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Flux condition

Trial 1 Estimate area. A, for maximum flux condition, limiting Q/A to 12,000 Btu/hr-fT surface for organic materials. Experience has shown that a value of 6,000-8,000 is a good starting value for Q/A for organics. [Pg.198]

Testing procedures for corrosion inhibitors in heat flux conditions are discussed below. [Pg.1003]

T2. Tippets, F. E., Analysis of the critical heat flux condition in high pressure boiling water flow, ASME Paper No. 62-WA-161 (1962). [Pg.293]

This velocity profile is commonly called drag flow. It is used to model the flow of lubricant between sliding metal surfaces or the flow of polymer in extruders. A pressure-driven flow—typically in the opposite direction—is sometimes superimposed on the drag flow, but we will avoid this complication. Equation (8.51) also represents a limiting case of Couette flow (which is flow between coaxial cylinders, one of which is rotating) when the gap width is small. Equation (8.38) continues to govern convective diffusion in the flat-plate geometry, but the boundary conditions are different. The zero-flux condition applies at both walls, but there is no line of symmetry. Calculations must be made over the entire channel width and not just the half-width. [Pg.290]

The zero flux condition at the closed outlet requires a zero gradient, thus... [Pg.248]

Another approach to the determination of surface kinetics in these systems has been to combine molecular beams in the 10 2-10 1 mbar pressure range with the use of the infrared chemiluminescence of the C02 formed during steady-state NO + CO reactions. This methodology has been used to follow the kinetics of the reaction over Pd(110) and Pd(l 11) surfaces [49], The activity of the NO + CO reaction on Pd(l 10) was determined to be much higher than on Pd(lll), as expected based on the UHV work discussed in previous sections but in contrast with result from experiments under higher pressures. On the basis of the experimental data on the dependence of the reaction rate on CO and NO pressures, the coverages of NO, CO, N, and O were calculated under various flux conditions. Note that this approach relied on the detection of the evolution of gas-phase... [Pg.77]

Because the components of the analytical expression for C are not sufficiently known to permit an analytical evaluation, C is determined empirically as a function of the local quality at the point of DNB, XDNB, (under nonuniform heat flux conditions) and the bulk mass flux, G. The empirically determined expression for C is... [Pg.362]

Predictions of a nonuniform heat flux, DNB non obtained by using <7dNB(W.3), f°r uniform heat flux in a single tube and the shape factor, Fc, agree very well with the measured nonuniform flux condition, DNB non of Biancone et al. (1965), Judd et al. (1965), and Lee and Obertelli (1963), as shown in Figure 5.70. [Pg.438]

The correlation predicts the source data of 3,607 CHF data points under axially uniform heat flux condition from 65 test sections with an average ratio of 0.995 and RMS deviation of 7.2%. [Pg.452]

Flash photolysis studies with absorption or delayed fluorescence detection were performed to compare the binding of ground and excited state guests with DNA.113,136 The triplet lifetimes for 5 and 6 were shown to be lengthened in the presence of DNA.136 The decays were mono-exponential with the exception of the high excitation flux conditions where the triplet-triplet annihilation process, a bimo-lecular reaction, contributed to the decay. The residence time for the excited guest was estimated to be shorter than for the ground state, but no precise values for the rate constants were reported. However, the estimated equilibrium constants for the... [Pg.193]

We now get a fairly good feeling that handling boundary conditions in two dimensions is significantly more difficult than those of one-dimensional problems. Flux conditions can be applied to the boundaries using the method of fictitious points. [Pg.170]

For the one-dimensional equation with x as the space variable, the diffusion equation is a partial differential equation of the first order in time and the second order in x. It therefore requires concentration to be known everywhere at a given time (in general =0) and, at any time t>0, concentration, flux, or a combination of both, to be known in two points (boundary conditions). In the most general case, the diffusion equation is a partial differential equation of the first order in time and the second order in the three space coordinates x, y, z. Concentration or flux conditions valid at any time >0 must then be given along the entire boundary. [Pg.420]

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 6. Normalized NILS hydrogen concentration CL / C at steady state vs. normalized distance R/b from the crack tip for the full-field (crack depth wh=0.2) and MBL (domain size L=h-a) solutions under zero hydrogen flux conditions on the OD surface and remote boundary, respectively. The parameter b denotes the crack tip opening displacement for each case. The inset shows the concentrations near the crack tip. Figure 6. Normalized NILS hydrogen concentration CL / C at steady state vs. normalized distance R/b from the crack tip for the full-field (crack depth wh=0.2) and MBL (domain size L=h-a) solutions under zero hydrogen flux conditions on the OD surface and remote boundary, respectively. The parameter b denotes the crack tip opening displacement for each case. The inset shows the concentrations near the crack tip.
The factors 4 and 4 accormt for the heterogeneity of the interface. The interfacial flux conditions. Equations (6.56) and (6.57), can be straightforwardly applied at plain interfaces of the PEM with adjacent homogeneous phases of water (either vapor or liquid). However, in PEFCs with ionomer-impregnated catalyst layers, the ionomer interfaces with vapor and liquid water are randomly dispersed inside the porous composite media. This leads to a highly distributed heterogeneous interface. An attempt to incorporate vaporization exchange into models of catalyst layer operation has been made and will be described in Section 6.9.4. [Pg.403]

