TY - JOUR
T1 - Anomaly of specific heat in high quality single crystal of PrAg2In
AU - Sato, Y.
AU - Morodomi, H.
AU - Inagaki, Y.
AU - Kawae, T.
AU - Suzuki, H. S.
N1 - Publisher Copyright:
© Published under licence by IOP Publishing Ltd.
PY - 2014
Y1 - 2014
N2 - PrAg2In has a non-Kramers doublet Λ3 ground state, which is expected to show a quadrupolar phenomena. Although many studies have been devoted to investigate the novel features of PrAg2In, there is no clear result how to remove the degeneracy of quadrupolar moment because this compound has a Heusler structure, in which the substitution between Pr and In ions is inevitable. We therefore prepare a high quality single crystal of PrAg2In with the residual resistivity ratio of 14, which is much larger than that of the previous samples. We measure the magnetic susceptibility with the SQUID magnetometer down to T 0.4 K and the specific heat in the magnetic fields up to H 8T along [100] crystal direction down to T =0.1 K. The susceptibility is consistent with the CEF calculation. The specific heat shows a sharp peak at around Tp 0.33 K. When the magnetic field is applied, the peak at TP does not move up to H 2.5 T. In contrast, it shifts to higher temperatures with broadening above H 2.5 T. The broad peak above H 2.5 T is well reproduced by the Schottky specific heat due to the splitting of the Λ3 doublet in the magnetic fields. From these results, we conclude that a phase transition related to the r3 doublet occurs at around TP.
AB - PrAg2In has a non-Kramers doublet Λ3 ground state, which is expected to show a quadrupolar phenomena. Although many studies have been devoted to investigate the novel features of PrAg2In, there is no clear result how to remove the degeneracy of quadrupolar moment because this compound has a Heusler structure, in which the substitution between Pr and In ions is inevitable. We therefore prepare a high quality single crystal of PrAg2In with the residual resistivity ratio of 14, which is much larger than that of the previous samples. We measure the magnetic susceptibility with the SQUID magnetometer down to T 0.4 K and the specific heat in the magnetic fields up to H 8T along [100] crystal direction down to T =0.1 K. The susceptibility is consistent with the CEF calculation. The specific heat shows a sharp peak at around Tp 0.33 K. When the magnetic field is applied, the peak at TP does not move up to H 2.5 T. In contrast, it shifts to higher temperatures with broadening above H 2.5 T. The broad peak above H 2.5 T is well reproduced by the Schottky specific heat due to the splitting of the Λ3 doublet in the magnetic fields. From these results, we conclude that a phase transition related to the r3 doublet occurs at around TP.
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U2 - 10.1088/1742-6596/568/4/042027
DO - 10.1088/1742-6596/568/4/042027
M3 - Conference article
AN - SCOPUS:84919683695
SN - 1742-6588
VL - 568
JO - Journal of Physics: Conference Series
JF - Journal of Physics: Conference Series
M1 - 042027
T2 - 27th International Conference on Low Temperature Physics, LT 2014
Y2 - 6 August 2014 through 13 August 2014
ER -