A THEORY OF TIDAL MIXING IN AN ESSENTIALLY VERTICALLY HOMOGENEOUS ESTUARY
1953
MAXIMON, L.C. | MORGAN, G.W.
An equation is derived governing the distribution of a solute in an estuary in which river flow and tides are the predominant factors and in which dynamic and mixing conditions can be described by a simple physical model. Various generalizations of the model are discussed, and an equation is derived which allows for time dependence of the quantities involved and the for introduction of solute into the estuary by an external agent.
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书目信息
其它主题
External; *water flow; Time dependence
语言
英语
许可
http://stinet.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0010185Approved for public release; distribution is unlimited.
类型
Text
来源
BROWN UNIV PROVIDENCE RI DIV OF APPLIED MATHEMATICSDTIC AND NTIS
团体作者
BROWN UNIV PROVIDENCE RI DIV OF APPLIED MATHEMATICS
2013-06-15
AGRIS AP
