research communications
Crystal structures of deuterated sodium molybdate dihydrate and sodium tungstate dihydrate from time-of-flight neutron powder diffraction
aISIS Facility, Rutherford Appleton Laboratory, Harwell Science and Innovation Campus, Didcot, Oxfordshire OX11 0QX, England, bDepartment of Earth Sciences, University College London, Gower Street, London WC1E 6BT, England, and cDepartment of Earth and Planetary Sciences, Birkbeck, University of London, Malet Street, London WC1E 7HX, England
*Correspondence e-mail: andrew.fortes@ucl.ac.uk
Time-of-flight neutron powder diffraction data have been measured from ∼90 mol% deuterated isotopologues of Na2MoO4·2H2O and Na2WO4·2H2O at 295 K to a resolution of sin (θ)/λ = 0.77 Å−1. The use of neutrons has allowed of structural parameters with a precision that varies by a factor of two from the heaviest to the lightest atoms; this contrasts with the X-ray based refinements where precision may be > 20× poorer for O atoms in the presence of atoms such as Mo and W. The accuracy and precision of interatomic distances and angles are in excellent agreement with recent X-ray single-crystal structure refinements whilst also completing our view of the hydrogen-bond geometry to the same degree of statistical certainty. The two structures are isotypic, space-group Pbca, with all atoms occupying general positions, being comprised of edge- and corner-sharing NaO5 and NaO6 polyhedra that form layers parallel with (010) interleaved with planes of XO4 (X = Mo, W) tetrahedra that are linked by chains of water molecules along [100] and [001]. The complete structure is identical with the previously described molybdate [Capitelli et al. (2006). Asian J. Chem. 18, 2856–2860] but shows that the purported three-centred interaction involving one of the water molecules in the tungstate [Farrugia (2007). Acta Cryst. E63, i142] is in fact an ordinary two-centred `linear' hydrogen bond.
1. Chemical context
Na2MoO4 and Na2WO4 are unusual amongst the alkali metal mono-molybdates and mono-tungstates in being highly soluble in water and forming polyhydrated crystals. Additionally, sodium apparently plays a significant role in the solvation of other alkali metal ions to form a range of double molybdate and tungstate hydrates (Klevtsova et al., 1990; Klevtsov et al., 1997; Mirzoev et al., 2010), for example, Na3K(MoO4)2·9H2O. Both dihydrate and decahydrate varieties of the two title compounds are known, their solubilities as a function of temperature being well characterised (Funk, 1900; Zhilova et al., 2008). The structures of the decahydrates have not yet been reported, although I have established that they are not isotypic with the sodium sulfate analogue, Na2SO4·10H2O, as had hitherto been thought.
The dihydrates have been the subject of extensive crystallographic studies, from descriptions of their density, habit and measurements of interfacial angles (Svanberg & Struve, 1848; Zenker, 1853; Rammelsberg, 1855; Marignac, 1863; Delafontaine, 1865; Ullik, 1867; Clarke, 1877; Zambonini, 1923), through to determination of absolute unit-cell parameters (Pistorius & Sharp, 1961), and subsequent solution and of their structures (Mitra & Verma, 1969; Okada et al., 1974; Matsumoto et al., 1975; Atovmyan & D'yachenko, 1969; Capitelli et al., 2006; Farrugia, 2007). However, the presence of heavy atoms in these materials makes it impossible to achieve a uniform precision on all structural parameters using X-rays, and even with single-crystal methods that purport to identify hydrogen positions there may be significant inaccuracies. Such problems are minimised using a neutron radiation probe since the coherent neutron scattering lengths of the constituent elements differ by less than a factor of two, being 6.715 fm for Mo, 4.86 fm for W, 3.63 fm for Na, 5.803 fm for O, and 6.67 fm for 2D (Sears, 1992). Thus one can locate accurately all of the light atoms and obtain a uniform level of precision on their coordinates and displacement parameters. Since the incoherent neutron scattering of 1H is large (80.3 barns) it is usual to prepare perdeuterated specimens whenever possible (the incoherent of 2D being only 2.1 barns) as this optimises the coherent Bragg scattering signal above the background, reducing the counting times required for a high-precision structure from many days to a matter of hours on the instrument used for these measurements. These data were therefore measured using Na2MoO4·2D2O and Na2WO4·2D2O samples.
The occurrence of polyhydrated forms of both Na2MoO4 and Na2WO4 suggests that both would be excellent candidates for the formation of hydrogen-bonded complexes with water-soluble organics, such as amino acids, producing metal-organic crystals with potentially useful optical properties (cf., glycine lithium molybdate; Fleck et al., 2006). High-pressure polymorphs of Na2MoO4·2H2O and Na2WO4·2H2O are indicated from Raman scattering studies (Luz-Lima et al., 2010; Saraiva et al., 2013). Characterising the structures and properties of the title compounds provides an essential foundation on which to build future studies of the high-pressure phases, of the as-yet incomplete decahydrate structures and any related organic-bearing hydrates.
2. Structural commentary
Na2MoO4·2H2O and Na2WO4·2H2O are isotypic, crystallizing in the orthorhombic Pbca; all atoms occupy general positions (Wyckoff sites 8c). Note that the atom labelling scheme and space-group setting used here follows Farrugia (2007); consequently there are some differences with respect to other literature sources, although equivalent contacts are referred to in Table 1 and Table 2. The X6+ ions (X = Mo, W) are tetrahedrally coordinated by O2−, the Mo—O and W—O bond lengths varying slightly according to the type of coordination adopted by a particular apex: O1 and O4 are each coordinated to Na+ and each also accepts two hydrogen bonds; O2 is coordinated to three Na+ ions and O3 is coordinated to two Na+ ions (Fig. 1). In both title compounds, X–O1 and X–O4 are the longest contacts and X–O3 is the shortest contact in the tetrahedral oxyanion. The mean Mo—O and W—O bond lengths are in good agreement with those found in the anhydrous crystals (Fortes, 2015). Furthermore, each of the absolute Mo—O bond lengths are identical (within error) to those found by Capitelli et al. (2006); the agreement in W—O bond lengths with Farrugia (2007) is marginally poorer.
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The Na+ ions occupy two inequivalent sites: in one, Na+ is six-fold coordinated by two water molecules and four XO42− oxygen atoms, yielding an octahedral arrangement; in the second, Na+ is five-fold coordinated by two water molecules and three XO42− oxygen atoms, yielding a square-pyramidal arrangement. These two polyhedra share a common edge (O2–O5) and are connected, moreover, with their inversion-centre-related neighbours along three other shared edges to form a cluster (Fig. 2a). The clusters corner-share via O6 to create a `slab' parallel to (010) (Fig. 2b). The mean Na—O bond lengths are statistically identical in Na2MoO4·2D2O and Na2WO4·2D2O being ∼1.6% longer in the NaO6 octahedra and ∼2.3% shorter in the NaO5 polyhedra than Na—O bonds in the anhydrous crystals (Fortes, 2015). The agreement in Na—O bond lengths with the X-ray single crystal studies of Capitelli et al. (2006) and Farrugia (2007) is very good. Overall, the agreement in bond lengths and angles for the two independently refined data sets is excellent (Tables 1 and 2).
