Journal
CHEMISTRY OF MATERIALS
Volume 33, Issue 13, Pages 4960-4970Publisher
AMER CHEMICAL SOC
DOI: 10.1021/acs.chemmater.1c00616
Keywords
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Funding
- U.S. Department of Energy, Office of Vehicle Technologies [DE-AC02-06CH11357]
- Argonne, a U.S. Department of Energy Office of Science laboratory [DE-AC02-06CH11357]
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The improved electrochemical performance of Si through the addition of multivalent cation salts is achieved by forming stable Li-M-Si ternary phases. High-resolution solid-state Li-7 and Si-29 nuclear magnetic resonance (NMR) reveals the lithiation process of Si from the surface Si-O layer to the formation of Si-4 anions in high lithiation states. Evidence of Mg-ion insertion and a lithium-deficient LiyMg0.1Si phase is found during charging, shedding light on possible mechanisms for stable Si-based anodes in lithium-ion batteries.
Improved electrochemical performance of Si was recently reported by adding multivalent cation salts (such as Mg2+, Al3+, Ca2+, etc.) in the electrolyte. This is achieved via the formation in an in situ manner of relatively more stable Li-M-Si ternary phases with less chemical reactivity. These phases stabilize Si anions and thus reduce side reactions with electrolytes at the surface and eventually benefit the overall electrochemistry. To understand the mechanism of ternary Zintl phase formation and its dynamics upon lithiation/delithiation, high-resolution solid-state Li-7 and Si-29 nuclear magnetic resonance (NMR) are utilized to directly probe the local Li and Si environments on Si electrodes harvested from coin and pouch cells at various states of (de)lithiation. The NMR spectra along with the electrochemical characterization reveal that lithiation of Si starts from the surface Si-O layer further confirmed by Li-7-Si-29 cross-polarization NMR. Lithiation progresses with heterogeneous silicon clustering with Si-4 anions at high states of lithiation. At a fully lithiated state, the formation of overlithiated Si species is detected. At a low-voltage region (below 100 mV), direct evidence for Mg-ion insertion is found, postulated by two possible mechanisms: ion exchange with fully or overlithiated binary domains (Li3.75+xSi) and/or a coinsertion with slightly underlithiated domains (similar to Li3.55Si). Upon delithiation, Li extraction starts from overlithiated Si domains. No evidence is found for electrochemical Mg removal. Evidence for a lithium-deficient LiyMg0.1Si phase is found as a result of Li removal during charging. This investigation sheds light on the possible mechanisms of a new Si anode chemistry, which could enable the development of stable Si-based anodes for lithium-ion batteries.
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