Nitscheite, (NH4)2[(UO2)2(SO4)3(H2O)2]•3H2O, a new mineral with an unusual uranyl-sulfate sheet

被引:4
作者
Kampf, Anthony R. [1 ]
Olds, Travis A. [2 ]
Plasil, Jakub [3 ]
Nash, Barbara P. [4 ]
Marty, Joe [1 ]
机构
[1] Nat Hist Museum Los Angeles Cty, Mineral Sci Dept, 900 Exposit Blvd, Los Angeles, CA 90007 USA
[2] Carnegie Museum Nat Hist, Sect Minerals & Earth Sci, 4400 Forbes Ave, Pittsburgh, PA 15213 USA
[3] Inst Phys ASCR Vvi, Slovance 1999-2, Prague 18221 8, Czech Republic
[4] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA
关键词
Nitscheite; new mineral; uranyl-sulfate sheet; crystal structure; Raman spectroscopy; Green Lizard mine; Red Canyon; Utah; BOND-VALENCE PARAMETERS; SAN-JUAN COUNTY; CRYSTAL-STRUCTURES; COMPLEXITY; HIERARCHY; INSIGHTS; LENGTHS; UTAH;
D O I
10.2138/am-2022-7994
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Nitscheite (IMA2020-078), (NH4)(2)[(UO2)(2)(SO4)(3)(H2O)(2)]center dot 3H(2)O, is a new mineral species from the Green Lizard mine, Red Canyon, San Juan County, Utah, U.S.A. It is a secondary phase found in association with chinleite-(Y), gypsum, pyrite, and Co-rich rietveldite. Nitscheite occurs in subparallel and divergent intergrowths of yellow prisms, up to about 0.3 mm in length. Crystals are elongated on [101] and exhibit the forms {100}, {010}, {001}, and {11 (1) over bar}. The mineral is transparent with vitreous luster and very pale-yellow streak. It exhibits bright green fluorescence under a 405 nm laser. The Mohs hardness is -2. The mineral has brittle tenacity, curved fracture, and one good cleavage on {010}. The measured density is 3.30(2) g.cm(-3). The mineral is easily soluble in H2O at room temperature. The mineral is optically biaxial (-), alpha = 1.560(2), beta = 1.582(2), gamma = 1.583(2) (white light); 2V(meas) =17(1)degrees; no dispersion; orientation X = b, Z approximate to [101]; pleochroism X colorless, Y and Z yellow; X < Y approximate to Z. Electron microprobe analysis provided the empirical formula (NH4)(1.99)U2.00S3.00O21H10.01. Nitscheite is monoclinic, P2(1)/n, a= 17.3982(4), b = 12.8552(3), c = 17.4054(12)angstrom, beta = 96.649(7)degrees, V= 3866.7(3) angstrom(3), and Z = 8. The structure (R-1 = 0.0329 for 4547 I > 3 sigma/reflections) contains [(UO2)(2)(SO4)(3)(H2O)(2)](2-) uranyl-sulfate sheets, which are unique among minerals, with NH4 and H2O groups between the sheets.
引用
收藏
页码:1174 / 1180
页数:7
相关论文
共 34 条
[1]   ON THE DETERMINATION OF URANIUM OXYGEN BOND LENGTHS IN DIOXOURANIUM(VI) COMPOUNDS BY RAMAN-SPECTROSCOPY [J].
BARTLETT, JR ;
COONEY, RP .
JOURNAL OF MOLECULAR STRUCTURE, 1989, 193 :295-300
[2]   U6+ minerals and inorganic compounds:: Insights into an expanded structural hierarchy of crystal structures [J].
Burns, PC .
CANADIAN MINERALOGIST, 2005, 43 :1839-1894
[3]  
Cejka J, 1999, REV MINERAL <D>, V38, P521
[4]  
Chenoweth W.L., 1993, The Geology and Production History of the Uranium Deposits in the White Canyon Mining District, San Juan County, Utah, P93
[5]   Comprehensive derivation of bond-valence parameters for ion pairs involving oxygen [J].
Gagne, Olivier Charles ;
Hawthorne, Frank Christopher .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE CRYSTAL ENGINEERING AND MATERIALS, 2015, 71 :562-578
[6]   Bond-valence parameters for ammonium-anion interactions [J].
García-Rodríguez, L ;
Rute-Pérez, A ;
Piñero, JR ;
Silgo, CG .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 2000, 56 :565-569
[7]  
Gunter Mickey E., 2004, Microscope, V52, P23
[8]   Structural complexity of natural uranyl sulfates [J].
Gurzhiy, Vladislav V. ;
Plasil, Jakub .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE CRYSTAL ENGINEERING AND MATERIALS, 2019, 75 (01) :39-48
[9]  
Higashi T., 1995, ABSCOR
[10]   Magnesioleydetite and straβmannite, two new uranyl sulfate minerals with sheet structures from Red Canyon, Utah [J].
Kampf, Anthony R. ;
Plasil, Jakub ;
Kasatkin, Anatoly, V ;
Nash, Barbara P. ;
Marty, Joe .
MINERALOGICAL MAGAZINE, 2019, 83 (03) :349-360