Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Equilibrium diffusion

With this relationship for all samples was calculated from ninh This M is used for evaluating the reaction data. The ultracen rifuge (u.c measurements were carried out in a Spinco model E analytical ultracentrifuge, with 0.4% solutions in 90% formic acid containing 2.3 M KCl. By means of the sedimenta- ion diffusion equilibrium method of Scholte (13) we determine M, M and M. The buoyancy factor (1- vd = -0.086) necessary for tSe calculation of these molecular weights from ultracentrifugation data was measured by means of a PEER DMA/50 digital density meter. [Pg.141]

Physical absorption depends on properties of the gas stream and liquid solvent, such as density and viscosity, as well as specific characteristics of the contaminants in the gas and the liquid stream (e.g., diffusivity, equilibrium solubility). [Pg.225]

CE is a technique with a very high power of resolution. This is attributed to low diffusion and high plate numbers obtained from the absence of band-broadening factors (e.g., eddy diffusion, equilibrium dynamics, etc.) other than diffusion, which is also minimized by short analysis time. [Pg.164]

Given the very small amount of protein present in a single crystal relative to the concentrations of DCL components, it is clear that amplification in the usual sense cannot occur. It is conceivable, however, that the protein structure influences equilibrium distribution of hydrazones in microcosm within the crystal. Conversely, it is possible that any DCC equilibrium is irrelevant, and that the hydrazone binding being observed by X-ray diffraction is due to a diffusion equilibrium of essentially static components between solution and solid state. [Pg.58]

Between the free CSF space and the extracellular space there is a diffusion equilibrium for macromolecules. The intra/extracellular barrier and the blood-brain barrier are essentially lipid barriers, retaining small hydrophilic molecules but allowing the passage of lipophilic molecules up to approximately 500 Da... [Pg.7]

In this chapter, we review the current status of doping of SiC by ion implantation. Section 4.2 examines as-implanted depth profiles with respect to the influence of channeling, ion mass, ion energy, implantation temperature, fluence, flux, and SiC-polytype. Experiments and simulations are compared and the validity of different simulation codes is discussed. Section 4.3 deals with postimplant annealing and reviews different annealing concepts. The influence of diffusion (equilibrium and nonequilibrium) on dopant profiles is discussed, as well as a comprehensive review of defect evolution and electrical activation. Section 4.4 offers conclusions and discusses technology barriers and suggestions for future work. [Pg.114]

Sorption of soil Advection - diffusion Equilibrium soil-water partitioning... [Pg.6]

Describe the relation between sedimentation/diffusion equilibrium and the barometric equation. [Pg.101]

In this chapter we shall thus study two electro-diffusion equilibrium phenomena are related to the above feature. (Note that the right-hand side of (2.1.2) satisfies the condition (2.1.4) but is not positive definite.) Both phenomena reflect the peculiar response of the equilibrium ionic systems described by (2.1.2) to the increase of the electric charge carried by some of their parts. [Pg.24]

Above 120 km. the atmosphere is essentially in diffusive equilibrium (34). For the altitude interval between 80 and 120 km. Colegrove et al. (6) estimated an average vertical eddy diffusion coefficient of 4 X 106 cm.2 sec."1 by a careful evaluation of the 0/02 concentration ratio profile over this altitude interval. Using their eddy diffusion coefficient and following the procedure of Kellogg (22) it is estimated that molecular... [Pg.148]

Section Type Auxiliary concentrations Mean diffusion Equilibrium Rate constant ... [Pg.328]

The earth s atmosphere extends some 600 to 1500 kilometers into space. Two factors are involved in this great extension of the atmosphere. First, above about 100 kilometers, the atmospheric temperature increases rapidly with altitude, causing an outward expansion of the atmosphere far beyond that which would occur were die temperature within the bounds observed at the earth s surface. Second above Ihis dislance. the atmosphere is sufficiently rarefied so that the different atmospheric constituents attain diffusive equilibrium distributions in the gravitational field the lighter... [Pg.155]

The simplest case is a mixture of gases with no thermodiffusion or entrainment. Under a temperature gradient, diffusion equilibrium in such a mixture is achieved for constant partial pressure of each component. [Pg.339]

When a state of sedimentation-diffusion equilibrium has been reached, the molecular or particle mass can, therefore, be evaluated without a knowledge of the diffusion coefficient (and, hence, independently of shape and solvation) by determining relative concentrations at various distances from the axis of rotation. Molecules as small as sugars have been studied by this technique. [Pg.36]

This standard method of density gradient centrifugation, however, has a serious disadvantage. Because of the sedimentation and diffusion equilibrium formation of the density profile the time needed for orie experiment amounts to more than 15 hours. [Pg.240]

Speciation is best carried out directly in the aquatic system, without sampling. This has been possible since the development of Diffusive Equilibrium in Thin Films (DET) and Diffusive Gradient in Thin Films (DGT) probes.31 The DET probe consists of a very thin gel layer that is immersed in the aquatic system and allowed to equilibrate with the bulk solution. The concentration of solutes in the gel is similar to that in the bulk solution for all solutes that can diffuse through the pore openings of the gel (some gels have open pores >5 nm and some gels have restricted pores <1 nm). The DGT... [Pg.123]

