The Effect of the Concentration of Water Droplets in an Aerosol Cloud on Their Evaporation Rate

Opis bibliograficzny
Parent link:Technical Physics Letters
Vol. 48, iss. 3.— 2022.— [P. 142-146]
1. autor: Volkov R. S. Roman Sergeevich
organizacja autorów: Национальный исследовательский Томский политехнический университет Инженерная школа энергетики Научно-образовательный центр И. Н. Бутакова (НОЦ И. Н. Бутакова), Национальный исследовательский Томский политехнический университет Исследовательская школа физики высокоэнергетических процессов
Kolejni autorzy: Kerimbekova S. A. Susanna Aleksandrovna, Strizhak P. A. Pavel Alexandrovich
Streszczenie:Title screen
The results of an experimental study of the integral evaporation characteristics of water droplets that are present in the composition of an aerosol cloud are described. Parameters, such as the initial radius of the droplets (0.1–0.25 mm), their concentration (0.03–0.1 L/m3), and the temperature of combustion products (573–873 K), are varied. The ranges of variation of the weight rate of water evaporation as function of the concentration of droplets in the aerosol cloud and their initial sizes are established. Approximation expressions for the established dependences are obtained. An approach is proposed for determining the rate of evaporation of aerosol droplets, which takes into account the known values of the evaporation rate of a single droplet.
Режим доступа: по договору с организацией-держателем ресурса
Wydane: 2022
Hasła przedmiotowe:
Dostęp online:https://doi.org/10.1134/S1063785022040137
Format: Elektroniczne Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=668514
Opis
Streszczenie:Title screen
The results of an experimental study of the integral evaporation characteristics of water droplets that are present in the composition of an aerosol cloud are described. Parameters, such as the initial radius of the droplets (0.1–0.25 mm), their concentration (0.03–0.1 L/m3), and the temperature of combustion products (573–873 K), are varied. The ranges of variation of the weight rate of water evaporation as function of the concentration of droplets in the aerosol cloud and their initial sizes are established. Approximation expressions for the established dependences are obtained. An approach is proposed for determining the rate of evaporation of aerosol droplets, which takes into account the known values of the evaporation rate of a single droplet.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1134/S1063785022040137