Crystal structure of the uranyl-oxide mineral rameauite
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F16%3A00111286" target="_blank" >RIV/00216224:14310/16:00111286 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/68378271:_____/16:00470086 RIV/00023272:_____/16:10133612
Výsledek na webu
<a href="https://www.researchgate.net/publication/304461313_Crystal_structure_of_the_uranyl-oxide_mineral_rameauite" target="_blank" >https://www.researchgate.net/publication/304461313_Crystal_structure_of_the_uranyl-oxide_mineral_rameauite</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/ejm/2016/0028-2568" target="_blank" >10.1127/ejm/2016/0028-2568</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Crystal structure of the uranyl-oxide mineral rameauite
Popis výsledku v původním jazyce
Rameauite is a rare supergene uranyl-oxide hydroxy-hydrate mineral that forms during hydration-oxidation weathering of uraninite. On the basis of single-crystal X-ray diffraction data collected on a microfocus source, rameauite is monoclinic, space group Cc, with a = 13.9458(19), b = 14.3105(19), c = 13.8959(18) angstrom, beta = 118.477(14)degrees, V = 2437.7(6) angstrom(3) and Z = 4, with D-calc = 5.467 g cm(-3). The structure of rameauite (R = 0.060 for 1698 unique observed reflections) contains sheets of the beta-U3O8 topology, with both UO6 and UO7 bipyramids, which is similar to the sheets found in spriggite, ianthinite and wyartite. The sheets alternate with the interlayer, which contains K+, Ca2+ and H2O molecules. Interstitial cations are linked into infinite chains that extend along [10-1]. Adjacent sheets are linked through K-O, Ca-O and H-bonds. The structural formula of rameauite is K2Ca((H2O)-O-[3]) 1((H2O)-O-[5])(4)[(UO2) O-6(6)(OH)(4)](H-2([4]) O)(1). The empirical formula obtained from the average of eight electron-microprobe analyses is (on the basis of 6 U p.f.u.) K-1.87(Ca1.10Sr0.04)(Sigma 1.14)[(UO2)(6)O-6(OH)(4.15)]center dot 6H(2)O. The Raman spectrum is dominated by U-O and O-H vibrations. A discussion of related uranyl- oxide minerals is given.
Název v anglickém jazyce
Crystal structure of the uranyl-oxide mineral rameauite
Popis výsledku anglicky
Rameauite is a rare supergene uranyl-oxide hydroxy-hydrate mineral that forms during hydration-oxidation weathering of uraninite. On the basis of single-crystal X-ray diffraction data collected on a microfocus source, rameauite is monoclinic, space group Cc, with a = 13.9458(19), b = 14.3105(19), c = 13.8959(18) angstrom, beta = 118.477(14)degrees, V = 2437.7(6) angstrom(3) and Z = 4, with D-calc = 5.467 g cm(-3). The structure of rameauite (R = 0.060 for 1698 unique observed reflections) contains sheets of the beta-U3O8 topology, with both UO6 and UO7 bipyramids, which is similar to the sheets found in spriggite, ianthinite and wyartite. The sheets alternate with the interlayer, which contains K+, Ca2+ and H2O molecules. Interstitial cations are linked into infinite chains that extend along [10-1]. Adjacent sheets are linked through K-O, Ca-O and H-bonds. The structural formula of rameauite is K2Ca((H2O)-O-[3]) 1((H2O)-O-[5])(4)[(UO2) O-6(6)(OH)(4)](H-2([4]) O)(1). The empirical formula obtained from the average of eight electron-microprobe analyses is (on the basis of 6 U p.f.u.) K-1.87(Ca1.10Sr0.04)(Sigma 1.14)[(UO2)(6)O-6(OH)(4.15)]center dot 6H(2)O. The Raman spectrum is dominated by U-O and O-H vibrations. A discussion of related uranyl- oxide minerals is given.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10504 - Mineralogy
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
European Journal of Mineralogy
ISSN
0935-1221
e-ISSN
1617-4011
Svazek periodika
28
Číslo periodika v rámci svazku
5
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
9
Strana od-do
959-967
Kód UT WoS článku
000399807600009
EID výsledku v databázi Scopus
2-s2.0-85010875051