Cafetite, Ca[Ti2O5](H2O):: Crystal structure and revision of chemical formula

被引:0
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作者
Krivovichev, SV
Yakovenchuk, VN
Burns, PC
Pakhomovsky, YA
Menshikov, YP
机构
[1] St Petersburg State Univ, Dept Crystallog, St Petersburg 199034, Russia
[2] Russian Acad Sci, Kola Sci Ctr, Inst Geol, Apatity 184200, Russia
[3] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA
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中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The crystal structure of cafetite, ideally Ca[Ti2O5](H2O). (monoclinic, P2(1)/n, a = 4.9436(15), b = 12.109(4), c = 15.911(5) Angstrom, beta = 98.937(5)degrees V = 940.9(5) Angstrom(3), Z = 8) has been solved by direct methods and refined to R-1 = 0.057 using X-ray diffraction data collected from a crystal pseudo-merohedrally twinned on (001). There are four symmetrically independent Ti cations; each is octahedrally coordinated by six O atoms. The coordination polyhedra around the Ti cations are strongly distorted with individual Ti-O bond lengths ranging from 1.743 to 2.223 Angstrom (the average <Ti-O> bond length is 1.98 Angstrom). Two symmetrically independent Ca cations are coordinated by six and eight anions for Ca1 and Ca2, respectively. The structure is based on [Ti2O5] sheets of TiO6 octahedra parallel to (001). The Ca atoms and H2O groups are located between the sheets and link them into a three-dimensional structure. The structural formula of cafetite confirmed by electron microprobe analysis is Ca[Ti2O5](H2O), in contrast to the formula (Ca,Mg)(Fe,Al)(2)Ti4O12 4H(2)O suggested by Kukharenko et al. (1959). The wrong chemical formula suggested for cafetite by Kukharenko et al. (1959) is probably due to admixtures of magnetite or titanomagnetite in their samples. Cafetite is chemically related to kassite, CaTi2O4(OH)(2), but differs from it in structure and structural formula.
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页码:424 / 429
页数:6
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