AustralieFrV1, Istex, Corpus, bibRecord, 002279

Pressure‐Induced Polyamorphism and Formation of ‘Aragonitic’ Amorphous Calcium Carbonate

Identifieur interne : 002279 ( Istex/Corpus ); précédent : 002278; suivant : 002280

Pressure‐Induced Polyamorphism and Formation of ‘Aragonitic’ Amorphous Calcium Carbonate

Auteurs : Alejandro Fernandez-Martinez ; Bora Kalkan ; Simon M. Clark ; Glenn A. Waychunas

Source :

Angewandte Chemie [ 0044-8249 ] ; 2013-08-05.

RBID : ISTEX:B9F3C88FC1EFADA1FCD621D7DDA1D2FB43897342

English descriptors

Abstract

Bei 10 GPa Druck geht amorphes Calciumcarbonat (ACC) einen reversiblen Amorph‐amorph‐Phasenübergang zu einer Aragonit‐ähnlichen lokalen Ordnung ein. Dieses Ergebnis spricht für einen Mechanismus, bei dem Mg2+ – ein deutlich kleineres Kation als Ca2+ – die lokale Ordnung in ACC modifiziert, indem es eine Verringerung des molaren Volumens der amorphen Phase gestattet.

Url:

https://api.istex.fr/document/B9F3C88FC1EFADA1FCD621D7DDA1D2FB43897342/fulltext/pdf

DOI: 10.1002/ange.201302974

Links to Exploration step

ISTEX:B9F3C88FC1EFADA1FCD621D7DDA1D2FB43897342

Le document en format XML

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<front><div type="abstract">Bei 10 GPa Druck geht amorphes Calciumcarbonat (ACC) einen reversiblen Amorph‐amorph‐Phasenübergang zu einer Aragonit‐ähnlichen lokalen Ordnung ein. Dieses Ergebnis spricht für einen Mechanismus, bei dem Mg2+ – ein deutlich kleineres Kation als Ca2+ – die lokale Ordnung in ACC modifiziert, indem es eine Verringerung des molaren Volumens der amorphen Phase gestattet.</div>
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   |texte=   Pressure‐Induced Polyamorphism and Formation of ‘Aragonitic’ Amorphous Calcium Carbonate
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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Pressure‐Induced Polyamorphism and Formation of ‘Aragonitic’ Amorphous Calcium Carbonate

Pressure‐Induced Polyamorphism and Formation of ‘Aragonitic’ Amorphous Calcium Carbonate

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