The crystal structure of eveite, ideally Mn(2)(AsO(4))(OH) [dimanganese(II) arsenate(V) hydroxide], was refined from a single crystal selected from a co-type sample from Långban, Filipstad, Varmland, Sweden. Eveite, dimorphic with sarkinite, is structurally analogous with the important rock-forming mineral andalusite, Al(2)OSiO(4), and belongs to the libethenite group. Its structure consists of chains of edge-sharing distorted [MnO(4)(OH)(2)] octa-hedra (..2 symmetry) extending parallel to [001]. These chains are cross-linked by isolated AsO(4) tetra-hedra (..m symmetry) through corner-sharing, forming channels in which dimers of edge-sharing [MnO(4)(OH)] trigonal bipyramids (..m symmetry) are located. In contrast to the previous refinement from Weissenberg photographic data [Moore & Smyth (1968 ▶). Am. Mineral.53, 1841-1845], all non-H atoms were refined with anisotropic displacement param-eters and the H atom was located. The distance of the donor and acceptor O atoms involved in hydrogen bonding is in agreement with Raman spectroscopic data. Examination of the Raman spectra for arsenate minerals in the libethenite group reveals that the position of the peak originating from the O-H stretching vibration shifts to lower wavenumbers from eveite, to adamite, zincolivenite, and olivenite.
The crystal structure of eveite, ideally Mn(2)(AsO(4))(OH) [dimanganese(II) arsenate(V) hydroxide], was refined from a single crystal selected from a co-type sample from Långban, Filipstad, Varmland, Sweden. Eveite, dimorphic with sarkinite, is structurally analogous with the important rock-forming mineral andalusite, Al(2)OSiO(4), and belongs to the libethenite group. Its structure consists of chains of edge-sharing distorted [MnO(4)(OH)(2)] octa-hedra (..2 symmetry) extending parallel to [001]. These chains are cross-linked by isolated AsO(4) tetra-hedra (..m symmetry) through corner-sharing, forming channels in which dimers of edge-sharing [MnO(4)(OH)] trigonal bipyramids (..m symmetry) are located. In contrast to the previous refinement from Weissenberg photographic data [Moore & Smyth (1968 ▶). Am. Mineral.53, 1841-1845], all non-H atoms were refined with anisotropic displacement param-eters and the H atom was located. The distance of the donor and acceptor O atoms involved in hydrogen bonding is in agreement with Raman spectroscopic data. Examination of the Raman spectra for arsenate minerals in the libethenite group reveals that the position of the peak originating from the O-H stretching vibration shifts to lower wavenumbers from eveite, to adamite, zincolivenite, and olivenite.
For background to eveite, see: Moore (1968 ▶); Moore & Smyth (1968 ▶); Hålenius & Westlund (1998 ▶). For other minerals of the libethenite group, see: Hawthorne (1976 ▶); Cordsen (1978 ▶); Toman (1978 ▶); Li et al. (2008 ▶). Correlations between O—H streching frequencies and O—H⋯O donor–acceptor distances were given by Libowitzky (1999 ▶).
Bruker APEXII CCD area-detector diffractometerAbsorption correction: multi-scan (SADABS; Sheldrick, 2005 ▶) T
min = 0.579, T
max = 0.6393315 measured reflections911 independent reflections849 reflections with I > 2σ(I)R
int = 0.015
Refinement
R[F
2 > 2σ(F
2)] = 0.021wR(F
2) = 0.055S = 1.09911 reflections49 parametersAll H-atom parameters refinedΔρmax = 1.28 e Å−3Δρmin = −1.15 e Å−3Data collection: APEX2 (Bruker, 2004 ▶); cell refinement: SAINT (Bruker, 2004 ▶); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008 ▶); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008 ▶); molecular graphics: XtalDraw (Downs & Hall-Wallace, 2003 ▶); software used to prepare material for publication: publCIF (Westrip, 2010 ▶).Crystal structure: contains datablock(s) I, global. DOI: 10.1107/S1600536811044266/wm2546sup1.cifStructure factors: contains datablock(s) I. DOI: 10.1107/S1600536811044266/wm2546Isup2.hklAdditional supplementary materials: crystallographic information; 3D view; checkCIF report
Primary atom site location: structure-invariant direct methods
Extinction coefficient: 0.0034 (7)
Geometry. All e.s.d.'s (except the e.s.d. in the dihedral angle between two l.s. planes)
are estimated using the full covariance matrix. The cell e.s.d.'s are taken
into account individually in the estimation of e.s.d.'s in distances, angles
and torsion angles; correlations between e.s.d.'s in cell parameters are only
used when they are defined by crystal symmetry. An approximate (isotropic)
treatment of cell e.s.d.'s is used for estimating e.s.d.'s involving l.s.
planes.
Refinement. Refinement of F2 against ALL reflections. The weighted R-factor
wR and goodness of fit S are based on F2, conventional
R-factors R are based on F, with F set to zero for
negative F2. The threshold expression of F2 >
σ(F2) is used only for calculating R-factors(gt) etc.
and is not relevant to the choice of reflections for refinement.
R-factors based on F2 are statistically about twice as large
as those based on F, and R- factors based on ALL data will be
even larger.
Authors: Gordon W Downs; Betty N Yang; Richard M Thompson; Michelle D Wenz; Marcelo B Andrade Journal: Acta Crystallogr Sect E Struct Rep Online Date: 2012-10-27