Nucleation of naturally occurring calcic amphibole asbestos.

Calcic amphibole Damage zone Natural occurred asbestos Nucleation

Journal

Environmental research
ISSN: 1096-0953
Titre abrégé: Environ Res
Pays: Netherlands
ID NLM: 0147621

Informations de publication

Date de publication:
01 08 2023
Historique:
received: 30 08 2022
revised: 16 11 2022
accepted: 22 11 2022
medline: 30 5 2023
pubmed: 26 3 2023
entrez: 25 3 2023
Statut: ppublish

Résumé

This article proposes an initial model of natural asbestiform minerals growing in four stages. Structures dating from the early stages of the development were observed in the damaged zone surrounding meso-fractures, more particularly in microfractures, microcavities and microcracks that lie in front of and along mesofractures. This study is limited to calcium amphiboles cross-fibers, which develop from altered calcium amphiboles. The observations were made using PLM, with some using TEM. The samples are amphibolites, dolerites and skarns from France. All these rocks have in common that they have been exposed to hydrothermal circulation which gives them a propylite character. The earliest phenomenon was the development of metasomatic veins. In these veins, actinolite form pseudomorphs after hornblendes. The new amphiboles preserve the original morphology of hornblende, in particular the appearance of the cleavages. In the second stage, hydrothermal Fluid circulation promotes the development of subgrains (DSG) with boundaries generally parallel to the cleavage. Some sub-grains become thinner and more and more individualized due to dissolution by the hydrothermal fluid. The third stage is fracturing. The irregular ends of DSGs and amphibole debris can form the substrate of asbestiform mineral nuclei. Further dissolution of DSGs can also lead to the creation of substrates. The last stage is the nucleation and growth. The nuclei have a conical shape and variable widths, from a few microns to about ten microns. The basal parts of the asbestos minerals (BPAMs) extend the DSGs along the c axis. BPAMs have variable widths and can divide during their development at the level of transverse microcracks. BPAMs when not dividing have a morphology comparable to that of whisker nanocrystals synthesized using the vapor-liquid-crystal mechanism. The shape of the fragments from BPMAs is close to that of DSGs as both have variable widths and both have lengths controlled by microcracks.

Identifiants

pubmed: 36965807
pii: S0013-9351(22)02267-8
doi: 10.1016/j.envres.2022.114940
pii:
doi:

Substances chimiques

Asbestos 1332-21-4
Asbestos, Amphibole 0
Calcium SY7Q814VUP
lime C7X2M0VVNH
Minerals 0

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

114940

Informations de copyright

Copyright © 2022 Elsevier Inc. 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:

Auteurs

Maxime Misseri (M)

Sorbonne University, UTC, EA 4297 UTC/ESCOM, F-60205, Compiègne, Cedex, France. Electronic address: maxime.misseri@ad-lab.fr.

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Classifications MeSH