Open Access Article
L. L.
Driscoll
*,
A. J.
Wright
and
P. R.
Slater
*
School of Chemistry, University of Birmingham, Edgbaston, Birmingham, West Midlands B15 2TT, UK. E-mail: p.r.slater@bham.ac.uk; l.l.driscoll@bham.ac.uk
First published on 11th September 2018
Alkali metal transition metal sulfates have attracted considerable interest as potential electrodes for Na ion battery materials. While there has been significant research on Fe based systems, research on V based systems has been lacking, apart from a recent report on Na2VO(SO4)2. This can be related to the complex synthetic routes previously reported to make sodium vanadium sulfate systems. In this paper, we report a simple route towards the synthesis of three such sodium vanadium sulfate systems, NaV(SO4)2, Na2VO(SO4)2, and Na3V(SO4)3. We analyse the resulting products through X-ray diffraction and Raman spectroscopy to highlight the formation of high quality samples via this simple solution route, with subsequent low temperature (<400 °C) heat treatment. This facile new route will allow these materials to be considered for future applications rather than as simply chemical curiosities.
22,23 and Na3V(PO3)3N.24 In contrast, there has been very little research on sodium vanadium sulfate systems, despite known examples such as NaV(SO4)2, Na3V(SO4)3, Na2VO(SO4)2.25–27
These sodium vanadium sulfate phases have previously attracted interest as they have been observed to form as a by-product of SO3 production. In this process, vanadium pentoxide, V2O5, is used as a catalyst in the following reaction:
| SO2(g) + ½O2(g) ↔ SO3(g). |
The alkali cation is added as a promoter for the process, and it has been found that the activity of the catalyst can be reduced due to the formation of A–V–S–O (where A = K or Na) phases when conducted below 400 °C.25–27 Beyond these initial reports related to their formation during the SO3 production process, only one paper has been published with regards to the properties of these materials, which can be attributed to the difficulty in synthesizing these phases under standard laboratory conditions.28 According to the previous literature on these materials, the only way to make these phases was to use a ‘mixing unit’ in which gases such as SO2, SO3, O2etc. were allowed to mix in a reactor.25–27 Moreover, in these syntheses, all the precursor materials needed to make these phases were handled in a nitrogen filled glove box, with some requiring additional pre-treatment before their use. The cells were heated up to 400–500 °C using a ratio Na2S2O7 and V2O5 under a controlled atmosphere of SO2/O2/N2 to produce a melt of the starting materials. Finally, after heating the melt overnight, the system is then washed with water to remove any leftover starting reagents.25–27 In most laboratories, repeating this synthesis would be difficult without constructing a specially designed piece of equipment for the synthesis to take place. A second issue is the amount of sample that can be made through this process. Only 1.5 ml of the melt can be added to the reactor due to fears of blocking the gas flow.
The potential applications of these systems is illustrated by recent work by Tarascon et al., which reported the successful operation of Na2VO(SO4)2 in a Na ion battery.28 In this work, the sample was synthesized by milling the precursor sulfates, Na2SO4 and α-VOSO4 (the latter, formed from the dehydration of VOSO4·xH2O, being a high cost reagent), before heating the sample in Ar at 400–415 °C for 12 h. The battery testing showed redox activity of 4.5 V vs. Na+/Na0 and a capacity of 60 mA h g−1.28
Consequently, considering the potential interest of these sodium vanadium sulfate systems for potential Na ion battery applications, we have investigated the development of a facile low cost synthetic method to eliminate the complexity of the previously established routes. The main difficulty with the synthesis of Na–V–S–O phases is the requirement to reduce the vanadium from VV to VIV/VIII. Although VIV and VIII precursors can be obtained commercially, they are expensive, and so we focused on developing a route using low cost V2O5. In particular, prior studies on the synthesis of VIIIPO4 have shown that such a phase can be formed using oxalic acid as a reducing agent, with the intermediate formation of VOC2O4.29 A modification of this route was therefore examined to prepare the sodium vanadium sulfate phases. In this paper, we demonstrate that this facile synthesis route is successful for the synthesis of NaV(SO4)2, Na2VO(SO4)2, and Na3V(SO4)3. We report a detailed characterisation of these phases utilising X-ray diffraction and Raman spectroscopy to demonstrate the high purity by this method.