Although it is more usual to find Na+ in octahedral coordination, there are abundant examples of Na+ in five-fold coordination, including instances where the NaO5 polyhedron adopts a square-pyramidal arrangement (Beurskens & Jeffrey, 1961; Císařová; et al., 2001; Sharma et al., 2005; Smith & Wermuth, 2014; Aksenov et al., 2014) or the alternative trigonal-bipyramidal arrangement (Mereiter, 2013; Smith, 2013). A similar combination of NaO6 and NaO5 polyhedra to that found in the title compounds occurs in the closely-related hydrates Na2CrO4·1.5H2O and Na2SeO4·1.5H2O (Kahlenberg, 2012; Weil & Bonneau, 2014). The two water molecules form hydrogen-bonded chains between the O1 and O4 atoms of the tetrahedral oxyanions; O5-related chains extend along [001] and O6-related chains crosslink them in a staggered fashion along [100]. Fig. 3(a) and 3(b) depict the spatial relationship between this `net' of water linked tetrahedra and the adjacent `slab' of corner-linked Na—O polyhedral clusters. The layers shown in Fig. 3(b) alternate to create the three-dimensional structure and are no doubt responsible for the macro-scale platy habit of the crystals.
There are no significant differences in the hydrogen bond geometries of the molybdate or tungstate crystals. The most recent X-ray single-crystal diffraction study of Na2WO4·2H2O (Farrugia, 2007) implied that one of the water molecules (O5) was involved in a weaker three-centred interaction, although a similarly recent measurement of Na2MoO4·2H2O (Capitelli et al., 2006) identified a `normal' linear two-centred interaction for this bond. This work, using neutrons, has been able to accurately and precisely characterise the hydrogen bond geometry, showing that the latter is true for both structures; there is no bifurcated bond and all hydrogen-bonded interactions are of the linear two-centred variety. Presumably the error in Farrugia's analysis arose due to the substantial absorption correction required (μ = 18.7 mm−1) for an accurate structure from X-ray single-crystal data.
Raman spectra of Na2MoO4·2H2O and Na2MoO4·2D2O were first reported by Mahadevan Pillai et al. (1997); subsequently, Luz-Lima et al. (2010) and Saraiva et al. (2013) published the Raman spectra of Na2MoO4·2H2O and Na2WO4·2H2O as a function of temperature (13–300 K) and as a function of hydrostatic pressure (to 5 GPa). Both compounds exhibit evidence of a `conformational change' on cooling through 120 K: the molybdate appears to undergo two high-pressure phase transitions, one at 3 GPa and the second at 4 GPa; the tungstate apparently undergoes a high-pressure at 3.9 GPa. The Raman spectra reported here (Figs. 4 and 5 and Supporting information) agree well with data in the literature (Table 3). The large blue-shifts in the internal vibrational frequencies of the deuterated water molecule are similar to the square root of the D:H mass ratio; the small blue-shifts of most of the internal modes of the tetrahedral oxyanions are consistent with stronger hydrogen bonding in the deuterated species, as expected (cf. Scheiner & Čuma, 1996; Soper & Benmore, 2008).
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3. Synthesis and crystallization
Coarse polycrystalline powders of Na2MoO4·2H2O (Sigma–Aldrich M1003 > 99.5%) and Na2WO4·2H2O (Sigma–Aldrich 14304 > 99%) were dehydrated by drying at 673 K in air. The resulting anhydrous materials were characterised by Raman spectroscopy, X-ray and neutron powder diffraction (Fortes, 2015). This material was dissolved in D2O (Aldrich 151882, 99.9 atom% D) and twice recrystallized by gentle evaporation at 323 K. The molybdate crystallised with a coarse platy habit whereas the tungstate was deposited as a finer-grained material. Once the supernatant liquid was decanted, the residue was air dried on filter paper and then ground to a fine powder with an agate pestle and mortar. The powders were loaded into standard vanadium sample-holder tubes of internal diameter 11 mm to a depth not less than 20 mm (this being the vertical neutron beam dimension at the sample position). Accurate volumes and masses were determined after the diffraction measurements were complete and used to correct the data for self-shielding. The level of deuteration was determined by Raman spectroscopy (see below) to be ∼91% for both compounds.
Raman spectra were acquired with a B&WTek i-Raman plus portable spectrometer; this device uses a 532 nm laser (37 mW power at the fiber-optic probe tip) to stimulate Raman scattering, which is measured in the range 170–4000 cm−1 with a spectral resolution of 3 cm−1. Data were collected for 600 sec at 17 mW for Na2MoO4·2H2O (as bought), 180 sec at 37 mW for Na2MoO4·2D2O, 300 sec at 17 mW for Na2WO4·2H2O (as bought) and 220 sec at 37 mW for Na2WO4·2D2O; after summation, the background was removed and peaks fitted using Pseudo-Voigt functions in OriginPro (OriginLab, Northampton MA). These data are provided as an electronic supplement in the form of an ASCII file. Small quantities of ordinary hydrogen were found to be present in both specimens, the proportion being determined by the ratio of the areas under the ν1/ν3 (H2O) bands after normalisation relative to the height of the strong ν1 (XO42−) band. The molar abundance of 1H was used to correct the diffraction data for absorption (see below) and to ensure accurate of the structure (see Refinement).
Time-of-flight neutron diffraction patterns were collected at 295 K using the High Resolution Powder Diffractometer, HRPD (Ibberson, 2009), at the ISIS spallation neutron source, Harwell Campus, Oxfordshire, UK. Data were acquired in the range of neutron flight times from 30–130 msec (equivalent to neutron wavelengths of 1.24–5.36 Å) for 15.17 hr from the molybdate and 14.40 hr from the tungstate, equivalent to 615 and 590 µAhr of integrated proton beam current, respectively. These data sets were normalized to the incident spectrum and corrected for detector efficiency by reference to a V:Nb null-scattering standard and then subsequently corrected for the sample-specific and wavelength-dependent self-shielding using Mantid (Arnold et al., 2014: Mantid, 2013). In the case of the molybdate, the of the specimen was determined to be 3.28 mol nm−3, with a scattering allowing for the water being 9.1 mol % 1H, σscatt = 93.81 b and an absorption σabs = 3.66 b; for the tungstate, the was 3.01 mol nm−3, the scattering allowing for the water being 8.6 mol % 1H, σscatt = 94.19 b and σabs = 19.48 b. Diffraction data were exported in GSAS format and analysed with the GSAS/Expgui Rietveld package (Larsen & Von Dreele, 2000: Toby, 2001). The fitted diffraction data are shown in Figs. 6 and 7.
4. Refinement
Profile refinements were done using GSAS/Expgui (Larsen & Von Dreele, 2000; Toby, 2001) starting from the coordinates reported by Farrugia (2007). Statistically significant anisotropic displacement parameters were refined for all atoms. An assumption was made that 1H was uniformly distributed on all 2D sites, so the neutron scattering length of 2D was edited in GSAS in accordance with the concentration of 1H determined by Raman spectroscopy; for the molybdate a value of 5.776 fm was used, and for the tungstate a value of 5.724 fm was adopted. Crystal data, data collection and structure details are summarized in Table 4.
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Supporting information
10.1107/S2056989015011354/wm5172sup1.cif
contains datablocks Na2MoO4.2D2O, Na2WO4.2D2O, New_Global_Publ_Block. DOI:Rietveld powder data: contains datablock Na2MoO4.2D2O. DOI: 10.1107/S2056989015011354/wm5172Na2MoO4.2D2Osup2.rtv
Rietveld powder data: contains datablock Na2WO4.2D2O. DOI: 10.1107/S2056989015011354/wm5172Na2WO4.2D2Osup3.rtv
Na2MoO4 and Na2WO4 are unusual amongst the alkali metal mono-molybdates and mono-tungstates in being highly soluble in water and forming polyhydrated crystals. Additionally, sodium apparently plays a significant role in the solvation of other alkali metal ions to form a range of double molybdate and tungstate hydrates (Klevtsova et al., 1990; Klevtsov et al., 1997; Mirzoev et al., 2010), for example, Na3K(MoO4)2·9H2O. Both dihydrate and decahydrate varieties of the two title compounds are known, their solubilities as a function of temperature being well characterised (Funk, 1900; Zhilova et al., 2008). The structures of the decahydrates have not yet been reported, although I have established that they are not isotypic with the sodium sulfate analogue, Na2SO4·10H2O, as had hitherto been thought.
