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A droplet can remain liquid below its equilibrium melting temperature through supercooling: a microscopic ice embryo must first pay an interfacial free-energy cost. The nucleation barrier can therefore delay freezing even when bulk ice is thermodynamically favoured. Solutes, available surfaces, temperature, droplet volume and exposure time affect the probability; zero degrees Celsius is not an automatic freezing threshold for every atmospheric droplet.

At least four physical routes are relevant:

Mineral particles provide nonbiological examples of heterogeneous nuclei. A particle's presence alone does not guarantee activity at a given temperature. The cloud ice nucleation versus ice growth distinction matters: the processes listed concern the formation of new ice; subsequent depositional growth, riming and aggregation are separate from initiating that first crystal.

Droplets remain supercooled because creating an ice embryo costs interfacial free energy: freezing has a nucleation barrier even below the equilibrium melting point. Small droplets also have a low probability of containing an effective ice-nucleating inclusion.

Three heterogeneous routes are immersion freezing around a particle already inside the droplet, contact freezing following a collision with a suitable mineral particle, and deposition nucleation from ice-supersaturated vapour onto a suitable surface. At sufficiently low temperature, homogeneous ice nucleation occurs without a foreign surface. Its onset depends on volume and observation time rather than being a universal exact temperature. No biological ice-nucleating agents are needed for these mechanisms.

Diamond can be metastable: its Gibbs free energy is higher than graphite's under ambient conditions, but transformation is kinetically inhibited. Conversion requires substantial rearrangement of the strong carbon-bond network and the formation and growth of a new thermodynamic phase, with an activation and nucleation barrier.

At room temperature the rate can be extremely small even though the free-energy change favors graphite. Thermodynamic stability specifies the preferred equilibrium state, not the time needed to reach it. Persistence of diamond therefore does not contradict graphite's ambient equilibrium stability.

Along the stipulated fixed-aspect-ratio pathway, substitute $h=d/k$ before differentiating:The nonzero stationary diameter isComparison with the stated diameter gives $k{\gamma }_f+2{\gamma }_e=6{\gamma }_f+2{\gamma }_e$, hence $k=d/h=6$, provided ${\gamma }_f$ is nonzero. This is a plate-like shape, qualitatively consistent with the cheaper broad coherent faces. For negative $\Delta G$, substitution shows the stationary point is a maximum along this size pathway, as required for a nucleation barrier.

A useful distinction is that this calculation holds shape fixed. Minimizing the interface energy at fixed volume separately gives $d/h={\gamma }_e/{\gamma }_f$ for the cylindrical model; if the selected aspect ratio is also an equilibrium shape, it would require ${\gamma }_e=6{\gamma }_f$. The given critical-diameter relation alone does not otherwise determine that energy ratio. In the degenerate zero-face-energy limit the coefficient comparison cannot determine $k$.