Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles

Calcium and oxygen are abundant elements in the Earth’s mantle, largely present as calcium oxide. Here the authors show, by experiments and computations, that calcium ozonide (CaO3) is stabilized at the high pressures and temperatures characteristic of the lower mantle, with implications for the dee...

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Autores principales:	Yanchao Wang, Meiling Xu, Liuxiang Yang, Bingmin Yan, Qin Qin, Xuecheng Shao, Yunwei Zhang, Dajian Huang, Xiaohuan Lin, Jian Lv, Dongzhou Zhang, Huiyang Gou, Ho-kwang Mao, Changfeng Chen, Yanming Ma
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/8e97a7ccfd684c1f845ec19c3e18b8a6
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

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spelling	oai:doaj.org-article:8e97a7ccfd684c1f845ec19c3e18b8a62021-12-02T15:15:45ZPressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles10.1038/s41467-020-18541-22041-1723https://doaj.org/article/8e97a7ccfd684c1f845ec19c3e18b8a62020-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-18541-2https://doaj.org/toc/2041-1723Calcium and oxygen are abundant elements in the Earth’s mantle, largely present as calcium oxide. Here the authors show, by experiments and computations, that calcium ozonide (CaO3) is stabilized at the high pressures and temperatures characteristic of the lower mantle, with implications for the deep Earth’s chemistry.Yanchao WangMeiling XuLiuxiang YangBingmin YanQin QinXuecheng ShaoYunwei ZhangDajian HuangXiaohuan LinJian LvDongzhou ZhangHuiyang GouHo-kwang MaoChangfeng ChenYanming MaNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-7 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Yanchao Wang Meiling Xu Liuxiang Yang Bingmin Yan Qin Qin Xuecheng Shao Yunwei Zhang Dajian Huang Xiaohuan Lin Jian Lv Dongzhou Zhang Huiyang Gou Ho-kwang Mao Changfeng Chen Yanming Ma Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
description	Calcium and oxygen are abundant elements in the Earth’s mantle, largely present as calcium oxide. Here the authors show, by experiments and computations, that calcium ozonide (CaO3) is stabilized at the high pressures and temperatures characteristic of the lower mantle, with implications for the deep Earth’s chemistry.
format	article
author	Yanchao Wang Meiling Xu Liuxiang Yang Bingmin Yan Qin Qin Xuecheng Shao Yunwei Zhang Dajian Huang Xiaohuan Lin Jian Lv Dongzhou Zhang Huiyang Gou Ho-kwang Mao Changfeng Chen Yanming Ma
author_facet	Yanchao Wang Meiling Xu Liuxiang Yang Bingmin Yan Qin Qin Xuecheng Shao Yunwei Zhang Dajian Huang Xiaohuan Lin Jian Lv Dongzhou Zhang Huiyang Gou Ho-kwang Mao Changfeng Chen Yanming Ma
author_sort	Yanchao Wang
title	Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
title_short	Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
title_full	Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
title_fullStr	Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
title_full_unstemmed	Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles
title_sort	pressure-stabilized divalent ozonide cao3 and its impact on earth’s oxygen cycles
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/8e97a7ccfd684c1f845ec19c3e18b8a6
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Pressure-stabilized divalent ozonide CaO3 and its impact on Earth’s oxygen cycles

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