“…Accordingly, oxidative leaching experiments were undertaken through refluxing 80 mL of alkaline hypochlorite (r2% alkalinity, Z8% available chlorine), with a fixed mass of LiMn 2 O 4 (m 0 = 0.1 g or 1.0 g) at a known temperature, T, in the range 50 o T/1C o 100, for a constant time period (1 h), see ESI1 (ESI †). Our previous work, 27 suggests that this time period is sufficient for the initial rate to be monitored. where the factor of 1 2 results from the 1 : 2 stoichiometry of LiMn 2 O 4 : MnO 4…”