Specific heat of Dy2Ti2O7 in magnetic fields: comparison between single-crystalline and polycrystalline data

Authors report the specific heat of single crystals of the spin ice compound Dy2Ti2O7 under magnetic fields down to 1.8 K. Polycrystalline results down to 0.4 K are consistent with the previous report by Ramirez et al. For the magnetic field along the [100] direction, Cspin/T is interpreted as one S...

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Published inThe Journal of physics and chemistry of solids Vol. 63; no. 6-8; pp. 1043 - 1046
Main Authors HIGASHINAKA, R, FUKAZAWA, H, YANAGISHIMA, D, MAENO, Y
Format Conference Proceeding Journal Article
LanguageEnglish
Published Oxford Elsevier 2002
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Summary:Authors report the specific heat of single crystals of the spin ice compound Dy2Ti2O7 under magnetic fields down to 1.8 K. Polycrystalline results down to 0.4 K are consistent with the previous report by Ramirez et al. For the magnetic field along the [100] direction, Cspin/T is interpreted as one Schottky peak characterized by the Zeemann splitting of the Ising levels of all four equivalent spins for each tetrahedron. However, for the magnetic field along the [111] direction, Cspin/T is interpreted as two-component Schottky peak reflecting the fact that there are two kinds of spin components. Along the [110] direction, it is also interpreted as two-component Schottky peak because of experimental misalignment. Authors found that the features of the polycrystalline data in magnetic fields cannot be reconstructed by simply taking appropriate averages of the present anisotropic single-crystalline data. 6 refs.
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ISSN:0022-3697
1879-2553
DOI:10.1016/S0022-3697(02)00065-3