In
the search for high energy density cathodes for next-generation
lithium-ion batteries, the disordered rocksalt oxyfluorides are receiving
significant attention due to their high capacity and lower voltage
hysteresis compared with ordered Li-rich layered compounds. However,
a deep understanding of these phenomena and their redox chemistry
remains incomplete. Using the archetypal oxyfluoride, Li
2
MnO
2
F, we show that the oxygen redox process in such materials
involves the formation of molecular O
2
trapped in the bulk
structure of the charged cathode, which is reduced on discharge. The
molecular O
2
is trapped rigidly within vacancy clusters
and exhibits minimal mobility unlike free gaseous O
2
, making
it more characteristic of a solid-like environment. The Mn redox process
occurs between octahedral Mn
3+
and Mn
4+
with
no evidence of tetrahedral Mn
5+
or Mn
7+
. We
furthermore derive the relationship between local coordination environment
and redox potential; this gives rise to the observed overlap in Mn
and O redox couples and reveals that the onset potential of oxide
ion oxidation is determined by the degree of ionicity around oxygen,
which extends models based on linear Li–O–Li configurations.
This study advances our fundamental understanding of redox mechanisms
in disordered rocksalt oxyfluorides, highlighting their promise as
high capacity cathodes.