Eddies definition

The field that generates these eddy currents is, by its nature, anisotropic, i e the eddy current signal response is directionally dependent on probe orientation. This can be used advantageously if one bears in mind that the corroded material one aims to detect usually displays random peaks and valleys, while man-made edges have a definite orientation. 

According to Eddy, as quoted by Small, the analgesic action of neopine, n omorphine, 6-acetylneomorphine or 3 6-diacetylneomorphine (p. 218) is definitely less than that of morphine and its corresponding analogues. The first two are about half as toxic as codeine and morphine respectively, and the second pair are more toxic than their morphine analogues. None of the four shows the Straub reaction and the convulsant action is less marked. 

The work of Higbie laid the basis of the penetration theory in which it is assumed that the eddies in the fluid bring an element of fluid to the interface where it is exposed to the second phase for a definite interval of time, after which the surface element is mixed with the bulk again. Thus, fluid whose initial composition corresponds with that of the bulk fluid remote from the interface is suddenly exposed to the second phase. It is assumed that equilibrium is immediately attained by the surface layers, that a process... 

The mean velocity of eddies changes at a definitive distance called the scale of motion (SOM) (11). The bigger these eddies are, the longer is the SOM [(9), Sec. 4]. Apart from large scale eddies, a number of small scale eddies ... 

Equation (4) applies to the steady flow of a fluid between parallel plates. The velocity is the time average for the flow at the point in question. A corresponding definition of eddy viscosity in a circular conduit may be evolved in which the radial deficiency is substituted for the distance from the wall in Eq. (4). 

The term A is related to the flow profile of the mobile phase as it traverses the stationary phase. The size of the stationary phase particles, their dimensional distribution, and the uniformity of the packing are responsible for a preferential path and add mainly to the improper exchange of solute between the two phases. This phenomenon is the result of Eddy diffusion or turbulent diffusion, considered to be non-important in liquid chromatography or absent by definition in capillary columns, and WCOT (wall coated open tubular) in gas phase chromatography (Golay s equation without term A, cf. 2.5). 

As shown in Table III, several authors (Fidaleo and Moresi, 2005a Kraaijeveld et al., 1995 Kuroda et al., 1983 Sonin and Isaacson, 1974) established power function relationships between the Sherwood number (Sh) and the Reynolds (Re) and Schmidt (Sc) numbers in ED cells equipped with different eddy promoters, even if different definitions of the equivalent diameter were used to calculate the Reynolds number. 

For multiphase flow that is normally encountered in fluidized bed reactors, there are two kinds of definitions of the micro-scale first, it is the scale with respect to the smaller one between Kolmogorov eddies and particles second, it is the scale with respect to the smallest space required for two-phase continuum. If the first definition is adopted, the... 

The boundary conditions normally associated with Equation (9.14) are known as the Danckwerts or closed boundary conditions. They are obtained from mass balances across the inlet and outlet of the reactor. We suppose that the piping to and from the reactor is small and has a high Re. Thus, if we were to apply the axial dispersion model to the inlet and outlet streams, we would find Din = Dout = 0, which is the definition of a closed system. See Figure 9.8. The flux in the inlet pipe is due solely to convection and has magnitude Qi ain. The flux just inside the reactor at location z = 0+ has two components. One component, Qina(0+), is due to convection. The other component, —DAc[da/dz 0+, is due to diffusion (albeit eddy diffusion) from the relatively high concentrations at the inlet toward the lower concentrations within the reactor. The inflow to the plane at z = 0 must be matched by material leaving the plane at z = 0+ since no reaction occurs in a region that has no volume. Thus,... 

When the turbulence is not too large, the main force on the droplets is caused by the shear imposed by the surrounding eddies. With the help of the Kolmogorov theory for turbulent flow, the external, disrupting force is can estimated as Text = V(e /c)- We then end up with a definition of the critical Weber number ... 

These redox cells can operate on a number of scales that depend on the length of the diffusion path from the point that the oxidised form becomes reduced to the point where it reduces another sediment constituent. In some pelagic cores these diffusion paths can be observed in linear portions of the pore-water profiles (e.g. Sawlan Murray, 1983). Here the sedimentation rate and the carbon burial rate are sufficiently low, relative to diffusion, to extend the processes of early diagenesis over tens of metres into the sediment. In coastal environments the sedimentation rate and the concentration and reactivity of the organic matter is often high, which results in a much more complex pattern. In this case, the distances between the cells are much shorter, since by definition the adjustment must occur more rapidly. Like laminar and turbulent flow, there may come a point where the flow of electrons downwards is better dispersed through eddies , which in this case are transitory micro-environments with small-scale three dimensional diffusion, rather than more stable... 

The eddy concept was thus introduced. An eddy still eludes precise definition, but in one interpretation it is conceived to be a turbulent motion, localized within a region of a certain size, that is at least moderately coherent over this region. The region of a large eddy can also contain smaller eddies. 

The cyclonic eddy-like structures, similar to eddies 10 and 15 (Figure la) and 9-11 (Figure 4), are typical of the Kuroshio Current area east of Taiwan. They have been detected on many ERS-1/2 SAR images however, their position is variable. These eddies were observed due to their radar contrast against the background and/or the presence of definite structures (narrow spiral lines), resulting from the modulation of surface roughness by variable currents. Filamentary slicks were much less common here to favour their detection. Estimates of the current velocity for two eddies obtained by the analysis of the oil spill displacements were found to be 0.07-0.08 ms"1 and 0.3 ms"1. 

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