J 2014

Mathesiusite, K-5(UO2)(4)(SO4)(4)(VO5)(H2O)(4), a new uranyl vanadate-sulfate from Jachymov, Czech Republic

PLÁŠIL, Jakub, František VESELOVSKÝ, Jan HLOUŠEK, Radek ŠKODA, Milan NOVÁK et. al.

Základní údaje

Originální název

Mathesiusite, K-5(UO2)(4)(SO4)(4)(VO5)(H2O)(4), a new uranyl vanadate-sulfate from Jachymov, Czech Republic

Autoři

PLÁŠIL, Jakub (203 Česká republika, garant), František VESELOVSKÝ (203 Česká republika), Jan HLOUŠEK (203 Česká republika), Radek ŠKODA (203 Česká republika, domácí), Milan NOVÁK (203 Česká republika, domácí), Jiří SEJKORA (203 Česká republika), Jiří ČEJKA (203 Česká republika), Pavel ŠKÁCHA (203 Česká republika) a Anatoly KASATKIN (643 Rusko)

Vydání

American Mineralogist, CHANTILLY, Mineralogical Society of America, 2014, 0003-004X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.964

Kód RIV

RIV/00216224:14310/14:00080021

Organizační jednotka

Přírodovědecká fakulta

DOI

UT WoS

000333881800009

Klíčová slova anglicky

Mathesiusite; new mineral; uranyl sulfate; vanadate; crystal structure; Raman spectroscopy; oxidation zone; Jachymov

Štítky

Změněno: 13. 4. 2015 15:30, Ing. Andrea Mikešková

Anotace

V originále

Mathesiusite, K-5(UO2)(4)(SO4)(4)(VO5)(H2O)(4), a new uranyl vanadate-sulfate mineral from Jachymov, Western Bohemia, Czech Republic, occurs on fractures of gangue associated with adolfpateraite, schoepite, cejkaite, zippeite, gypsum, and a new unnamed K-UO2-SO4 mineral. It is a secondary mineral formed during post-mining processes. Mathesiusite is tetragonal, space group P4/n, with the unit-cell dimensions a = 14.9704(10). c = 6.8170(5) angstrom. V = 1527.78(18) angstrom(3), and Z = 2. Acicular aggregates of mathesiusite consist of prismatic crystals up to 200 mu m long and several micrometers thick. It is yellowish green with a greenish white streak and vitreous luster. The Mohs hardness is similar to 2. Mathesiusite is brittle with an uneven fracture and perfect cleavage on (110} and weaker on {001}. The calculated density based on the empirical formula is 4.02 g/cm(3). Mathesiusite is colorless in fragments, uniaxial (-), with omega = 1.634(3) and epsilon = 1.597(3). Electron microprobe analyses (average of 7) provided: K2O 12.42, SO3 18.04, V2O5 4.30, UO(3)61.46, H2O 3.90 (structure), total 100.12 (all in wt%). The empirical formula (based on 33 O atoms pfu) is: K-4.87(U0.99O2)(4)(S1.04O4),(V087O5)(H2O)(4). The eight strongest powder X-ray diffraction lines are [d(obs) in angstrom (hkl) I-rel]: 10.64 (110) 76, 7.486 (200) 9, 6.856 (001) 100, 6.237 (101) 85, 4.742 (310) 37, 3.749 (400) 27, 3.296 (401) 9, and 2.9409 (510) 17. The crystal structure of mathesiusite was solved from single-crystal X-ray diffraction data and refined to R-1 = 0.0520 for 795 reflections with I > 3 sigma(I). It contains topologically unique heteropolyhedral sheets based on [(UO2)(4)(SO4)(4)(VO5)](5-) clusters. These clusters arise from linkages between corner-sharing quartets of uranyl pentagonal bipyramids, which define a square-shaped void at the center that is occupied by V5+ cations. Each pair of uranyl pentagonal bipyramids shares two vertices of SO4 tetrahedra. Each SO4 shares a third vertex with another cluster to form the sheets. The K. cations are located between the sheets, together with a single H2O group. The corrugated sheets are stacked perpendicular to c. These heteropolyhedral sheets are similar to those in the structures of synthetic uranyl chromates. Raman spectral data are presented confirming the presence of UO22+, SO4, and molecular H2O.