DIFFUSION OF MATTER EMITTED FROM A LINE SOURCE IN A NON-ISOTROPIC TURBULENT FLOW

dc.contributor.author	Fleishman, B. A.
dc.contributor.author	Frenkiel, F. N.
dc.date.accessioned	2017-06-09T14:11:12Z
dc.date.available	2017-06-09T14:11:12Z
dc.date.copyright	1955/04/01
dc.date.issued	1955
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14150.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4149680
dc.description.abstract	Turbulent diffusion from an infinite line source in a homogeneous, stationary, non-isotropic turbulent flow is studied. Spatial mean-concentration distributions are determined as functions of the statistical characteristics of turbulence. Particular attention is given to the evaluation of mean concentrations at relatively small distances from the source both upstream and downstream. At high intensities of turbulence, the resulting mean-concentration values may differ considerably from those obtained when the turbulent diffusion in the wind direction is neglected.
dc.publisher	American Meteorological Society
dc.title	DIFFUSION OF MATTER EMITTED FROM A LINE SOURCE IN A NON-ISOTROPIC TURBULENT FLOW
dc.type	Journal Paper
dc.journal.volume	12
dc.journal.issue	2
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1955)012<0141:DOMEFA>2.0.CO;2
dc.journal.fristpage	141
dc.journal.lastpage	145
dc.tree	Journal of Meteorology:;1955:;volume( 012 ):;issue: 002
dc.contenttype	Fulltext