2 edition of Slag transport models for vertical and horizontal surfaces found in the catalog.
Slag transport models for vertical and horizontal surfaces
L. S. H. Chow
1978 by Dept. of Energy, [Office of Energy Research], Argonne National Laboratory, for sale by the National Technical Information Service] in Argonne, Ill, [Springfield, Va .
Written in English
|Statement||by L. S. H. Chow and T. R. Johnson, Engineering Division|
|Series||ANL/MHD ; 78-1|
|Contributions||Johnson, Terry R., joint author, Argonne National Laboratory. Engineering Division, United States. Dept. of Energy|
|The Physical Object|
|Pagination||60 p. :|
|Number of Pages||60|
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Get this from a library. Slag transport models for vertical and horizontal surfaces. [L S H Chow; Terry R Johnson; Argonne National Laboratory.
Engineering Division.; United States. Department of Energy.]. Horizontal convergence and divergence of air in the general circulation induce vertical motions (Figure and Figure ) but the associated vertical wind speeds are only in the range m s-1 (compare to m s-1 for typical horizontal wind speeds).
The resulting time scale for vertical transport from the surface to the tropopause. 10 Vertical transport near the surface Vertical transport near the surface is often modeled with a turbulent diffusion coefficient K z = α z where αis a constant and z is Size: 36KB.
During the mids, Pasquill () and Gifford () described the estimation of the horizontal and vertical standard deviation of a continuous plume concentration distribution, which constituted the basis for the construction of the so-called Gaussian dispersion models.
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The thermophysical and chemical properties of the slag are defining the Slag transport models for vertical and horizontal surfaces book and limitations of the gasification process. In this study, the fundamental thermophysical properties of bioliq slags are determined, in order to describe the heat transfer and the flow of the slag across the reactor by CDF-modelling of the bioliq-gasifier within Cited by: 7.
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The motion is driven by an externally applied constant heat flux imposed across the vertical cylinder while the horizontal surfaces are adiabatic. All surfaces. In both seasons, poleward transport of already warm air masses contributes around 20% and is favored by a poleward shift of the North Atlantic storm track.
Finally, about 40% of the air masses in winter are of an Arctic origin and experience diabatic heating by surface Author: Lukas Papritz. The South China Sea (SCS) is located within the tropical-subtropical rim of the western North Pacific Ocean and is among one of the largest marginal seas in the world with an area that measures approximately × 10 6 km 2 ().There is a wide shallow continental shelf (isobaths.
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The freeze lining microstructure forming on water cooled steel surface in a high-silica, slag cleaning furnace slag of a direct-to-blister copper smelter is mostly glassy or amorphous.
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As such, they produce forecasts for the average over an atmospheric layer between the vertical-coordinate surfaces, not on the surfaces themselves. This File Size: KB. For a horizontal surface, the pressure is uniform over the area so that the pressure force acts at the centroid of the area.
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A vertical take-off and landing (VTOL) aircraft is one that can hover, take off, and land vertically. This classification can include a variety of types of aircraft including fixed-wing aircraft as well as helicopters and other aircraft with powered rotors, such as cyclogyros/cyclocopters and tiltrotors.
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These measurements have a spatial and temporal resolution of about km and 12 hr, by: 8. Convection From a Rectangular Plate Abstract Introduction Thermodynamic and Transport Properties of Air Characteristic Length Dimensionless Quantities Natural Convection Vertical Plate Horizontal Plate T Inclined Plate The natural convective surface conductivity from a vertical plate is between the conductivities of upward facing and.
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In transport theory, the transport rate per unit surface area of a certain quantity (e.g. of mass, momentum, heat) is called flux; for example, the dimensions of mass flux are M t-1 L Also, the change of a certain quantity with distance is called gradient; for example, the File Size: KB.
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Past studies of the climatic behavior of water on Mars have universally assumed that the atmosphere is the sole pathway available for volatile exchange between the planet's crustal and polar reservoirs of H 2 O. However, if the planetary inventory of outgassed H 2 O exceeds the pore volume of the cryosphere by more than a few percent, then a subpermafrost groundwater system of global extent Cited by: Outboard tail.
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