Our method utilizes an initial solution processing approach which is advantageous for future applications due to ease in scalability, while also utilizing lower temperatures for the resultant final heat treatment. In addition, Na2VO(SO4)2, can be synthesized in air, while N2 is used for the final heat treatment to produce the VIII compounds Na3V(SO4)3 and NaV(SO4)2.
| V2O5 + 3H2C2O4·2H2O → 2VOC2O4 + 9H2O + 2CO2 |
The formation of a dark blue solution provides an initial indication that vanadium reduction has been successful. In order to form the desired Na–V–S–O phases, the following reaction schemes were applied with the stoichiometric ratios of (NH4)2SO4 and Na2SO4 added to the solution in the fume cupboard:
After the additions, the solutions were stirred on a hotplate for 4 hours at 70 °C. Once the mixing stage was complete, the solutions were then transferred to an oven and dried over night at 100–110 °C. The samples were then ground in an agate pestle and mortar before heating either in air (Na2VO(SO4)2) or under a nitrogen atmosphere (Na3V(SO4)3 and NaV(SO4)2). Thermogravimetric analysis studies were conducted using a Netzsch STA 449 F1 Jupiter thermogravimetric analyser coupled with a Netzsch 403 C mass spectrometer (heating rate of 0.5 °C min−1 under a nitrogen atmosphere) to help to determine the optimum temperature to heat the precipitate. The samples were heated in the range of 50–650 °C. The TGA results for the precipitate to form the Na3V(SO4)3 phase are displayed below in Fig. 1. All phases show a mass loss accompanied by the evolution of NH3, H2O and CO2 in between the temperature range of 225–425 °C. This provides an initial temperature range for the investigation of the formation of Na–V–S–O phases (see ESI† for TGA data for NaV(SO4)2 and Na2VO(SO4)2). The origin of the continued mass loss at higher temperature in all three Na–V–S–O systems relates to decomposition of the sulfates.
Following the temperature range suggested from the TGA experiments, the samples were heated between 250–400 °C at a rate of 0.5 °C min−1 for 1–12 hours, and the products analysed by X-ray diffraction using a Bruker D8 diffractometer (Cu Kα radiation) or a Bruker D2 phaser (Co Kα radiation) operating in reflection mode. Structural determination was performed using X-ray diffraction. Structure refinements were carried out using the GSAS suite of programs.30,31 Further characterisation of these systems was performed using Raman spectroscopy (Renishaw in Via Raman microscope equipped with a He–Ne 633 nm laser).
