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Structural transitions in nanosized Zn0.97Al0.03O powders under high pressure analyzed by in situ angle-dispersive X-ray diffraction
Journal article   Open access

Structural transitions in nanosized Zn0.97Al0.03O powders under high pressure analyzed by in situ angle-dispersive X-ray diffraction

Chih-Ming Lin, Hsin-Tzu Liu, Shi-Yao Zhong, Chia-Hung Hsu, Yi-Te Chiu, Ming-Fong Tai, Jenh-Yih Juang, Yu-Chun Chuang and Yen-Fa Liao
Materials, Vol.9(7), 561
2016

Abstract

Aluminum-doped zinc oxide Angle-dispersive X-ray diffraction Phase transition Zinc-blende Materials Science (all)
Nanosized aluminum-doped zinc oxide Zn 1-x Al x O (AZO) powders (AZO-NPs) with x = 0.01, 0.03, 0.06, 0.09 and 0.11 were synthesized by chemical precipitation method. The thermogravimetric analysis (TGA) indicated that the precursors were converted to oxides from hydroxides near 250 °C, which were then heated to 500 °C for subsequent thermal processes to obtain preliminary powders. The obtained preliminary powders were then calcined at 500 °C for three hours. The structure and morphology of the products were measured and characterized by angle-dispersive X-ray diffraction (ADXRD) and scanning electron microscopy (SEM). ADXRD results showed that AZO-NPs with Al content less than 11% exhibited würtzite zinc oxide structure and there was no other impurity phase in the AZO-NPs, suggesting substitutional doping of Al on Zn sites. The Zn 0.97 Al 0.03 O powders (A 3 ZO-NPs) with grain size of about 21.4 nm were used for high-pressure measurements. The in situ ADXRD measurements revealed that, for loading run, the pressure-induced würtzite (B4)-to-rocksalt (B1) structural phase transition began at 9.0(1) GPa. Compared to the predicted phase-transition pressure of ~12.7 GPa for pristine ZnO nanocrystals of similar grain size (~21.4 nm), the transition pressure for the present A 3 ZO-NPs exhibited a reduction of ~3.7 GPa. The significant reduction in phase-transition pressure is attributed to the effects of highly selective site occupation, namely Zn 2+ and Al 3+ , were mainly found in tetrahedral and octahedral sites, respectively.
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https://doi.org/10.3390/MA9070561View
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