| Abstract | Petewilliamsite, ideally (Ni,Co)30(As2O7)15, monoclinic, space group C2, a = 33.256(5), b = 8.482(1), c = 14.191(2) à, à = 104.145(3)°, V = 3881.6(11) à3, a:b:c = 3.9209:1:1.6731, Z = 2, is a new
mineral found on a single nickeline-veined quartz specimen from Johanngeorgenstadt, Saxony, Germany. The mineral possesses a pronounced subcell-supercell: a (subcell) = 1/5 a (supercell); b (subcell) = b (supercell); c (subcell) = 1/3 c (supercell),
and the strongest six lines of the X-ray powder-diffraction pattern are [d in à (I) (hkl)]: 4.235(30)(020) ; 3.118(100)(513, 023); 3.005(60)"http://www.w3.org/1999/xlink" mime-subtype="gif" xlink:type="simple" xlink:href="S0026461X00032369 inline1" ;
2.567(50)"http://www.w3.org/1999/xlink" mime-subtype="gif" xlink:type="simple" xlink:href="S0026461X00032369 inline2" ; 1.637(50)(536 ); 1.507(30b)(553, "http://www.w3.org/1999/xlink" mime-subtype="gif" xlink:type="simple"
xlink:href="S0026461X00032369 inline3" ). It occurs predominantly as scattered patches of mm-sized aggregates which are intimately associated with varicoloured xanthiosite; additional associations include bunsenite, aerugite, rooseveltite, native
bismuth, paganoite and two undefined arsenates. Subhedral equant crystals with rounded faces are intimately intergrown in 1 mm-sized aggregates and individual grains do not exceed 0.5 mm in maximum diameter. The average crystal size is variable from
20 μm to 0.3 mm. The colour varies from dark violet-red to dark brownish-red and the streak is pale reddish-brown to pale purplish-brown. Crystals are translucent, brittle, vitreous, and do not fluoresce under ultraviolet light. The mineral shows
neither twinning nor cleavage, has an uneven fracture, and the calculated density (for the empirical formula) is 4.904 g/cm3. Electron-microprobe analyses gave NiO 19.45, CoO 18.39, CuO 3.40, CaO 0.17, FeO 0.04, As2O5 60.32, total 101.77 wt.%. The
empirical formula, derived from crystal-structure analysis and electron-microprobe analyses, is (Ni14.662+Co13.822+Cu2.412+Ca0.17Fe0.032+)Σ31.09(As1.975+O7)15, based on O = 105 atoms per formula unit (a.p.f.u.). In reflected plane-polarized light in
air, petewilliamsite is dark grey with orange to spectral (multicoloured) internal reflections and no obvious bireflectance, anisotropy or pleochroism. Measured reflectance values in air are tabulated; the index of refraction calculated at 589 nm is
1.88. The mineral name honours Professor Peter (-Pete-) Allan Williams of the University of Western Sydney, New South Wales, Australia, for his contributions to the study of secondary minerals.The crystal structure of petewilliamsite has been solved
by direct methods and refined on the basis of F2 using 9212 unique reflections measured with Mo-Kα X-radiation on a diffractometer equipped with a CCDbased detector. The final R1 was 7.68%, calculated for 1273 observed reflections. The structure
contains 15 symmetrically distinct As5+ cations, each of which is tetrahedrally coordinated by four O atoms, and pairs of these AsO4 tetrahedra share a vertex which results in As2O7 pyroarsenate groups that are in layers parallel to (010). The
structure also has 16 distinct transition-metal M (M: Ni,Co) sites of which there are one tetrahedral, four square bipyramidal, and 11 octahedral arrangements. Adjacent pyroarsenate groups are linked through bonds to M cations. The structure of
petewilliamsite is not closely related to other naturally occurring arsenates and it is the first pyroarsenate mineral. |