Crystal structure of the (REE)-uranyl carbonate mineral
shabaite-(Nd)

J 2017

Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd)

PLÁŠIL, Jakub a Radek ŠKODA

Základní údaje

Originální název

Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd)

Autoři

PLÁŠIL, Jakub (203 Česká republika) a Radek ŠKODA (203 Česká republika, garant, domácí)

Vydání

Journal of Geosciences, Praha, Česká geologická společnost, 2017, 1802-6222

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.415

Kód RIV

RIV/00216224:14310/17:00100335

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.3190/jgeosci.232

UT WoS

000403154700004

Klíčová slova anglicky

shabaite-(Nd); uranyl carbonate; rare-earth elements; crystal structure; mineral evolution

Štítky

NZ, rivok

Změněno: 30. 3. 2018 22:51, Ing. Nicole Zrilić

Anotace

V originále

Shabaite-(Nd) is a rare supergene mineral formed during alteration-hydration weathering of uraninite; its structure has remained unknown until now. Based on single-crystal X-ray diffraction data, shabaite-(Nd) is triclinic, twinned (leading to a pseudo-monoclinic diffraction pattern), space group P-1, with a = 8.3835(5), b = 9.2766(12), c = 31.7519(3) angstrom, alpha = 90.058(3), beta = 89.945(4), gamma = 90.331(4)degrees, V = 2469.3(4) angstrom(3) and Z = 4. The structure was refined from diffraction data to R = 0.060 for 8434 unique observed reflections. The structure of shabaite-(Nd) is based upon finite clusters of polyhedra, the well-known uranyl-tricarbonate cluster (referred to as UTC), the Ca-polyhedra linked to UTC and infinite sheets of Nd-polyhedra with internal Nd-O-C linkages. The infinite sheets of Nd-polyhedra are stacked perpendicular to c; to the UTC are staggered approximately perpendicular to the Nd-based sheets (thus approx. parallel to c), forming electroneutral ({Nd-2(3+)(CO3)(2-)(2)(H2O)(2)}(2+){Ca(H2O)(5)}(2+)[(UO2)(CO3)(3)](4-))(0) layers. Adjacent layers are linked by hydrogen bonds. The ratio of elements in the chemical formula of shabaite-(Nd), obtained from the structure refinement, Nd2Ca[(UO2)(CO3)(3)] (CO3)(2)(H2O)(10.5), Z = 4, was confirmed by an electron-microprobe study. The resulting empirical formula for the average of six analyses is Ca-1.01(Nd0.64Ce0.32Sm0.28Gd0.19Y0.19Pr0.13Dy0.10La0.07Tb0.05Ho0.01)(Sigma 1.98)(UO2)(CO3)(4.98)(H2O)(10.5)(based on 1 U apfu). A discussion of the crystal-structural relationships of shabaite-(Nd) and chemically related minerals is given as well as discussion of complexities of their crystal structures.

Návaznosti

MUNI/A/1316/2015, interní kód MU

Název: Geologické, geodynamické a environmentální procesy východního okraje Českého masívu (Akronym: Geodyn)

Investor: Masarykova univerzita, Geologické, geodynamické a environmentální procesy východního okraje Českého masívu, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Citovat

PLÁŠIL, Jakub a Radek ŠKODA. Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd). Journal of Geosciences. Praha: Česká geologická společnost, 2017, roč. 62, č. 2, s. 97-105. ISSN 1802-6222. Dostupné z: https://dx.doi.org/10.3190/jgeosci.232.

@article{1411005,
   author = {Plášil, Jakub and Škoda, Radek},
   article_location = {Praha},
   article_number = {2},
   doi = {http://dx.doi.org/10.3190/jgeosci.232},
   keywords = {shabaite-(Nd); uranyl carbonate; rare-earth elements; crystal structure; mineral evolution},
   language = {eng},
   issn = {1802-6222},
   journal = {Journal of Geosciences},
   title = {Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd)},
   volume = {62},
   year = {2017}
}

TY  - JOUR
ID  - 1411005
AU  - Plášil, Jakub - Škoda, Radek
PY  - 2017
TI  - Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd)
JF  - Journal of Geosciences
VL  - 62
IS  - 2
SP  - 97-105
EP  - 97-105
PB  - Česká geologická společnost
SN  - 18026222
KW  - shabaite-(Nd)
KW  - uranyl carbonate
KW  - rare-earth elements
KW  - crystal structure
KW  - mineral evolution
N2  - Shabaite-(Nd) is a rare supergene mineral formed during alteration-hydration weathering of uraninite; its structure has remained unknown until now. Based on single-crystal X-ray diffraction data, shabaite-(Nd) is triclinic, twinned (leading to a pseudo-monoclinic diffraction pattern), space group P-1, with a = 8.3835(5), b = 9.2766(12), c = 31.7519(3) angstrom, alpha = 90.058(3), beta = 89.945(4), gamma = 90.331(4)degrees, V = 2469.3(4) angstrom(3) and Z = 4. The structure was refined from diffraction data to R = 0.060 for 8434 unique observed reflections. The structure of shabaite-(Nd) is based upon finite clusters of polyhedra, the well-known uranyl-tricarbonate cluster (referred to as UTC), the Ca-polyhedra linked to UTC and infinite sheets of Nd-polyhedra with internal Nd-O-C linkages. The infinite sheets of Nd-polyhedra are stacked perpendicular to c; to the UTC are staggered approximately perpendicular to the Nd-based sheets (thus approx. parallel to c), forming electroneutral ({Nd-2(3+)(CO3)(2-)(2)(H2O)(2)}(2+){Ca(H2O)(5)}(2+)[(UO2)(CO3)(3)](4-))(0) layers. Adjacent layers are linked by hydrogen bonds. The ratio of elements in the chemical formula of shabaite-(Nd), obtained from the structure refinement, Nd2Ca[(UO2)(CO3)(3)] (CO3)(2)(H2O)(10.5), Z = 4, was confirmed by an electron-microprobe study. The resulting empirical formula for the average of six analyses is Ca-1.01(Nd0.64Ce0.32Sm0.28Gd0.19Y0.19Pr0.13Dy0.10La0.07Tb0.05Ho0.01)(Sigma 1.98)(UO2)(CO3)(4.98)(H2O)(10.5)(based on 1 U apfu). A discussion of the crystal-structural relationships of shabaite-(Nd) and chemically related minerals is given as well as discussion of complexities of their crystal structures.
ER  -

PLÁŠIL, Jakub a Radek ŠKODA. Crystal structure of the (REE)-uranyl carbonate mineral shabaite-(Nd). \textit{Journal of Geosciences}. Praha: Česká geologická společnost, 2017, roč.~62, č.~2, s.~97-105. ISSN~1802-6222. Dostupné z: https://dx.doi.org/10.3190/jgeosci.232.

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