The
precipitation kinetics of calcium oxalate was investigated
using a novel acidic reaction rate control and pH-monitoring method
and a sequence of acid–base, coordination, nucleation, and
growth differential equations. The results indicate that the complex
formation is remarkably favorable and is diffusion rate-limited. The
nucleation reaction is shown to initiate via the molecular assembly
of near-zwitterionically polarized complexes. From experimental results,
growth and formation of the crystal phase leads to an enthalpically
less stabilized state.
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