The dihydrates have been the subject of extensive crystallographic studies, from descriptions of their density, habit and measurements of interfacial angles (Svanberg & Struve, 1848; Zenker, 1853; Rammelsberg, 1855; Marignac, 1863; Delafontaine, 1865; Ullik, 1867; Clarke, 1877; Zambonini, 1923), through to determination of absolute unit-cell parameters (Pistorius & Sharp, 1961), and subsequent solution and
of their structures (Mitra & Verma, 1969; Okada et al., 1974; Matsumoto et al., 1975; Atovmyan & D'yachenko, 1969; Capitelli et al., 2006; Farrugia, 2007). However, the presence of heavy atoms in these materials makes it impossible to achieve a uniform precision on all structural parameters using X-rays, and even with single-crystal methods that purport to identify hydrogen positions there may be significant inaccuracies. Such problems are minimised using a neutron radiation probe since the coherent neutron scattering lengths of the constituent elements differ by less than a factor of two, being 6.715 fm for Mo, 4.86 fm for W, 3.63 fm for Na, 5.803 fm for O, and 6.67 fm for 2D (Sears, 1992). Thus one can locate accurately all of the light atoms and obtain a uniform level of precision on their coordinates and displacement parameters. Since the incoherent neutron scattering of 1H is large (80.3 barns) it is usual to prepare perdeuterated specimens whenever possible (the incoherent of 2D being only 2.1 barns) since this optimises the coherent Bragg scattering signal above the background, reducing the counting times required for a high-precision structure from many days to a matter of hours on the instrument used for these measurements. These data were therefore measured using Na2MoO4·2D2O and Na2WO4·2D2O samples.The occurrence of polyhydrated forms of both Na2MoO4 and Na2WO4 suggests that both would be excellent candidates for the formation of hydrogen-bonded complexes with water-soluble organics, such as amino acids, producing metal-organic crystals with potentially useful optical properties (cf., glycine lithium molybdate; Fleck et al., 2006). High-pressure polymorphs of Na2MoO4·2H2O and Na2WO4·2H2O are indicated from Raman scattering studies (Luz-Lima et al., 2010; Saraiva et al., 2013). Characterising the structures and properties of the title compounds provides an essential foundation on which to build future studies of the high-pressure phases, of the as-yet incomplete decahydrate structures and any related organic-bearing hydrates.
Na2MoO4·2H2O and Na2WO4·2H2O are isotypic, crystallizing in the orthorhombic
Pbca; all atoms occupy general positions (Wyckoff sites 8c). Note that the atom labelling scheme and space-group setting used here follows Farrugia (2007); consequently there are some differences with respect to other literature sources, although equivalent contacts are referred to in Table 1 and Table 2. The X6+ ions (X = Mo, W) are tetrahedrally coordinated by O2-, the Mo—O and W—O bond lengths varying slightly according to the type of coordination adopted by a particular apex: O1 and O4 are each coordinated to Na+ and each also accepts two hydrogen bonds; O2 is coordinated to three Na+ ions and O3 is coordinated to two Na+ ions (Fig. 1). In both title compounds, X–O1 and X–O4 are the longest contacts and X–O3 is the shortest contact in the tetrahedral oxyanion. The mean Mo—O and W—O bond lengths are in good agreement with those found in the anhydrous crystals (Fortes, 2015). Furthermore, each of the absolute Mo—O bond lengths are identical (within error) to those found by Capitelli et al. (2006); the agreement in W—O bond lengths with Farrugia (2007) is marginally poorer.The Na+ ions occupy two inequivalent sites: in one, Na+ is six-fold coordinated by two water molecules and four XO42- oxygen atoms, yielding an octahedral arrangement; in the second, Na+ is five-fold coordinated by two water molecules and three XO42- oxygen atoms, yielding a square-pyramidal arrangement. These two polyhedra share a common edge (O2–O5) and are connected, moreover, with their inversion-centre-related neighbours along three other shared edges to form a cluster (Fig. 2a). The clusters corner-share via O6 to create a `slab' parallel to (010) (Fig. 2b). The mean Na—O bond lengths are statistically identical in Na2MoO4·2D2O and Na2WO4·2D2O being ~1.6 % longer in the NaO6 octahedra and ~2.3 % shorter in the NaO5 polyhedra than Na—O bonds in the anhydrous crystals (Fortes, 2015). The agreement in Na—O bond lengths with the X-ray single crystal studies of Capitelli et al. (2006) and Farrugia (2007) is very good. Overall, the agreement in bond lengths and angles for the two independently refined data sets is excellent (Tables 1 and 2).
Although it is more usual to find Na+ in octahedral coordination, there are abundant examples of Na+ in five-fold coordination, including instances where the NaO5 polyhedron adopts a square-pyramidal arrangement (Beurskens & Jeffrey, 1961; Císarová et al., 2001; Sharma et al., 2005; Smith & Wermuth, 2014; Aksenov et al., 2014) or the alternative trigonal-bipyramidal arrangement (Mereiter, 2013; Smith, 2013). A similar combination of NaO6 and NaO5 polyhedra to that found in the title compounds occurs in the closely-related hydrates Na2CrO4·1.5H2O and Na2SeO4·1.5H2O (Kahlenberg, 2012; Weil & Bonneau, 2014). The two water molecules form hydrogen-bonded chains between the O1 and O4 atoms of the tetrahedral oxyanions; O5-related chains extend along [001] and O6-related chains crosslink them in a staggered fashion along [100]. Figs. 3(a) and 3(b) depict the spatial relationship between this `net' of water linked tetrahedra and the adjacent `slab' of corner-linked Na—O polyhedral clusters. The layers shown in Fig. 3(b) alternate to create the three-dimensional structure and are no doubt responsible for the macro-scale platy habit of the crystals.
