Saccoite, Ca<sub>2</sub>Mn<sup>+3</sup><sub>2</sub>F(OH)<sub>8</sub>⋅0.5(SO<sub>4</sub>), a new, microporous mineral from the Kalahari Manganese Field, South Africa

Author(s)
Gerald Giester, Christian Lengauer, Chutimun Chanmuang Nasdala, Dan Topa, Jens Gutzmer, Karl-Ludwig Von Bezing
Abstract

Saccoite, Ca2Mn3+2F(OH)8⋅0.5(SO4 ), is a new mineral found at the N’Chwaning III mine, Kalahari Manganese Field, Northern Cape Province, Republic of South Africa. It occurs as fillings of voids in hydrothermally altered manganese ore (comprising mostly of bixbyite and baryte). Further associated minor minerals are braunite, gypsum, chlorite, sturmanite and ettringite. Saccoite forms small needles, felted crystal masses or crusts. The new mineral is olive green, transparent, with white streak and vitreous lustre. No luminescence is observed. Saccoite is uniaxial (–) with refractive indices at 589(1) nm of ω = 1.705(5) and ε = 1.684(2). Pleochroism is distinct, i.e. bluish green (ω) and yellowish green (ε). The chemical composition was studied by means of an electron probe micro-analyser (EPMA) using wavelength-dispersive X-ray spectrometry (WDS). The empirical mineral formula is Ca2.06Mn3+1.78Cu0.10Mg0.07F0.97(OH)8.02(SO4)0.39. The unit-cell dimensions of saccoite (space group P4/ncc) are a = 12.834(3) Å, c = 5.622(2) Å, V = 926.0(4) Å3 ), and the calculated mass dens-
ity is 2.73 g⋅cm–3 . Saccoite exhibits a heteropolyhedral framework structure that is composed of edge- and corner sharing CaF2(OH)and M(OH)6 polyhedra (M = Mn3+ and Cu2+ ) with large channels along [001], which host disordered and only partially occupied groups, especially SO2–. The hydrogen atoms of the OH groups point into the channel to form hydrogen bonds with the channel anions. Ca–F distances are ∼2.3 Å, the Ca–OH distances in the range of 2.44–2.58 Ǻ, and the M(OH)6 octahedron is strongly 4+2 Jahn-Teller distorted (4 × ∼1.92 Å, 2 × 2.27 Å). The F atom is tetrahedrally coordinated to calcium atoms. The strongest lines in the powder X-ray diffraction pattern [d in Å (relative intensity) (hkl)] are: 9.0735 (35) (110), 4.5370 (95) (220), 4.0644 (20) (310), 3.0105 (100) (321), 2.8117 (20) (002), 2.7242 (75) (411), 1.9755 (35) (611), and 1.8142 (20) (550). 

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
Helmholtz-Zentrum Dresden-Rossendorf, Naturhistorisches Museum Wien (NHM), University of Johannesburg (UJ)
Journal
Mineralogical Magazine
Volume
86
Pages
814-820
No. of pages
7
ISSN
0026-461X
DOI
https://doi.org/doi:10.1180/mgm.2022.60
Publication date
07-2022
Peer reviewed
Yes
Austrian Fields of Science 2012
104026 Spectroscopy, 105116 Mineralogy, 105113 Crystallography
Keywords
ASJC Scopus subject areas
Geochemistry and Petrology
Portal url
https://ucris.univie.ac.at/portal/en/publications/saccoite-ca2mn32foh805so4-a-new-microporous-mineral-from-the-kalahari-manganese-field-south-africa(4b993ab5-e188-4155-a72e-4a39d5f9a6f1).html