Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov,
Czech Republic.

J 2013

Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic.

PLÁŠIL, Jakub; Jan HLOUŠEK; Radek ŠKODA; Milan NOVÁK; Jiří SEJKORA et al.

Základní údaje

Originální název

Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic.

Autoři

PLÁŠIL, Jakub; Jan HLOUŠEK; Radek ŠKODA; Milan NOVÁK; Jiří SEJKORA; Jiří ČEJKA; František VESELOVSKÝ a Juraj MAJZLAN

Vydání

Mineralogical Magazine, Mineralogical Society, 2013, 0026-461X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.898

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/13:00072902

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1180/minmag.2013.077.8.01

UT WoS

000333054700001

Klíčová slova anglicky

vysokýite; new mineral; uranium(IV) tetrakis[dihydrogen arsenate] tetrahydrate; crystal structure; oxide zone; Jáchymov

Štítky

AKR, rivok

Změněno: 10. 4. 2014 20:14, Ing. Andrea Mikešková

Anotace

V originále

Vysokýite, U4+[(AsO2(OH)2] 4(H2O)4 (IMA 2012-067), was found growing on an altered surface of massive native As in the Geschieber vein, Jáchymov ore district, Western Bohemia, Czech Republic. The new mineral was found in association with běhounekite, štěpite, kaatialaite, arsenolite, claudetite and gypsum. It forms extremely fibrous light-green crystals up to 8 mm long. Crystals have an alabaster lustre and a greenish-white to greyish streak. Vysokýite is brittle with uneven fracture and perfect cleavage along (100) and (001); the Mohs hardness is ~2. A density of 3.393 g/cm3 was calculated using the empirical formula and unit-cell parameters obtained from a single-crystal diffraction experiment. Vysokýite is non-fluorescent under short or long wavelength UV radiation. The average of five spot wavelength dispersive spectroscopy (WDS) analyses is 29.44 UO2, 1.03 SiO2, 48.95 As2O5, 0.12 SO3, 15.88 H2O (calc.), total 95.42 wt.%. The empirical formula of vysokýite (based on 20 O a.p.f.u.) is U1.00[AsO2(OH)2] 3.90(SiO4)0.16 (SO4)0.014H 2O. The As-O-H and O-H vibrations dominate in the Raman spectrum. Vysokýite is triclinic, space group P1, with a = 10.749(2), b = 5.044(3), c = 19.1778(7) A, alpha = 89.872(15) , beta = 121.534(15) , gamma = 76.508(15) , and V = 852.1(6) A3, Z = 2 and D calc = 3.34 gcm-3. The strongest diffraction peaks in the X-ray powder diffraction pattern are [d obs in A (I rel.)(hkl)]: 8.872(100)(100), 8.067(50)(002), 6.399(7)(103), 4.773(6)(104), 3.411(10)(302), 3.197(18)(313). The crystal structure of vysokýite was solved from single-crystal X-ray diffraction data by the charge-flipping method and refined to R 1 = 0.0595 based on 2718 unique observed reflection, and to wR 2 = 0.1160 for all 4173 unique reflections. The structure of vysokýite consists of UO8 square antiprisms sharing all of their vertices with 8 As-tetrahedra to form infinite chains parallel to [010]. These chains are linked by hydrogen bonds involving terminal (OH) groups of the double-protonated As-tetrahedra and molecules of H2O located between the chains. The new mineral is named in honour of Arnošt Vysoký (1823-1872), the former chief of the Jáchymov mines and smelters, chemist and metallurgist.

Citovat

PLÁŠIL, Jakub; Jan HLOUŠEK; Radek ŠKODA; Milan NOVÁK; Jiří SEJKORA; Jiří ČEJKA; František VESELOVSKÝ a Juraj MAJZLAN. Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic. Mineralogical Magazine. Mineralogical Society, 2013, roč. 77, č. 8, s. 3055-3066. ISSN 0026-461X. Dostupné z: https://doi.org/10.1180/minmag.2013.077.8.01.