There are no significant differences in the hydrogen bond geometries of the molybdate or tungstate crystals. The most recent X-ray single-crystal diffraction study of Na2WO4·2H2O (Farrugia, 2007) implied that one of the water molecules (O5) was involved in a weaker three-centred interaction, although a similarly recent measurement of Na2MoO4·2H2O (Capitelli et al., 2006) identified a 'normal' linear two-centred interaction for this bond. This work, using neutrons, has been able to accurately and precisely characterise the hydrogen bond geometry, showing that the latter is true for both structures; there is no bifurcated bond and all hydrogen-bonded interactions are of the linear two-centred variety. Presumably the error in Farrugia's analysis arose due to the substantial absorption correction required (µ = 18.7 mm-1) for an accurate structure
from X-ray single-crystal data.Raman spectra of Na2MoO4·2H2O and Na2MoO4·2D2O were first reported by Mahadevan Pillai et al. (1997); subsequently, Luz-Lima et al. (2010) and Saraiva et al. (2013) published the Raman spectra of Na2MoO4·2H2O and Na2WO4·2H2O as a function of temperature (13–300 K) and as a function of hydrostatic pressure (to 5 GPa). Both compounds exhibit evidence of a 'conformational change' on cooling through 120 K: the molybdate appears to undergo two high-pressure phase transitions, one at 3 GPa and the second at 4 GPa; the tungstate apparently undergoes a high-pressure
at 3.9 GPa. The Raman spectra reported here (Figs. 4 and 5 and Supporting information) agree well with data in the literature (Table 3). The large blue-shifts in the internal vibrational frequencies of the deuterated water molecule are similar to the square root of the D:H mass ratio; the small blue-shifts of most of the internal modes of the tetrahedral oxyanions are consistent with stronger hydrogen bonding in the deuterated species, as expected (cf. Scheiner & Čuma, 1996; Soper & Benmore, 2008).Coarse polycrystalline powders of Na2MoO4·2H2O (Sigma-Adrich M1003 > 99.5%) and Na2WO4·2H2O (Sigma-Adrich 14304 > 99%) were dehydrated by drying at 673 K in air. The resulting anhydrous materials were characterised by Raman spectroscopy, X-ray and neutron powder diffraction (Fortes, 2015). This material was dissolved in D2O (Aldrich 151882, 99.9 atom% D) and twice recrystallized by gentle evaporation at 323 K. The molybdate crystallised with a coarse platy habit whereas the tungstate was deposited as a finer-grained material. Once the supernatant liquid was decanted, the residue was air dried on filter paper and then ground to a fine powder with an agate pestle and mortar. The powders were loaded into standard vanadium sample-holder tubes of internal diameter 11 mm to a depth not less than 20 mm (this being the vertical neutron beam dimension at the sample position). Accurate volumes and masses were determined after the diffraction measurements were complete and used to correct the data for self-shielding. The level of deuteration was determined by Raman spectroscopy (see below) to be ~91% for both compounds.
Raman spectra were acquired with a B&WTek i-Raman plus portable spectrometer; this device uses a 532 nm laser (37 mW power at the fiber-optic probe tip) to stimulate Raman scattering, which is measured in the range 170–4000 cm-1 with a spectral resolution of 3 cm-1. Data were collected for 600 sec at 17 mW for Na2MoO4·2H2O (as bought), 180 sec at 37 mW for Na2MoO4·2D2O, 300 sec at 17 mW for Na2WO4·2H2O (as bought) and 220 sec at 37 mW for Na2WO4·2D2O; after summation, the background was removed and peaks fitted using Pseudo-Voigt functions in OriginPro (OriginLab, Northampton MA). These data are provided as an electronic supplement in the form of an ASCII file. Small quantities of ordinary hydrogen were found to be present in both specimens, the proportion being determined by the ratio of the areas under the ν1/ν3 (H2O) bands after normalisation relative to the height of the strong ν1 (XO42-) peak. The molar abundance of 1H was used to correct the diffraction data for absorption (see below) and to ensure accurate of the structure (see Refinement).
Time-of-flight neutron diffraction patterns were collected at 295 K using the High Resolution Powder Diffractometer, HRPD (Ibberson, 2009), at the ISIS spallation neutron source, Harwell Campus, Oxfordshire, U.K. Data were acquired in the range of neutron flight times from 30–130 msec (equivalent to neutron wavelengths of 1.24–5.36 Å) for 15.17 hr from the molybdate and 14.40 hr from the tungstate, equivalent to 615 and 590 µAhr of integrated proton beam current, respectively. These data sets were normalized to the incident spectrum and corrected for detector efficiency by reference to a V:Nb null-scattering standard and then subsequently corrected for the sample-specific and wavelength-dependent self-shielding using Mantid (Arnold et al., 2014: Mantid, 2013). In the case of the molybdate, the σscatt = 93.81 b and an absorption σabs = 3.66 b; for the tungstate, the was 3.01 mol nm-3, the scattering allowing for the water being 8.6 mol % 1H, σscatt = 94.19 b and σabs = 19.48 b. Diffraction data were exported in GSAS format and analysed with the GSAS/Expgui Rietveld package (Larsen & Von Dreele, 2000: Toby, 2001). The fitted diffraction data are shown in Figs. 6 and 7.
