“…The major DTA peak at 635-675 • C may be due to the formation of ferrous/ferric pyrophosphate, Fe 3 (P 2 O 7 ) 2 or Fe 2+ Fe 3+ 2 (P 2 O 7 ) 2 [14,25], or to similar Q 0 , Q 1 and Q 2 crystalline species (where Q = number of bridging oxygens bonds per PO 4 group) [28]. It may also be due to the formation of FePO 4 , as occurred during heat treatment of P 2 O 5 Fe 2 O 3 Na 2 O glasses in oxygen [45] and P 2 O 5 Fe 2 O 3 glasses in argon [46]. In addition to the chemical composition, the Fe 2+ / Fe redox ratio can influence the temperature at which crystallisation occurs [14,16,25,31,46], and increasing the Fe 2+ / Fe ratio can reduce crystallisation temperature [46].…”