“…The observed deviation of the chemical formulation from the stoichiometric composition is often encountered in phosphate materials of the alluaudite type viz. Na 1.50 Mn 2.48 Al 0.85 (PO 4 ) 3 (Hatert, 2006), Na 1.25 Mg 1.10 Fe 1.90 -(PO 4 ) 3 (Hidouri et al, 2008), NaFe 3.67 (PO 4 ) 3 (Korzenski et al, 1998), Na 1.79 Mg 1.79 Fe 1.21 (PO 4 ) 3 (Hidouri et al, 2003), Na 0.38 Ca 0.31 MgFe 2 (PO 4 ) 3 (Zid et al, 2005), -Na 0.67 FePO 4 (Kim et al, 2013), Li 0.5 Na 0.5 MnFe 2 (PO 4 ) 3 (Trad et al, 2010), Na 1.5 Mn 1.5 Fe 1.5 (PO 4 ) 3 (Hatert, 2004), Na 1.86 Fe 3 (PO 4 ) 3 (Essehli et al, 2016) (Bouraima et al, 2017). Generally, in this structure the interconnected sheets produce two types of hexagonal channels parallel to the c-axis direction (Hatert, 2008): channel (1) at ( 1 2 , 0, z) and (0, 1 2 , z), while channel (2) is located at (0, 0, z) and ( 1 2 , 1 2 , z) (Leroux et al, 1995).…”