Rapid metasomatism
of lead sulfide toward lead sulfate under acidic
conditions is a geochemical phenomenon that can access the immobilization
route of toxic heavy lead; however, the molecular mechanism has not
yet been elucidated. Here, we succeeded in studying the alternation
mechanism of galena to anglesite under sulfuric acid conditions by
an extended mechanistic theory of nucleation, where diffusion and
reactions of molecules at mineral interfaces are taken into consideration.
There exist large nanovoids with a size of ∼6 Å at the
interfaces acting as diffusion pathways of solution molecules with
an activation energy of ∼0.1 eV. In addition, protons available
in solution readily react with interior surfaces of the above-mentioned
nanovoids because of close interaction involving an energy cost of
∼0.2 eV. The diffusive nature and reactive nature of solution
molecules at the mineral interfaces govern the anglesite formation,
triggering off a low energy cost of ∼0.3 eV under sulfuric
acid conditions.