| Literature DB >> 30679371 |
Zhaoyong Zou1, Wouter J E M Habraken1, Galina Matveeva2, Anders C S Jensen1, Luca Bertinetti1, Matthew A Hood1, Chang-Yu Sun3, Pupa U P A Gilbert3,4, Iryna Polishchuk5, Boaz Pokroy5, Julia Mahamid6,7, Yael Politi1, Steve Weiner8, Peter Werner9, Sebastian Bette10, Robert Dinnebier10, Ute Kolb2,11, Emil Zolotoyabko5, Peter Fratzl12.
Abstract
As one of the most abundant materials in the world, calcium carbonate, CaCO3, is the main constituent of the skeletons and shells of various marine organisms. It is used in the cement industry and plays a crucial role in the global carbon cycle and formation of sedimentary rocks. For more than a century, only three polymorphs of pure CaCO3-calcite, aragonite, and vaterite-were known to exist at ambient conditions, as well as two hydrated crystal phases, monohydrocalcite (CaCO3·1H2O) and ikaite (CaCO3·6H2O). While investigating the role of magnesium ions in crystallization pathways of amorphous calcium carbonate, we unexpectedly discovered an unknown crystalline phase, hemihydrate CaCO3·½H2O, with monoclinic structure. This discovery may have important implications in biomineralization, geology, and industrial processes based on hydration of CaCO3.Entities:
Year: 2019 PMID: 30679371 DOI: 10.1126/science.aav0210
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728