Back to Search
Start Over
Adolfpateraite, K(UO2)(SO4)(OH)(H2O), a new uranyl sulphate mineral from Jáchymov, Czech Republic.
- Source :
- American Mineralogist; Feb/Mar2012, Vol. 97 Issue 2/3, p447-454, 8p
- Publication Year :
- 2012
-
Abstract
- Adolfpateraite, monoclinic K(UO<subscript>2</subscript>)(SO<subscript>4</subscript>)(OH)(H<subscript>2</subscript>O), is a new supergene mineral from the Svornost mine, Jáchymov ore district, Czech Republic. It forms sulfur yellow to greenish yellow crystalline aggregates, up to 2 mm in diameter. Crystals are transparent to translucent with a vitreous luster, without observable cleavage. The streak is pale yellow. The Mohs hardness is ~2. The mineral shows a green fluorescence in long-wave ultraviolet radiation. Adolfpateraite is pleochroic, with a = colorless and γ = yellow (β could not been examined). It is biaxial, with α = 1.597(2), γ = 1.659(2) (β could not been measured), birefringence 0.062. The empirical chemical formula (mean of 4 electron microprobe point analyses) was calculated based on 8 O apfu and is K<subscript>0.94</subscript>(UO<subscript>2</subscript>)<subscript>1.00</subscript> (SO<subscript>4</subscript>)<subscript>1.02</subscript>(OH)<subscript>0.90</subscript> (H<subscript>2</subscript>O)<subscript>1.00</subscript> (water content calculated). The simplified formula is K(UO<subscript>2</subscript>)(SO<subscript>4</subscript>)(OH)(H<subscript>2</subscript>O), requiring K<subscript>2</subscript>O 10.70, UO<subscript>3</subscript> 64.97, SO<subscript>3</subscript> 18.19, H<subscript>2</subscript>O 6.14, total 100.00 wt%. Adolfpateraite is monoclinic, space group P2<subscript>1</subscript>/c, a = 8.0462(1), b = 7.9256(1), c = 11.3206(2) Å, β = 107.726(2)°, V = 687.65(2) ų, Z = 4, and D<subscript>calc</subscript> = 4.24 g/cm³. The five strongest reflections in the X-ray powder diffraction pattern are [d<subscript>obs</subscript> in Å (I) (hkl)]: 7.658 (76) (100), 5.386 (1̅00) (002), 5.218 (85) (102), 3.718 (46) (021), 3.700 (37) (2̅02). The crystal structure has been refined from single-crystal X-ray diffraction data to R<subscript>1</subscript> = 0.0166 with GOF = 1.30, based on 1915 observed reflections [I<subscript>obs</subscript> > 3σ(I)]. The crystal structure consists of chains of uranyl polyhedra extended along [010], with OH- located on the shared vertex between the bipyramids. The sulfate tetrahedra decorate the outer side of the chain with bridging bidentate linkages between the uranyl pentagonal bipyramids. H<subscript>2</subscript>O groups are located on the edges of the chains on the non-linking vertex of each uranyl pentagonal bipyramid. K+ atoms are located between the chains providing additional linkage of these together with H-bonds. The fundamental vibrational modes of uranyl ion, sulfate tetrahedra, and H<subscript>2</subscript>O groups were tentatively assigned in the infrared and Raman spectra. The new mineral is named to honor Adolf Patera (1819-1894), Czech chemist, mineralogist, and metallurgist. [ABSTRACT FROM AUTHOR]
- Subjects :
- CRYSTALS
MINERALS
URANYL compounds
CRYSTAL structure research
Subjects
Details
- Language :
- English
- ISSN :
- 0003004X
- Volume :
- 97
- Issue :
- 2/3
- Database :
- Complementary Index
- Journal :
- American Mineralogist
- Publication Type :
- Academic Journal
- Accession number :
- 72887514
- Full Text :
- https://doi.org/10.2138/am.2012.3976