Evaluation Of Plume Rise Models From Tall Stacks In Moist Atmospheres

This paper presents a plume rise model, called Ml, capable of dealing with complex atmospheric profiles -wind shear and thermal stratification- since it performs a numerical integration, along the plume trajectory, of a set of differential equations derived from the balance of mass, momentum and ene...

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Published inWIT Transactions on Ecology and the Environment Vol. 9
Main Authors Gangoiti, G, Sancho, J, Ibarra, G, Alonso, L, Garcia, J A, Navazo, M, Durana, N, Ilardia, J L
Format Journal Article
LanguageEnglish
Published Southampton W I T Press 01.01.1995
Subjects
Atmospheric models
Differential equations
Evaporation
Numerical integration
Thermal stratification
Water
Water vapor
Wind shear
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Summary:This paper presents a plume rise model, called Ml, capable of dealing with complex atmospheric profiles -wind shear and thermal stratification- since it performs a numerical integration, along the plume trajectory, of a set of differential equations derived from the balance of mass, momentum and energy in the plume. The model deals with a mixture of four components -dry combustion gas, dry air, water vapor and liquid water- to allow for condensation and/or re-evaporation within the plume. Profile shapes of temperature and velocity of the pl
Bibliography:SourceType-Other Sources-1
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ISSN:1746-448X
1743-3541
DOI:10.2495/AIR950161