of the specimen was determined to be 3.28 mol nm-3, with a scattering allowing for the water being 9.1 mol % 1H,Profile refinements were done using GSAS/Expgui (Larsen & Von Dreele, 2000; Toby, 2001) starting from the coordinates reported by Farrugia (2007). Statistically significant anisotropic displacement parameters were refined for all atoms. An assumption was made that 1H was uniformly distributed on all 2D sites, so the neutron scattering length of 2D was edited in GSAS in accordance with the concentration of 1H determined by Raman spectroscopy; for the molybdate a value of 5.776 fm was used, and for the tungstate a value of 5.724 fm was adopted. Crystal data, data collection and structure
details are summarized in Table 4.For both compounds, data collection: HRPD control software; cell
GSAS/Expgui (Larsen & Von Dreele, 2000: Toby, 2001); data reduction: Mantid (Arnold et al., 2014: Mantid, 2013); program(s) used to solve structure: n/a; program(s) used to refine structure: GSAS/Expgui (Larsen & Von Dreele, 2000: Toby, 2001); molecular graphics: DIAMOND (Putz & Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).Fig. 1. First and second coordination shell of Mo6+/W6+ in the title compounds, revealing differences in the environment of each apical O2- that are responsible for the variations in Mo–O and W–O bond lengths. Anisotropic displacement ellipsoids are drawn at the 50% probability level. [Symmetry codes: (i) 1 - x, 1 - y, 1 - z; (ii) 1/2 + x, 1.5 - y, 1 - z; (iii) -1/2 + x, 1.5 - y, 1 - z; (iv) 1/2 - x, 1/2 + y, z; (v) 1.5 - x, 1/2 + y, z; (vi) 1 - x, 1/2 + y, 1.5 - z.] | |
Fig. 2. (a) Arrangement of NaOx polyhedra into edge-sharing clusters comprised of two Na1O6 octahedra and two Na2O5 square pyramids; (b) Arrangement of the clusters shown in (a) by corner sharing to form `slabs' parallel (010). Ellipsoids are drawn at the 50% probability level. [Symmetry codes: (i) 1 - x, 1 - y, 1 - z; (ii) 1/2 + x, 1.5 - y, 1 - z; (iii) -1/2 + x, 1.5 - y, 1 - z; (iv) 0.5 - x, -1/2 + y, z; (v) 1/2 + x, y, 1.5 - z; (vi) 0.5 - x, 1 - y, 1/2 + z; (vii) 1.5 - x, -1/2 + y, z.] | |
Fig. 3. (a) View down the b axis of the network of water-linked tetrahedral oxyanions; chains linked by O5 extend along [001] whereas crosslinkages through O6 are staggered along [100]. (b) View of the same structure along the c axis. Ellipsoids are drawn at the 50% probability level. [Symmetry codes: (i) 1 - x, 1 - y, 1 - z; (ii) 1 - x, 1/2 + y, 1.5 - z; (iii) 1/2 + x, 1.5 - y, 1 - z; (iv) 1/2 + x, y, 1.5 - z; (v) x, 1.5 - y, -1/2 + z; (vi) x, 1.5 - y, 1/2 + z.] | |
Fig. 4. Raman spectra of Na2MoO4·2H2O and Na2MoO4·2H2O in the range 200–3900 cm-1. Band positions and vibrational assignments are indicated (see also Table 4). Vertical scales show intensities relative to ν1 (XO42-). | |
Fig. 5. Raman spectra of Na2WO4·2H2O and Na2WO4·2H2O in the range 200–3900 cm-1. Band positions and vibrational assignments are indicated (see also Table 4). Vertical scales show intensities relative to ν1 (XO42-). | |
Fig. 6. Neutron powder diffraction data for Na2MoO4·2H2O; red points are the observations, the green line is the calculated profile and the pink line beneath the diffraction pattern represents Obs-Calc. Vertical black tick marks report the expected positions of the Bragg peaks. The inset shows the data measured at short flight times (i.e. small d-spacings). | |
Fig. 7. Neutron powder diffraction data for Na2WO4·2H2O; red points are the observations, the green line is the calculated profile and the pink line beneath the diffraction pattern represents Obs–Calc. Vertical black tick marks report the expected positions of the Bragg peaks. The inset shows the data measured at short flight times (i.e. small d-spacings). |
Na2MoO4·2D2O | Dx = 2.636 Mg m−3 |
Mr = 245.99 | Melting point: 353 K |
Orthorhombic, Pbca | Neutron radiation |
Hall symbol: -P 2ac 2ab | µ = 0.03+ 0.0007 * λ mm−1 |
a = 8.482961 (14) Å | T = 295 K |
b = 10.566170 (17) Å | white |
c = 13.83195 (3) Å | cylinder, 38 × 11 mm |
V = 1239.79 (1) Å3 | Specimen preparation: Prepared at 323 K and 100 kPa |
Z = 8 |
HRPD, High resolution neutron powder diffractometer | Absorption correction: analytical Data were corrected for self shielding using σscatt = 93.812 barns and σab(λ) = 3.657 barns at 1.798 Å during the normalisation procedure. The is wavelength dependent and is calculated as: µ = 0.0308 + 0.0007 * λ [mm-1] |
Radiation source: ISIS Facility, Neutron spallation source | Tmin = 0.685, Tmax = 0.706 |
Specimen mounting: vanadium tube | 2θfixed = 168.329 |
Data collection mode: transmission | Distance from source to specimen: 95000 mm |
Scan method: time of flight | Distance from specimen to detector: 965 mm |
Least-squares matrix: full | Excluded region(s): none |
Rp = 0.013 | Profile function: TOF profile function #3 (21 terms). Profile coefficients for exp pseudovoigt convolution [Von Dreele, 1990 (unpublished)] (α) = 0.1414, (β0) = 0.026250, (β1) = 0.004690, (σ0) = 0, (σ1) = 194.5, (σ2) = 13.5, (γ0) = 0, (γ1) = 0, (γ2) = 0, (γ2s) = 0, (γ1e) = 0, (γ2e) = 0, (εi) = 0, (εa) = 0, (εA) = 0, (γ11) = 0.057, (γ22) = 0, (γ33) = 0.059, (γ12) = -0.087, (γ13) = -0.014, (γ23) = -0.018. Peak tails ignored where intensity <0.0010x peak. Aniso. broadening axis 0.0 0.0 1.0 |
Rwp = 0.013 | 133 parameters |
Rexp = 0.007 | 0 restraints |
R(F2) = 0.05255 | 0 constraints |
χ2 = 3.534 | (Δ/σ)max = 0.03 |
