Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones

Subduction of oceanic crust introduces huge amounts of carbonates into Earth’s mantle, contributing to the global carbon cycle. Here, based on high-pressure-temperature experiments, the authors present a reversible temperature-induced transition from aragonite to amorphous CaCO3.

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Autores principales:	Mingqiang Hou, Qian Zhang, Renbiao Tao, Hong Liu, Yoshio Kono, Ho-kwang Mao, Wenge Yang, Bin Chen, Yingwei Fei
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/746f30287f5f4ec38b75fa891083a78b
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spelling	oai:doaj.org-article:746f30287f5f4ec38b75fa891083a78b2021-12-02T16:58:19ZTemperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones10.1038/s41467-019-09742-52041-1723https://doaj.org/article/746f30287f5f4ec38b75fa891083a78b2019-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-09742-5https://doaj.org/toc/2041-1723Subduction of oceanic crust introduces huge amounts of carbonates into Earth’s mantle, contributing to the global carbon cycle. Here, based on high-pressure-temperature experiments, the authors present a reversible temperature-induced transition from aragonite to amorphous CaCO3.Mingqiang HouQian ZhangRenbiao TaoHong LiuYoshio KonoHo-kwang MaoWenge YangBin ChenYingwei FeiNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-8 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Mingqiang Hou Qian Zhang Renbiao Tao Hong Liu Yoshio Kono Ho-kwang Mao Wenge Yang Bin Chen Yingwei Fei Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
description	Subduction of oceanic crust introduces huge amounts of carbonates into Earth’s mantle, contributing to the global carbon cycle. Here, based on high-pressure-temperature experiments, the authors present a reversible temperature-induced transition from aragonite to amorphous CaCO3.
format	article
author	Mingqiang Hou Qian Zhang Renbiao Tao Hong Liu Yoshio Kono Ho-kwang Mao Wenge Yang Bin Chen Yingwei Fei
author_facet	Mingqiang Hou Qian Zhang Renbiao Tao Hong Liu Yoshio Kono Ho-kwang Mao Wenge Yang Bin Chen Yingwei Fei
author_sort	Mingqiang Hou
title	Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
title_short	Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
title_full	Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
title_fullStr	Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
title_full_unstemmed	Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones
title_sort	temperature-induced amorphization in caco3 at high pressure and implications for recycled caco3 in subduction zones
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/746f30287f5f4ec38b75fa891083a78b
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Temperature-induced amorphization in CaCO3 at high pressure and implications for recycled CaCO3 in subduction zones

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