Luminescence Properties of Delafossite-Type CuYO2 Doped with Calcium, Oxygen or Rare Earth Tb
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概要
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Delafossite-type CuYO2 and CuY1-xCaxO2 ($x\leq 0.05$) samples exhibited a green-PL-emission band due to the Cu+ interconfiguration transition from 3d94s1 to 3d10 at room temperature. With increasing Ca concentration, the Cu+ emission shifted slightly to the shorter-wavelength side with a slightly weaker emission intensity. This slight change in Cu+ emission property is considered to be caused by the increase in hole concentration within the Cu+ layer arising from the increase in Ca concentration. On the other hand, oxygen-annealed CuYO2 samples exhibited no emissions. The increase in nonradiative relaxation processes in the oxygen-annealed CuYO2 samples is possibly related to structural changes such as orthorhombic distortion during the oxygen annealing. In the photoluminescence of delafossite-type CuY1-yTbyO2 ($y=0.05$) at room temperature, no Cu+ emission band was observed, but sharp emission lines were observed. All the emission lines were assigned to the f-f transitions of Tb3+ (5D4$\rightarrow$7FJ, $J=3--6$).
- 2005-01-15
著者
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Tsuboi Nozomu
Faculty Of Engineering Niigata University
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Kaneko Futao
Faculty Of Engineering Niigata University
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OHARA Hiroshi
Graduated School of Science and Technology, Niigata University
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KATO Keizo
Faculty of Engineering, Niigata University
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Kobayashi Satoshi
Faculty Of Engineering Niigata University
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Hoshino Takanobu
Graduated School Of Science And Technology Niigata University
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Kaneko Futao
Faculty of Engineering, Niigata University, 2-8050 Ikarashi, Niigata 950-2181, Japan
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Kato Keizo
Faculty of Engineering, Niigata University, 2-8050 Ikarashi, Niigata 950-2181, Japan
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Tsuboi Nozomu
Faculty of Engineering, Niigata University, 2-8050 Ikarashi, Niigata 950-2181, Japan
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Hoshino Takanobu
Graduated School of Science and Technology, Niigata University, 2-8050 Ikarashi, Niigata 950-2181, Japan
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Kobayashi Satoshi
Faculty of Engineering, Niigata University, 2-8050 Ikarashi, Niigata 950-2181, Japan
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