Origin of Unusual Acidity and Li+ Diffusivity in a Series of Water-in-Salt Electrolytes

Phase separation visualized in 20 m LiTFSI/H2O water-in-salt electrolyte (WiSE) from MD simulations. In this representation, the largest water and ionic aggregates are highlighted in color.

Scientific Achievement

The origin of strong acidity and explanation of ion diffusion along nanometric channels were uncovered in an important family of LiTFSI/H2O water-in-salt electrolytes (WiSEs).

Significance and Impact

Structural similarities were discovered on the nanometer scale between LiTFSI/H2O WiSEs and hydrated Nafion® membranes, suggesting that Li+ ions in these WiSEs diffuse along complex pathways involving both water- and TFSI- rich regimes.

Research Details

  • DFT calculations suggest that the origin of the unusual acidity of LiTFSI based WiSEs (e.g., a pH of of 2.4 at 20 m concentration) is due to the deprotonation of water molecules bridged over at least two Li+ ions as part of the multimeric salt structures within anion-rich regimes.
  • PFG-NMR experiments and MD simulations disclose the phase separation of water- and TFSI- rich regimes and the existence of interfacial water between these two regimes.
  • NMR spectroscopy and PFG-NMR measurements reveal the structural similarity of water-in-salt electrolyte with hydrated Nafion® membrane on the nanometer scale.

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DOI:  10.1021/acs.jpcb.0c02483

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