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    Initial Stage of Natural Convection Over a Hot Aerosol Sphere

    Source: Journal of Fluids Engineering:;2007:;volume( 129 ):;issue: 006::page 695
    Author:
    Elaad Mograbi
    ,
    Ezra Bar-Ziv
    DOI: 10.1115/1.2734195
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: Background: Analytical study is presented on the transient problem of buoyancy-induced motion due to the presence of a hot aerosol sphere in unbounded quiescent fluid. Method of Approach: Because the initial flow field is identically zero, the initial stage of the process is governed by viscous and buoyancy forces alone where the convective inertial terms in the momentum and energy balances are negligible, i.e., the initial development of the field is a linear process. The previous statement is examined by analyzing the scales of the various terms in the Navier-Stokes and energy equations. This scale analysis gives qualitative limitations on the validity of the linear approximation. A formal integral solution is obtained for arbitrary Prandtl number and for transient temperature field. Results: We consider, in detail, the idealized case of vanishing Prandtl number for which the thermal field is developed much faster than momentum. In this case, analytical treatment is feasible and explicit expressions for the field variables and the drag acting on the particle are derived. Detailed quantitative analysis of the spatial and temporal validity of the solution is also presented. Conclusions: The linear solution is valid throughout space for t<10 diffusion times. For t>10, an island in space appears in which inertial effects become dominant. The transient process is characterized by two different time scales: for short times, the development of the field is linear, while for small distances from the sphere and finite times, it is proportional to the square root of time. The resultant drag force acting on the sphere is proportional to the square root of time throughout the process.
    keyword(s): Force , Momentum , Flow (Dynamics) , Buoyancy , Temperature , Drag (Fluid dynamics) , Natural convection , Approximation , Equations , Particulate matter , Aerosols , Diffusion (Physics) AND Motion ,
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      Initial Stage of Natural Convection Over a Hot Aerosol Sphere

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    https://yetl.yabesh.ir/yetl1/handle/yetl/135978
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    contributor authorElaad Mograbi
    contributor authorEzra Bar-Ziv
    date accessioned2017-05-09T00:24:11Z
    date available2017-05-09T00:24:11Z
    date copyrightJune, 2007
    date issued2007
    identifier issn0098-2202
    identifier otherJFEGA4-27247#695_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/135978
    description abstractBackground: Analytical study is presented on the transient problem of buoyancy-induced motion due to the presence of a hot aerosol sphere in unbounded quiescent fluid. Method of Approach: Because the initial flow field is identically zero, the initial stage of the process is governed by viscous and buoyancy forces alone where the convective inertial terms in the momentum and energy balances are negligible, i.e., the initial development of the field is a linear process. The previous statement is examined by analyzing the scales of the various terms in the Navier-Stokes and energy equations. This scale analysis gives qualitative limitations on the validity of the linear approximation. A formal integral solution is obtained for arbitrary Prandtl number and for transient temperature field. Results: We consider, in detail, the idealized case of vanishing Prandtl number for which the thermal field is developed much faster than momentum. In this case, analytical treatment is feasible and explicit expressions for the field variables and the drag acting on the particle are derived. Detailed quantitative analysis of the spatial and temporal validity of the solution is also presented. Conclusions: The linear solution is valid throughout space for t<10 diffusion times. For t>10, an island in space appears in which inertial effects become dominant. The transient process is characterized by two different time scales: for short times, the development of the field is linear, while for small distances from the sphere and finite times, it is proportional to the square root of time. The resultant drag force acting on the sphere is proportional to the square root of time throughout the process.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleInitial Stage of Natural Convection Over a Hot Aerosol Sphere
    typeJournal Paper
    journal volume129
    journal issue6
    journal titleJournal of Fluids Engineering
    identifier doi10.1115/1.2734195
    journal fristpage695
    journal lastpage701
    identifier eissn1528-901X
    keywordsForce
    keywordsMomentum
    keywordsFlow (Dynamics)
    keywordsBuoyancy
    keywordsTemperature
    keywordsDrag (Fluid dynamics)
    keywordsNatural convection
    keywordsApproximation
    keywordsEquations
    keywordsParticulate matter
    keywordsAerosols
    keywordsDiffusion (Physics) AND Motion
    treeJournal of Fluids Engineering:;2007:;volume( 129 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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