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Microscopic mechanism of biphasic interface relaxation in lithium iron phosphate after delithiation.


ABSTRACT: Charge/discharge of lithium-ion battery cathode material LiFePO4 is mediated by the structure and properties of the interface between delithiated and lithiated phases. Direct observations of the interface in a partially delithiated single crystal as a function of time using scanning transmission electron microscopy and electron energy-loss spectroscopy help clarify these complex phenomena. At the nano-scale, the interface comprises a thin multiphase layer whose composition varies monotonically between those of the two end-member phases. After partial delithiation, the interface does not remain static, but changes gradually in terms of orientation, morphology and position, as Li ions from the crystal bulk diffuse back into the delithiated regions. First-principles calculations of a monoclinic crystal of composition Li2/3FePO4 suggest that the interface exhibits higher electronic conductivity than either of the end-member phases. These observations highlight the importance of the interface in enabling LiFePO4 particles to retain structural integrity during high-rate charging and discharging.

SUBMITTER: Kobayashi S 

PROVIDER: S-EPMC6054635 | biostudies-literature | 2018 Jul

REPOSITORIES: biostudies-literature

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Microscopic mechanism of biphasic interface relaxation in lithium iron phosphate after delithiation.

Kobayashi Shunsuke S   Kuwabara Akihide A   Fisher Craig A J CAJ   Ukyo Yoshio Y   Ikuhara Yuichi Y  

Nature communications 20180720 1


Charge/discharge of lithium-ion battery cathode material LiFePO<sub>4</sub> is mediated by the structure and properties of the interface between delithiated and lithiated phases. Direct observations of the interface in a partially delithiated single crystal as a function of time using scanning transmission electron microscopy and electron energy-loss spectroscopy help clarify these complex phenomena. At the nano-scale, the interface comprises a thin multiphase layer whose composition varies mono  ...[more]

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