The stability of typical vanadium flow battery (VFB) catholytes with respect to precipitation of V 2 O 5 was investigated at temperatures in the range 30-60 • C. In all cases a precipitate formed after an induction time, which decreased with increasing temperature and concentration of V V and increased with concentration of sulfate. Arrhenius-type plots are shown for two typical solutions. These have excellent linearity and have similar slopes which yield an apparent activation energy of 1.79 eV (172 kJ mol −1 ). The variation of induction time with temperature for various concentrations of V V was simulated, and stability diagrams for additive-free VFB catholytes were generated. Vanadium flow batteries 1,2 (VFBs), also known as vanadium redox flow batteries (VRFBs), are currently the subject of much interest and recent research 3-7 because they are attractive for a variety of largescale energy storage applications. 8 An important advantage of a flow battery is that its energy storage capacity and its power capability can be scaled independently.2 VFBs have the additional advantage that cross-contamination due to transport through the membrane is effectively eliminated because the anolyte and catholyte differ only in the oxidation state of the vanadium.9 Also, since aqueous vanadium species are highly colored, the state-of-charge may be precisely monitored using ultraviolet-visible spectroscopy.
10,11The energy density of VFBs is limited by the solubility of V II , V III , V IV and V V in the electrolyte. In the anolyte, the solubility of V 2+ and V 3+ generally increases with temperature and decreases with increasing concentration of H 2 SO 4 and this is also true for the solubility of the V IV species, VO 2+ , in the catholyte. 12 The predominant V V species 13 present in strongly acidic solutions such as typical VFB catholytes is the pervanadyl ion VO 2 + . The solubility of vanadium (V) oxide, V 2 O 5 , in this region of pH is ∼0.1 mol dm −3 or less. 14 Thus, at the concentrations typically encountered in VFB catholytes, V V is expected to be thermodynamically unstable in solution with respect to precipitation as V 2 O 5 . However, precipitation is usually found to be very slow and, in practice, supersaturated solutions of V V in sulfuric acid can persist for very long periods of time. The stability of these metastable solutions (VFB catholytes) decreases, as expected, as the concentration of V V increases. 15 This is reflected in a lowering of stability at a particular vanadium concentration as the state-of-charge (i.e. the fraction of vanadium present as V V ) of the catholyte increases.
16Stability improves with increasing concentration of sulfate 17 and in the presence of certain additives 1 such as H 3 PO 4 . Thus, there have been several studies 7,[15][16][17][18][19] of the stability of V V in the catholyte of VFBs, and several mechanisms of precipitation have been proposed. 7,18 However, there is an absence in the literature of detailed kinetic studies of the precipitation process and the variation w...