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- Yoshida Shun-ichi
- Division of Physics, Graduate School of Science, Hokkaido University
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- Nemoto Koji
- Division of Physics, Graduate School of Science, Hokkaido University
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- Wada Koh
- Division of Physics, Graduate School of Science, Hokkaido University
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説明
We found that the true ground state of a dipolar spin ice system under a [110] magnetic field is a “Q=X” structure, which is consistent with both experiments and Monte Carlo simulations. We performed a Monte Carlo simulation to confirm the existence of a first-order phase transition under a [110] magnetic field. The result indicates the existence of the first-order phase transition to the “Q=X” phase in a magnetic field above 0.35 T for Dy2Ti2O7. In this letter we show a magnetic field-temperature phase diagram to summarize the ordered states of this system.
収録刊行物
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- Journal of the Physical Society of Japan
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Journal of the Physical Society of Japan 73 (7), 1619-1622, 2004
一般社団法人 日本物理学会
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詳細情報 詳細情報について
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- CRID
- 1390282679163599232
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- NII論文ID
- 110001954862
- 210000104873
- 130004538813
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- NII書誌ID
- AA00704814
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- BIBCODE
- 2004JPSJ...73.1619Y
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- ISSN
- 13474073
- 00319015
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- NDL書誌ID
- 7003783
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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- CiNii Articles
- KAKEN
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