CRYSTAL-STRUCTURE OF PB-6[GE6O18]CENTER-DOT-2H(2)O, A LEAD CYCLO-GERMANATE SIMILAR TO THE MINERAL DIOPTASE

Authors
Citation
Hh. Otto et Hj. Brandt, CRYSTAL-STRUCTURE OF PB-6[GE6O18]CENTER-DOT-2H(2)O, A LEAD CYCLO-GERMANATE SIMILAR TO THE MINERAL DIOPTASE, European journal of mineralogy, 8(2), 1996, pp. 301-310
Citations number
29
Categorie Soggetti
Mineralogy
ISSN journal
09351221
Volume
8
Issue
2
Year of publication
1996
Pages
301 - 310
Database
ISI
SICI code
0935-1221(1996)8:2<301:COPALC>2.0.ZU;2-#
Abstract
Pb-6[Ge6O18]. 2H(2)O crystallizes as transparent and colourless trigon al needles, having space group <R(3)over bar>, lattice parameters a = 15.6476(7) and c = 7.3119(4)Angstrom, with Z = 3 formula units per uni t cell. The density of 6.44 gcm(-3) is comparatively low. Powder X-ray diffraction data lead to a crystal structure yielding a final residua l of R(F) = 0.033 (wR2 = 0.070, R(p) = 0.106, R(wp) = 0.133) after lea st squares refinement. The structure consists of sandwiched hetero-pol yhedral rings with straight channels down [001]. Isolated and partly e xpanded rings of six corner-sharing GeO4 tetrahedra are bonded togethe r vertically by crown-shaped Sechser rings of flat PbO5+1 pyramids wit h shared corners, which themselves share edges laterally. Lone electro n pairs of lead, which complete the pyramids in a psi-octahedral arran gement, point towards the channel centres. The channels have a free di ameter of about 2.5 Angstrom and confine well-ordered pairs of water m olecules which can be degassed by heating. A crystal-chemical and morp hological comparison is drawn with the mineral dioptase, Cu-6[Si6O18]. 6H(2)O. Lead cyclo-germanate is the first compound observed with pure [Ge6O18](12-) single rings.