Ghazisaeed Seyedayat, Kiefer Boris, Plášil Jakub
Department of Physics, New Mexico State University Las Cruces NM 88003 USA.
Institute of Physcis, Academy of Sciences of the Czech Republic v.v.i, Na Slovance 2 Prague 18221 Czech Republic
RSC Adv. 2019 Mar 29;9(18):10058-10063. doi: 10.1039/c8ra09557d. eCollection 2019 Mar 28.
The crystal structure of lead uranyl-oxide hydroxy-hydrate mineral curite, ideally Pb(HO)[(UO)O(OH)], was studied by means of single-crystal X-ray diffraction and theoretical calculations in order to localize positions of hydrogen atoms in the structure. This study has demonstrated that hydrogen atoms can be localized successfully also in materials for which the conventional approach of structure analysis failed, here due to very high absorption of X-rays by the mineral matrix. The theoretical calculations, based on the Torque method, provide a robust, fast real-space method for determining HO orientations from their rotational equilibrium condition. In line with previous results we found that curite is orthorhombic, with space group , unit-cell parameters = 12.5510(10), = 8.3760(4), = 13.0107(9) Å, = 1367.78(16) Å, and two formula units per unit cell. The structure ( = 3.58% for 1374 reflections with > 3) contains uranyl-hydroxo-oxide sheets of the unique topology among uranyl oxide minerals and compounds and an interlayer space with Pb cations and a single HO molecule, which is coordinated to the Pb-site. Current results show that curite is slightly non-stoichiometric in Pb content (∼3.02 Pb per unit cell, = 2); the charge-balance mechanism is (OH) ↔ O substitution within the sheets of uranyl polyhedra. Disproving earlier predictions, the current study shows that curite contains only one HO group, with [4]-coordinated oxygen. The hydrogen bonding network maintains the bonding between the sheets in addition to Pb-O bonds; among them, a H-bond is crucial between the OH group on an apical O atom of an adjacent sheet that stabilizes the entire structure. The results show that the combination of experimental X-ray data and the Torque method can successfully reveal hydrogen bonding especially for complex crystal structures and materials where X-rays fail to provide unambiguous hydrogen positions.
通过单晶X射线衍射和理论计算研究了铀酰氧化铅氢氧化物水合物矿物板铅铀矿(理想化学式为Pb(HO)[(UO)O(OH)])的晶体结构,以确定结构中氢原子的位置。该研究表明,对于传统结构分析方法失效的材料,由于矿物基质对X射线的高吸收,氢原子也能成功定位。基于扭矩法的理论计算提供了一种强大、快速的实空间方法,可根据HO的旋转平衡条件确定其取向。与之前的结果一致,我们发现板铅铀矿为正交晶系,空间群为 ,晶胞参数 = 12.5510(10)、 = 8.3760(4)、 = 13.0107(9) Å、 = 1367.78(16) Å,每个晶胞有两个化学式单元。该结构(对于1374个I > 3的反射,R = 3.58%)包含铀酰氧化物矿物和化合物中独特拓扑结构的铀酰羟基氧化物层,以及一个含有Pb阳离子和单个HO分子的层间空间,该HO分子与Pb位点配位。目前的结果表明,板铅铀矿在Pb含量上略有非化学计量比(每个晶胞约3.02个Pb,Z = 2);电荷平衡机制是在铀酰多面体层内(OH) ↔ O取代。与早期预测相反,目前的研究表明板铅铀矿仅包含一个具有[4]配位氧的HO基团。氢键网络除了Pb - O键外,还维持了层间的键合;其中,相邻层顶端O原子上的OH基团之间的氢键对于稳定整个结构至关重要。结果表明,实验X射线数据和扭矩法的结合能够成功揭示氢键,特别是对于X射线无法提供明确氢位置的复杂晶体结构和材料。