Monod kinetics are often a better description of the reactions occurring in sediment. Assume that the flux conditions are similar to problem 2 for SOD. The maximum bacterial growth rate is 0.5 hr in these sediments, and the halfsaturation coefficient is 1 g/m of oxygen. What is the microbacterial population for the 0.5- and 5-g/m -day cases (Hint, use a change of variables to solve for / = dCIdz.) Plot oxygen concentration for each case on the same scale as for problem 2 and compare the two plots. [Pg.53]

These boundary conditions, illustrated in Figure E5.5.2, will give us a concentration front, but in two dimensions. In addition, we have a zero flux condition that will require an image solution. We will use the solution of Example 2.7 to develop a solution for this problem. The solution, before applying boundary conditions, was... [Pg.118]

However, a quadratic representation of the radial concentration profile may not be adequate since application of zero flux conditions at the inner thermal well and outer cooling wall with a quadratic profile reduces to an assumption of uniform radial concentrations. Although additional radial... [Pg.147]

Modeling of the packed bed catalytic reactor under adiabatic operation simply involves a slight modification of the boundary conditions for the catalyst and gas energy balances. A zero flux condition is needed at the outer reactor wall and can be obtained by setting the outer wall heat transfer coefficients /iws and /iwg (or corresponding Biot numbers) equal to zero. Simulations under adiabatic operation do not significantly alter any of the conclusions presented throughout this work and are often used for verification... [Pg.149]

Until now we have tacitly assumed that the boundary separates two identical media, for instance, hypolimnetic and epilimnetic water bodies, as in Illustrative Example 19.1. We can intuitively understand that (as stated by Eqs. 19-3 and 19-12) the net flux across the boundary is zero if the concentrations are equal on either side. Yet, how do we treat a boundary separating different phases, for instance, water and air Obviously, the equations have to be modified since we cannot just subtract two concentrations, CA and CB, which refer to different phases, for instance, mole per m3 of water and mole per m3 of air. In such a situation the equilibrium (no flux) condition between the two phases is not given by CA = CB. [Pg.844]

This boundary condition might apply for solute absorption with its rate moderated by some thin passive surface layer. Note that the surface concentration at x = 0 must be a function of time to maintain the constant-flux condition (see Fig. 5.7). [Pg.112]

To deal with this more complex problem, we follow Sekerka et al. [2] and Sekerka and Wang [3] and first establish a general analysis that allows for these changes of volume. The previous melting problem was solved by first obtaining independent solutions to the diffusion equation in each phase and then coupling them via the Stefan flux condition at the interface, similar approach can be employed for the present problem. To accomplish this, it is necessary to identify suitable frames for analyzing the diffusion in each phase and then to find the relations between them necessary to construct the Stefan condition. [Pg.504]


See other pages where Flux condition is mentioned: [Pg.159]    [Pg.1740]    [Pg.685]    [Pg.302]    [Pg.337]    [Pg.70]    [Pg.177]    [Pg.15]    [Pg.182]    [Pg.335]    [Pg.436]    [Pg.572]    [Pg.879]    [Pg.340]    [Pg.130]    [Pg.171]    [Pg.271]    [Pg.124]    [Pg.164]    [Pg.47]    [Pg.174]    [Pg.104]    [Pg.880]    [Pg.72]    [Pg.225]    [Pg.128]    [Pg.241]   
See also in sourсe #XX -- [ Pg.91 , Pg.93 , Pg.97 , Pg.98 ]

See also in sourсe #XX -- [ Pg.108 , Pg.109 , Pg.114 , Pg.116 ]




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Boundary conditions flux condition

Boundary conditions heal flux

Boundary conditions specified heal flux

Boundary conditions specified heat flux

Boundary conditions surface flux

Boundary conditions zero-flux wall

Case study prediction of permeate flux decay during ultrafiltration performed in pulsating conditions by a hybrid neural model

Case study prediction of permeate flux decay during ultrafiltration performed in pulsating conditions by a neural model

Conditional fluxes

Conditional fluxes

Conditional fluxes acceleration

Conditional fluxes reaction/diffusion

Conditional fluxes the unclosed terms

Constant flux boundary condition

Critical heat flux, local condition concept

Equal flux condition

F Approximate Results for Surface Temperature with Specified Heat Flux or Mixed Boundary Conditions

FLUX RELATIONS UNDER REACTIVE CONDITIONS

Flux boundary conditions

Flux-Matching Conditions at a Surface

Heat Conduction with Flux Boundary Conditions

Heat flux boundary conditions

Self-flux condition

Separation of Variables for Parabolic PDEs with Two Flux Boundary Conditions

Slab with Nonhomogeneous Flux Boundary Conditions

Slab with Nonhomogeneous Flux Boundary Conditions during Charging of a Battery

Zero flux boundary condition

Zero-flux surface condition

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