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Vortex-chemical

Vortex-Chemical Its incipient development phase does not allow its use a degree of force level is called for. [Pg.241]

Figure 7-9. Agitator flow patterns, (a) Axial or radial impellers without baffles produoe vortex, (b) Off-oenter looation reduoes the vortex, (o) Axial impeller with baffles, (d) Radial impeller with baffles. (Source Wales, S. M., Chemioal Prooess Equipment—Seleotion and Design, Butterworths Series in Chemical Engineering, 1988.)... Figure 7-9. Agitator flow patterns, (a) Axial or radial impellers without baffles produoe vortex, (b) Off-oenter looation reduoes the vortex, (o) Axial impeller with baffles, (d) Radial impeller with baffles. (Source Wales, S. M., Chemioal Prooess Equipment—Seleotion and Design, Butterworths Series in Chemical Engineering, 1988.)...
In the 1990s, Bakker and Van den Akker (1994, 1996)—see also R.A. Bakker s PhD thesis (1996)—continued this mechanistic modeling approach by attempting a completely deterministic description of the 3-D small-scale flow field in which the chemical reactions take place at the pace the various species meet. Starting point is a lamellar structure of layers intermittently containing the species involved in the reaction. These authors conceived such small-scale structures as Cylindrical Stretched Vortex (CSV) tubes being strained in the direction of their axis and—as a result—shrinking in size in a plane normal to... [Pg.210]

R possesses a spherical core of radius a consisting of quark matter with CFL condensate surrounded by a spherical shell of hadronic matter with thickness R — a containing neutron and proton superfluids. The triangular lattice of singly quantized neutron vortices with quantum of circulation irh/jj, forms in response to the rotation. Since the quark vortices carry SttTj/fi quantum of circulation, the three singly quantized neutron vortices connect at the spherical interface with one singly quantized quark vortex so that the baryon chemical potential is continuous across the interface [19]. [Pg.270]

These speculations about the ionic, polar, or electronic nature of chemical bonding, which arose largely from solution theory, resulted mostly in static models of the chemical bond or atom structure. In contrast is another tradition, which is more closely identified with ether theory and electrodynamics. This tradition, too, may be associated with Helmholtz, especially by way of his contributions to nineteenth-century theories of a "vortex atom" that would explain chemical affinities as well as the origin of electromagnetism, radiation, and spectral lines. [Pg.150]

What kind of solution was expected from physicists As we have seen, many chemists, from Lavoisier on, expected that fundamental chemical problems would be accessible to mathematical solution, meaning not just precise quantification or geometrical explanation but algebraic formulation on mechanical principles. 32 For all the resentment of statements by Kelvin or Boltzmann that chemistry could be reduced to vortex atoms or the kinetics of atoms,33 many nineteenth-century chemists shared Kekule s vague presentiment... [Pg.292]

The first step in all RNA isolation protocols involves lysing the cell in a chemical environment that denatures ribonucleases. The RNA is then fractionated from other cellular macromolecules by either homogenizing the tissue (dissected brain tissue) or simply vortexing the sample (very small tissues and laser-microdissected sample) without further homogenization. The cell type from which the RNA is to be isolated, the sample size, and the eventual use of the RNA will determine which procedure described here is appropriate. [Pg.352]

For example, while the vortex-averaged 03 concentration at one altitude in the Arctic in the spring of 1994 was measured to decrease by 10%, the net chemical loss was estimated at 20% but this was partially compensated by an increase due to transport of air containing higher ozone concentrations from higher altitudes (Manney et al., 1995). Similar amounts of chemical ozone loss in the Arctic polar vortex have been calculated based on measurements of CIO, BrO, and 03 (e.g., Brune et al., 1991 Salawitch et al., 1993). [Pg.697]

Tuck, A. F., Synoptic and Chemical Evolution of the Antarctic Vortex in Late Winter and Early Spring, 1987, J. Geophys. Res., 94, 11687-11737 (1989). [Pg.724]

Simulation of the Dynamical Response of the Arctic Vortex to Aerosol-Associated Chemical Perturbations in the Lower Stratosphere, Geophys. Res. Lett., 23, 1525-1528 (1996). [Pg.726]

The details of the transitions and the vortex behavior depend on the actual channel dimensions and wall-temperature distributions. In general, however, for an application like a horizontal-channel chemical-vapor-deposition reactor, the system is designed to avoid these complex flows. Thus the ideal boundary-layer analysis discussed here is applicable. Nevertheless, one must exercise caution to be sure that the underlying assumptions of one s model are valid. [Pg.329]

Figure 1. This graph shows the rapid variation of CIO and 03 as the edge of the chemically perturbed region in the Antarctic polar vortex is penetrated by the National Aeronautics and Space Administration (NASA) ER-2 high-altitude aircraft over the Palmer Peninsula of Antarctica on September 16, 1987 (5). It is one of a series of 12 snapshots, or individual flights, during the Airborne Antarctic Ozone Experiment (AAOE) that show the development of an anticorrelation between CIO and 03 that began as a correlation in mid-August. When these two measurements are combined with all the others from the ER-2 aircraft, the total data set provides a provocative picture of how such chemistry occurs and what it is capable of doing to ozone. Figure 1. This graph shows the rapid variation of CIO and 03 as the edge of the chemically perturbed region in the Antarctic polar vortex is penetrated by the National Aeronautics and Space Administration (NASA) ER-2 high-altitude aircraft over the Palmer Peninsula of Antarctica on September 16, 1987 (5). It is one of a series of 12 snapshots, or individual flights, during the Airborne Antarctic Ozone Experiment (AAOE) that show the development of an anticorrelation between CIO and 03 that began as a correlation in mid-August. When these two measurements are combined with all the others from the ER-2 aircraft, the total data set provides a provocative picture of how such chemistry occurs and what it is capable of doing to ozone.
Many draw nozzles, especially those in the bottom of vessels, plug because of the presence of vortex breakers. Many designers routinely add complex vortex breakers to prevent cavitation in pumps. But vortex breakers are needed only in nozzles operating with high velocities and low liquid levels. Corrosion products, debris, and products of chemical degradation can more easily foul and restrict nozzles equipped with vortex breakers. [Pg.336]


See other pages where Vortex-chemical is mentioned: [Pg.380]    [Pg.198]    [Pg.668]    [Pg.376]    [Pg.440]    [Pg.1138]    [Pg.198]    [Pg.198]    [Pg.210]    [Pg.264]    [Pg.294]    [Pg.338]    [Pg.352]    [Pg.206]    [Pg.885]    [Pg.68]    [Pg.82]    [Pg.344]    [Pg.343]    [Pg.431]    [Pg.73]    [Pg.411]    [Pg.223]    [Pg.92]    [Pg.112]    [Pg.210]    [Pg.216]    [Pg.220]    [Pg.34]    [Pg.127]    [Pg.674]    [Pg.700]    [Pg.720]    [Pg.721]    [Pg.495]    [Pg.290]    [Pg.155]    [Pg.157]   
See also in sourсe #XX -- [ Pg.241 ]




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