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Concentration fluctuations and averaging time in vapor clouds /

This book contributes to more reliable and realistic predictions by focusing on sampling times from a few seconds to a few hours. Its objectives include developing clear definitions of statistical terms, such as plume sampling time, concentration averaging time, receptor exposure time, and other ter...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Wilson, David J.
Autor Corporativo: American Institute of Chemical Engineers
Formato: Electrónico eBook
Idioma:Inglés
Publicado: New York, NY : Center for Chemical Process Safety of the American Institute of Chemical Engineers, ©1995.
Temas:
Acceso en línea:Texto completo

MARC

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245 1 0 |a Concentration fluctuations and averaging time in vapor clouds /  |c David J. Wilson. 
260 |a New York, NY :  |b Center for Chemical Process Safety of the American Institute of Chemical Engineers,  |c ©1995. 
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504 |a Includes bibliographical references (pages 157-168) and index. 
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505 0 |a Concentration Fluctuations and Averaging Time in Vapor Clouds; Contents; PREFACE; ACKNOWLEDGMENTS; 1. Background and Objectives; 2. Sampling and Averaging Time Definitions; 3. Effect of Averaging Time on Mean Calculations; 4. Concentration Fluctuation Modeling; 5. Probability Distributions; 6. Release Height and Source Size Effects on Fluctuation Intensity; 7. Source Density Effects on Fluctuations; 8. Buildings and Obstacles; 9. Threshold Crossing and Peak Levels; 10. Framework for an Operational Model. 
520 |a This book contributes to more reliable and realistic predictions by focusing on sampling times from a few seconds to a few hours. Its objectives include developing clear definitions of statistical terms, such as plume sampling time, concentration averaging time, receptor exposure time, and other terms often confused with each other or incorrectly specified in hazard assessments; identifying and quantifying situations for which there is no adequate knowledge to predict concentration fluctuations in the near-field, close to sources, and far downwind where dispersion is dominated by atmospheric t. 
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