The crystal structure of magnesiozippeite,
Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan
County, Utah (USA)

J 2013

The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA)

PLÁŠIL, Jakub; Karla FEJFAROVÁ; Radek ŠKODA; Michal DUŠEK; Joe MARTY et al.

Základní údaje

Originální název

The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA)

Autoři

PLÁŠIL, Jakub; Karla FEJFAROVÁ; Radek ŠKODA; Michal DUŠEK; Joe MARTY a Jiří ČEJKA

Vydání

Mineralogy and Petrology, Austria, Springer Verlag, 2013, 0930-0708

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Rakousko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.598

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/13:00072872

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1007/s00710-012-0241-7

UT WoS

000317350300008

Klíčová slova anglicky

magnesiozippeite; crystal structure

Štítky

AKR, rivok

Změněno: 9. 4. 2014 16:58, Ing. Andrea Mikešková

Anotace

V originále

The crystal structure of natural magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle mine, San Juan County, U.S.A., has been determined by single-crystal X-ray diffraction analysis and refined to R (obs) = 0.0348. The mineral is monoclinic, crystallizing in the space group C2/m, with unit cell parameters a = 8.7005(5), b = 14.2541(6), c = 8.8433(5), beta = 104.408(5)A degrees, V = 1062.24(9) (3) and Z = 4. The structure consists of the structural sheets of zippeite topology, represented by a structure unit [(UO2)(2)O-2(SO4)](2-), and an interlayer where two Mg2+ I broken vertical bar(6) octahedra are located. The crystal structure of natural magnesiozippeite shows considerable differences to the structure of previously reported synthetic analogue, namely in coordination of Mg2+ in the interlayer.

Návaznosti

EE2.3.20.0052, projekt VaV

Název: Výzkumný tým pro ukládání radioaktivních odpadů a jadernou bezpečnost

Citovat

PLÁŠIL, Jakub; Karla FEJFAROVÁ; Radek ŠKODA; Michal DUŠEK; Joe MARTY a Jiří ČEJKA. The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA). Mineralogy and Petrology. Austria: Springer Verlag, 2013, roč. 107, č. 2, s. 211-219. ISSN 0930-0708. Dostupné z: https://doi.org/10.1007/s00710-012-0241-7.

@article{1174106,
   author = {Plášil, Jakub and Fejfarová, Karla and Škoda, Radek and Dušek, Michal and Marty, Joe and Čejka, Jiří},
   article_location = {Austria},
   article_number = {2},
   doi = {https://doi.org/10.1007/s00710-012-0241-7},
   keywords = {magnesiozippeite; crystal structure},
   language = {eng},
   issn = {0930-0708},
   journal = {Mineralogy and Petrology},
   title = {The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA)},
   volume = {107},
   year = {2013}
}

TY  - JOUR
ID  - 1174106
AU  - Plášil, Jakub - Fejfarová, Karla - Škoda, Radek - Dušek, Michal - Marty, Joe - Čejka, Jiří
PY  - 2013
TI  - The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA)
JF  - Mineralogy and Petrology
VL  - 107
IS  - 2
SP  - 211-219
EP  - 211-219
PB  - Springer Verlag
SN  - 09300708
KW  - magnesiozippeite
KW  - crystal structure
N2  - The crystal structure of natural magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle mine, San Juan County, U.S.A., has been determined by single-crystal X-ray diffraction analysis and refined to R (obs) = 0.0348. The mineral is monoclinic, crystallizing in the space group C2/m, with unit cell parameters a = 8.7005(5), b = 14.2541(6), c = 8.8433(5), beta = 104.408(5)A degrees, V = 1062.24(9) (3) and Z = 4. The structure consists of the structural sheets of zippeite topology, represented by a structure unit [(UO2)(2)O-2(SO4)](2-), and an interlayer where two Mg2+ I broken vertical bar(6) octahedra are located. The crystal structure of natural magnesiozippeite shows considerable differences to the structure of previously reported synthetic analogue, namely in coordination of Mg2+ in the interlayer.
ER  -

PLÁŠIL, Jakub; Karla FEJFAROVÁ; Radek ŠKODA; Michal DUŠEK; Joe MARTY a Jiří ČEJKA. The crystal structure of magnesiozippeite, Mg[(UO2)(2)O-2(SO4)](H2O)(3.5), from East Saddle Mine, San Juan County, Utah (USA). \textit{Mineralogy and Petrology}. Austria: Springer Verlag, 2013, roč.~107, č.~2, s.~211-219. ISSN~0930-0708. Dostupné z: https://doi.org/10.1007/s00710-012-0241-7.

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