Disordered Lithium-Rich Oxyfluoride as a Stable Host for Enhanced Li+ Intercalation Storage
Disordered Lithium-Rich Oxyfluoride as a Stable Host for Enhanced Li+ Intercalation Storage
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DOI:
10.1002/aenm.201401814
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发表时间:
2015-05-06
影响因子:
27.8
通讯作者:
Hahn, Horst
中科院分区:
文献类型:
--
作者:
Chen, Ruiyong;Ren, Shuhua;Hahn, Horst
DOI: 10.1002/aenm. 201401814 rock-salt structures, with Li+/TM evenly sharing cation sites and close-packed anion arrays, may be a reasonable alternative for efficient Li+ storage. After Li+ extraction, the TM may remain at the cation sublattice sites and uphold well the disordered rocksalt framework. A recent work based on ab initio computations revealed that Li+ transport can be facile in a disordered cubic rock-salt oxide (Li 1.211Mo 0.467Cr 0.3O 2) with Li-excess.[8] It was found that such framework is stable with a maximum of 45% of the cation sites vacant. Herein, we demonstrate that a new dilithium disordered rock-salt Li 2VO 2F intercalation material can deliver up to about 1.8 Li+ capacity per TM (420 mAh g− 1) at≈ 2.5 V (1000 Wh kg− 1) with only minor lattice volume change (≈ 3%). Such material with mixed O 2−/F− anion environment has been synthesized by a simple ball-milling method. The two Li+ storage with V 3+/V 5+ redox reactions (Li 2VO 2F↔ 2 Li++ 2e−+ VO 2F) leads to an attractively high theoretical capacity of 462 mAh g− 1. Moreover, Li 2VO 2F shows good capacity retention and minor increase in polarization upon fast charging/discharging or upon low-temperature operation. The crystal structure of the target phase for the as-milled Li 2VO 2F is determined by Rietveld structural refinement of powder neutron (Figure 1a) and X-ray (Figure 1 b) diffraction patterns. The refinement precludes a layered rock-salt structure (R-3 m space group)(Figure S1, Supporting Information).[11] Instead, the diffraction patterns can be well indexed in a disordered cubic rock-salt phase (space group Fm-3 m, Table S1, Supporting Information). The atomic displacement parameters were constrained to the same for all atoms in the course of the refinements. As illustrated in the inset of Figure 1 a, Li and V atoms distribute randomly on the cationic sublattice (4 a Wyckoff sites) with a refined occupancy ratio of 0.64: 0.36. The accurate occupancy refinements for O and F on the anionic sublattice (4 b sites) cannot be obtained from the diffraction data because O and F have low contrast in scattering properties for X-rays and neutrons.[12] On an average, cations are coordinated with four O and two F atoms to form the (Li/V) O4f 2 octahedral units in the stoichiometric Li 2VO 2F. In addition, the refinement yields a material density of 4.25 g cm− 3 as compared with 5 g cm− 3 for LiCoO 2 and 3.5 g cm− 3 for LiFePO 4.[13] High-resolution transmission electron microscopy (HRTEM) image shows the nanocrystalline character (≈ 10 nm) of the as-synthesized Li 2VO 2F (Figure 1 c). The cubic structure of Li 2VO 2F was also confirmed by the corresponding fast Fourier transform (FFT) image (inset in Figure 1 c). Some nanocrystals (marked with white circle in Figure 1 c) show clear stacking faults, arising probably from the local distortion of (Li/V) O xF y octahedra. Energy-dispersive spectroscopy (EDS, Figure 1 d)Advanced cathode materials with superior energy storage capability are highly demanded for mobile and stationary applications. The inherent structural feature of Li+ hosts is critical for the battery performance. High-capacity conversion cathode materials often encounter large voltage hysteresis (low energy efficiency) accompanied with the structural reconstruction.[1] The current commercial cathode materials are still dominated by intercalation materials with intrinsic structural integrity for accommodating Li+.[2] However, the known intercalation materials have limited theoretical capacity (< 300 mAh g− 1).[3] In addition, structural transition/degradation have often been observed for the common intercalation hosts with ordered Li+/transition metal (TM) lattice sites …