Last edited by JoJocage
Monday, April 13, 2020 | History

2 edition of Behavior of a tall stack plume in flow over a ridge found in the catalog.

Behavior of a tall stack plume in flow over a ridge

Los Alamos Scientific Laboratory.

Behavior of a tall stack plume in flow over a ridge

  • 281 Want to read
  • 5 Currently reading

Published by [Dept. of Energy], Los Alamos Scientific Laboratory, for sale by the National Technical Information Service] in Los Alamos, N.M, [Springfield, Va .
Written in English

    Subjects:
  • Plumes (Fluid dynamics),
  • Sulphur dioxide.

  • Edition Notes

    StatementTeymoor Gedayloo ... [et al.].
    SeriesLA ; 7632-MS, LA (Series) (Los Alamos, N.M.) -- 7632-MS.
    ContributionsGedayloo, Teymoor.
    The Physical Object
    Pagination15 p. :
    Number of Pages15
    ID Numbers
    Open LibraryOL17651309M

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Behavior of a tall stack plume in flow over a ridge by Los Alamos Scientific Laboratory. Download PDF EPUB FB2

Door jet(s) given by a stack effect may produce significant effects on the flamelplume behavior. And stack effect problems imply also that the present models, such as a free plume model, are not applicable or insufficient for a confined plume.

Knowledge of flame behavior has been playing an important role in the fire safety design. On days with, neutral flow, the plume from a stack located 13 ridge heights downwind from a m ridge was carried down to ground level within a very short distance. This phenomenon could well be a result of the strong downwash that occurs near.

Volume Source. • Source Release Height is the center of the Volume Source: If the Source is from a building, the release height is set equal to one half of the building height.

• Volume sources are modeled as a square in Screen3. If the source is not square, the width should be set to the minimum Size: 4MB. Subscripts will be described in the text. Figure 1 contains a cross section of a typical through-bolted joint.

It consists of a bolt, two washers, two materials, and a nut. For the purposes of this version of the document, washers can either be considered part of the bolt or as individual layers of clamped Size: 1MB. The tall, thin building was 10 cm by 10 cm and cm tall.

The long building was 10 cm wide, 61 cm long and cm tall. The model stack had an inside diameter of cm and a wall thickness of cm. The effluent speed was main- tained in all tests at cm/sec.

Stack downwash can be avoided if the average exit velocity in the plume is more than times the mean wind speed at the stack top. To avoid the adverse effect of building downwash the height of the stack should be to the height of the nearby building whose wake can cause the plume downwash and its entrapment into the lee of the building.

Contaminants discharged into the air are transported over long distances by large-scale air-flows and dispersed by small-scale air-flows or turbulence, which mix contaminants with clean air. This dispersion by the wind is a very complex process due to the presence of different-sized eddies in atmospheric Size: 2MB.

Fig. 13 shows a SAR image of the Columbia plume front, in which the generation of multiple internal wave packets can be seen. Fig. 14 shows multiple shipborne X-band radar images, showing the passage Behavior of a tall stack plume in flow over a ridge book an internal wave packet during a plume front event over the course of about half an hour (Pan and Jay, a).

SEPUnit 6 Atmospheric Stability Subsidence Inversion Form when an extensive layer of atmosphere slowly sinks beneath a large ridge of high pressure. SEPUnit 6 Atmospheric Stability Lowering Subsidence Inversion Subsidence is a slow process that can occur over several days.

a lava flow cools very rapidly, causing the flow to shatter in a chaotic pattern B. a lava flow encounters groundwater, which causes the flow to rapidly fracture C. a lava flow erupts under deep water D.

during the final stages of cooling, a lava flow. Lee-side lows: as westerly winds blow over a mountain range, the air flow is deflected in such a way that a trough forms on the downwind (leeward) side of the mountain. Jet Streams: as the polar jet stream and its area of max winds swings over a developing mid-latitude cyclone, an area of divergence draws warm surface air upward.

Type Language Publication Year Top Authors Concepts Research Units Collaborators Open access. The influence of the rooftop structure on plume behavior for the normal wind diminished as building height increased because of an increase in size of the separated flow. Elongation distribution between tension leveler and temper mill for pickling line in Baosteel Article in Frontiers of Mechanical Engineering in China 2(3) July with 23 Reads.

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At any point in the flow, the eddies produce fluctuations in the flow velocity and pressure. If we were to measure the streamwise velocity in turbulent pipe flow, we would see a variation in time as shown in figure Figure Velocity at a point in a turbulent flow as a function of time.

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When the wind speed is above about 25 knots and flowing perpendicular to the ridge lines, the air flow can form waves, much like water flowing over rocks in a stream bed.

The waves form down wind from the ridge line and will be composed of very strong up and down drafts, plus dangerous rotor action under the crests of the waves.

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