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1. 南京工业大学 材料学院,江苏 南京,210009
2. 南京工业大学 电光源材料研究所,江苏 南京,210015
收稿日期:2009-11-02,
修回日期:2010-01-31,
网络出版日期:2010-08-27,
纸质出版日期:2010-08-27
移动端阅览
印 琰, 张晓明, 刘光熙, 王海波. LiAl<sub>5</sub>O<sub>8</sub> ∶ Fe<sup>3+</sup>发光粉的发光性能[J]. 发光学报, 2010,31(4): 473-476
YIN Yan, ZHANG Xiao-ming, LIU Guang-xi, WANG Hai-bo. Luminescence Properties of LiAl<sub>5</sub>O<sub>8</sub> ∶ Fe<sup>3+</sup> Phosphor[J]. 发光学报, 2010,31(4): 473-476
Fe
3+
激活的铝酸锂是深红色发射的红色荧光粉
其发射的峰值波长为675 nm
呈现出少有的纯正的深红色发光。本文对LiAl
5
O
8
∶ Fe
3+
荧光粉的基质组成和激活剂浓度进行了研究。结果表明 ∶ Fe
3+
掺杂LiAl
5
O
8
的激发光谱
在
em
=673 nm的波长监测下
有序相的激发光谱在284 nm处有强吸收带
为Fe
3+
-O
2-
电荷迁移带;激发波长
ex
=254 nm的有序相样品的发射波长峰值为673 nm
并伴随一个在长波方向轻微不对称得
发射是属于
4
T
1
(
4
G)-
6
A
1
(
6
S)的跃迁。当原料Li
2
CO
3
与Al
2
O
3
的量的比为0.21时
样品的发光强度最好;样品的发光强度随激活剂Fe
3+
的浓度的增加而提高
当浓度达到0.5%时
发光强度达到最大值
超过0.5%时呈现出浓度猝灭效应。
Iron-activated LiAl
5
O
8
is one of red emitting phosphors
exhibiting a broad-band photoluminescence peaked around 675 nm. The component of the matrix and the content of activation ion in LiAl
5
O
8
∶ Fe
3+
phosphors were studied in this paper. The results shown that
under the monitoring at 673 nm
the ordered phase of excitation spectra indicated that there is a strong absorption band at 284 nm
which is charge transfer band of Fe
3+
-O
2-
.And there is a single emission band at 673 nm emission under 254 nm excitation. And the emission band is slight asymmetry in the direction of longer wavelength
which belongs to
4
T
1
(
4
G)
6
A
1
(
6
S) transition.The luminescent intensity is the strongest when the content ratio of Li
2
CO
3
and Al
2
O
3
is 0.21. The emission intensity enhances as the content of Fe
3+
increases. When the content of Fe
3+
is 0.5%
the luminescent intensity is the strongest. But the luminescent intensity decreases when the content of Fe
3+
increases over 0.5%.
Palumbo D T. Electronic states of Fe3+ in LiAlO2 and LiAl5O8 phosphors
. J. Lumin., 1971, 4 (2):89-97.
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. J. Alloys and Compounds, 2006, 416 (1-2):250-255.
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Chen Yonghu, Liu Bo, Shi Chaowei, et al. VUV spectroscopy of GdPO4 ∶ Eu3+ and GdBO3 ∶ Eu3+
. J. Chin. Rare Earth Society (中国稀土学报), 2005, 23 (4):429-433 (in Chinese).
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