Leermakers, M., Y. Gao, C. Gabeille, et al. 2005a. Determination of high resolution pore water profiles of trace metals in sediments of the Rupel River (Belgium) using DET (diffusive equilibrium in thin films) and DGT (diffusive gradients in thin films) techniques. Water Air Soil Pollut. 166 265-286. [Pg.134]

Two experimental runs were performed. The H2S- and CO2 mole fluxes were obtained from the measured concentration curves by numerical differentiation and are plotted in figure 8a,b together with penetration and film model calculations. It is evident that forced desorption can be realized under practical conditions and can be predicted by the model. In general, measured H2S mole fluxes are between the values predicted by the models, whereas the CO2 forced desorption flux is larger than calculated by the models. The CO2 absorption flux, on the other hand, can correctly be calculated by the models. This probably implies that the rate of the reverse reaction, incorporated in equation (5), is underestimated. Moreover, it should be kept in mind that especially the results of the calculations in the forced desorption range are very sensitive to indirectly obtained parameters (diffusion, equilibrium constants and mass transfer coefficients) and the numerical differentiation technique applied. [Pg.389]

Scholte, Th. G., "Determination of Thermodynamic Parameters of Polymer-Solvent Systems from Sedimentation-Diffusion Equilibrium in the Ultracentrifuge," J. Polym. Sci., Part A-2, 8, 841 (1970b). [Pg.180]

Afer the foaming is complete, the blowing agent is replaced with air due to diffusion. The moment at which the diffusion equilibrium is achieved is influenced by the following factors ... [Pg.209]

From all these factors the time necessary fo a diffusion equilibrium may be a few years, as shown by Kiister (Fig. 33b). Carbon dioxide which is often used as a blowing agent has a lower heat conductivity (0.014 kcal/mxh°C) than air (0.023 kcal/m x h °C at 20 °C). Thus, COj would seem tobe of advantage in the manufacture of high-quality heat insulating fomns. However, most polymers are much more permeable to COj than to air, thus the former tends to be rapidly displaced by the latter. Hence, despite its attractively low thermoconductivity. [Pg.210]

Kt, for a simple diffusion process is unity. That is, at diffusion equilibrium, the concentration of the solute is the same on both sides of thfe membrane, Thus, the AC for the movement of the solute from side 1 to side 2 under nonequilibrium conditions is given by ... [Pg.194]

Fractionation within the hydrosphere occurs almost exclusively during vapor-to-liquid or vapor-to-solid phase changes. For example, it is evident from the vapor pressure data for water (21.0, 20.82, and 19.51 mm Hg for H2 0, H2 0, and HD O, respectively) that the vapor phase is preferentially enriched in the lighter molecular species, the extent depending on the temperature (Raleigh distillation). The progressive formation and removal of raindrops from a cloud and the formation of crystals from a solution too cool to allow diffusive equilibrium between the crystal interior and the liquid, that is, isotopic reactions carried out in such a way that the products are isolated immediately after formation from the reactants, show a characteristic trend in isotopic composition. [Pg.199]

We now pass to the explicit calculation of entropy production. We shall consider here the very important special case in which mechanical and thermal equilibrium are already established. Mechanical equilibrium excludes the production of entropy by viscous flow, while uniformity of temperature, which is necessary for thermal equilibrium, excludes the internal production of entropy arising from the transport of heat between two regions at different temperatures. Similarly we assume that diffusion equilibrium has been attained within each phase of the system. The only production of entropy which can take place in a system of this kind is that associated with chemical reactions, with the transport of matter from one phase to another, or in general with any change which can be expressed in terms of a reaction co-ordinate... [Pg.37]

In these numbers Gc is the interfacial concentration gradient and under diffusive equilibrium given by... [Pg.372]

Equation (3) applies strictly to the diffusive equilibrium with Gint = G jk at the interface. However, for large ratios of thermal to solutal diffusivity, it has been shown to hold also in the transient stage , if G c/k is replaced by the time-dependent interfacial concentration Cint t)- Hence... [Pg.384]


See other pages where Equilibrium diffusion is mentioned: [Pg.2185]    [Pg.450]    [Pg.247]    [Pg.187]    [Pg.343]    [Pg.322]    [Pg.41]    [Pg.328]    [Pg.1941]    [Pg.130]    [Pg.211]    [Pg.211]    [Pg.2434]    [Pg.386]    [Pg.29]   
See also in sourсe #XX -- [ Pg.375 ]

See also in sourсe #XX -- [ Pg.215 ]




SEARCH



Correlation function equilibrium diffusion

Diffuse equilibrium in thin films

Diffusion and Phase Equilibrium

Diffusion equilibrium techniques

Diffusion equilibrium times

Diffusion equilibrium with sedimentation

Diffusivities under equilibrium conditions

Dynamic equilibrium solid-state diffusion

Equilibrium Between Sedimentation and Diffusion

Equilibrium and diffusivities

Equilibrium diffusion, globally-coupled

Equilibrium solid-state diffusion

Global dynamics equilibrium diffusion

Non-equilibrium distribution of adsorbing ions along the diffuse layer

Non-equilibrium surface forces of diffusion-electrical nature in

Perfectly mobile equilibria the mean diffusion coefficient

Sedimentation-diffusion equilibrium

Sedimentation-diffusion equilibrium method

Sorbent Selection Equilibrium Isotherms, Diffusion, Cyclic

© 2024 chempedia.info