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Verification of the plume rise/dispersion model USPR: plume rise for single stack emissions
Ecological Modelling, 1985Abstract Despite proliferation of the use of air pollution models for regulatory application, major discrepancies still occur between models and also between models and observations, especially when oversimplistic models are used. The problem of predicting plume rise (and subsequently ground level concentrations) from a single source is evaluated ...
B. Henderson-Sellers, S.E. Allen
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Journal of Wind Engineering and Industrial Aerodynamics, 2011
Antonio Donateo +2 more
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Antonio Donateo +2 more
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Science of the Total Environment, 2023
CO2 emissions from power plants are the dominant source of global CO2 emissions, thus in the context of global warming, accurate estimation of CO2 emissions from power plants is essential for the effective control of carbon emissions.
Yingsong Li +11 more
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CO2 emissions from power plants are the dominant source of global CO2 emissions, thus in the context of global warming, accurate estimation of CO2 emissions from power plants is essential for the effective control of carbon emissions.
Yingsong Li +11 more
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Stable Plume Rise in a Shear Layer
Journal of the Air & Waste Management Association, 2007Solutions are given for plume rise assuming a power-law wind speed profile in a stably stratified layer for point and finite sources with initial vertical momentum and buoyancy. For a constant wind speed, these solutions simplify to the conventional plume rise equations in a stable atmosphere.
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Buoyant plume rise in a Lagrangian framework
Atmospheric Environment. Part A. General Topics, 1992For the dispersion of buoyant material, the interaction with the environment by entrainment forms a serious obstacle for a formulation in a Lagrangian framework. Nevertheless an outline is given here on how buoyant plume rise in a Lagrangian sense could be described.
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1982
Anyone involved with diffusion calculations becomes well aware of the strong dependence of maximum ground concentrations on the “effective stack height,” he. For most conditions χmax is approximately proportional to he−2, as has been recognized at least since 1936 (Bosanquet and Pearson).
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Anyone involved with diffusion calculations becomes well aware of the strong dependence of maximum ground concentrations on the “effective stack height,” he. For most conditions χmax is approximately proportional to he−2, as has been recognized at least since 1936 (Bosanquet and Pearson).
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Journal of Engineering Physics, 1979
Measurements have been made on the hydrodynamic and thermal components of plume rise above stacks; working formulas are derived.
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Measurements have been made on the hydrodynamic and thermal components of plume rise above stacks; working formulas are derived.
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Measurements of the rise of hot plumes
Atmospheric Environment (1967), 1968Abstract Measurements of plume rise from a 76.3 m stack situated on the highveld of South Africa indicate that: 1. (I) The plume rise at 1000 m downwind is greater than that given by presently used equations. The plume shape is often scimitar-like, convex to the ground, instead of concave to the ground. It is suggested that convection effects are
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The Rise of Strongly Radioactive Plumes
Journal of Applied Meteorology, 1967Abstract The presence of radioactive gases in a plume, such as could occur in the event of a nuclear reactor accident, leads to the addition of buoyancy to the plume at an approximately linear rate. Buoyancy might also be added to plumes by chemical reactions, radiation, or latent heat exchange. The resulting plume rise is calculated by a model similar
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On the rise of vertical plumes
1977The equations expressing the conservation of mass, vertical momentum and energy are solved analytically for the rise of buoyant plumes in calm atmospheric conditions. The separate and joint effects of entrainment and drag on plume behavior are discussed.
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