Project/Area Number |
14350008
|
Research Category |
Grant-in-Aid for Scientific Research (B)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Applied materials science/Crystal engineering
|
Research Institution | Osaka University |
Principal Investigator |
UYEDA Chiaki Osaka University, Graduate School of Science, Associated Professor, 大学院・理学研究科, 助教授 (50176591)
|
Project Period (FY) |
2002 – 2005
|
Project Status |
Completed (Fiscal Year 2005)
|
Budget Amount *help |
¥4,300,000 (Direct Cost: ¥4,300,000)
Fiscal Year 2005: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 2004: ¥1,100,000 (Direct Cost: ¥1,100,000)
Fiscal Year 2003: ¥1,100,000 (Direct Cost: ¥1,100,000)
Fiscal Year 2002: ¥1,500,000 (Direct Cost: ¥1,500,000)
|
Keywords | diamagnetic anisotropy / chemical bond / magnetic orientation / magnetic alignment / microgravity / horseshoe magnet / paramagnetic anisotropy / 磁気異方性 / 磁気回転 / 磁気振動 / 水素結合 / 磁気異方性測定 / 低温 / 弱磁場 / 生セッコウ / KDP / 磁場整列能率 / 無機酸化物 |
Research Abstract |
Magnetic alignment, commonly used in various devices, is believed to occur only on materials which possess spontaneous magnetic moment. We have recently found that many of the ordinary "nonmagnetic" crystals show rotational oscillation with respect to magnetic field [page 22,49,53]. Oscillations have been observed for popular materials such as calcite, gypsum, graphite, quartz, forsterite, mica, Rochelle salt or urea (see picture below) ; the motion is similar to that of a compass caused by terrestrial field. The oscillations derived from anisotropy of diamagnetic susceptibility (Δχ)_<DIA>. The magnitude of (Δχ)_<DIA> directly indicates the efficiency of magnetic alignment of a given material, however its existence is not recognized for most of the materials at present.
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