国内发现锌铝磷酸盐矿物──水羟磷铝锌石
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The Discovery of Kleemanite,a Zinc Aluminium Phosphate in China
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    摘要:

    水羟磷铝锌石是一种罕见的磷酸盐类矿物,在我国该矿物于1983年始发现于广东宝坑的锰矿区。该矿物的化学成分为ZnO 20.79,P2O5 34.76,FeO 0.67,Al2O3 24.38,H2O 19.79(%)。晶体浅黄色、透明,X射线衍射特征强线为:4.76(10),9.095(8),3.638(6),3.333(6),3.313(6),3.095(6),4.91(5),晶胞参数a0=7.274A,b0=7.185A,c0=9.788A,β=110.244°,单斜晶系,其矿物学特征与澳大利亚发现的水羟磷铝锌石基本一致。

    Abstract:

    Kleemanite, a rare phosphate mineral, was found in the Baokeng manganese oxide deposit, Guangdong, in 1983. It has the same mineralogical characteristics as kleemanite from the Iron Knob deposit in Australia. Its chemical composition is ZnO 20.79%,P2O5 34.76%,Fe0 0.67%,A1203 24.38 % (by EPMA) and H20 19.79% (by DTA and TGA),giving a chemical formula of Zn1.02 (Al1.90 Feo.04) (P04)1.95 (OH)2.01.3.14 H20. Its crystals are pale yellow in color and transparent D=2.84 H=3. Average refractive index 1.606. Stronger lines in X-ray diffraction pattern are 4.76(10),9.095 (8),3.638(6), 3.333(6),3.313(6),3.095(6),4.91(5),4.733(5),3.977(5),3.134(5),2.857(5)。 Calculated unit cell parameters: ao=7.274A,bo=7.185A,c0=9.788A,β=110.244° and Z=2, being of monoclinic system. Space group:P2, P21, P2/m or P21/m. Infrared spectra show absozption bands at 3600, 3510, 3430, 3160, 1163, 1130, 1040, 592, 530 and 490(cm-1),and differential thermal analysis demons- trated endothermal peaks at 235, 311 and 651(℃).

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赖来仁,孙燕燕,1993,国内发现锌铝磷酸盐矿物──水羟磷铝锌石[J].岩石矿物学杂志,12(3):279~283. Lai Lairen, Sun Yanyan Research Institute of Geology for Mineral Resources, CNNC, Guilin ,1993,The Discovery of Kleemanite, a Zinc Aluminium Phosphate in China[J]. Acta Petrologica et Mineralogica,12(3):279~283.

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