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Katsarosite Zn(C2O4)·2H2O, a new humboldtine-group mineral from the Lavrion Mining District, Greece

矿物硬度莫氏标度 单斜晶系 闪锌矿 结晶学 矿物 矿物学 化学 群(周期表) 劈理(地质) 黄钾铁矾 石膏 板状 晶体结构 分析化学(期刊) 材料科学 冶金 黄铁矿 断裂(地质) 复合材料 有机化学 色谱法
作者
Gerald Giester,Branko Rieck,Christian L. Lengauer,Uwe Kolitsch,Lutz Nasdala
出处
期刊:Mineralogy and Petrology [Springer Science+Business Media]
卷期号:117 (2): 259-267 被引量:4
标识
DOI:10.1007/s00710-023-00810-9
摘要

Abstract Katsarosite, ideally Zn(C 2 O 4 )·2H 2 O, named for Īraklīs Katsaros, is a new mineral found at the Esperanza Mine in the Kaminiza area of the Lavrion Mining District, Greece. Katsarosite usually occurs directly on sphalerite or embedded in jarosite and/or hydrozincite, often intimately intergrown with gypsum and overgrown by goslarite and/or epsomite. Crystal aggregates are mostly fine granular to earthy, with individual crystals being usually rounded with an average diameter of 30 µm, sometimes prismatic along [001] or platy, exhibiting the indistinct forms {100}, {001}, {110}, and {101}. Katsarosite is malleable with a Mohs hardness of 1½ – 2 and exhibits a perfect cleavage on {110}; the fracture is uneven in all other directions. The colour depends on the iron (Fe 2+ ) content, ranging from pure white in almost Fe-free samples to yellow in Fe-rich specimens. It has a resinous luster and a white streak; no luminescence has been observed under either short- or long-wave ultraviolet radiation. Katsarosite is optically biaxial (+). Refractive indices measured at a wavelength of 589 nm are n α = 1.488(2), n β = 1.550(2), n γ = 1.684(2), with 2 V obs = 71(3)°. Chemical analysis gave on average C 2 O 3 38.32 wt%, ZnO 38.99 wt%, FeO 1.92 wt%, and H 2 O 19.04 wt% (the latter was deduced based on the crystal-structure refinement), with traces of MgO and MnO. The new mineral is readily soluble in dilute acids. Katsarosite is monoclinic, space group C 2/ c , with unit-cell parameters a = 11.768(3), b = 5.3882(12), c = 9.804(2) Å, β = 127.045(8)°, V = 496.2(2) Å 3 ( Z = 4). The strongest lines in the Gandolfi X-ray powder pattern [ d obs in Å, I obs / I 100 , ( hkl )] are: 4.6745, 100, (200); 4.7678, 94, (20 $$\overline{2 }$$ 2 ¯ ); 2.9533, 51, (40 $$\overline{2 }$$ 2 ¯ ); 4.7030, 37, (1 $$\overline{1 }\,\overline{1 }$$ 1 ¯ 1 ¯ ); 3.9266, 33, (002); 3.5686, 27, (111); 2.6574, 22, (1 $$\overline{1 }\,\overline{3 }$$ 1 ¯ 3 ¯ ); 3.5992, 8, (1 $$\overline{1 }\,\overline{2 }$$ 1 ¯ 2 ¯ ); 2.7032, 4, (020). The crystal structure was refined based on single-crystal X-ray diffraction data to R ( F ) = 0.08. The observed mass density of 2.50(2) g cm −3 compares well with the calculated value (2.508 g cm −3 ). Katsarosite belongs to the humboldtine group, whose crystal-structure type is well described for both isotypic minerals and synthetic compounds in the literature. The atomic arrangement in Zn(C 2 O 4 )·2H 2 O is characterized by chains consisting of isolated ZnO 6 octahedra which are alternately linked along [010] via oxalate anions. These chains are interconnected through hydrogen bonds only, with Ow···O (with Ow denoting the O atom of the H 2 O molecule) donor–acceptor distances of ~ 2.8 Å.

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