4610 data points | Background function: GSAS Background function number 1 with 12 terms. Shifted Chebyshev function of 1st kind 1: 4.30598, 2: 1.54022, 3: -0.237828 4: -6.992080x10-2, 5: -0.113274, 6: -1.736560x10-2, 7: -1.996810x10-2, 8: 2.118030x10-5, 9: -4.698340x10-3, 10: -2.646770x10-2, 11: 2.772870x10-2, 12: -1.690170x10-3 |
Na2MoO4·2D2O | V = 1239.79 (1) Å3 |
Mr = 245.99 | Z = 8 |
Orthorhombic, Pbca | Neutron radiation |
a = 8.482961 (14) Å | µ = 0.03+ 0.0007 * λ mm−1 |
b = 10.566170 (17) Å | T = 295 K |
c = 13.83195 (3) Å | cylinder, 38 × 11 mm |
HRPD, High resolution neutron powder diffractometer | Tmin = 0.685, Tmax = 0.706 |
Specimen mounting: vanadium tube | 2θfixed = 168.329 |
Data collection mode: transmission | Distance from source to specimen: 95000 mm |
Scan method: time of flight | Distance from specimen to detector: 965 mm |
Absorption correction: analytical Data were corrected for self shielding using σscatt = 93.812 barns and σab(λ) = 3.657 barns at 1.798 Å during the normalisation procedure. The is wavelength dependent and is calculated as: µ = 0.0308 + 0.0007 * λ [mm-1] |
Rp = 0.013 | χ2 = 3.534 |
Rwp = 0.013 | 4610 data points |
Rexp = 0.007 | 133 parameters |
R(F2) = 0.05255 | 0 restraints |
x | y | z | Uiso*/Ueq | ||
Mo1 | 0.51477 (10) | 0.80193 (8) | 0.52313 (8) | 0.01137 | |
Na1 | 0.3438 (3) | 0.4964 (2) | 0.58515 (17) | 0.02371 | |
Na2 | 0.7433 (2) | 0.5509 (2) | 0.64802 (16) | 0.0216 | |
O1 | 0.45103 (15) | 0.82353 (12) | 0.40216 (9) | 0.01917 | |
O2 | 0.55667 (15) | 0.64011 (10) | 0.54111 (10) | 0.01665 | |
O3 | 0.68676 (15) | 0.89087 (11) | 0.53936 (11) | 0.02282 | |
O4 | 0.37187 (15) | 0.85121 (12) | 0.60907 (10) | 0.0194 | |
O5 | 0.53793 (19) | 0.40846 (16) | 0.70077 (14) | 0.0252 | |
O6 | 0.2281 (2) | 0.64176 (17) | 0.70081 (11) | 0.02505 | |
D51 | 0.5576 (2) | 0.32908 (18) | 0.66668 (13) | 0.03656 | |
D52 | 0.5585 (2) | 0.39149 (15) | 0.76825 (14) | 0.03068 | |
D61 | 0.1235 (2) | 0.64696 (14) | 0.67235 (12) | 0.03034 | |
D62 | 0.27890 (19) | 0.71840 (16) | 0.67765 (12) | 0.03232 |
U11 | U22 | U33 | U12 | U13 | U23 | |
Mo1 | 0.0103 (6) | 0.0083 (5) | 0.0156 (6) | 0.0001 (4) | 0.0009 (5) | 0.0003 (5) |
Na1 | 0.0249 (13) | 0.0213 (11) | 0.0250 (15) | −0.0011 (10) | 0.0026 (10) | 0.0012 (9) |
Na2 | 0.0196 (12) | 0.0180 (12) | 0.0272 (14) | −0.0037 (9) | 0.0008 (9) | −0.0006 (10) |
O1 | 0.0188 (7) | 0.0191 (7) | 0.0196 (8) | 0.0025 (6) | 0.0004 (6) | 0.0017 (6) |
O2 | 0.0161 (6) | 0.0086 (6) | 0.0252 (8) | −0.0008 (6) | −0.0019 (6) | 0.0017 (6) |
O3 | 0.0197 (7) | 0.0199 (7) | 0.0289 (9) | −0.0079 (6) | −0.0020 (6) | −0.0022 (7) |
O4 | 0.0187 (6) | 0.0163 (6) | 0.0233 (8) | 0.0040 (6) | 0.0050 (6) | −0.0011 (6) |
O5 | 0.0272 (9) | 0.0207 (9) | 0.0277 (10) | −0.0006 (7) | −0.0036 (8) | 0.0001 (8) |
O6 | 0.0264 (9) | 0.0257 (9) | 0.0231 (10) | −0.0018 (8) | −0.0031 (7) | 0.0060 (7) |
D51 | 0.0432 (11) | 0.0272 (9) | 0.0393 (11) | 0.0030 (8) | −0.0107 (9) | −0.0006 (9) |
D52 | 0.0399 (9) | 0.0292 (8) | 0.0229 (8) | 0.0008 (8) | −0.0003 (8) | 0.0027 (8) |
D61 | 0.0233 (9) | 0.0340 (9) | 0.0337 (9) | 0.0004 (7) | −0.0062 (8) | 0.0030 (8) |
D62 | 0.0338 (10) | 0.0248 (8) | 0.0384 (12) | −0.0056 (8) | −0.0024 (8) | 0.0028 (8) |
Mo1—O1 | 1.7732 (17) | Na2—O3v | 2.339 (3) |
Mo1—O2 | 1.7640 (14) | Na2—O5 | 2.415 (3) |
Mo1—O3 | 1.7499 (16) | Na2—O6vi | 2.305 (3) |
Mo1—O4 | 1.7759 (17) | O5—D51 | 0.9766 (19) |
Na1—O2 | 2.437 (3) | O5—D52 | 0.9664 (18) |
Na1—O2i | 2.417 (3) | O6—D61 | 0.9722 (16) |
Na1—O3ii | 2.482 (3) | O6—D62 | 0.9719 (18) |
Na1—O4iii | 2.410 (3) | D51—O1i | 1.874 (2) |
Na1—O5 | 2.476 (2) | D52—O4vii | 1.846 (3) |
Na1—O6 | 2.426 (3) | D61—O1ii | 1.816 (2) |
Na2—O1iv | 2.312 (3) | D62—O4 | 1.868 (3) |
Na2—O2 | 2.363 (3) | ||
O1—Mo1—O2 | 108.62 (8) | O2i—Na1—O6 | 174.75 (13) |
O1—Mo1—O3 | 107.83 (8) | O4iii—Na1—O5 | 100.22 (10) |
O1—Mo1—O4 | 112.69 (8) | O4iii—Na1—O6 | 90.30 (9) |
O2—Mo1—O3 | 109.54 (7) | O5—Na1—O6 | 94.63 (10) |
O2—Mo1—O4 | 109.11 (8) | O1iv—Na2—O2 | 95.39 (9) |
O3—Mo1—O4 | 109.01 (8) | O1iv—Na2—O3v | 91.65 (9) |
O2—Na1—O2i | 86.12 (8) | O1iv—Na2—O5 | 176.34 (12) |
O2—Na1—O3ii | 85.70 (9) | O1iv—Na2—O6vi | 94.37 (9) |
O2—Na1—O4iii | 173.42 (12) | O2—Na2—O3v | 93.22 (9) |
O2—Na1—O5 | 84.40 (9) | O2—Na2—O5 | 87.38 (8) |
O2—Na1—O6 | 94.02 (10) | O2—Na2—O6vi | 111.35 (10) |
O3ii—Na1—O2i | 88.43 (9) | O3v—Na2—O5 | 85.79 (9) |
O3ii—Na1—O4iii | 89.62 (9) | O3v—Na2—O6vi | 153.97 (12) |
O3ii—Na1—O5 | 170.10 (11) | O5—Na2—O6vi | 86.84 (10) |
O3ii—Na1—O6 | 86.35 (9) | D51—O5—D52 | 106.0 (2) |
O2i—Na1—O4iii | 89.13 (9) | D61—O6—D62 | 103.0 (2) |
O2i—Na1—O5 | 90.61 (10) |
Symmetry codes: (i) −x+1, −y+1, −z+1; (ii) x−1/2, −y+3/2, −z+1; (iii) −x+1/2, y−1/2, z; (iv) x+1/2, −y+3/2, −z+1; (v) −x+3/2, y−1/2, z; (vi) x+1/2, y, −z+3/2; (vii) −x+1, y−1/2, −z+3/2. |
Na2WO4·2D2O | Dx = 3.562 Mg m−3 |
Mr = 333.87 | Melting point: 373 K |
Orthorhombic, Pbca | Neutron radiation |
Hall symbol: -P 2ac 2ab | µ = 0.03+ 0.0033 * λ mm−1 |
a = 8.482514 (15) Å | T = 295 K |
b = 10.595156 (19) Å | white |
c = 13.85640 (3) Å | cylinder, 50 × 11 mm |
V = 1245.32 (1) Å3 | Specimen preparation: Prepared at 323 K and 100 kPa |
Z = 8 |
HRPD, High resolution neutron powder diffractometer | Absorption correction: analytical Data were corrected for self shielding using σscatt = 94.190 barns and σab(λ) = 19.484 barns at 1.798 Å during the normalisation procedure. The is wavelength dependent and is calculated as: µ = 0.0284 + 0.0033 * λ [mm-1] |
