Single crystals of Fe1.59Zn1.41B7O13Br were grown by a chemical vapour
transport technique, commonly called the three-crucibles method, reported by
Schmid (1965). Growth takes place in a closed quartz ampoule. Chemical
transport reactions were carried out by heating the ampoule at about 1173 K in
a resistance-heated vertical furnace, with gradients of 850 K (above) and 650 K (below), over a period of 72 h. The reactants were placed in the following
order: 1.7 g of B2O3 (which was obtained by dehydrating H3BO3) was
placed in the first crucible; 0.5 g of each one of both metal oxides (ZnO and
FeO) in the second crucible; and 0.8 g of each one of both divalent metal
halides (FeCl2 and ZnCl2) in the third crucible. Crystals of
Fe1.59Zn1.41B7O13Br as large as 2 mm in size were commonly obtained.
X-ray Fluorescence (XRF) spectroscopy was used to estimate the Fe/Zn ratio. A
small crystallite was irradiated using the "SANDRA" system developed at
Instituto de Fisica, UNAM, equipped with a 75 W Mo X-ray tube (50 kV, 1.5 mA,
XTF5011 model from Oxford Instruments) and AmpTeK Si-Pin detector. The system
was calibrated using reference standard materials from NIST (SRM 2711).
The average percent atomic content with standard uncertainty for each element
in the sample were 53 (4) % for iron, and 47 (4) % for zinc, and give a Fe:Zn
ratio of 1.13. Then the stichiometric formula is
Fe1.59 (12)Zn1.41 (12)B7O13Br.
The characterization of powdered Fe1.59Zn1.41B7O13Br mixed boracite by
conventional X-ray powder diffraction data indicated the presence of a well
crystallized phase showing reflections that matched with the isostructural
phase trembathite, Mg1.56Fe1.44Mn0.02B7O13Cl (PDF 01–089-6198)
reported by Schindler & Hawthorne (1998). The starting structural
parameters
to perform a Rietveld refinement of the Fe1.59Zn1.41B7O13Br boracite
were taken from the isostructural data reported for Zn3B7O13Cl (ICSD
55444) by Mao et al. (1991). The following parameters were
refined:
zero point, scale factor, background parameters, unit cell dimensions,
half-width, pseudo-Voigt and asymmetry parameters for the peak shape; position
and thermal isotropic factors. For the case of boron, the thermal isotropic
factors were fixed to 0.24 Å2, which is a reasonable value for the boron
atom and for obtaining a good refinement. The occupation factors for Fe and Zn
atoms sharing the same position were fixed to the values of 0.53 and 0.47
respectively, obtained by a quantitative chemical analysis from X-ray
fluorescence (XRF) spectroscopy. Due to the very low scattering power of boron
atoms to the X-rays, one rigid body group (RBG) containing the boron atoms was
defined as ilustrated in figure 1. This RBG has its centre in O(1) atom. Then,
eight atoms define the complete RGB (including the centre) and are labelled as
B(1), B(2), B(3), O(1), O(2), O(3), O(4) and O(5). Each atom has their
spherical internal coordinates (dm, φm, θm) fixed
according to the rigid character of the RBG formed by these eight atoms. The
parameters χc, Θc, Φc, xo, yo, zo, that
were refined in a first step are represented in fig. 1 b, c and were limited
by the symmetry allowed movements for the RBG as a whole. At the end of this
step, B(1)O4, B(2)O4 tetrahedra, and B(3)O3 triangle kept their
interatomic angles and distances. In a second and final step of refinement the
spherical internal coordinates for B(3) and O(2) were refined in such a way to
allow to bring the B(3)O3 triangle closer to the O(1) atom. The RBG
subroutine has been included in the program FULLPROF (Rodriguez &
Rodriguez-Carvajal, 1997). The use of the RBG reduced significantly the
number
of positional parameters in the Rietveld refinement. The results of the
refinement are shown in figure 2.
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The new iron-zinc heptaborate bromine Fe1.59Zn1.41B7O13Br, belongs to the family of boracites with general formula Me3B7O13X, where Me could be a divalent ion and X a halogen. Boracites have attracted the attention of researchers since Häuy, who observed pyroelectricity in the mineral boracite Mg3B7O13Cl (Dana, 1951). Unusual physical properties can be cited for a given cations located in the crystalographic sites for Me and X. Depending on this, potential applications such as an optic stopper (Smart & Moore, 1992); ferroelectric non volatile memory (Mathews, et al., 1997); and infrared (IR) detection (Campa -Molina et al., 1994, 2002) have been reported and in some sense, can be modulated by the presence of some specific types of cations. The aim of this research was to synthesize a new boracite with Zn and Fe in the crystalographic sites for Me in the general formula, in order to stablish in first instance, its structural and crystal chemistry properties. They are needed for the understanding of its physical properties. The representation of the crystal structure of the Fe1.59Zn1.41B7O13Br mixed boracite appear in figure 3. Bond valence calculations were made using the recommended bond-valence parameters for oxides published by Brese & O'Keeffe (1991) and considering those coordination polyhedra whose bond valence calculations were based on distances and angles that were allowed to refine (this was partially true in some cases). Bond valence sum around Br is found to be 0.82 and 1.10, for BrZn6 and BrFe6 distorted octahedra respectively. The resulting average value is then 0.97 if a composition of 53% Fe and 47% Zn is considered for this site, which is almost equal to the expected value of 1 for Br. Around the Fe/Zn site, four O atoms and Br are coordinated. The bond valence sums that result here are 1.97 and 1.76 when the site is only occupyied by Fe and Zn respectively. The average value for 53% Fe and 47% Zn is then 1.87 with good proximity to the expected value of 2. For the B(3) atom, the contribution of the fourth oxygen atom O(1) to the bond valence sum obtained for the B(3)O3 triangle of 2.8 is increased to 2.86 (i.e. only 0.06 v. u. indicating the presence of a very weak bond in the right position for have a distorted tetrahedral coordination around the planar triangle coordination for the third boron atom B(3). This fact is also a feature for the reported boracites Fe3B7O13Cl (ICSD 60504, Mendoza-Alvarez et al., 1985), and Zn3B7O13Cl (ICSD 55444, Mao et al., 1991).