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采用坩埚下降法生长了Nd3+掺杂浓度分别为15%、8%和2.5%原子分数的Sr3Ga2Ge4O14晶体,所得晶体最大尺寸为φ26mm×15mm.Nd3+掺杂Sr3Ga2Ge4O14晶体的特征吸收峰波长为806nm,与Nd3+离子在YAG中的特征吸收峰相比,向短波方向发生了微小的偏离.这是Sr3Ga2Ge4O14晶格中Ga3+和Ge4+的统计分布所致.Nd3+:SGG晶体的这些特性将有助于泵浦效率的提高和泵浦阈值的降低,因此Nd3+:SGG晶体有望成为一种新型的LD泵浦固体激光材料.

参考文献

[1] Koechner W.Solid-state Laser Engineering[M].Berlin:Springer-Verlag,1992
[2] KAMINSKY A A .Generation of Stimulated Nd-ion Radiation in Trigonal Acentric La3Ga5SiO14 Crystal[R].Report of the U. S. S.R. Academy of Science,1982.
[3] 武安华,徐家跃,周娟,范世(马山豆).硅酸镓镧结构的新型压电晶体的研究进展[J].硅酸盐学报,2003(05):480-484.
[4] 武安华,徐家跃.La3Ga5SiO14单晶的生长、性能及SAW应用[J].人工晶体学报,2002(06):559-564.
[5] Eichler H J;Ashkenasi D;Jian H .Acentric Disordered Nd3+: La3Ga5SiO14 Crystal. A Broadband Luminescence Material with High Thermal Conductivity to Generate Picosecond Laser Pulses[J].Physica Status Solidi A,1993,146:833-841.
[6] KAMINSKY A A .Nonlinearity-active Material (La1 - xNdx)3Ga5SiO14 Crystal[J].Izv of the U S S R Academy of science,1983,47(10):1903-1909.
[7] Kaminskii A A;Butashin A V;Demidovich A A .Broad-band Tunable Stimulated Emission from Octahedral Cr Ions in New Acentric Crystals with Ca-gallogermenate Structure[J].Physica Status Solidi A,1989,112:197-206.
[8] Kaminskii A A;Belokoneva E L;Mill B V .Pure and Nd-doped Ca3Ga2Ge4O14 and Sr3Ga2Ge4O14 Single Crystals, Their Structure, Optical Spectral, Luminescence, Electromechanical Properties, and Stimulated Emission[J].Physica Status Solidi A,1984,86:345-363.
[9] 周娟 .新型压电单晶Sr<,3>Ga<,2>Ge<,4>O<,14>的坩埚下降法生长与表征[D].中国科学院上海硅酸盐研究所,2003.
[10] Kochurikhin VV.;Shimamura K.;Takagi H.;Fukuda T.;Kumatoriya M. .CZOCHRALSKI GROWTH OF SR3GA2GE4O14 SINGLE CRYSTALS FOR PIEZOELECTRIC APPLICATIONS[J].Journal of Crystal Growth,1997(4):452-454.
[11] Juan Zhou;Jiayue Xu;Wangxiang Hua;Shiji Fan .Bridgman growth of new piezoelectric single crystal Sr_3Ga_2Ge_4O_(14)[J].Materials Science & Engineering, B. Solid-State Materials for Advanced Technology,2004(issue 2):213-217.
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