The Study of Crystal Structure on Grossular-Andradite Solid Solution

被引:8
|
作者
Wang, Yichuan [1 ,2 ]
Sun, Qiang [1 ,2 ]
Duan, Dengfei [3 ]
Bao, Xinjian [1 ,2 ,4 ]
Liu, Xi [1 ,2 ]
机构
[1] Peking Univ, Key Lab Orogen Belts & Crustal Evolut, MOE, Beijing 100871, Peoples R China
[2] Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[3] Yangtze Univ, Coll Resources & Environm, Wuhan 430074, Hubei, Peoples R China
[4] China Automot Battery Res Inst Co Ltd, Beijing 100088, Peoples R China
基金
中国国家自然科学基金;
关键词
grossular-andradite; X-ray diffraction; bond length; excess volume; distortion; THERMODYNAMIC-MIXING PROPERTIES; HIGH-PRESSURE; POWDER DIFFRACTION; ALMANDINE-PYROPE; GARNET; CHEMISTRY; VOLUME; TRANSFORMATION; SPECTROSCOPY; STABILITY;
D O I
10.3390/min9110691
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The effects of Al3+-Fe3+ substitution on 10 synthesized garnet samples along the grossular-andradite binary solid solution were investigated using both powder and single-crystal X-ray diffraction. Results showed that cell volume increased with andradite content. Small negative excess volume was observed in the Al-rich samples. By measuring the bond length, polyhedral volume, octahedral distortion parameter (sigma), and tetrahedral rotation angle (alpha), we determined that the distortion occurred on the dodecahedral site. The width of the diffraction peaks was obviously related to the composition of the solid solution. Full width at half maximum of diffraction peaks was used to calculate the microstrain, which may have a relationship with enthalpy of mixing.
引用
收藏
页数:17
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