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Diffusion near-steady-state

When a clean steel coupon is placed in oxygenated water, a rust layer will form quickly. Corrosion rates are initially high and decrease rapidly while the rust layer is forming. Once the oxide forms, rusting slows and the accumulated oxide retards diffusion. Thus, Reaction 5.2 slows. Eventually, nearly steady-state corrosion is achieved (Fig. 5.2). Hence, a minimum exposure period, empirically determined by the following equation, must be satisfied to obtain consistent corrosion-rate data for coupons exposed in cooling water systems (Figs. 5.2 and 5.3) ... [Pg.99]

When the pollutant concentration difference between the source and collection reservoir becomes smaller (i. e., when the concentration of pollutants in the collection reservoir approaches that of the source reservoir), the flux rate of pollutants decreases, and a near steady state flux (Js) is obtained (Fig. 3c). At this time, the diffusion parameter (D) can be calculated using Fick s model as follows ... [Pg.201]

The diffusion parameter calculated by the root time method is an average parameter, and is generally considered to be operative over the range of time from initial diffusion flux to near steady state flux conditions. The method is applicable for the situation where adsorption and desorption occur, and for various pH values of the influent. The closer (DE) is to (DB) in Fig. 5 d, the greater is the accuracy of the D coefficient. It is important to note that in the case of low pH values of the influent, desorption of cations from a clay soil could produce conditions where C2 > C1. Accordingly, the experimental values for relative change in concentration would then become negative. [Pg.205]

Figure 32 shows a typical microelectrode voltammogram for an electro-chemically reversible system under near steady-state conditions. Of course at very fast scan rates the behaviour returns to that of planar diffusion and a characteristic transient-type cyclic voltammetric response is obtained as the mass transport changes from convergent to linear diffusion. [Pg.66]

Marcus and Noyes have discussed the effect of diffusion on observed reaction rates. Near steady state, t 5s Consequently, the real Tjct can be... [Pg.113]

It is clear that both the Thiele modulus and F increase continuously during the ignition of the catalyst, representing the shift from control by chemical kinetics to control by washcoat diffusion and external mass transfer. At near-steady state (/ = 25 sec) the process is almost completely controlled by external mass transfer, indicated by the F value of 90%. [Pg.162]

Figure 6.29 shows some example linear sweep voltammograms assuming different scan rates (Osrrefers to the dimensionless scan rate Osr = F/RT)(yrl/D)). As the experimental time scale decreases, the diffusional behavior changes from near-steady-state to near-planar diffusion. With respect to the different shapes of microparticles, the mass transport-limiting current was found to be fairly consistent that is, a difference of less than 2% for sphere and hemispheres of equal surface area. [Pg.210]

It is interesting to estimate the effective tip radius immersed in the water layer, which is responsible for a tip current of 1 pA at 1.5 V bias. As shown in Fig. 11, a polyurethane-coated W tip behaves as a microelectrode. A sigmoidal diffusion-limited current superimposed on the linear background current was obtained for the reduction of 1 mM Ru(NH3)g+ in 10 mM NaC104 solution. An effective radius estimated from the nearly steady-state current is 3 /xm. Also shown in Fig. 11 is the anodic background current due to the oxidation of W at potentials positive of 0.4 V versus SCE (curve b). From the data shown in curve c of Fig. 10 and curve b of Fig. 11, if one assumes that similar effective tip radius is responsible for both anodic and cathodic redox processes, an estimated effective contact radius of 3 nm can be obtained for a background current flow of 1 pA at a bias voltage of 1.5 V. [Pg.129]

The Gaussian expressions are not expected to be valid descriptions of turbulent diffusion close to the surface because of spatial inhomogeneities in the mean wind and the turbulence. To deal with diffusion in layers near the surface, recourse is generally made to the atmospheric diffusion equation, in which, as we have noted, the key problem is proper specification of the spatial dependence of the mean velocity and eddy diffusivities. Under steady-state conditions, turbulent diffusion in the direction of the mean wind is usually neglected (the slender plume approximation), and if the wind direction coincides with the jc axis, then =0. Thus it is necessary to specify only the lateral, Ky, and vertical, A --, coefficients. It is generally assumed that horizontal homogeneity exists so that u and A are independent of y. Hence (18.52) becomes... [Pg.943]

