Abstract
Extreme fast charging (XFC, i.e., achieving at least 80% state of charge within 15 minutes) and high current rate cycling remain high desirability criteria for next-generation lithium batteries. While anodes, e.g., graphite and lithium, have been historically acknowledged as the critical hurdles for fast- charging batteries, the stability of cathodes under sustained high current rate cycling has not been well studied. In this work, we have investigated the fast cycling (≦ 15 mins charging time) of LiMn2O4 (LMO) under practical cycling conditions (i.e., 90% loading of cathode material with an areal capacity of 1 mAh/cm2). We find that in the presence of a conventional LiPF6-based carbonate electrolyte, the high rate cycling of LMO brings forth a cascade of bulk LiMn2O4→LiMnO2 phase changes, accompanied by oxygen release, which initiates electrolyte degradation. Together, these factors play a compounding role in the capacity loss during cycling, even with high current rate compatible anodes, e.g., Li4Ti5O12 (LTO). The application of a novel lithium salt, Lithium 1,1,1,3,3,3, (tetrakis) hexafluoroisopropoxy borate (LiBHFip), in a mixture with commercial electrolyte overcomes these limitations due to the formation of a facilitative boron-rich cathode electrolyte interface. Cycling of LMO|LTO cells with the novel electrolyte shows 91% capacity retention after 1500 cycles, thereby demonstrating the long-term stability of this type of Li-ion battery under XFC conditions (e.g., 66% charge within 10 mins) for the first time with 1 mAh/cm2 loading of cathode materials.
Supplementary materials
Title
Extreme fast charging and stable cycling of LiMn2O4 – Li4Ti5O12 system by suppression of cathode phase change
Description
Supporting information for the manuscript entitled Extreme fast charging and stable cycling of LiMn2O4 – Li4Ti5O12 system by suppression of cathode phase change provides further information related to the novelty of the lithium salt, choice of electrolyte, the relation between the cathode phase change, oxygen evolution and electrolyte degradation.
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