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TECHNOLOGICAL MINERALOGY
Название Hypervalent states of Fe-Co-Ni elements triad as forms of their entry into the Earth's core
Автор Zuev V. V.
Информация об авторе

Mekhanobr Engineering JSC (Russia):

Zuev V. V., Leading Researcher,  office@mekhanobr.spb.ru

Реферат

Additional arguments are presented in support of the considered in the article «On the problem about nature of Earth’s inner core and possibilities of the existence of substances harder than diamond» (Gornyi Zhurnal, 2012, No 2, pp. 4–7) composition (Fe0,9Ni0,1), structure (bodycentered cubic lattice with elementary cell parameter a0 = 2.49 Å) and the Earth's inner core. New hypothesis on possible cobalt entry into the Earth's inner core central part as separate phase-homoatomic covalent crystal with CN = 9 and realization of 3d54sp3 hybrid interconnections and 9-valent metal, is formulated and substantiated. The formation conditions (Р = 265 GPa and T ≈ 4000–4500 K), as well as unique energy and physical parameters of Co (IX) phase, significantly exceeding those of Fe(VIII)0,9Ni(VIII)0,1 phase, are discussed. The issue of quantitative (evidently, quite insignificant) occurrence of new phase remains open, however, the very presence of Fe-Co-Ni elements triad in hypervalent states in the Earth's inner core seems quite real and natural.

Ключевые слова Fe-Co-Ni triad in the Earth's core, energy density and matter extreme properties, new ultra-hard materials
Библиографический список

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Language of full-text русский
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