@article{1179274,
   author = {Plášil, Jakub and Hloušek, Jan and Škoda, Radek and Novák, Milan and Sejkora, Jiří and Čejka, Jiří and Veselovský, František and Majzlan, Juraj},
   article_number = {8},
   doi = {https://doi.org/10.1180/minmag.2013.077.8.01},
   keywords = {vysokýite; new mineral; uranium(IV) tetrakis[dihydrogen arsenate] tetrahydrate; crystal structure; oxide zone; Jáchymov},
   language = {eng},
   issn = {0026-461X},
   journal = {Mineralogical Magazine},
   title = {Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic.},
   volume = {77},
   year = {2013}
}

TY  - JOUR
ID  - 1179274
AU  - Plášil, Jakub - Hloušek, Jan - Škoda, Radek - Novák, Milan - Sejkora, Jiří - Čejka, Jiří - Veselovský, František - Majzlan, Juraj
PY  - 2013
TI  - Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic.
JF  - Mineralogical Magazine
VL  - 77
IS  - 8
SP  - 3055-3066
EP  - 3055-3066
PB  - Mineralogical Society
SN  - 0026461X
KW  - vysokýite
KW  - new mineral
KW  - uranium(IV) tetrakis[dihydrogen arsenate] tetrahydrate
KW  - crystal structure
KW  - oxide zone
KW  - Jáchymov
N2  - Vysokýite, U4+[(AsO2(OH)2] 4(H2O)4 (IMA 2012-067), was found growing on an altered surface of massive native As in the Geschieber vein, Jáchymov ore district, Western Bohemia, Czech Republic. The new mineral was found in association with běhounekite, štěpite, kaatialaite, arsenolite, claudetite and gypsum. It forms extremely fibrous light-green crystals up to 8 mm long. Crystals have an alabaster lustre and a greenish-white to greyish streak. Vysokýite is brittle with uneven fracture and perfect cleavage along (100) and (001); the Mohs hardness is ~2. A density of 3.393 g/cm3 was calculated using the empirical formula and unit-cell parameters obtained from a single-crystal diffraction experiment. Vysokýite is non-fluorescent under short or long wavelength UV radiation. The average of five spot wavelength dispersive spectroscopy (WDS) analyses is 29.44 UO2, 1.03 SiO2, 48.95 As2O5, 0.12 SO3, 15.88 H2O (calc.), total 95.42 wt.%. The empirical formula of vysokýite (based on 20 O a.p.f.u.) is U1.00[AsO2(OH)2] 3.90(SiO4)0.16 (SO4)0.014H 2O. The As-O-H and O-H vibrations dominate in the Raman spectrum. Vysokýite is triclinic, space group P1, with a = 10.749(2), b = 5.044(3), c = 19.1778(7) A, alpha = 89.872(15) , beta = 121.534(15) , gamma = 76.508(15) , and V = 852.1(6) A3, Z = 2 and D calc = 3.34 gcm-3. The strongest diffraction peaks in the X-ray powder diffraction pattern are [d obs in A (I rel.)(hkl)]: 8.872(100)(100), 8.067(50)(002), 6.399(7)(103), 4.773(6)(104), 3.411(10)(302), 3.197(18)(313). The crystal structure of vysokýite was solved from single-crystal X-ray diffraction data by the charge-flipping method and refined to R 1 = 0.0595 based on 2718 unique observed reflection, and to wR 2 = 0.1160 for all 4173 unique reflections. The structure of vysokýite consists of UO8 square antiprisms sharing all of their vertices with 8 As-tetrahedra to form infinite chains parallel to [010]. These chains are linked by hydrogen bonds involving terminal (OH) groups of the double-protonated As-tetrahedra and molecules of H2O located between the chains. The new mineral is named in honour of Arnošt Vysoký (1823-1872), the former chief of the Jáchymov mines and smelters, chemist and metallurgist.
ER  -

PLÁŠIL, Jakub; Jan HLOUŠEK; Radek ŠKODA; Milan NOVÁK; Jiří SEJKORA; Jiří ČEJKA; František VESELOVSKÝ a Juraj MAJZLAN. Vysokýite, U4+[AsO2(OH)2]4·4H2O, a new mineral from Jáchymov, Czech Republic. \textit{Mineralogical Magazine}. Mineralogical Society, 2013, roč.~77, č.~8, s.~3055-3066. ISSN~0026-461X. Dostupné z: https://doi.org/10.1180/minmag.2013.077.8.01.

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