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| Fig. 2 XRD data for the precipitate of NaV(SO4)2 in the range of 250–400 °C (0.5 °C min−1/12 hours) under Nitrogen (Co Kα1/Kα2). | ||
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| Fig. 3 XRD data for the precipitate of Na2VO(SO4)2 in the range of 250–400 °C (0.5 °C min−1/4 hours) in air (Co Kα1/Kα2). | ||
As observed in the synthesis of NaV(SO4)2, an amorphous phase is observed up to 300 °C. Beyond 300 °C, phase pure Na2VO(SO4)2 is obtained at 350 °C (4 hours/0.5 °C min−1) in air, contrary to the reported need to use heat treatment in Ar to synthesise this phase by Tarascon et al.28
H
| Atom type | Site multiplicity | x | y | z | U iso × 100 (Å2) |
|---|---|---|---|---|---|
| Na1 | 18 | 0.7452(4) | 0.1095(5) | 0.4903(5) | 2.5(2) |
| V1 | 3 | 0 | 0 | 0 | 0.8(2) |
| V2 | 3 | 0 | 0 | 0.5 | 1.3(3) |
| S1 | 18 | −0.0246(5) | 0.1657(4) | 0.2595(5) | 3.2(1) |
| O1 | 18 | 0.0304(6) | 0.1374(6) | 0.375(1) | 1.7(3) |
| O2 | 18 | 0.8452(6) | 0.0981(6) | 0.2870(7) | 0.3(3) |
| O3 | 18 | 0.0238(9) | 0.2924(8) | 0.254(1) | 4.7(3) |
| O4 | 18 | 0.0037(7) | 0.1321(8) | 0.113(1) | 4.3(4) |
| Atom type | Site multiplicity | x | y | z | U iso × 100 (Å2) |
|---|---|---|---|---|---|
| Na1 | 2 | 0 | 0 | 0.5 | 3.2(2) |
| V1 | 2 | 0 | 0 | 0 | 1.08(9) |
| S1 | 4 | 0.3585(4) | 0 | 0.2172(4) | 2.8(1) |
| O1 | 4 | 0.2276(7) | 0 | 0.0608(8) | 4.4(2) |
| O2 | 4 | 0.2925(7) | 0 | 0.4145(8) | 4.3(2) |
| O3 | 8 | 0.4672(4) | 0.2306(6) | 0.2018(6) | 3.3(1) |
| Atom type | Site multiplicity | x | y | z | U iso × 100 (Å2) |
|---|---|---|---|---|---|
| Na1 | 4 | 0.665(2) | 0.147(2) | 0.596(1) | 4.4(4) |
| Na2 | 4 | 0.372(2) | 0.103(2) | 0.2397(8) | 4.6(4) |
| V1 | 4 | 0.533(1) | 0.147(1) | 0.9104(5) | 4.6(2) |
| S1 | 4 | 0.033(2) | 0.092(2) | 0.9283(7) | 5.2(3) |
| S2 | 4 | 0.861(1) | 0.100(2) | 0.2494(7) | 4.1(3) |
| O1 | 4 | 0.214(2) | 0.190(2) | 0.904(1) | 2.5(6) |
| O2 | 4 | 0.539(3) | 0.409(4) | 0.980(1) | 13.2(8) |
| O3 | 4 | 0.530(4) | 0.371(4) | 0.811(1) | 7.7(7) |
| O4 | 4 | 0.854(3) | 0.180(3) | 0.899(1) | 5.8(6) |
| O5 | 4 | 0.524(3) | −0.070(2) | 0.816(1) | 2.8(5) |
| O6 | 4 | 0.524(3) | −0.011(3) | 0.981(1) | 3.4(6) |
| O7 | 4 | 0.046(2) | −0.126(3) | 0.903(1) | 4.3(5) |
| O8 | 4 | 0.283(3) | −0.234(3) | 0.236(1) | 3.1(5) |
| O9 | 4 | −0.281(4) | −0.057(4) | 0.222(1) | 6.9(6) |
| Composition | a (Å) | b (Å) | c (Å) | α (°) | β (°) | γ (°) | Cell vol. (Å3) |
|---|---|---|---|---|---|---|---|
| NaV(SO4)2 | 8.0573(5) | 5.1544(3) | 7.1459(5) | 90 | 92.099 (4) | 90 | 296.57(4) |
| Na2VO(SO4)2 | 6.3107(1) | 6.8137(2) | 16.6932(4) | 90 | 90 | 90 | 717.80(4) |
| Na3V(SO4)3 | 13.4460(6) | 13.4460(6) | 9.0781(5) | 90 | 90 | 120 | 1421.4(2) |
The parameters of the materials obtained using the oxalic acid reduction route used in this work are in good agreement with those obtained through the original complex gas mixing method used by Fehrmann et al.,25–27 indicating the success of the facile new route reported here. In addition to XRD, the Raman spectra for each Na–V–S–O phase were collected to confirm the success of this novel route, the results of which yielded similar spectra to those published previously (see ESI – Fig. 3†). Two of the materials form 3-dimensional frameworks (Na3V(SO4)3 and Na2VO(SO4)2) while the third forms a 2-dimensional structure (NaV(SO4)2). Each system will be discussed in greater detail below.
