首页> 外文期刊>Journal of Geosciences >New crystallographic data?and formula?revision of phuralumite,?Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9
【24h】

New crystallographic data?and formula?revision of phuralumite,?Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9

机译:蒙脱石?Al2 [(UO2)3(PO4)2O(OH)](OH)3(H2O)9的新晶体学数据和分子式修订

获取原文
           

摘要

The crystal structure of phuralumite, Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9, from the Kobokobo pegmatite (Kivu, Democratic Republic of Congo), was refined from single crystal X-ray diffraction data. Four samples have been investigated in this study, and the crystal structure was to R1 = 0.0566, 0.0544, 0.0661 and 0.0353, for 5739, 5953, 6007 and 5793 unique observed reflections, for the samples VC2048, VC2048, VC2054 and VC2055, respectively. Phuralumite is monoclinic, space group P21, a = 9.4407(3), b = 20.8596(8), c = 13.4326(4) ?, ? = 107.905(4)°, V = 2517.40(17) ?3, and Z = 4 (sample VC2048). The structure consists of [(UO2)3(PO4)2O(OH)]3- layers, parallel to (010), which are connected by Al3+ ions and H2O molecules. The uranyl phosphate sheets show the phosphuranylite anion topology, while the Al3+ ions occur in 5- and 6-fold coordination and are connected together to form Al4O4(OH)6(H2O)4 clusters. The crystallographic data?obtained from the four structural models converge and confirm the previously determined structure for phuralumite. However, these new data?also show some discrepancies in the bond-valence analysis, especially in the assignment of the OH- groups and water molecules. As a?consequence of this study, the structural formula?of phuralumite, previously reported as Al2[(UO2)3(PO4)2(OH)2](OH)4(H2O)10, must be modified to?Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9.
机译:从单晶X射线精制了来自Kobokobo伟晶岩(刚果民主共和国基伍)的亚硫酸铝蒙脱石Al2 [(UO2)3(PO4)2O(OH)](OH)3(H2O)9的晶体结构。衍射数据。在此研究中研究了四个样品,对于VC2048,VC2048,VC2054和VC2055样品,分别观察到5739、5953、6007和5793的唯一反射,晶体结构分别为R1 = 0.0566、0.0544、0.0661和0.0353。铝矾土为单斜晶,空间群P21 / n,a = 9.4407(3),b = 20.8596(8),c = 13.4326(4)?,? = 107.905(4)°,V = 2517.40(17)θ3,Z = 4(样本VC2048)。该结构由平行于(010)的[(UO2)3(PO4)2O(OH)] 3-层组成,这些层通过Al3 +离子和H2O分子连接。磷酸双氧铀片显示出磷铀矿阴离子拓扑结构,而Al3 +离子以5倍和6倍配位形式出现并连接在一起形成Al4O4(OH)6(H2O)4簇。从四个结构模型获得的晶体学数据收敛并证实了先前确定的亚硫酸铝镁铁矿的结构。但是,这些新数据也显示了键价分析中的某些差异,尤其是在OH-基团和水分子的分配方面。这项研究的结果是,以前报道为Al2 [(UO2)3(PO4)2(OH)2](OH)4(H2O)10的亚硫酸铝镁石的结构式必须修改为ΔAl2[( UO2)3(PO4)2O(OH)](OH)3(H2O)9。

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