398 APPLICATIONS IN MASS TRANSFER WITH CHEMICAL REACTION
two markedly different length scales. In particular, we considered chemisorption
whereby the solubility of a transferring solute is enhanced by chemical reaction.
The microscale–macroscale modeling methodology developed in this chapter for
mass transfer with chemical reaction can be applied equally well to other processes
involving momentum, heat, or mass transfer occurring on multiple scales, such as
phase-transition phenomena, heat transfer in dispersed phase systems, and others.
In Section 6.2 we provided an example illustrating microscale and macroscale
elements. An important consideration is that for mass transfer with chemical reac-
tions the microscale element becomes a homogeneous point source or sink term in
the macroscale balance.
Scaling analysis was applied to the microscale species-balance equations for
mass transfer in Section 6.3. Scaling led to three time scales associated with the
diffusion, reaction, and contact times. When the ratio of the diffusion to contact
time was very small, steady-state mass transfer can be assumed for the microscale
element for which film theory models are applicable. When this ratio is large,
the mass transfer is inherently unsteady-state, for which penetration theory models
can be used. For purely diffusive mass transfer a film theory model interrelated
the mass-transfer coefficient and the microscale fluid layer thickness, whereas a
penetration theory model interrelated it to the contact time.
Scaling analysis was used in Section 6.4 to develop a criterion for the slow
reaction regime for which the ratio of the diffusion to the reaction time was very
small for the microscale element. Since the chemical reaction does not occur in
the microscale element, the mass-transfer coefficient for the slow reaction regime
is the same as for purely physical absorption.
In Section 6.5, scaling analysis was used to identify a criterion for the inter-
mediate reaction regime for which the diffusion and reaction times are of equal
magnitude. For this reaction regime the chemical reaction occurs on the microscale,
which implies that the mass-transfer coefficient is greater than that for purely phys-
ical absorption.
In Section 6.6, scaling analysis was used to develop the criterion for the fast
reaction regime for which the reaction time is sufficiently fast to maintain the
bulk liquid at the reaction equilibrium concentration. In the fast reaction regime a
reaction boundary layer or region of influence exists within the microscale liquid
layer, within which the concentration of the absorbing component undergoes a
characteristic change.
In Section 6.7 we considered the criterion for the instantaneous reaction regime
for which the reaction is so fast that the reacting components cannot co-exist at
any point within the microscale element. This regime implies that the nonvolatile
liquid-phase reactant becomes rate-limiting, owing to its depletion in the microscale
liquid layer. The inner domain of the instantaneous reaction regime corresponds
to a reaction plane within the liquid layer of the microscale element at which the
concentrations of the reacting components are reduced to zero. The surface domain
of the instantaneous reaction regime corresponds to the reaction plane being at the
gas–liquid interface, for which the mass transfer becomes gas-phase controlled.