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Diffusive type transport

The data of figure 2 demonstrate, that at the present choice (3=0,25 in reesterification reaction course only antipersistent (subdiffusive) transport processes are possible (a=l is achieved for low-molecular substances with Df= 0 only), i.e., active time is always smaller than real time. This indicates on the important role of Levy flights in strange diffusion type definition. [Pg.246]

In natural systems there are two types of transport phenomena (1) transport by random motion, and (2) transport by directed motion. Both types occur at a wide range of scales from molecular to global distances, from microseconds to geological times. Well-known examples of these types are molecular diffusion (random transport) and advection in water currents (directed transport). There are many other manifestations such as dispersion as a random process (see Chapters 24 and 25) or settling of suspended particles due to gravitation as a directed transport. For simplicity we will subdivide such transport processes into those we will call diffusive for ones caused by random motions and those called advective for ones resulting from directed motions. [Pg.779]

Strictly speaking, equations 19-52 and 19-53 are valid only if the pollutant cloud is infinitely long. A more realistic situation is treated in Box 19.2 here a pollutant patch of finite length L along the x-axis is eroded on both edges due to diffusion processes (turbulence, dispersion, etc.). Again, the boundary is of the diffusive type since the transport characteristics on both sides of the boundary are assumed to be identical. [Pg.868]

Besides Knudsen diffusion, permselective transport of gases can occur by various mechanisms involving molecular scale interactions of the sorption-diffusion type. These can be broadly classified into three groups as described below and pictured in Fig. 7. [Pg.356]

Figure 3.10 Contour lines represented by the ratio (v), defined as the diffusive salt transport (tidal driven) to the total landward salt flux as related to contours of Froude [Fm = Uf/(ghAp/p)1/2] Richardson numbers [Rig = (g[Ap/p][U( /b])/U ]. A clear decrease is found when moving from Type 1 to Type 3 estuaries (From Fisher, 1976, as modified by Jay et al., 2000, with permission.)... Figure 3.10 Contour lines represented by the ratio (v), defined as the diffusive salt transport (tidal driven) to the total landward salt flux as related to contours of Froude [Fm = Uf/(ghAp/p)1/2] Richardson numbers [Rig = (g[Ap/p][U( /b])/U ]. A clear decrease is found when moving from Type 1 to Type 3 estuaries (From Fisher, 1976, as modified by Jay et al., 2000, with permission.)...
The driving force for the transport is provided by a concentration gradient as the reactant moves further towards the center of the pellet its concentration is decreased by reaction. The resistance to the transport mainly originates from collisions of the molecules, either with each other or with the pore walls. The latter dominate when the mean free path of the molecules is larger than the pore diameter. Usually both type of collisions are totally random, which amounts to saying that the transport mechanism is of the diffusion type. Hence the rate of transport, expressed as a molar flux in mol mp2 s-1, in the case of equimolar counterdiffusion can be written as ... [Pg.270]

Now, we have to identify V2 and Vu. To do so, we consider the case of two connected stochastic processes where each process is a diffusion type with two states. The example concerns one marked particle that is subjected to a two-state diffusion displacement. The particle can be considered as a molecular species (so the particle movement describes a mass transport process) and we can also take into account the total enthalpy of the process (heat transport process). This particular case of stochastic model, can be described with the assembly of relations (4.79). In the model, the mean probability of the existence of local species (e nj) and the mean probability of the existence of local enthalpy (ej 2) given by the assembly... [Pg.240]

Applications of ultrasonic techniques to solid-gas systems rely on the fact that velocity and attenuation of US-waves in porous materials is closely related to pore size, porosity, tortuosity, permeability and flux resistivity. Thus, the flux resistivity of acoustic absorbents oan be related to US attenuation [118,119], while the velocity of slow longitudinal US is related to pore tortuosity and diffusion, and transport properties, of other porous materials [120]. Ultrasound attenuation is very sensitive to the presence of an external agent suoh as moisture in the pore space [121] and has been used to monitor wetting and drying prooesses [122] on the other hand, US velocity has been used to measure the elastic coefficients of different types of paper and correlate them with properties such as tensile breaking strength, compressive strength, etc. [123]. [Pg.382]

Flow along uncharged surfaces has been considered in secs. I.6.4f and e. surface conduction in sec. I.6.6d and mixed transport phenomena, simultaneously involving electrical, mechanical and diffusion types of transport In sec. 1.6.7. Specifically the Nemst-Planck equation ((1.6.7.1 or 2]) is recalled, formulating ion fluxes caused by the sum-effect of diffusion, conduction and convection. [Pg.478]

The main processes governing the pharmacokinetics of a chemical are absorption, distribution, metabolism, and excretion. In PBPK models, distribution of a chemical is characterized by blood flow rates to each organ and tissue, and partitioning of the chemical between tissue and blood. These processes are commonly modeled using two alternative types of assumptions flow-Umited and diffusion-limited transport. The flow-limited assumption implies that equilibration between free and bound fractions in blood and tissue is rapid, and that concentrations of the chemical in the venous blood exiting a tissue and in the tissue are at equilibrium. The tissue is assumed to be a homogeneous... [Pg.1072]


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