as tracers of black crusts formation under volcanic and non-volcanic atmospheric conditions in Sicily (Italy).
Black crust
Oxygen isotope
Stone degradation
Sulphur isotope
Volcanic emissions
Δ(17)O anomaly
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:
01 Jan 2021
01 Jan 2021
Historique:
received:
12
06
2020
revised:
04
09
2020
accepted:
07
09
2020
entrez:
13
11
2020
pubmed:
14
11
2020
medline:
14
11
2020
Statut:
ppublish
Résumé
The deterioration of monument or building stone materials is mostly due to the growth of black crusts that cause blackening and disaggregation of the exposed surface. This study reports on new oxygen (δ
Identifiants
pubmed: 33182218
pii: S0048-9697(20)35812-5
doi: 10.1016/j.scitotenv.2020.142283
pii:
doi:
Types de publication
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
142283Informations de copyright
Copyright © 2020 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.