Radiation source: ISIS Facility, Neutron spallation source | Tmin = 0.603, Tmax = 0.700 |
Specimen mounting: vanadium tube | 2θfixed = 168.329 |
Data collection mode: transmission | Distance from source to specimen: 95000 mm |
Scan method: time of flight | Distance from specimen to detector: 965 mm |
Least-squares matrix: full | Excluded region(s): none |
Rp = 0.014 | Profile function: TOF profile function #3 (21 terms). Profile coefficients for exp pseudovoigt convolution [Von Dreele, 1990 (unpublished)] (α) = 0.1414, (β0) = 0.026250, (β1) = 0.004690, (σ0) = 0, (σ1) = 322.9, (σ2) = 15.7, (γ0) = 0, (γ1) = 0, (γ2) = 0, (γ2s) = 0, (γ1e) = 0, (γ2e) = 0, (εi) = 0, (εa) = 0, (εA) = 0, (γ11) = 0.023, (γ22) = 0, (γ33) = 0.006, (γ12) = 0.050, (γ13) = 0.016, (γ23) = 0.017. Peak tails ignored where intensity <0.0010x peak. Aniso. broadening axis 0.0 0.0 1.0 |
Rwp = 0.013 | 133 parameters |
Rexp = 0.007 | 0 restraints |
R(F2) = 0.04597 | 0 constraints |
χ2 = 3.312 | (Δ/σ)max = 0.04 |
4610 data points | Background function: GSAS Background function number 1 with 12 terms. Shifted Chebyshev function of 1st kind 1: 3.91163, 2: 1.22805, 3: -0.206144, 4: -8.53351x10-2, 5: -9.966470x10-2, 6: -1.847470x10-2, 7: -1.38195x10-2, 8: 9.956170x10-4, 9: 4.49839x10-3, 10: -2.199010x10-2, 11: 2.57524x10-2, 12: -2.00574x10-3 |
Na2WO4·2D2O | V = 1245.32 (1) Å3 |
Mr = 333.87 | Z = 8 |
Orthorhombic, Pbca | Neutron radiation |
a = 8.482514 (15) Å | µ = 0.03+ 0.0033 * λ mm−1 |
b = 10.595156 (19) Å | T = 295 K |
c = 13.85640 (3) Å | cylinder, 50 × 11 mm |
HRPD, High resolution neutron powder diffractometer | Tmin = 0.603, Tmax = 0.700 |
Specimen mounting: vanadium tube | 2θfixed = 168.329 |
Data collection mode: transmission | Distance from source to specimen: 95000 mm |
Scan method: time of flight | Distance from specimen to detector: 965 mm |
Absorption correction: analytical Data were corrected for self shielding using σscatt = 94.190 barns and σab(λ) = 19.484 barns at 1.798 Å during the normalisation procedure. The is wavelength dependent and is calculated as: µ = 0.0284 + 0.0033 * λ [mm-1] |
Rp = 0.014 | χ2 = 3.312 |
Rwp = 0.013 | 4610 data points |
Rexp = 0.007 | 133 parameters |
R(F2) = 0.04597 | 0 restraints |
x | y | z | Uiso*/Ueq | ||
W1 | 0.51352 (13) | 0.80186 (10) | 0.52310 (10) | 0.01206 | |
Na1 | 0.3444 (2) | 0.4957 (2) | 0.58501 (16) | 0.02213 | |
Na2 | 0.7422 (2) | 0.54966 (18) | 0.64745 (14) | 0.02166 | |
O1 | 0.44940 (14) | 0.82253 (11) | 0.40144 (8) | 0.01858 | |
O2 | 0.55647 (14) | 0.63936 (9) | 0.54135 (9) | 0.01675 | |
O3 | 0.68666 (14) | 0.89213 (10) | 0.53870 (10) | 0.02256 | |
O4 | 0.36916 (14) | 0.85058 (11) | 0.60895 (9) | 0.01972 | |
O5 | 0.53794 (17) | 0.40814 (14) | 0.70116 (12) | 0.02505 | |
O6 | 0.2276 (2) | 0.64134 (14) | 0.70148 (11) | 0.02531 | |
D51 | 0.5576 (2) | 0.32926 (17) | 0.66767 (12) | 0.03829 | |
D52 | 0.55912 (18) | 0.39189 (14) | 0.76800 (13) | 0.03325 | |
D61 | 0.1229 (2) | 0.64645 (13) | 0.67384 (10) | 0.03267 | |
D62 | 0.27774 (17) | 0.71764 (15) | 0.67874 (12) | 0.03524 |
U11 | U22 | U33 | U12 | U13 | U23 | |
W1 | 0.0099 (7) | 0.0064 (6) | 0.0199 (7) | −0.0002 (5) | 0.0009 (6) | 0.0002 (6) |
Na1 | 0.0209 (11) | 0.0167 (9) | 0.0289 (13 | 0.0004 (9) | 0.0028 (9) | 0.0003 (8) |
Na2 | 0.0192 (10) | 0.0183 (11) | 0.0275 (13) | 0.0001 (8) | −0.0006 (8) | 0.0000 (9) |
O1 | 0.0170 (6) | 0.0192 (6) | 0.0195 (7) | 0.0008 (5) | 0.0010 (6) | 0.0031 (5) |
O2 | 0.0176 (6) | 0.0079 (5) | 0.0248 (7) | 0.0014 (5) | −0.0004 (5) | 0.0035 (5) |
O3 | 0.0193 (7) | 0.0190 (6) | 0.0293 (8) | −0.0083 (5) | −0.0002 (6) | −0.0015 (6) |
O4 | 0.0201 (6) | 0.0176 (6) | 0.0214 (7) | 0.0045 (5) | 0.0052 (6) | 0.0008 (6) |
O5 | 0.0305 (9) | 0.0206 (9) | 0.0241 (8) | −0.0027 (7) | −0.0031 (7) | −0.0023 (7) |
O6 | 0.0246 (8) | 0.0247 (8) | 0.0266 (9) | −0.0004 (7) | −0.0046 (7) | 0.0061 (7) |
D51 | 0.0448 (10) | 0.0304 (9) | 0.0397 (9) | −0.0001 (8) | −0.0104 (8) | −0.0032 (8) |
D52 | 0.0415 (9) | 0.0323 (8) | 0.0259 (8) | −0.0027 (7) | −0.0001 (8) | 0.0004 (7) |
D61 | 0.0259 (9) | 0.0354 (9) | 0.0367 (9) | −0.0011 (7) | −0.0030 (7) | 0.0046 (8) |
D62 | 0.0347 (9) | 0.0270 (8) | 0.0440 (11) | −0.0059 (7) | −0.0029 (7) | 0.0059 (7) |
W1—O1 | 1.7849 (19) | Na2—O3v | 2.328 (2) |
W1—O2 | 1.7779 (15) | Na2—O5 | 2.409 (3) |
W1—O3 | 1.7659 (17) | Na2—O6vi | 2.311 (2) |
W1—O4 | 1.7834 (18) | O5—D51 | 0.9702 (18) |
Na1—O2 | 2.433 (2) | O5—D52 | 0.9591 (16) |
Na1—O2i | 2.412 (3) | O6—D61 | 0.9684 (16) |
Na1—O3ii | 2.479 (3) | O6—D62 | 0.9664 (16) |
Na1—O4iii | 2.399 (2) | D51—O1i | 1.873 (2) |
Na1—O5 | 2.479 (3) | D52—O4vii | 1.863 (2) |
Na1—O6 | 2.443 (3) | D61—O1ii | 1.834 (2) |
Na2—O1iv | 2.320 (2) | D62—O4 | 1.876 (2) |
Na2—O2 | 2.355 (2) | ||
O1—W1—O2 | 108.40 (9) | O2i—Na1—O6 | 174.55 (12) |
O1—W1—O3 | 107.61 (8) | O4iii—Na1—O5 | 99.82 (9) |
O1—W1—O4 | 112.66 (8) | O4iii—Na1—O6 | 90.40 (8) |
O2—W1—O3 | 109.67 (7) | O5—Na1—O6 | 94.37 (10) |
O2—W1—O4 | 109.03 (9) | O1iv—Na2—O2 | 95.10 (8) |
O3—W1—O4 | 109.43 (9) | O1iv—Na2—O3v | 91.90 (8) |
O2—Na1—O2i | 86.16 (7) | O1iv—Na2—O5 | 176.73 (11) |
O2—Na1—O3ii | 85.82 (8) | O1iv—Na2—O6vi | 93.43 (9) |
O2—Na1—O4iii | 173.55 (11) | O2—Na2—O3v | 93.36 (8) |
O2—Na1—O5 | 84.60 (8) | O2—Na2—O5 | 87.87 (7) |
O2—Na1—O6 | 93.95 (9) | O2—Na2—O6vi | 111.09 (9) |
