The crystal structure of niobium-rich calciotantite, Ca (Ta2.82Nb1.18) Oil,
hexagonal, a 6.2261(6), c 12.280(1) Angstrom, V412.18(8) Angstrom(3), spac
e group P6(3)22, Z = 1, D-calc. = 6.735 g/cm(3), has been refined to an R i
ndex of 1.8% based on 414 observed (4 sigma) reflections measured with MoK
alpha X-radiation. There is one unique Ca site occupied by Ca and coordinat
ed by eight O-atoms with a <Ca-O> distance of 2.512 Angstrom. There are two
unique Ta sites both occupied by Ta and Nb; the Ta(1) site is coordinated
by seven O atoms in a distorted pentagonal dipyramidal arrangement, and the
Ta(2) site is coordinated by six O atoms in a distorted octahedral arrange
ment. The Ta(2)O-6 and CaO8 polyhedra occupy alternate vertices of a 6(3) n
et to form an open network of edge-sharing polyhedra of the form [CaTaO8].
The Ta(1)O-7 polyhedra share four of their pentagonal edges to form a [Ta3O
11] sheet with triangular holes at the vertices of a 6(3) net. These sheets
alternate along [001] to form a dense framework structure. The structure o
f calciotantite is topologically similar to that of natrotantite, Na2Ta4O11
; the [Ta3O11] sheets are topologically identical in both structures, and t
he [CaTaO8] and [Na2TaO8] sheets are the same if they are written as [squar
e CaTaO8] and [Na2TaO8]. The [Ta3O11] sheet is also topologically identical
to the [(UO2)(3 phi 5)] (phi = O,OH) in billietite, protasite, becquerelit
e and alpha-U3O8. Niobium is slightly preferentially ordered (relative to T
a) at the Ta(1) site, indicating a slight difference in the crystal-chemica
l behavior of Ta and Nb.