Mixing Ca²⁺ and CO₃²⁻ solutions (e.g. CaCl₂ + Na₂CO₃) drives classical nucleation once the supersaturation ratio S = [Ca²⁺][CO₃²⁻]/Ksp is high enough to overcome the nucleation barrier:
ΔG* = 16πγ³Vm² / (3(RT lnS)²)
J = A·exp(−ΔG*/RT)
Higher S and higher T shrink ΔG*, so the nucleation rate J (particles per second, shown live) rises steeply — this simulator drives it directly from your S and T sliders.
Which polymorph forms is governed by Ostwald's step rule plus a real inhibitor effect: freshly nucleated CaCO₃ tends to appear first as the least-stable, lowest-surface-energy phase — spherical vaterite — which normally redissolves and reprecipitates as the thermodynamically stable calcite (rhombohedral) within seconds to minutes. Dissolved Mg²⁺ ions adsorb onto calcite's growth steps and strongly poison that step, which is why seawater and biomineralizing organisms — both Mg²⁺-rich — form needle-shaped aragonite or stabilized vaterite instead of calcite, even though calcite is the more stable form in pure water.
- S (supersaturation) — sets the nucleation rate J and the growth speed of every particle.
- Mg²⁺/Ca²⁺ — raises the odds a nucleus forms as aragonite instead of calcite, and slows (or blocks) vaterite → calcite conversion, matching the real inhibition mechanism above.
- Temperature — speeds growth and the vaterite → calcite transformation rate (an Arrhenius-type effect).
- pH — more CO₃²⁻ is available at high pH, which raises the effective nucleation rate.
This is the same competition exploited to engineer CaCO₃ drug-delivery nanoparticles: colloidal or biomineralization-style synthesis routes tune S, Mg²⁺ and pH specifically to lock in the porous, higher-surface-area vaterite phase (good for loading drugs into pores) instead of letting it age into denser, less useful calcite.