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Convective fluxes, heat transfer, atmospheric

At later times, solar heat fluxes and convective heat transfer from the atmosphere become important. For a spill onto an insulated dike floor these fluxes may be the only energy contributions. This approach seems to work adequately for liquefied natural gas (LNG) and perhaps for ethane and ethylene. The higher hydrocarbons (C3 and above) require a more detailed heat transfer mechanism. This model also neglects possible water freezing effects in the ground, which can significantly alter the heat transfer behavior. More details on boiling pools is provided elsewhere.19... [Pg.158]

We have developed a thermal approach based on a heat balance on a reference cylinder volume in the sample to evaluate the atomic oxygen recombination. The surface of this cylinder, 6 mm diameter and 3 mm height, represents the measurement area by pyrometry. Convective phenomena are neglected (rarefied gas flows) compared to the radiative fluxes to establish the equations for steady state heat transfer under different environments. The thermal balance is established under each atmosphere standard air, air plasma, standard argon and argon plasma, the determination of the recombination flux being done by difference between the experiments under air plasma (reactive) and ai on plasma (inert) [1, 2]. [Pg.392]


See other pages where Convective fluxes, heat transfer, atmospheric is mentioned: [Pg.32]    [Pg.188]    [Pg.336]    [Pg.339]    [Pg.257]    [Pg.258]    [Pg.323]    [Pg.1030]    [Pg.201]    [Pg.368]    [Pg.258]    [Pg.864]    [Pg.16]    [Pg.2136]    [Pg.206]    [Pg.821]    [Pg.135]    [Pg.437]   


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Atmosphere fluxes

Atmospheric convection

Atmospheric flux

Convection heat flux

Convective flux

Convective heat flux

Convective heating

Heat convective

Transfer flux

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