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Titlebook: Atmospheric Dispersion of Heavy Gases and Small Particles; Symposium, Delft, Th Gijsbert Ooms,Hendrik Tennekes Conference proceedings 1984

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https://doi.org/10.1007/978-3-658-32672-2sion is derived for the rate constant for long term resuspension for which we can assume most of the particles in the well are in quasi-equilibrium at the point of minimum potential. The rate constant is seen to depend upon:
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Von der Funktionenlehre zur Analysistion of liquid aerosols, the mean density and temperature of the cloud. Finally, when the effects of gravity are small, the transition from the gravity spreading model to a turbulent diffusion model takes place. Results are presented for pressurized propane releases at various exit velocities and different initial aerosol mass fraction.
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Zur Autonomie der Literaturwissenschaft,ich becomes more pronounced as the relative heaviness of the plume is increased..A comparison of plume boundary data and mean concentration data with available wind and water tunnel data show reasonable agreement and indicate that water channel modelling of heavy gas spills may be an attractive alternative to wind tunnel modelling.
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978-3-642-82291-9Springer-Verlag Berlin, Heidelberg 1984
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