Linked from
The 53 pages that link to Nucleation, each with the reason it gives.
Boiling pointRelated: Bubble formation depends on sites where vapor nuclei can grow.
AerosolRelated: Vapor condensation onto newly formed clusters can create aerosol particles.
Igneous rockRelated: The number of crystal seeds helps determine igneous grain size.
CondensationRelated: Water droplets often need tiny particles or surfaces to begin forming.
SupersaturationRelated: Nucleation often determines how long excess solute remains dissolved.
QuenchingRelated: Quenching can limit the time available for new phases to nucleate and grow.
BoilingRelated: Bubbles form at nucleation sites before rising through the cooking liquid.
SupercoolingNarrower topic: Supercooled water remains liquid while ice nuclei fail to form or grow.
NephrolithiasisRelated: Stone crystals begin when dissolved compounds nucleate in urine.
Kidney stoneRelated: It is one route by which the first crystals of a stone can form.
Porphyritic textureRelated: The timing and abundance of crystal nuclei help determine grain size.
Metastable stateRelated: A critical nucleus often enables the transition out of a metastable phase.
Thin-film depositionRelated: Deposited atoms often begin a film by forming stable surface clusters.
Mineral precipitationBroader topic: It is the first step that creates a solid mineral phase.
GelatoRelated: Rapid freezing creates many small ice crystals in gelato.
Solid-state reactionRelated: A product phase often begins as nuclei at reactant contacts or defects.
Manganese noduleRelated: A nucleus provides the surface around which a nodule begins to form.
Flash evaporationRelated: Vapor bubbles need nuclei to form and grow during liquid flashing.
MistRelated: Water droplets often begin growing around aerosol particles suspended in the air.