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1 South Australian Museum, North Terrace, Adelaide, South Australia 5000, Australia
2 School of Earth and Environmental Sciences, University of Adelaide, Adelaide, South Australia 5005, Australia
3 Bragg Institute, ANSTO, PMB 1, Menai, New South Wales 2234, Australia
4 Museum of Geology and Institute of Mineralogy and Geochemistry, University, UNIL-BFSH-2, CH 1015 Lausanne, Switzerland
5 Czech Geological Survey, Geologická 6, CZ–15200 Prague, Czech Republic
6 National Museum, Václavské nám. 68, CZ–11579 Prague 1, Czech Republic
Correspondence: * E-mail: joel.brugger{at}adelaide.edu.au
Pseudojohannite is a hydrated copper(II) uranyl sulfate described from Jáchymov, Northern Bohemia, Czech Republic (type locality). Pseudojohannite also occurs at the Musonoï quarry near Kolwezi, Shaba, Congo, and the La Creusaz prospect, Western Swiss Alps. At all three localities, pseudojohannite formed through the interaction of acid sulfate mine drainage waters with uraninite (Jáchymov and La Creusaz) or uranyl silicates (Musonoï). Pseudojohannite forms moss green, non UV-fluorescent aggregates consisting of irregularly shaped crystals measuring up to 25 µm in length and displaying an excellent cleavage parallel to (
01). dmeas is 4.31 g/cm3, dcalc 4.38 g/cm3, and the refractive indices are nmin = 1.725 and nmax = 1.740.
A high-resolution synchrotron powder diffraction pattern on the material from Musonoï shows that pseudojohannite is triclinic (P1 or P), with a = 10.027(1) Å, b = 10.822(1) Å, c = 13.396(1) Å, 
= 87.97(1)°, ß = 109.20(1)°, 
= 90.89(1)°, V = 1371.9(5) Å3. The location of the uranium and sulfur atoms in the cell was obtained by direct methods using 1807 reflections extracted from the powder diffractogram. Pseudojohannite contains zippeite-type layers oriented parallel to (01). The empirical chemical formula calculated for a total of 70 O atoms is Cu6.52U7.85S4.02O70H55.74, leading to the simplified chemical formula Cu6.5[(UO2)4O4(SO4)2]2(OH)5·25H2O. The distance of 9.16 Å between the uranyl-sulfate sheets in pseudojohannite shows that neighboring layers do not share O atoms with the same Cu
6 [ = (O,OH)] distorted octahedrons, such as in magnesium-zippeite. Rather, it is expected that Cu6 forms a layer bound to the zippeite-type layers by hydrogen bonding, as in marécottite, or one apex of the Cu6 polyhedron only is shared with a zippeite-type layer, as in synthetic SZIPPMg. The higher number of cations in the interlayer of pseudojohannite (Cu:S = 1.6:1) compared to marécottite (3:4) and SZIPPMg (1:1) indicates that pseudojohannite has a unique interlayer topology.
Ab-initio powder structure solution techniques can be used to obtain important structural information on complex micro-crystalline minerals such as those found in the weathering environment. Pseudojohannite represents a new member of the zippeite group of minerals, and further illustrates the structural complexity of zippeite-group minerals containing divalent cations, which have diverse arrangements in the interlayer. Peudojohannite and other divalent zippeites are common, easily overlooked minerals in acid drainage environments around uranium deposits and wastes.
Key Words: New mineral • pseudojohannite • uranyl sulfate • XRD data • IR spectroscopy • Jáchymov • La Creusaz • Musonoï
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