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Type: | Journal article |
Title: | Description and crystal structure of a new mineral, edwardsite, Cu3Cd2 (SO4)2(OH)6.4H2O, from Broken Hill, New South Wales, Australia |
Author: | Elliott, P. Brugger, J. Caradoc-Davies, T. |
Citation: | Mineralogical Magazine, 2010; 74(1):39-53 |
Publisher: | Mineralogical Society |
Issue Date: | 2010 |
ISSN: | 0026-461X 1471-8022 |
Statement of Responsibility: | Elliott, P.; Brugger, J. and Caradoc-Davies, T. |
Abstract: | <jats:title>Abstract</jats:title><jats:p>Edwardsite, Cu<jats:sub>3</jats:sub>Cd<jats:sub>2</jats:sub>(SO<jats:sub>4</jats:sub>)<jats:sub>2</jats:sub>(OH)<jats:sub>6</jats:sub>·4H<jats:sub>2</jats:sub>O, is a new mineral from the Block 14 Opencut, Broken Hill, New South Wales, Australia. It occurs as druses of tabular and bladed crystals up to 0.06 mm in size, associated with niedermayrite and christelite. Edwardsite is pale blue, transparent with vitreous lustre and has excellent cleavage parallel to {100}. Density was not measured but the calculated density, from the empirical formula, is 3.53 g cm<jats:sup>–3</jats:sup>and the Mohs hardness is ∼3. Optically, it is biaxial negative with α ∼ 1.74, β = 1.762(4), γ ∼ 1.77 and 2V<jats:sub>calc.</jats:sub>∼ +62°. The optical orientation is X =<jats:italic>b</jats:italic>, Y ∼<jats:italic>a</jats:italic>, Z ∼<jats:italic>c</jats:italic>. Electron microprobe analysis gave (wt.%): CdO 32.43, CuO 28.06, ZnO 2.26, FeO 0.08, SO<jats:sub>3</jats:sub>20.35, H<jats:sub>2</jats:sub>O<jats:sub>calc.</jats:sub>(from crystal-structure analysis) 14.14, totalling 99.32. The empirical formula, calculated on the basis of 18 oxygen atoms is Cu<jats:sub>2.77</jats:sub>Cd<jats:sub>1.98</jats:sub>Zn<jats:sub>0.22</jats:sub>Fe<jats:sub>0.01</jats:sub>(SO<jats:sub>4</jats:sub>)<jats:sub>2.00</jats:sub>(OH)<jats:sub>5.95</jats:sub>·4.06H<jats:sub>2</jats:sub>O. Edwardsite is monoclinic, space group<jats:italic>P</jats:italic>2<jats:sub>1</jats:sub>/<jats:italic>c</jats:italic>, with<jats:italic>a</jats:italic>= 10.863(2) Å,<jats:italic>b</jats:italic>= 13.129(3) Å,<jats:italic>c</jats:italic>= 11.169(2) Å, β = 113.04(3)°,<jats:italic>V</jats:italic>= 1465.9(5) Å<jats:sup>3</jats:sup>(single-crystal data) and<jats:italic>Z</jats:italic>= 4. The eight strongest lines in the powder diffraction pattern are [<jats:italic>d</jats:italic>(Å), (<jats:italic>I</jats:italic>/<jats:italic>I</jats:italic><jats:sub>0</jats:sub>), (<jats:italic>hkl</jats:italic>)]: 9.991, (90), (100); 5.001, (90), (200, 21<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline01.png" />); 4.591, (45), (20<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline002.png" />); 3.332, (60), (300, 032); 3.005, (30), (0<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline002.png" />3); 2.824, (40), (<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline01.png" /><jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline03.png" />2); 2.769, (55), (20<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline03.png" />, 042, 10<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline03.png" />); 2.670, (45), (2<jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline03.png" /><jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" mime-subtype="png" xlink:href="S0026461X00056991_inline002.png" />). The crystal structure was determined by direct methods and refined to<jats:italic>R</jats:italic>1 = 3.21% using 1904 observed reflections with<jats:italic>F</jats:italic><jats:sub>o</jats:sub>> 4σ(<jats:italic>F</jats:italic><jats:sub>o</jats:sub>) collected using synchrotron X-ray radiation (λ = 0.773418 Å). The structure is based on infinite sheets of edge-sharing Cuϕ<jats:sub>6</jats:sub>(ϕ: O<jats:sup>2–</jats:sup>, OH) octahedra and Cdϕ<jats:sub>7</jats:sub>(ϕ: O<jats:sup>2–</jats:sup>, H<jats:sub>2</jats:sub>O) polyhedra parallel to (100). The sheets are decorated on both sides by corner-sharing (SO<jats:sub>4</jats:sub>) tetrahedra, which also corner-link to isolated Cdϕ<jats:sub>6</jats:sub>octahedra, thus connecting adjacent sheets. Moderate-strong to weak hydrogen bonding provides additional linkage between sheets.</jats:p> |
Keywords: | Edwardsite New Mineral Species Crystal Structure Cd Oxysalt Sulphate Broken Hill New South Wales |
DOI: | 10.1180/minmag.2010.074.1.39 |
Published version: | http://dx.doi.org/10.1180/minmag.2010.074.1.39 |
Appears in Collections: | Aurora harvest Earth and Environmental Sciences publications |
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