Studied on Characteristics of Mg (4.5 Mol%)-Doped LiNbO3 Crystal Using Li Vapor Transport Equilibration

2013 ◽  
Vol 785-786 ◽  
pp. 706-709
Author(s):  
Li Zhu Zhang ◽  
Ping Rang Hua

It is studied that influence of Li vapor transport equilibration (VTE) on surface refractive index of congruent Mg (4.5 mol%):LiNbO3crystal at wavelength of 1536 nm. The results show the ordinary index nodecreases when t < 40 h, then recoveries slightly and tends to a constant when t >100 h. The extraordinary index nehas the VTE effects as similar as no, but the alteration amplitude is smaller than no. The secondary ion mass spectrometry) study shows that the VTE induces Mg diffusion within the crystal in an inhomogeneous Mg depth profile, depending on the VTE duration. The neutron activation analysis shows that the VTE hardly induces Mg evaporation away from the crystal. First, the Mg ions of crystal internal diffused to the surface in the early stage of VTE, and then they diffused slowly back into the bulk of the crystal toward equilibrium when Li concentration tends to equilibrium.

2010 ◽  
Vol 25 (9) ◽  
pp. 1817-1821 ◽  
Author(s):  
De-Long Zhang ◽  
Hui Zheng ◽  
Ping-Rang Hua ◽  
Edwin Yue-Bun Pun

A number of congruent LiNbO3 crystals homogeneously doped with 5 mol% Mg in growth melt were subjected to Li-rich vapor transport equilibration (VTE) treatments at 1100 °C for different durations. Secondary ion mass spectrometry study shows that the VTE induces the Mg diffusion within the crystal and an inhomogeneous Mg depth profile. The surface Mg concentration, determined from measured ordinary refractive index, shows a strong VTE duration dependence. Neutron activation analysis shows that the amount of MgO diffusing out of the crystal is ignorable, allowing to conclude that the Mg ions counter diffuse to the crystal surface at the early stage of VTE and then come back toward equilibrium as the Li concentration comes to equilibrium. The VTE-induced Li2O content increase in crystal was determined by the gravimetric method. The crystalline phase, crystal composition, and site occupation of Mg and Li are discussed.


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