Transport of solute from a fluid phase to a spherical or nearly spherical shape is important in a vari of separation operations such as liquid-liquid extraction, crystallization from solution, and ion exchange. The situation depicted in Fig. 2.3-12 assumes that there is no forced or natural convection in the fluid about the particle so that transport is governed entirely by molecular diffusion. A steady-state solution can be obtained for the case of a sphere of fixed radius with a constant concentration at the interface as well as in the bulk fluid. Such a model will be useful for crystallization from vaqxtrs and dilute solutions (slow-moving boundary) or for ion exchange with rapid irreversible reaction. Bankoff has reviewed moving-boundary problems and Chapters 11 and 12 deal with adsorption and ion exchange. [Pg.92]

The semi-infinite models of Palermo [1] or van Genuchten [2] are accurate predictions of contaminant migration and resulting concentrations only imtil near steady-state conditions are reached and the influence of the conditions at the upper boimdary can no longer be ignored. The time required to achieve steady state can be estimated from the relationships below. A separate relationship is provided for advectively dominated transport and diffusion... [Pg.167]

Amatore CA, Eosset B (1992) Space variables weU fitted for the study of steady state and near-steady-state diffusion at a microdisk. J Electroanal Chem 328 21-32 Posset B, Amatore CA, Bartelt JE, Michael AC, Wightman RM (1991) Use of conformal maps to model the voltammetric response of collector-generator double-band electrodes. Anal Chem 63 306-314... [Pg.224]

Amatore CA, Fosset B (1992) Space variables well fitted for the study of steady state and near-steady-state diffusion at a microdisk. J Electroanal Chem 328 21-32... [Pg.328]

FIGURE 2-17 Principles of SECM. (a) Tip far from the substrate surface diffusion of O leads to steady-state current. (b) Tip near a conductive substrate positive feedback of O. (c) Tip near the insulating substrate hindered diffusion of O. c = concentration a = radius of tip. (Reproduced with permission from reference 55.)... [Pg.51]

The evolution of the profiles of the isotope ratio is shown in Figure 8-12, which plots the profiles at various times in the calculation. Early in the calculation, isotope ratios at shallow depths have been driven more negative by the release of isotopically light respiration carbon, but little change has occurred at greater depths. As the evolution proceeds, the ratios at shallow depths become more positive as the result of the dissolution and diffusion of heavier carbon from both above and below. In the final steady state, after some 15,000 years, the isotope ratio is nearly constant at about -0.6 per mil at depths below 100 centimeters, rising rapidly to the seawater value, +2 per mil in the top 100 centimeters. The final values reflect a balance between the release of isotopically light carbon by respiration and the release of isotopically heavy carbon by dissolution, with the additional influence of the diffusion of isotopically heavy seawater carbon. [Pg.179]

Dispersion in packed tubes with wall effects was part of the CFD study by Magnico (2003), for N — 5.96 and N — 7.8, so the author was able to focus on mass transfer mechanisms near the tube wall. After establishing a steady-state flow, a Lagrangian approach was used in which particles were followed along the trajectories, with molecular diffusion suppressed, to single out the connection between flow and radial mass transport. The results showed the ratio of longitudinal to transverse dispersion coefficients to be smaller than in the literature, which may have been connected to the wall effects. The flow structure near the wall was probed by the tracer technique, and it was observed that there was a boundary layer near the wall of width about Jp/4 (at Ret — 7) in which there was no radial velocity component, so that mass transfer across the layer... [Pg.354]

As the field of electrochemical kinetics may be relatively unfamiliar to some readers, it is important to realize that the rate of an electrochemical process is the current. In transient techniques such as cyclic and pulse voltammetry, the current typically consists of a nonfaradaic component derived from capacitive charging of the ionic medium near the electrode and a faradaic component that corresponds to electron transfer between the electrode and the reactant. In a steady-state technique such as rotating-disk voltammetry the current is purely faradaic. The faradaic current is often limited by the rate of diffusion of the reactant to the electrode, but it is also possible that electron transfer between the electrode and the molecules at the surface is the slow step. In this latter case one can define the rate constant as ... [Pg.381]


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See also in sourсe #XX -- [ Pg.199 ]




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