O3ii—Na1—O2i | 88.32 (8) | O3v—Na2—O5 | 86.57 (8) |
O3ii—Na1—O4iii | 89.72 (8) | O3v—Na2—O6vi | 154.35 (11) |
O3ii—Na1—O5 | 170.42 (10) | O5—Na2—O6vi | 86.74 (9) |
O3ii—Na1—O6 | 86.26 (8) | D51—O5—D52 | 105.96 (19) |
O2i—Na1—O4iii | 89.05 (8) | D61—O6—D62 | 103.18 (19) |
O2i—Na1—O5 | 91.07 (9) |
Symmetry codes: (i) −x+1, −y+1, −z+1; (ii) x−1/2, −y+3/2, −z+1; (iii) −x+1/2, y−1/2, z; (iv) x+1/2, −y+3/2, −z+1; (v) −x+3/2, y−1/2, z; (vi) x+1/2, y, −z+3/2; (vii) −x+1, y−1/2, −z+3/2. |
Na2MoO4·2D2O | Na2MoO4·2H2O | Na2WO4·2D2O | Na2WO4·2H2O | |
This work | Capitelli et al. (2006) | This work | Farrugia (2007) | |
X—O1 | 1.773 (2) | 1.772 (1) | 1.785 (2) | 1.776 (3) |
X—O2 | 1.764 (1) | 1.767 (1) | 1.778 (2) | 1.778 (3) |
X—O3 | 1.750 (2) | 1.751 (1) | 1.766 (2) | 1.761 (3) |
X—O4 | 1.776 (2) | 1.778 (1) | 1.783 (2) | 1.787 (3) |
Mean X—O | 1.766 | 1.767 | 1.778 | 1.776 |
Na1—O2 | 2.437 (3) | 2.446 (2) | 2.433 (2) | 2.442 (3) |
Na1—O2(i) | 2.417 (3) | 2.419 (2) | 2.412 (3) | 2.416 (3) |
Na1—O3(ii) | 2.482 (3) | 2.481 (2) | 2.479 (3) | 2.480 (3) |
Na1—O4(iii) | 2.410 (3) | 2.395 (2) | 2.399 (2) | 2.388 (3) |
Na1—O5 | 2.476 (3) | 2.456 (2) | 2.479 (3) | 2.464 (4) |
Na1—O6 | 2.426 (3) | 2.423 (2) | 2.443 (3) | 2.433 (3) |
Mean Na1—O | 2.441 | 2.437 | 2.441 | 2.437 |
Na2—O1iv | 2.312 (3) | 2.319 (2) | 2.320 (2) | 2.323 (3) |
Na2—O2 | 2.363 (3) | 2.354 (2) | 2.355 (2) | 2.346 (3) |
Na2—O3v | 2.339 (3) | 2.341 (2) | 2.328 (2) | 2.331 (3) |
Na2—O5 | 2.415 (3) | 2.403 (2) | 2.409 (3) | 2.396 (3) |
Na2—O6vi | 2.305 (3) | 2.300 (2) | 2.311 (2) | 2.304 (3) |
Mean Na2—O | 2.347 | 2.343 | 2.345 | 2.340 |
Symmetry codes: (i) 1-x, 1-y, 1-z; (ii) -0.5+x, 1.5-y, 1-z; (iii) 0.5-x, -0.5+y, z; (iv) 0.5+x, 1.5-y, 1-z; (v) 1.5-x, -0.5+y, z; (vi) 0.5+x, y, 1.5-z. |
Na2MoO4·2D2O | Na2MoO4·2H2O | Na2WO4·2D2O | Na2WO4·2H2O | |
This work | Capitelli et al. (2006) | This work | Farrugia (2007) | |
O5—D51 | 0.977 (2) | 0.68 (3) | 0.970 (2) | 0.86 (3) |
O5—D52 | 0.966 (2) | 0.76 (3) | 0.959 (2) | 0.86 (3) |
D51—O5—D52 | 106.0 (2) | 98 (4) | 106.0 (2) | 100 (5) |
D51···O1(i) | 1.874 (2) | 2.16 (3) | 1.873 (2) | 2.09 (4) |
O5—D51···O1(i) | 167.9 (2) | 167 (4) | 168.2 (2) | 145 (6) |
D51···O3(ii) | – | – | – | 2.70 (6) |
O5—D51···O3(ii) | – | – | – | 122 (5) |
D52···O4(ii) | 1.846 (3) | 2.07 (3) | 1.863 (2) | 1.98 (3) |
O5—D52···O4(ii) | 171.2 (2) | 176 (3) | 170.9 (2) | 174 (6) |
O6—D61 | 0.972 (2) | 0.83 (3) | 0.968 (2) | 0.86 (3) |
O6—D62 | 0.972 (2) | 0.71 (3) | 0.966 (2) | 0.86 (3) |
D61—O6—D62 | 103.0 (2) | 105 (3) | 103.2 (2) | 95 (5) |
D61···O1 | 1.816 (2) | 2.01 (3) | 1.834 (2) | 1.95 (3) |
O6—D61···O1 | 167.0 (2) | 167 (3) | 167.0 (2) | 167 (6) |
D62···O4(iii) | 1.868 (4) | 2.08 (3) | 1.876 (2) | 2.02 (4) |
O6—D62···O4(iii) | 168.7 (2) | 170 (3) | 168.7 (2) | 159 (6) |
Symmetry codes: (i) 1-x, 1-y, 1-z; (ii) 1-x, -0.5+y, 1.5-z; (iii) -0.5+x, 1.5-y, 1-z. |
Na2MoO4·2H2O | Na2WO4·2H2O | |||||
This work (1H) | This work (2D) | Busey & Keller (1964) | This work (1H) | This work (2D) | Busey & Keller (1964) | |
ν2 (XO42-) | 279 | 271 | 285 | 276 | 269 | 276 |
319 | 315 | 325 | 324 | 321 | 325 | |
335 | 331 | 330 | 331 | |||
ν4 (XO42-) | 359 | 358 | 358 | 355 | ||
ν3 (XO42-) | 804 | 801 | 805 | 804 | 802 | 808 |
833 | 826 | 836 | 836 | 831 | 838 | |
842 | 840 | 843 | 840 | |||
ν1 (XO42-) | 891 | 889 | 893 | |||
894 | 894 | 897 | 929 | 928 | 931 |
Experimental details
(Na2MoO4.2D2O) | (Na2WO4.2D2O) | |
Crystal data | ||
Chemical formula | Na2MoO4·2D2O | Na2WO4·2D2O |
Mr | 245.99 | 333.87 |
Crystal system, space group | Orthorhombic, Pbca | Orthorhombic, Pbca |
Temperature (K) | 295 | 295 |
a, b, c (Å) | 8.482961 (14), 10.566170 (17), 13.83195 (3) | 8.482514 (15), 10.595156 (19), 13.85640 (3) |
V (Å3) | 1239.79 (1) | 1245.32 (1) |
Z | 8 | 8 |
Radiation type | Neutron | Neutron |
µ (mm−1) | 0.03+ 0.0007 * λ | 0.03+ 0.0033 * λ |
Specimen shape, size (mm) | Cylinder, 38 × 11 | Cylinder, 50 × 11 |
Data collection | ||
Diffractometer | HRPD, High resolution neutron powder diffractometer | HRPD, High resolution neutron powder diffractometer |
Specimen mounting | Vanadium tube | Vanadium tube |
Data collection mode | Transmission | Transmission |
Scan method | Time of flight | Time of flight |
Absorption correction | Analytical Data were corrected for self shielding using σscatt = 93.812 barns and σab(λ) = 3.657 barns at 1.798 Å during the normalisation procedure. The is wavelength dependent and is calculated as: µ = 0.0308 + 0.0007 * λ [mm-1] | – |
Tmin, Tmax | 0.685, 0.706 | – |
2θ values (°) | 2θfixed = 168.329 | 2θfixed = 168.329 |
Distance from source to specimen (mm) | 95000 | 95000 |
Distance from specimen to detector (mm) | 965 | 965 |
Refinement | ||
R factors and goodness of fit | Rp = 0.013, Rwp = 0.013, Rexp = 0.007, R(F2) = 0.05255, χ2 = 3.534 | Rp = 0.014, Rwp = 0.013, Rexp = 0.007, R(F2) = 0.04597, χ2 = 3.312 |
No. of data points | 4610 | 4610 |
No. of parameters | 133 | 133 |
Computer programs: HRPD control software, GSAS/Expgui (Larsen & Von Dreele, 2000: Toby, 2001), Mantid (Arnold et al., 2014: Mantid, 2013), n/a, DIAMOND (Putz & Brandenburg, 2006), publCIF (Westrip, 2010).
Acknowledgements
The author thanks the STFC ISIS facility for beam-time access and acknowledges financial support from STFC (grant No. ST/K000934/1).
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