Bragg Institute, B87, Australian Nuclear Science and Technology Organization, Locked Bag 2001, Kirrawee DC NSW 2232, Australia.
Inorg Chem. 2013 Aug 5;52(15):8685-93. doi: 10.1021/ic400870x. Epub 2013 Jul 11.
The magnetic structure and properties of polycrystalline NaFePO4 polymorphs, maricite and triphylite, both derived from the olivine structure type, have been investigated using magnetic susceptibility, heat capacity, and low-temperature neutron powder diffraction. These NaFePO4 polymorphs assume orthorhombic frameworks (space group No. 62, Pnma), built from FeO6 octahedral and PO4 tetrahedral units having corner-sharing and edge-sharing arrangements. Both polymorphs demonstrate antiferromagnetic ordering below 13 K for maricite and 50 K for triphylite. The magnetic structure and properties are discussed considering super- and supersuperexchange interactions in comparison to those of triphylite-LiFePO4.
多晶 NaFePO4 多晶型物(镁橄榄石型)赤磷铁矿和磷铁锂矿的磁性结构和性质已通过磁化率、比热容和低温中子粉末衍射进行了研究。这些 NaFePO4 多晶型物具有由 FeO6 八面体和 PO4 四面体单元通过角共享和边共享排列构成的正交骨架(空间群 No. 62,Pnma)。两种多晶型物均在 13 K 以下表现出反铁磁有序,而磷铁锂矿则在 50 K 以下表现出反铁磁有序。与磷铁锂矿相比,通过超交换和超超交换相互作用来讨论磁性结构和性质。