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First described by Wilhelm Ostwald in 1896.
Etymology from Wiktionary, CC BY-SA 4.0.
Today it means: An observed phenomenon in solid solutions or liquid sols, where an inhomogeneous structure changes over time, i.e. small crystals or particles dissolve and redeposit onto larger crystals or particles. Full definition →
First described by Wilhelm Ostwald in 1896.
Etymology from Wiktionary, CC BY-SA 4.0.