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Wednesday, April 15, 2020 | History

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

Slag transport models for vertical and horizontal surfaces

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  • 30 Currently reading

Published 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

    Subjects:
  • Magnetohydrodynamic generators,
  • Thin films,
  • Slag

  • Edition Notes

    Statementby L. S. H. Chow and T. R. Johnson, Engineering Division
    SeriesANL/MHD ; 78-1
    ContributionsJohnson, Terry R., joint author, Argonne National Laboratory. Engineering Division, United States. Dept. of Energy
    The Physical Object
    Pagination60 p. :
    Number of Pages60
    ID Numbers
    Open LibraryOL14863378M

    This book is targeted at graduate students and researchers at HORIZONTAL SURFACES Pool boiling Nucleate boiling Film boiling Leidenfrost effect VERTICAL SURFACES Film boiling CONDENSATION Film condensation 7 FLOW PATTERNS INTRODUCTION File Size: 6MB.   Fundamentals of Transportation/Networks. From Wikibooks, open books for an open world and smoother surface, especially in urban areas, which allows faster travel, especially of wheeled vehicles. Relevant concerns include the alignment of the road, its horizontal and vertical curvature, its super-elevation or banking around curves, its. A flashcard set of 36 important terms and definitions in aeronautics. Learn with flashcards, games, and more — for free. the aircraft may be unsafe to fly as the control surfaces will have insufficient authority to safely control the aircraft. Rotation in a horizontal plane about the normally vertical axis - .


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Slag transport models for vertical and horizontal surfaces by L. S. H. Chow Download PDF EPUB FB2

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.

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