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Mass transport migration component

The mass transport of package components to the product is known as migration and the mass transport of product components to the package as scalping. Permeation means the mass transport of components through the package in both directions. [Pg.6]

Under realistic conditions a balance is secured during current flow because of additional mechanisms of mass transport in the electrolyte diffusion and convection. The initial inbalance between the rates of migration and reaction brings about a change in component concentrations next to the electrode surfaces, and thus gives rise to concentration gradients. As a result, a diffusion flux develops for each component. Moreover, in liquid electrolytes, hydrodynamic flows bringing about convective fluxes Ji j of the dissolved reaction components will almost always arise. [Pg.20]

If the overall mass control comprises three components - migration, convection and diffusion - which form of mass transport is the most effective ... [Pg.23]

The first two terms describe the contributions to the mass transport that are the result of forces that act on the species O. The first term is the diffusion component, which relates to the forces that act on O in the concentration gradient close to an electrode. (Do is the diffusion coefficient of O, C0(x, t) is the concentration of the species O at the distance x and the time t and thus 3Cq(x, t)/dx is the concentration gradient.) The second term is the migration... [Pg.139]

The flux, Jo(x, t), is defined as the transport of O per unit area (mol s cm ). It can be divided into three components, diffusion, migration, and convection, as originally expressed in the Nernst-Planck equation, written for one-dimensional mass transport along the x-axis in Eq. 18. [Pg.504]

Mass transport assumes the flow of all dissolved components together with water, underground gas or oil in the direction of their flow. That is why the path and rate of mass transport depend first of all on the nature and rate of fluid migration. Mass transport by water is subject to the laws of hydrodynamics and are defined by gradients of hydrostatic head. Rates of the mass transport cannot exceed average real velocity of migration of the transporter itself Exactly mass transport is responsible for mass exchange within boxmdaries of the lithosphere and for the formation of most deposits of economic minerals. [Pg.495]

The solution of equations (2.40) and (2.41) with the total accounting of all acting factors is quite complex. So the problem is simplified by excluding secondary factors, which may be disregarded. The exact solution of the migration problem of individual component in conditions of advective-dispersive mass transport without approximations is called the analytical solution. [Pg.513]

The rate of mass transport depends not only on the diffuse and advective mixing. Significant impact on the rate of mass transport have chemical and biochemical processes. In the process of migration, components may form. [Pg.525]

The mass transport toward the electrode has three components diffusion, migration, and convection. [Pg.3735]

Migration Cell Population Dynamics and Mass Transport Continuous, Discrete, and Hybrid Models for Tissue Growth A Modeling Framework for Jn Vitro Tissue Cultivation Components of the Hybrid Multiscale Model Results and Discussion References... [Pg.194]

Uncharged reaction components are transported by diffusion and convection, even though their migration fluxes are zero. The total flux density Jj of species j is the algebraic (vector) sum of densities of all flux types, and the overall equation for mass balance must be written not as Eq. (4.1) but as... [Pg.20]

Advective transport, or simply advection, refers to movement of chemical mass within a flowing fluid or gas. For our purposes, it is most commonly migration of aqueous species along with groundwater. In constructing a transport model, we prefer to consider how much of the thermodynamic components - the total masses of the basis entries Aw, A(, A, and Am - move, rather than track migration of the free masses of each individual aqueous species. [Pg.287]


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See also in sourсe #XX -- [ Pg.2 , Pg.16 ]




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