The finite-size effect on the antiferromagnetic (AF) transition and electronic configuration of iron has been observed in LiFePO4. Determination of the scaling behavior of the AF transition temperature (TN ) vs. the particle size dimension (L) in the critical regime, 1 −∼ L −1 , reveals that the activation nature of the AF ordering strongly depends on the surface energy. In addition, the effective magnetic moment that reflects the electronic configuration of iron in LiFePO4 is found sensitive to the particle size. An alternative structural view based on the polyatomic ion groups of PO 3− 4 is proposed. LiFePO 4 has been considered as an ideal cathode electrode material with a workable redox potential of 3.45 V and a high theoretical capacity of 170 mAh/g.[1] LiFePO 4 is a band insulator in bulk crystal form in agreement with the calculated large band gap,[2] however, the fast electron/ion charge/discharge process has been shown to be possible only when the particle size is reduced to below ∼100 nm.[3] While significant progress has been made to demonstrate the impact of nanoscaling on defect chemistry, electrochemical behavior, electron-ion conductivity, lithium ion diffusion, and the charge/discharge rate in general,[4-6] the fundamental question of "why nano-scaling matters?" remains. Generally, there have been two major approaches to interpret the property improvement for LiFePO 4 using nano-scaling induced electron/ion transport: the first is called the "domino-cascade" model, which describes a fast anisotropic lithium insertion/extraction action coupled to the LiFePO 4 -FePO 4 interface movement through an electron polaronic hopping mechanism in nano-crystallites, [5] and the second focuses on the surface effect with carbon coating and miscibility gap size reduction as a result of nano-scaling. [4,7] Conventionally, the iron ion has been viewed as Fe
2+with oxygen ligands to form the octahedral crystal electric field (CEF) of e g -t 2g splitting.[8] However, the magnitude of the effective magnetic moment (µ ef f ) obtained from the Curie-Weiss law fitting was inconsistent and spread in the range of µ ef f ∼4.7-5.5 µ B , which has been interpreted that Fe 2+ must be in the high-spin state (HS) as t 4 2g e 2 g of S=2 with a spin-only value of µ ef f = 4.9µ B , and the inconsistent moment above 4.9 µ B has often been described by incomplete orbital-quenching, i.e., the theoretically calculated value from the Lande g-factor with J=L+S (S=2, L=2) without orbital quenching should be µ ef f =6.7µ B .[9, 10] Considering a typical iron ion in the crystal field composed of oxygen ligands with high electronegativity, the HS choice of d 6 implies an unexpectedly small crystal field splitting between e g − t 2g , unless the influence of the nearby PO 3− 4 phosphate groups are included. In addition, within the explanation of in-