Structural Changes in a High-Energy Density VO2F Cathode upon Heating and Li Cycling

被引:14
|
作者
Wang, Xiaoya [1 ]
Lin, Yuh-Chieh [4 ]
Zhou, Hui [2 ]
Omenya, Fredrick [2 ]
Chu, Iek-Heng [5 ]
Karki, Khim [1 ,6 ]
Sallis, Shawn [1 ,3 ]
Rana, Jatinkumar [1 ,3 ]
Piper, Louis F. J. [1 ,3 ]
Chernova, Natasha A. [1 ]
Ong, Shyue Ping [5 ]
Whittingham, M. Stanley [1 ,2 ]
机构
[1] Binghamton Univ, NECCES, Binghamton, NY 13902 USA
[2] Binghamton Univ, Chem & Mat, Binghamton, NY 13902 USA
[3] Binghamton Univ, Dept Phys Appl Phys & Astron, Binghamton, NY 13902 USA
[4] Univ Calif San Diego, Mat Sci & Engn Program, 9500 Gilman Dr 0418, La Jolla, CA 92093 USA
[5] Univ Calif San Diego, Dept NanoEngn, 9500 Gilman Dr, La Jolla, CA 92093 USA
[6] Brookhaven Natl Lab, Ctr Funct Nanomat, Upton, NY 11973 USA
来源
ACS APPLIED ENERGY MATERIALS | 2018年 / 1卷 / 09期
关键词
lithium ion battery; cathode; vanadium oxyfluoride; thermal stability; structure evolution; ELECTRODE MATERIALS; LITHIUM; BATTERY; INTERCALATION; STABILITY; EVOLUTION; OXIDE;
D O I
10.1021/acsaem.8b00473
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Structural changes in VO2F, which allow two electron transfer during electrochemical Li cycling, were investigated. This compound adopts a rhombohedral structure, space group R (3) over barc, with O and F sharing one site, and was synthesized by high-energy ball-milling. The thermal stability of VO2F, which is related to the battery safety, is studied by in situ XRD upon heating and by thermal gravimetric analysis. VO2F is found to be stable up to 160 degrees C under inert atmosphere; above this temperature, it converts into vanadium oxide with fluorine loss. The structure evolution upon lithium cycling was studied by ex situ X-ray diffraction and absorption techniques. The results show that lithiation of VO2F goes through a solid-solution reaction, and the rhombohedral structure is preserved if no more than one lithium ion is intercalated. Upon a second Li insertion, an irreversible transition to a rock-salt structure occurs. We show using first-principles calculations that this irreversible transformation can be explained by an asymmetric energetic preference between the rhombohedral and rock-salt forms of LixVO2F, which result in large thermodynamic driving forces to convert to the rock-salt structure at x > 1 and relatively small thermodynamic driving forces to convert back to the rhombohedral structure when delithiating to x < 1.
引用
收藏
页码:4514 / 4521
页数:15
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