Magnetic susceptibility of HCP iron and seismic anisotropy of the Earth’s core

The seismic anisotropy of the Earth was proposed to be due to a preferred orientation of HCP iron crystals that constitutes the dominating element in the core. The suggested mechanism involves the anisotropy of the magnetic susceptibility χ of HCP iron, and it is argued that if χ is sufficiently ani...

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Бібліографічні деталі
Дата:2003
Автори: Grechnev, G.E., Ahuja, R., Eriksson, O.
Формат: Стаття
Мова:English
Опубліковано: Донецький фізико-технічний інститут ім. О.О. Галкіна НАН України 2003
Назва видання:Физика и техника высоких давлений
Онлайн доступ:http://dspace.nbuv.gov.ua/handle/123456789/167954
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Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Цитувати:Magnetic susceptibility of HCP iron and seismic anisotropy of the Earth’s core / G.E. Grechnev, R. Ahuja, O. Eriksson // Физика и техника высоких давлений. — 2003. — Т. 13, № 1. — С. 14-18. — Бібліогр.: 19 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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Резюме:The seismic anisotropy of the Earth was proposed to be due to a preferred orientation of HCP iron crystals that constitutes the dominating element in the core. The suggested mechanism involves the anisotropy of the magnetic susceptibility χ of HCP iron, and it is argued that if χ is sufficiently anisotropic, a preferential orientation of the HCP crystals may occur. We have calculated ab initio χ and the anisotropy energy of HCP iron for pressures and temperatures corresponding to the Earth's inner core conditions. Our calculations demonstrate that χ is smaller when the field is along the c-axis of HCP iron. Hence, a toroidal magnetic field is shown to orient HCP Fe with c-axis along the north–south direction, and combined with the data on elastic constants this explains the seismic anisotropy.