首页> 外文期刊>Mineralogical Magazine >Vysokyite, U~(4+)[AsO_2(OH)_2]_4·4H_2O, a new mineral from Jachymov, Czech Republic
【24h】

Vysokyite, U~(4+)[AsO_2(OH)_2]_4·4H_2O, a new mineral from Jachymov, Czech Republic

机译:Vysokyite,U〜(4 +)[AsO_2(OH)_2] _4·4H_2O,来自捷克Jachymov的新矿物

获取原文
获取原文并翻译 | 示例
       

摘要

Vysokyite, U~(4+)[AsO_2(OH)_2]_4 (IMA 2012-067), was found growing on an altered surface of massive native As in the Geschieber vein, Jachymov ore district, Western Bohemia, Czech Republic. The new mineral was found in association with behounekite, stepite, kaatialaite, arsenolite, claudetite and gypsum. It forms extremely fibrous light-green crystals up to 8 mm long. Crystals have an alabaster lustre and a greenish-white to greyish streak. Vysokyite is brittle with uneven fracture and perfect cleavage along (100) and (001); the Mohs hardness is ~2. A density of 3.393 g/cm~3 was calculated using the empirical formula and unit-cell parameters obtained from a single-crystal diffraction experiment. Vysokyite is non-fluorescent under short or long wavelength UV radiation. It is colourless under the microscope, measured refractive indices are α' = 1.617(3), γ' = 1.654(3); the estimated optical orientation is α' ~ X, γ' ~ Z. The average of five spot wavelength dispersive spectroscopy (WDS) analyses is 29.44 UO_2, 1.03 SiO_2, 48.95 As_2O_5, 0.12 SO_3, 15.88 H_2O (calc.), total 95.42 wt.%. The empirical formula of vysokyite (based on 20 O a.p.f.u.) is U_(100)[AsO_2(OH)_2]_(3.90)(SiO_4)_(0.16) (SO_4)_(0.01)·4H_2O. The As—O—H and O—H vibrations dominate in the Raman spectrum. Vysokyite is triclinic, space group P1, with a = 10.749(2), b = 5.044(3), c = 19.1778(7) A, α = 89.872(15)°, β = 121.534(15)°, γ = 76.508(15)°, and V = 852.1(6) A~3, Z = 2 and D_(calc) = 3.34 g·cm~(-3). The strongest diffraction peaks in the X-ray powder diffraction pattern are [d_(obs) in A(I_(rel.))(hkl)]: 8.872(100)(100), 8.067(50)(002), 6.399(7)(103), 4.773(6)(104), 3.411(10)(302), 3.197(18)(313). The crystal structure of vysokyite was solved from single-crystal X-ray diffraction data by the charge-flipping method and refined to R_1 = 0.0595 based on 2718 unique observed reflection, and to wR_2 = 0.1160 for all 4173 unique reflections. The structure of vysokyite consists of UO_8 square antiprisms sharing all of their vertices with 8 As-tetrahedra to form infinite chains parallel to [010]. These chains are linked by hydrogen bonds involving terminal (OH) groups of the double-protonated As-tetrahedra and molecules of H_2O located between the chains. The new mineral is named in honour of Arnost Vysoky (1823—1872), the former chief of the Jachymov mines and smelters, chemist and metallurgist.
机译:在捷克共和国西波西米亚Jachymov矿区的Geschieber矿脉中,发现了Vysokyite U〜(4 +)[AsO_2(OH)_2] _4(IMA 2012-067)。发现该新矿物是与贝尼凯特石,Stepite,Kaatialaite,毒砂岩,青铜石和石膏相关的。它形成纤维状的浅绿色晶体,长达8毫米。晶体具有雪花石膏的光泽和绿白色至灰色的条纹。脉石钠钙石易碎,断裂不均匀,沿(100)和(001)的卵裂完美;莫氏硬度为〜2。使用经验公式和从单晶衍射实验获得的晶胞参数计算出密度为3.393 g / cm〜3。脉石在短波或长波紫外线辐射下均不发荧光。在显微镜下为无色,测得的折射率为α'= 1.617(3),γ'= 1.654(3);估计的光学取向为α'〜X,γ'〜Z。五点波长色散光谱(WDS)分析的平均值为29.44 UO_2、1.03 SiO_2、48.95 As_2O_5、0.12 SO_3、15.88 H_2O(计算),总计95.42 wt 。%。脉石的经验公式(基于20 O a.p.f.u.)为U_(100)[AsO_2(OH)_2] _(3.90)(SiO_4)_(0.16)(SO_4)_(0.01)·4H_2O。在拉曼光谱中,As-OH和O-H振动占主导地位。脉石为三斜晶系,空间群为P1,a = 10.749(2),b = 5.044(3),c = 19.1778(7)A,α= 89.872(15)°,β= 121.534(15)°,γ= 76.508 (15)°,V = 852.1(6)A〜3,Z = 2,D_(calc)= 3.34 g·cm〜(-3)。 X射线粉末衍射图中最强的衍射峰为[A(I_(相对))(hkl)中的d_(obs)]:8.872(100)(100),8.067(50)(002),6.399( 7)(103),4.773(6)(104),3.411(10)(302),3.197(18)(313)。通过电荷翻转法从单晶X射线衍射数据中解析出方石英的晶体结构,并基于2718次观察到的独特反射将其精炼为R_1 = 0.0595,对于所有4173次独特反射将其精炼为wR_2 = 0.1160。皂石的结构由UO_8方形反棱镜组成,它们与8个As-tetrahedra共享所有顶点,形成与[010]平行的无限链。这些链通过氢键连接,氢键涉及双质子化的As-tetrahedra的末端(OH)基和位于链之间的H_2O分子。新矿物的名称是为纪念Jachymov矿山和冶炼厂,化学家和冶金学家的前任负责人Arnost Vysoky(1823-1872)。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号