“…resulted in continuous migration paths noted in Table in column 2 for the confirmed Li‐ion conductors LiFePO 4 and Li 3 VO 4 and for the potential Li‐ion conductors LiGeBO 4 , CsLiB 6 O 10 , Li 2 Ti 3 O 7 , LiMn 0.88 Fe 0.17 PO 4 (lithiophilite), Li 2 NaPO 4 , and LiNaSO 4 . Similarly, using the procedure of Meutzner et al . resulted in continuous migration paths for the confirmed Na‐ion conductors Na 4 P 2 O 7 , and Na 2 SO 4 (thenardite), Na 6 Mg(SO 4 ) 4 (vanthoffite), and for the potential Na‐ion conductors Na 6 Mg 2 (CO 3 ) 4 SO 4 (tychite), Na 2 TiSiO 5 (natisite), NaPO 3 (Kurrol A), Na 3 SO 4 F (kogarkoite), Na 6 (SO 4 ) 2 FCl (sulfohalite), Na 15 (SO 4 ) 5 F 4 Cl (galeite), Na 21 (SO 4 ) 7 F 6 Cl (schairerite), Na 22 K(CO 3 ) 2 (SO 4 ) 9 Cl (hanksite), and Na 2 SeO 4 .…”