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Overhauser Dynamic Nuclear Polarization of Lithiated Graphite Anodes: Probing Bulk and Surface Structures

Accepted version
Peer-reviewed

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Abstract

Graphite is used, almost ubiquitously, as an anode material in today’s high energy density Li-ion batteries. Both artificial and natural graphites are widely used, and there are large differences in the production methods, cost, particle morphologies, sizes and percentage of defects in their structures, all these parameters affecting use and performance. The success of graphite as an anode depends on the formation of a Li-ion conducting passivation layer (the solid electrolyte interphase (SEI)) on the first cycle, the nature of this layer still being under investigation with a range of approaches. During lithiation (charge in a full-cell), graphite is lithiated in stages and becomes electronically conductive. The conduction electrons of lithiated graphite anodes are exploited in this work to enhance the nuclear magnetic resonance (NMR) signal of bulk and surface nuclei via Overhauser dynamic nuclear polarization (DNP). The parameters directly affecting the enhancement factor (leakage factor, saturation factor and coupling factor) are examined in detail for an artificial graphite at different lithiation stages. Four additional (natural and artificial) graphites are then studied to explore the effects of particle size and morphology, electron relaxation times and conductivity on the observed DNP enhancements. Finally, the polarisation transfer between bulk and surface (SEI) species is explored through 6,7Li, 1 H and 13C DNP NMR experiments.

Description

Journal Title

Chemistry of Materials

Conference Name

Journal ISSN

0897-4756
1520-5002

Volume Title

Publisher

American Chemical Society (ACS)

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Except where otherwised noted, this item's license is described as Attribution 4.0 International
Sponsorship
European Commission Horizon 2020 (H2020) ERC (835073)
T.I. and C.P.G. were supported by an ERC Advanced Investigator Grant to C.P.G. (EC H2020 835073). Prof Anne Lesage, SalahEddine Akrial and PANACEA (EC H2020 101008500) are gratefully acknoledged for facilitating the experiments run at the CRMN in Lyon. Drs Marie Juramy and Dylan Maxwell are acknowledged for taking the SEM images of the Lifun and SPG graphites respectively and for helpful discussions; Dr Euan Bassey is thanked for help in preparing the BM sample and for helpful discussions; Dr Katharina Märker is thanked for initial training on the DNP spectrometer.