The formation of solid barium sulfate, (BaSO4)
n
, known as barite when a crystalline
solid in space
group Pnma, is a classic system with a range of applicability
in and consequences for the petroleum and other industries. Herein,
we search for a minimum mechanism for (BaSO4)
n
formation via, first, a critical review of the literature
since the 1950s, literature revealing that (BaSO4)
n
formation is an early, important model system
with which to study nucleation, growth, and any accompanying aggregation.
The literature also teaches that solid (BaSO4)
n
forms via non-classical, continuous nucleation,
as first identified in 1997. Second, key literature kinetics data
sets are reanalyzed in light of five classes of established minimum
mechanisms for particle and solid formation. The resulting working
hypothesis for (BaSO4)
n
formation
is a 4-step mechanism consisting of nucleation (A → B), autocatalytic
growth (A + B → 2B), bimolecular aggregation (B + B →
C), and secondary autocatalytic aggregation (B + C → 1.5 C),
with rate constants k
1, k
2, k
3, and k
4, respectively, and where A = precursor, B = smaller
particles, and C = larger particles. Also provided are sections on
caveats, engineering models, remaining questions, suggestions for
moving forward, and a short summary.