4.6 Article

Electrochemical (de) lithiation of silver ferrite and composites: mechanistic insights from ex situ, in situ, and operando X-ray techniques

期刊

PHYSICAL CHEMISTRY CHEMICAL PHYSICS
卷 19, 期 33, 页码 22329-22343

出版社

ROYAL SOC CHEMISTRY
DOI: 10.1039/c7cp04012a

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资金

  1. Center for Mesoscale Transport Properties, an Energy Frontier Research Center
  2. U.S. Department of Energy (DOE), Office of Science, Basic Energy Sciences (BES) [DE-SC0012673]
  3. DOE Office of Science by Brookhaven National Laboratory [DE-AC02-98CH10886, DE-SC0012704]
  4. DOE Office of Science by Argonne National Laboratory [DE-AC02-06CH11357]
  5. U.S. Department of Energy (DOE) [DE-SC0012673] Funding Source: U.S. Department of Energy (DOE)

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The structure of pristine AgFeO2 and phase makeup of Ag0.2FeO1.6 (a one-pot composite comprised of nanocrystalline stoichiometric AgFeO2 and amorphous gamma-Fe2O3 phases) was investigated using synchrotron X-ray diffraction. A new stacking-fault model was proposed for AgFeO2 powder synthesized using the co-precipitation method. The lithiation/de-lithiation mechanisms of silver ferrite, AgFeO2 and Ag0.2FeO1.6 were investigated using ex situ, in situ, and operando characterization techniques. An amorphous gamma-Fe2O3 component in the Ag0.2FeO1.6 sample is quantified. Operando XRD of electrochemically reduced AgFeO2 and Ag0.2FeO1.6 composites demonstrated differences in the structural evolution of the nanocrystalline AgFeO2 component. As complimentary techniques to XRD, ex situ X-ray Absorption Spectroscopy (XAS) provided insight into the short-range structure of the (de) lithiated nanocrystalline electrodes, and a novel in situ high energy X-ray fluorescence nanoprobe (HXN) mapping measurement was applied to spatially resolve the progression of discharge. Based on the results, a redox mechanism is proposed where the full reduction of Ag+ to Ag-0 and partial reduction of Fe3+ to Fe2+ occur on reduction to 1.0 V, resulting in a (Li1+yFeFeyO2)-Fe-III-O-II phase. The (Li1+yFeFeyO2)-Fe-III-O-II phase can then reversibly cycle between Fe3+ and Fe2+ oxidation states, permitting good capacity retention over 50 cycles. In the Ag0.2FeO1.6 composite, a substantial amorphous gamma-Fe2O3 component is observed which discharges to rock salt LiFe2O3 and Fe-0 metal phase in the 3.5-1.0 V voltage range (in parallel with the AgFeO2 mechanism), and reversibly reoxidizes to a nanocrystalline iron oxide phase.

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