The (3+3) commensurately modulated structure of the uranyl silicate mineral swamboite-(Nd), Nd0.333[(UO2)(SiO3OH)](H2O)2.41

Author:

Plášil Jakub1,Petříček Václav2,Locock Andrew J.3,Škoda Radek4,Burns Peter C.56

Affiliation:

1. Institute of Physics of the Czech Academy of Sciences , Na Slovance 2, 182 21 Praha 8 , Czech Republic , Tel.: 00420772212757

2. Institute of Physics of the Czech Academy of Sciences , Na Slovance 2, 182 21 Praha 8 , Czech Republic

3. Department of Earth and Atmospheric Sciences , University of Alberta , Edmonton, Alberta T6G 2E3 , Canada

4. Department of Geological Sciences, Faculty of Science , Masaryk University, Kotlářská 2 , 611 37 Brno , Czech Republic

5. Department of Civil and Environmental Engineering and Earth Sciences , University of Notre Dame , Notre Dame, IN 46556 , USA

6. Department of Chemistry and Biochemistry , University of Notre Dame , Notre Dame, IN 46556 , USA

Abstract

Abstract The uranyl mineral swamboite has been redefined to swamboite-(Nd) and its structure has been solved and refined as a commensurate structure in six-dimensional superspace. The structure is monoclinic, superspace group P21 /m(a1,b1,g1)00(−a1,b1,g1)00 (a2,0,g2)0s, cell parameters a=6.6560(3), b=6.9881(5), c=8.8059(6), c=11.3361(16) Å, β=102.591(5)°, modulation wave-vectors q 1 =1/3 1/3 0; q 2 =−1/3 1/3 0; q 3 =1/2 0 1/2. The structure was refined from 8717 reflections to a final R=0.0610. The model includes modulation both of atomic positions and displacement parameters, as well as occupancy waves. The structure is based upon uranyl-silicate sheets of uranophane topology alternating with an interlayer of partly occupied Nd3+ sites and H2O molecules. The strong (3+3) dimensional modulation of the structure originates from the distribution of the Nd-dominated sites and further accommodation of the suitable geometry within the sheets and charge distribution within the structure. The separation distances between the corresponding occupied Nd sites are rationals of the super-cell vectors corresponding to the modulation vectors of the structure. The case of swamboite-(Nd) is the first example of a modulated structure within the oxysalts of U6+.

Publisher

Walter de Gruyter GmbH

Subject

Inorganic Chemistry,Condensed Matter Physics,General Materials Science

Reference44 articles.

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4. R. J. Finch, T. Murakami, Systematics and paragenesis of uranium minerals. in Uranium: Mineralogy, Geochemistry and the Environment, (Eds. P. C. Burns and R. J. Finch) Reviews in Mineralogy and Geochemistry, Vol. 38, Mineralogical Society of America and Geochemical Society, Washington, D.C., p. 91, 1999.

5. S. V. Krivovichev, J. Plášil, Mineralogy and crystallography of uranium. in Uranium, from Cradle to Grave (Eds. P. C. Burns and G. E. Sigmon) Mineralogical Association of Canada Short Course, Mineralogical Society of Canada, Vol. 43, Winnipeg, MB, p. 15. 2013.

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