Na3V(SO4)3 crystallizes in a hexagonal cell and the structure consists of corner sharing vanadium octahedra and sulfate tetrahedra. Each vanadium site is surrounded by six sulfate tetrahedra; three above and three below. This bonding is repeated to form the pillars that support the material in the direction of the c-axis (This creates a ‘windmill’ pattern when observed directly down the axis) (Fig. 7). The pillars do not bond directly with each other. Two oxygens in the sulfate tetrahedra are involved in their formation (O1 and O4) while the other two oxygens (O2 and O3) point towards the gap between parallel pillars, which is occupied by sodium. The sodium site is coordinated to seven oxygens.
The structure of Na2VO(SO4)2 also consists of corner sharing of octahedra and tetrahedra. In this system, five sulfate tetrahedra surround the octahedral site with the sixth site occupied by the oxygen which forms the vanadyl (V
O) bond. This bond is much shorter than the other V–O bonds and causes the vanadium site to show a distortion in this direction (Fig. 8). There are two crystallographically distinct sulfate sites in this material (Fig. 9). One of these sulfate sites bonds to three vanadium octahedra while the fourth S–O bond points towards the cavity which accommodates Na. This site will be defined as the terminal sulfate (S1). The second sulfate site acts as a bridge which bonds to two vanadium octahedra with two oxygens pointing in the direction of the cavity which accommodates the sodium. These sites will be defined as the bridging sulfate (S2). The material possesses two cavities for sodium to occupy; a rectangular shaped cavity (Na1) and a diamond shaped cavity (Na2) suggesting the possibility of a 3-dimensional ionic diffusion pathway, in line with the successful use of this materials in a Na ion battery.28 The coordination also varies across the sites; Na1 site is six coordinate, while the Na2 site is eight coordinate.
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| Fig. 8 (a) Crystal structure of Na2VO(SO4)2; (b) observed, calculated and difference XRD profiles for Na2VO(SO4)2 (Rwp – 5.17%, Rp – 3.65%) (Co Kα1/Kα2). | ||
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| Fig. 9 The structure of Na2VO(SO4)2 viewed down the b-axis to show the bonding of the two sulfate sites. | ||
NaV(SO4)2 forms a layered 2-dimensional structure unlike those observed for Na3V(SO4)3 and Na2VO(SO4)2. The vanadium octahedra corner share to six sulfate tetrahedra. The sulfate tetrahedra bond to three vanadium octahedra with the fourth S–O bond pointing towards the layers of sodium. The sodium in the layers is six coordinate and adopts an octahedral geometry (Fig. 10). NaV(SO4)2 is isostructural to NaFe(SO4)2 which has recently been shown to be an active battery material which allows for Na-ion insertion.16
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| Fig. 10 (a) Crystal structure of NaV(SO4)2; (b) observed, calculated and difference XRD profiles for NaV(SO4)2 (Rwp – 3.67%, Rp – 2.85%) (Cu Kα1/Kα2). | ||
O bond helps to stabilise the resultant highly charged V5+ cation on Na extraction. In addition, Na2VO(SO4)2 possesses a 3D structure with Na ion channels to potentially promote sodium-ion conduction. To further improve the materials properties, substitution of O for F (Na2VIVO(SO4)2 → Na2VIIIF(SO4)2) may also be possible through carbofluoro-reduction which may allow for an increase in capacity. In conclusion, the discovery of this novel facile route allows for the exploration of these materials in more detail, as well as offering further inspiration in the development of similar synthetic approaches to other thermally unstable transition metal sulfate systems.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: 10.1039/c8dt02308e |
| This journal is © The Royal Society of Chemistry 2018 |