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Titlebook: Viscous Flows; Stretching and Shrin Ahmer Mehmood Book 2017 Springer International Publishing AG 2017 Boundary layer flow.Stretching / shri

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書目名稱Viscous Flows
副標題Stretching and Shrin
編輯Ahmer Mehmood
視頻videohttp://file.papertrans.cn/984/983581/983581.mp4
概述Provides in-depth insight into boundary layer flow problems.Covers the turbulent flow due to stretching and shrinking.Written by an expert in the field.Includes supplementary material:
叢書名稱Mathematical Engineering
圖書封面Titlebook: Viscous Flows; Stretching and Shrin Ahmer Mehmood Book 2017 Springer International Publishing AG 2017 Boundary layer flow.Stretching / shri
描述This authored monograph provides a detailed discussion of the?boundary layer flow due to a moving plate. The topical focus lies on the 2- and 3-dimensional case, considering axially symmetric and unsteady flows.?The author derives a?criterion for the self-similar and non-similar?flow, and the turbulent flow due to a stretching or shrinking sheet is also discussed. The target audience primarily comprises research experts in the field of boundary layer flow, but the book will also be beneficial for graduate students..
出版日期Book 2017
關(guān)鍵詞Boundary layer flow; Stretching / shrinking surface; Self-similar flow; Non-similar flow; Turbulent flow
版次1
doihttps://doi.org/10.1007/978-3-319-55432-7
isbn_softcover978-3-319-85659-9
isbn_ebook978-3-319-55432-7Series ISSN 2192-4732 Series E-ISSN 2192-4740
issn_series 2192-4732
copyrightSpringer International Publishing AG 2017
The information of publication is updating

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Ahmer Mehmood sciences. According to these arguments, it is a necessary condition for the existence of objective values that values form part of what John Mackie called ‘the fabric of the world’ (Mackie 1977, 15). On this view, objectivity entails mind independence: the domain of objectivity is a domain of exist
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Turbulent Flow Due to Moving Continuous SurfacesThe turbulent flow due to moving continuous surfaces is another aspect of the viscous boundary-layers in addition to the laminar flows presented in the previous two?parts.
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