Abstract

The crystal structure of brackebuschite, ideally Pb2Mn(3+)(VO4)2(OH) [dilead(II) manganese(III) vanadate(V) hydroxide], was redetermined based on single-crystal X-ray diffraction data of a natural sample from the type locality Sierra de Cordoba, Argentina. Improving on previous results, anisotropic displacement parameters for all non-H atoms were refined and the H atom located, obtaining a significant improvement of accuracy and an unambiguous hydrogen-bonding scheme. Brackebuschite belongs to the brackebuschite group of minerals with general formula A 2 M(T1O4)(T2O4)(OH, H2O), with A = Pb(2+), Ba, Ca, Sr; M = Cu(2+), Zn, Fe(2+), Fe(3+), Mn(3+), Al; T1 = As(5+), P, V(5+); and T2 = As(5+), P, V(5+), S(6+). The crystal structure of brackebuschite is based on a cubic closest-packed array of O and Pb atoms with infinite chains of edge-sharing [Mn(3+)O6] octa-hedra located about inversion centres and decorated by two unique VO4 tetra-hedra (each located on a special position 2e, site symmetry m). One type of VO4 tetra-hedra is linked with the (1) ∞[MnO4/2O2/1] chain by one common vertex, alternating with H atoms along the chain, while the other type of VO4 tetra-hedra link two adjacent octa-hedra by sharing two vertices with them and thereby participating in the formation of a three-membered Mn2V ring between the central atoms. The (1) ∞[Mn(3+)(VO4)2OH] chains run parallel to [010] and are held together by two types of irregular [PbO x ] polyhedra (x = 8, 11), both located on special position 2e (site symmetry m). The magnitude of the libration component of the O atoms of the (1) ∞[Mn(3+)(VO4)2OH] chain increases linearly with the distance from the centerline of the chain, indicating a significant twisting to and fro of the chain along [010]. The hy-droxy group bridges one Pb(2+) cation with two Mn(3+) cations and forms an almost linear hydrogen bond with a vanadate group of a neighbouring chain. The O⋯O distance of this inter-action determined from the structure refinement agrees well with Raman spectroscopic data.

Highlights

  • Manganese(III) vanadate(V) hydroxide], was redetermined based on singlecrystal X-ray diffraction data of a natural sample from the type locality Sierra de Cordoba, Argentina

  • Pb atoms with infinite chains of edge-sharing [Mn3+O6] octahedra located about inversion centres and decorated by two unique VO4 tetrahedra

  • Structure refinement of the latter converged at a reliability factor R1 of 0.056 and was based on anisotropic displacement parameters for all non-O atoms [note that the deposited data in the Inorganic Crystal Structure Database (ICSD, 2016), entry #89256, report only isotropic displacement parameters], and the H atom undetermined

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Summary

Mineralogical and crystal-chemical context

Brackebuschite, ideally Pb2Mn3+(VO4)2(OH), belongs to the brackebuschite group of minerals with monoclinic symmetry and space group type P21/m. Other secondary lead minerals within this group include arsenbrackebuschite [Pb2(Fe3+,Zn)(AsO4)2(OH,H2O)] (Abraham et al, 1978), calderónite [Pb2Fe3+(VO4)2(OH)] (González del Tánago et al, 2003), tsumebite [Pb2Cu(PO4)(SO4)(OH)] (Nichols, 1966), arsentsumebite [Pb2Cu(AsO4)(SO4)(OH)] (Bideaux et al, 1966; Zubkova et al, 2002), bushmakinite [Pb2Al(PO4)(VO4)(OH)]. Structure refinement of the latter converged at a reliability factor R1 of 0.056 and was based on anisotropic displacement parameters for all non-O atoms [note that the deposited data in the Inorganic Crystal Structure Database (ICSD, 2016), entry #89256, report only isotropic displacement parameters], and the H atom undetermined. All nonhydrogen atoms were refined with anisotropic displacement parameters, and the H atom was located, leading to a significant improvement of accuracy and precision, and to an unambiguous hydrogen bonding scheme

Structural commentary
Synthesis and crystallization
Refinement
Full Text
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