Gerald Giester, Branko Rieck, Christian L. Lengauer, Uwe Kolitsch, Lutz Nasdala
{"title":"Katsarosite Zn(C2O4)·2H2O, a new humboldtine-group mineral from the Lavrion Mining District, Greece","authors":"Gerald Giester, Branko Rieck, Christian L. Lengauer, Uwe Kolitsch, Lutz Nasdala","doi":"10.1007/s00710-023-00810-9","DOIUrl":null,"url":null,"abstract":"<div><p>Katsarosite, ideally Zn(C<sub>2</sub>O<sub>4</sub>)·2H<sub>2</sub>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<sup>2+</sup>) 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 <i>n</i><sub>α</sub> = 1.488(2), <i>n</i><sub>β</sub> = 1.550(2), <i>n</i><sub>γ</sub> = 1.684(2), with 2<i>V</i><sub>obs</sub> = 71(3)°. Chemical analysis gave on average C<sub>2</sub>O<sub>3</sub> 38.32 wt%, ZnO 38.99 wt%, FeO 1.92 wt%, and H<sub>2</sub>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 <i>C</i>2/<i>c</i>, with unit-cell parameters <i>a</i> = 11.768(3), <i>b</i> = 5.3882(12), <i>c</i> = 9.804(2) Å, <i>β</i> = 127.045(8)°, <i>V</i> = 496.2(2) Å<sup>3</sup> (<i>Z</i> = 4). The strongest lines in the Gandolfi X-ray powder pattern [<i>d</i><sub>obs</sub> in Å, <i>I</i><sub>obs</sub>/<i>I</i><sub>100</sub>, (<i>hkl</i>)] are: 4.6745, 100, (200); 4.7678, 94, (20<span>\\(\\overline{2 }\\)</span>); 2.9533, 51, (40<span>\\(\\overline{2 }\\)</span>); 4.7030, 37, (1 <span>\\(\\overline{1 }\\,\\overline{1 }\\)</span>); 3.9266, 33, (002); 3.5686, 27, (111); 2.6574, 22, (1 <span>\\(\\overline{1 }\\,\\overline{3 }\\)</span>); 3.5992, 8, (1 <span>\\(\\overline{1 }\\,\\overline{2 }\\)</span>); 2.7032, 4, (020). The crystal structure was refined based on single-crystal X-ray diffraction data to <i>R</i>(<i>F</i>) = 0.08. The observed mass density of 2.50(2) g cm<sup>−3</sup> compares well with the calculated value (2.508 g cm<sup>−3</sup>). 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<sub>2</sub>O<sub>4</sub>)·2H<sub>2</sub>O is characterized by chains consisting of isolated ZnO<sub>6</sub> 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<sub>2</sub>O molecule) donor–acceptor distances of ~ 2.8 Å.\n</p></div>","PeriodicalId":18547,"journal":{"name":"Mineralogy and Petrology","volume":null,"pages":null},"PeriodicalIF":1.4000,"publicationDate":"2023-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00710-023-00810-9.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mineralogy and Petrology","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00710-023-00810-9","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Katsarosite, ideally Zn(C2O4)·2H2O, 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 (Fe2+) 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 nα = 1.488(2), nβ = 1.550(2), nγ = 1.684(2), with 2Vobs = 71(3)°. Chemical analysis gave on average C2O3 38.32 wt%, ZnO 38.99 wt%, FeO 1.92 wt%, and H2O 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 C2/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) Å3 (Z = 4). The strongest lines in the Gandolfi X-ray powder pattern [dobs in Å, Iobs/I100, (hkl)] are: 4.6745, 100, (200); 4.7678, 94, (20\(\overline{2 }\)); 2.9533, 51, (40\(\overline{2 }\)); 4.7030, 37, (1 \(\overline{1 }\,\overline{1 }\)); 3.9266, 33, (002); 3.5686, 27, (111); 2.6574, 22, (1 \(\overline{1 }\,\overline{3 }\)); 3.5992, 8, (1 \(\overline{1 }\,\overline{2 }\)); 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(C2O4)·2H2O is characterized by chains consisting of isolated ZnO6 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 H2O molecule) donor–acceptor distances of ~ 2.8 Å.
Katsarosite,理想情况下是Zn(C2O4)·2H2O,以Īraklīs Katsaros命名,是在希腊Lavrion矿区Kaminiza地区的Esperanza矿山发现的一种新矿物。钾辉石通常直接生长在闪锌矿上或嵌埋在黄钾铁矾和/或氢锌矿中,常与石膏紧密共生,并被钠辉石和/或磷辉石覆盖。晶体聚集体大多为细颗粒到土质,单个晶体通常为圆形,平均直径为30 μ m,有时沿[001]或板状呈棱柱状,呈现模糊的{100}、{001}、{110}和{101}形状。卡萨罗赛特具有延展性,莫氏硬度为1½- 2,在{110}度上具有完美的解理;骨折在其他方向上是不均匀的。颜色取决于铁(Fe2+)的含量,从几乎不含铁的纯白色到富含铁的黄色不等。它具有树脂般的光泽和白色条纹;在短波或长波紫外线照射下均未观察到发光现象。katsaroite是光学双轴(+)。在589 nm波长处测得的折射率为:nα = 1.488(2), nβ = 1.550(2), nγ = 1.684(2), 2Vobs = 71(3)°。化学分析平均C2O3为38.32 wt%, ZnO 38.99 wt%, FeO 1.92 wt%, and H2O 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 C2/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) Å3 (Z = 4). The strongest lines in the Gandolfi X-ray powder pattern [dobs in Å, Iobs/I100, (hkl)] are: 4.6745, 100, (200); 4.7678, 94, (20\(\overline{2 }\)); 2.9533, 51, (40\(\overline{2 }\)); 4.7030, 37, (1 \(\overline{1 }\,\overline{1 }\)); 3.9266, 33, (002); 3.5686, 27, (111); 2.6574, 22, (1 \(\overline{1 }\,\overline{3 }\)); 3.5992, 8, (1 \(\overline{1 }\,\overline{2 }\)); 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(C2O4)·2H2O is characterized by chains consisting of isolated ZnO6 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 H2O molecule) donor–acceptor distances of ~ 2.8 Å.
期刊介绍:
Mineralogy and Petrology welcomes manuscripts from the classical fields of mineralogy, igneous and metamorphic petrology, geochemistry, crystallography, as well as their applications in academic experimentation and research, materials science and engineering, for technology, industry, environment, or society. The journal strongly promotes cross-fertilization among Earth-scientific and applied materials-oriented disciplines. Purely descriptive manuscripts on regional topics will not be considered.
Mineralogy and Petrology was founded in 1872 by Gustav Tschermak as "Mineralogische und Petrographische Mittheilungen". It is one of Europe''s oldest geoscience journals. Former editors include outstanding names such as Gustav Tschermak, Friedrich Becke, Felix Machatschki, Josef Zemann, and Eugen F. Stumpfl.