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Mixed Forced and Natural Convection Mass Transfer

2 Mixed Forced and Natural Convection Mass Transfer [Pg.35]

The data correlations presented in the previous section include both forced convection and free convection processes. In nature as well as engineering applications, there are [Pg.35]

Additivity of Grashof numbers. For the combined mixed free-convection heat and mass transfer the procedure is to replace the Grj or GrA with Grj + GrA, the sum. For example. Equation 2.31 in Table 2.3 becomes [Pg.36]

The limitation on this procedure is Sca — Pr and this is frequently the case for transport processes in air. Since the thermal Grashoff number is normally much larger, neglecting the interaction would greatly underestimate the MTC. [Pg.36]

Free convection heat transfer as a source of forced convection mass transfer. It has been demonstrated on numerous occasions that the Chilton-Colburn analogy appearing in Table 2.3 is applicable for converting a forced-convection Nusselt number to a forced-convection Sherwood number as a means of converting the imbedded HTC into its equivalent MTC. In the present situation, the thermal buoyant forces provide the momentum source, which in effect provides the forced-convective flow that drives the mass transfer process. In addition, Grj Gta and Sc Pr. For this case the alternative equation is [Pg.36]




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Convection mass transfer

Convection mixing

Convective mixing

Forced convection

Forced convection mass transfer

Forced mixing

Mass convection

Mass force

Mass forced convection

Mass transfer/mixing

Mixing and mass transfer

Mixing nature

Natural and forced convection

Natural convection

TRANSFER MIXING

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