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Titlebook: Environmental Hydraulics: Stratified Flows; Stratified Flows Flemming Bo Pedersen Textbook 1986 Springer-Verlag Berlin Heidelberg 1986 Ocea

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書目名稱Environmental Hydraulics: Stratified Flows
副標(biāo)題Stratified Flows
編輯Flemming Bo Pedersen
視頻videohttp://file.papertrans.cn/313/312693/312693.mp4
叢書名稱Coastal and Estuarine Studies
圖書封面Titlebook: Environmental Hydraulics: Stratified Flows; Stratified Flows Flemming Bo Pedersen Textbook 1986 Springer-Verlag Berlin Heidelberg 1986 Ocea
描述The present lecture notes cover a first course in th~ most common types of stratified flows encountered in Environ- mental Hydraulics. Most of the flows are buoyancy flows, i.e. currents in which gravity acts on small density differences. Part I presents the basic concepts of stagnant, densit- stratified water, and of flowing non-miscible stratified fluids. The similarity to the (presumed) well-known open channel flow, subject to a reduced gravity, is illustrated. Part II treats the miscible density stratified flows. In outlining the governing equations, the strong coupling between the turbulence (the mixing) and the mean flow is emphasized. The presentation and discussions of the basic governing equa- tions are followed by illustrative examples. Separate chapters are devoted to Dense Bottom Currents, Free Penetrative Convec- tion, Wind-driven Stratified Flow, Horizontal Buoyancy Flow and Vertical jet/plumes. Part III presents some examples of practical problems solved on the basis of knowledge given in the present lecture notes. It is the author‘s experience that the topics treated in chapter 8 and in the subsequent chapters are especially well- suited for self-tuition, followed b
出版日期Textbook 1986
關(guān)鍵詞Ocean; convection; environment; flow; hydraulics; turbulence; wind; fluid- and aerodynamics
版次1
doihttps://doi.org/10.1007/978-3-642-86600-5
isbn_softcover978-3-540-16792-1
isbn_ebook978-3-642-86600-5Series ISSN 0724-5890
issn_series 0724-5890
copyrightSpringer-Verlag Berlin Heidelberg 1986
The information of publication is updating

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0724-5890 of the flows are buoyancy flows, i.e. currents in which gravity acts on small density differences. Part I presents the basic concepts of stagnant, densit- stratified water, and of flowing non-miscible stratified fluids. The similarity to the (presumed) well-known open channel flow, subject to a redu
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A Comparative Study of Korean Literaturef ambient water into the jet, and the sediment fall-out from the jet. Based on a large number of laboratory experiments the rate of entrainment is determined, as well as the condition for incipient sediment fall-out. Further, a simple model for the sediment fall-out along the path line of the jet has been outlined and checked upon measurements.
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Siebrecht van der Spoel,Robert Pieter Heyman Contrary to homogeneous fluids, this weight generally is a function of space and time due to the mixing of water masses of different temperature, salinities, concentration of suspended particles etc. The density of sea water is discussed in Appendix (read it!).
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