Editing Crystallization (section)

== Thermodynamic view ==
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[[Image:LT-SEM snow crystal magnification series-3.jpg|thumb|upright|Low-temperature [[Scanning electron microscope|SEM]] magnification series for a snow crystal. The crystals are captured, stored, and sputter-coated with platinum at cryo-temperatures for imaging.]]

The crystallization process appears to violate the [[second principle of thermodynamics]]. Whereas most processes that yield more orderly results are achieved by applying heat, crystals usually form at lower temperatures{{snd}}especially by [[supercooling]]. However, the release of the heat of fusion during crystallization causes the entropy of the universe to increase, thus this principle remains unaltered.

The molecules within a pure, ''perfect crystal'', when heated by an external source, will become liquid. This occurs at a sharply defined temperature (different for each type of crystal). As it liquifies, the complicated architecture of the crystal collapses. Melting occurs because the [[entropy]] (''S'') gain in the system by spatial randomization of the molecules has overcome the [[enthalpy]] (''H'') loss due to breaking the crystal packing forces:
:<math>T(S_\text{liquid} - S_\text{solid}) > H_\text{liquid} - H_\text{solid},</math>
:<math>G_\text{liquid} < G_\text{solid}.</math>
Regarding crystals, there are no exceptions to this rule. Similarly, when the molten crystal is cooled, the molecules will return to their crystalline form once the temperature falls beyond the turning point. This is because the thermal randomization of the surroundings compensates for the loss of entropy that results from the reordering of molecules within the system. Such liquids that crystallize on cooling are the exception rather than the rule.

The nature of the crystallization process is governed by both thermodynamic and kinetic factors, which can make it highly variable and difficult to control. Factors such as impurity level, mixing regime, vessel design, and cooling profile can have a major impact on the size, number, and shape of crystals produced.
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