White T J, ZhiLi Dong
Centre for Advanced Research of Ecomaterials, Institute for Environmental Science and Engineering, Innovation Centre, Nanyang Technological University, Block 2, Unit 237, 18 Nanyang Drive, Singapore 637723.
Acta Crystallogr B. 2003 Feb;59(Pt 1):1-16. doi: 10.1107/s0108768102019894. Epub 2003 Jan 28.
The crystal structures of the [A(1)(2)]A(2)(3)(3)X apatites and the related compounds [A(1)(2)]A(2)(3)(3)X and [A(1)(2)]A(2)(3)(3)X are collated and reviewed. The structural aristotype for this family is Mn(5)Si(3) (D8(8) type, P6(3)/mcm symmetry), whose cation array approximates that of all derivatives and from which related structures arise through the systematic insertion of anions into tetrahedral, triangular or linear interstices. The construction of a hierarchy of space-groups leads to three apatite families whose high-symmetry members are P6(3)/m, Cmcm and P6(3)cm. Alternatively, systematic crystallographic changes in apatite solid-solution series may be practically described as deviations from regular anion nets, with particular focus on the O(1)-A(1)-O(2) twist angle phi projected on (001) of the A(1)O(6) metaprism. For apatites that contain the same A cation, it is shown that phi decreases linearly as a function of increasing average ionic radius of the formula unit. Large deviations from this simple relationship may indicate departures from P6(3)/m symmetry or cation ordering. The inclusion of A(1)O(6) metaprisms in structure drawings is useful for comparing apatites and condensed-apatites such as Sr(5)(BO(3))(3)Br. The most common symmetry for the 74 chemically distinct [A(1)(2)]A(2)(3)(3)X apatites that were surveyed was P6(3)/m (57%), with progressively more complex chemistries adopting P6(3) (21%), P3; (9%), P6 (4.3%), P2(1)/m (4.3%) and P2(1) (4.3%). In chemically complex apatites, charge balance is usually maintained through charge-coupled cation substitutions, or through appropriate mixing of monovalent and divalent X anions or X-site vacancies. More rarely, charge compensation is achieved through insertion/removal of oxygen to produce BO(5) square pyramidal units (as in ReO(5)) or BO(3) triangular coordination (as in AsO(3)). Polysomatism arises through the ordered filling of [001] BO(4) tetrahedral strings to generate the apatite-nasonite family of structures.
对[A₁₂]A₂₃₃X磷灰石以及相关化合物[A₁₂]A₂₃₃X和[A₁₂]A₂₃₃X的晶体结构进行了整理和综述。该族的结构原型是Mn₅Si₃(D8⁸型,P6₃/mcm对称性),其阳离子排列与所有衍生物的近似,相关结构通过将阴离子系统插入四面体、三角形或线性间隙中产生。空间群层次结构的构建导致了三个磷灰石族,其高对称成员为P6₃/m、Cmcm和P6₃cm。或者,磷灰石固溶体系列中的系统晶体学变化实际上可描述为与规则阴离子网络的偏差,特别关注投影在A₁O₆偏棱柱(001)面上的O(1)-A(1)-O(2)扭转角φ。对于含有相同A阳离子的磷灰石,结果表明φ随化学式单元平均离子半径的增加呈线性减小。与这种简单关系的较大偏差可能表明偏离P6₃/m对称性或阳离子有序排列。在结构图中包含A₁O₆偏棱柱对于比较磷灰石和诸如Sr₅(BO₃)₃Br的缩合磷灰石很有用。在所研究的74种化学组成不同的[A₁₂]A₂₃₃X磷灰石中,最常见的对称性是P6₃/m(57%),化学组成越复杂,采用P6₃(21%)、P3;(9%)、P6(4.3%)、P2₁/m(4.3%)和P2₁(4.3%)的越多。在化学组成复杂的磷灰石中,电荷平衡通常通过电荷耦合阳离子取代,或通过单价和二价X阴离子或X位空位的适当混合来维持。更罕见的是,通过插入/去除氧以产生BO₅四方锥单元(如在ReO₅中)或BO₃三角配位(如在AsO₃中)来实现电荷补偿。多体现象通过[001]方向上BO₄四面体链的有序填充产生磷灰石-钠锆石族结构而出现。