Effect of hydrostatic pressure on magnetostriction and magnetocrystalline anisotropy of magnetite

Details Effect of hydrostatic pressure on magnetostriction and magnetocrystalline anisotropy of magnetite Effect of hydrostatic pressure on magnetostriction and magnetocrystalline anisotropy of magnetite

Oct 1967

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1967pepi....1...44n&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 1, Issue 1, p. 44-48.

Physics

3

Scientific paper

The saturation magnetostriction coefficients, λ100 and λ111, and the magnetocrystalline anisotropy constants, K1 and K2, of single crystals of magnetite are measured under the effect of hydrostatic pressure P of 0-2 kbar in range at the room temperature. Both | λ100 | and λ111 increase with increasing hydrostatic pressure with rate of about 15%/kbar, whereas both | K1 | and | K2 | decrease with increase of hydrostatic pressure with rate of about -5%/kbar.

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