Insights into the amorphous calcium carbonate (ACC) → ikaite → calcite transformations

Author:

Lázár Anett12,Molnár Zsombor3,Demény Attila1ORCID,Kótai László2ORCID,Trif László2ORCID,Béres Kende Attila24ORCID,Bódis Eszter2ORCID,Bortel Gábor5ORCID,Aradi László Előd6ORCID,Karlik Máté1,Szabó Máté Zoltán1,Pekker Áron5ORCID,Németh Gergely5ORCID,Kamarás Katalin5ORCID,Garvie Laurence A. J.7,Németh Péter13ORCID

Affiliation:

1. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences (MTA Centre of Excellence), Eötvös Loránd Research Network, Budaörsi Street 45, 1112 Budapest, Hungary

2. Institute of Materials and Environmental Chemistry, Research Center for Natural Sciences (MTA Centre of Excellence), Magyar Tudósok Körútja 2, 1117 Budapest, Hungary

3. Research Institute of Biomolecular and Chemical Engineering, Nanolab, Hungary, University of Pannonia, Egyetem út 10, 8200 Veszprém, Hungary

4. György Hevesy PhD School of Chemistry, Institute of Chemistry, Eötvös Loránd University, Pázmány Péter sétány no. 1/c, H-1117, Budapest, HU, Hungary

5. Institute for Solid State Physics and Optics, Wigner Research Centre for Physics, Konkoly Thege u. 29–33, Budapest H-1121, Hungary

6. Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány Péter sétány no. 1/c, H-1117, Budapest, HU, Hungary

7. School of Earth and Space Exploration, Arizona State University, Tempe, Arizona 85287-6004, USA

Abstract

Ikaite formation and its transformation to calcite occurs via distinct amorphous calcium carbonates (referred to as I and II) that differ in their morphology, particle size, water content and stability.

Funder

Nemzeti Kutatási Fejlesztési és Innovációs Hivatal

Publisher

Royal Society of Chemistry (RSC)

Subject

Condensed Matter Physics,General Materials Science,General Chemistry

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