Many layered oxide
and sulfide intercalation compounds used in
secondary batteries undergo stacking-sequence-change phase transformations
during (de)intercalation. However, the underlying reasons why different
intercalants result in different stacking-sequence changes are not
well understood. This work reports on high-throughput density functional
theory calculations on the prototype systems A
x
CoO2 and A
x
TiS2 (where A = [Li, Na, K, Mg, and Ca]), which show that a few simple
rules explain the relative stability among the O1, O3, and P3 stacking
sequences. First, for large intercalants (Na, K, and Ca), P3 stacking
is favorable at intermediate concentrations (x ∼
0.5) as its intercalant site topology minimizes in-plane electrostatic
repulsion. At the extreme compositions (x ∼
0 and x ∼ 1), O1 or O3 are stable, with more
ionic compounds preferring O3 and covalent ones O1. These rules explain
why stacking-sequence changes are much more common in Na materials
than Li ones.