In the atmospheric ice accretion process, the spreading of the impinging droplet is an important factor in determining the deposit density and morphology. In this work we present low-density ice aggregates grown in laboratory by impinging supercooled monodisperse droplets in comparisons with results of ballistic numerical model.
Monodisperse droplet distribution in the ice accretion process
PRODI, Franco;PORCU', Federico
1996
Abstract
In the atmospheric ice accretion process, the spreading of the impinging droplet is an important factor in determining the deposit density and morphology. In this work we present low-density ice aggregates grown in laboratory by impinging supercooled monodisperse droplets in comparisons with results of ballistic numerical model.File in questo prodotto:
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