4.8 Article

Fluid-enhanced surface diffusion controls intraparticle phase transformations

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NATURE MATERIALS
卷 17, 期 10, 页码 915-+

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NATURE PUBLISHING GROUP
DOI: 10.1038/s41563-018-0168-4

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资金

  1. US Department of Energy (DOE), Office of Basic Energy Sciences, Division of Materials Sciences and Engineering [DE-AC02-76SF00515]
  2. Toyota Research Institute through D3BATT: Center for Data-Driven Design of Li-Ion Batteries
  3. DOE Office of Basic Energy Sciences [DE-AC02-76SF00515, DE-AC02-05CH11231]
  4. EPSRC [EP/K016288]
  5. Archer HPC facilities through the Materials Chemistry Consortium [EP/L000202]
  6. NSF Graduate Research Fellowship [DGE-114747]
  7. Kwanjeong Education Foundation Fellowship
  8. Global Climate and Energy Project at Stanford University
  9. DOE Office of Basic Energy Sciences through the SUNCAT Center for Interface Science and Catalysis
  10. EPSRC [EP/K016288/1, EP/M009521/1] Funding Source: UKRI

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Phase transformations driven by compositional change require mass flux across a phase boundary. In some anisotropic solids, however, the phase boundary moves along a non-conductive crystallographic direction. One such material is LiXFePO4, an electrode for lithium-ion batteries. With poor bulk ionic transport along the direction of phase separation, it is unclear how lithium migrates during phase transformations. Here, we show that lithium migrates along the solid/liquid interface without leaving the particle, whereby charge carriers do not cross the double layer. X-ray diffraction and microscopy experiments as well as ab initio molecular dynamics simulations show that organic solvent and water molecules promote this surface ion diffusion, effectively rendering LiXFePO4 a three-dimensional lithium-ion conductor. Phase-field simulations capture the effects of surface diffusion on phase transformation. Lowering surface diffusivity is crucial towards supressing phase separation. This work establishes fluid-enhanced surface diffusion as a key dial for tuning phase transformation in anisotropic solids.

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