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Gradient limitations

A recent paper by Schechter and Farley (S3) presented a modification of the Hadamard approach to relate circulation and mass transfer rates to interfacial tension gradients. Limited to creeping flow regimes, their approach appears to be the best to date. [Pg.84]

Separation Dynamics. The mass transport dynamics of the system were examined with respect to extraction, back extraction, and time interval between extraction and back extraction. Concentration gradients limited by diffusion rate must be considered that is, equilibrium with homogenous concentrations of analyte does not describe this system. [Pg.347]

In Figure 25-31 c, we want to see whether a steeper gradient could be used to reduce the run time. The gradient limits were the same as in trace b, but tc was reduced to 20 min. Peaks 6 and 7 are not fully resolved with the shorter gradient time. Trace b represents reasonable conditions for the gradient separation. [Pg.583]

Two final points should be made regarding the hydrate pressure-temperature limits shown in Figures 7.11a,b. The intersection of the phase boundary with the geothermal gradient limits the lower stability depth of hydrates. In Section 7.4.2, it will be shown that this intersection usually coincides with the BSR, an approximate exploration tool, which is caused by a seismic velocity decrease from hydrates above, to gas below the reflector. [Pg.569]

The uptake of compounds from the atmosphere by plants involves primarily direct partitioning of the compound into the leaf matrix or the deposition of contaminated particles on the leaf surface. In the former, one must consider both an equilibrium process and a kinetically limited transition where the concentration gradient limits diffusion into the leaf that has a high capacity to accept the compound. These three processes have been considered in a recent analysis" of the distribution of compounds from the atmosphere into plants. The rate of change in the amount of chemical in a plant resulting from gaseous uptake is expressed... [Pg.114]

The system of Eq. (17.4) is a partial derivative hyperbolic system, whose numerical solution is achieved using shock-capturing numerical methods [10-13]. These methods are characterized by second-order accuracy and therefore they give rise to spurious oscillation when high gradients are present in the solution field. To suppress the occurrence of numerical instabilities, flux limiting techniques, or gradient limiters are used [8]. [Pg.510]

End user considerations, for example, availability of technology, technique preferences, chromatographic gradient limitations. [Pg.435]

Consider a shear flow with a shear rate y = dux y)/dy. In this case, there is a tangential stress on the reference surface because of the velocity gradient normal to the plane. In the small gradient limit, the dynamic viscosity, t), is defined as the coefficient of proportionality between the tangential stress, pyx, and the normal gradient of the imposed velocity gradient. [Pg.13]


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See also in sourсe #XX -- [ Pg.199 ]




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