书签 分享 收藏 举报 版权申诉 / 66
上传文档赚钱

类型流体力学与传热课件Heterogeneous-Flow-and-Separation.ppt

  • 上传人(卖家):晟晟文业
  • 文档编号:5145357
  • 上传时间:2023-02-14
  • 格式:PPT
  • 页数:66
  • 大小:617.50KB
  • 【下载声明】
    1. 本站全部试题类文档,若标题没写含答案,则无答案;标题注明含答案的文档,主观题也可能无答案。请谨慎下单,一旦售出,不予退换。
    2. 本站全部PPT文档均不含视频和音频,PPT中出现的音频或视频标识(或文字)仅表示流程,实际无音频或视频文件。请谨慎下单,一旦售出,不予退换。
    3. 本页资料《流体力学与传热课件Heterogeneous-Flow-and-Separation.ppt》由用户(晟晟文业)主动上传,其收益全归该用户。163文库仅提供信息存储空间,仅对该用户上传内容的表现方式做保护处理,对上传内容本身不做任何修改或编辑。 若此文所含内容侵犯了您的版权或隐私,请立即通知163文库(点击联系客服),我们立即给予删除!
    4. 请根据预览情况,自愿下载本文。本站不保证下载资源的准确性、安全性和完整性, 同时也不承担用户因使用这些下载资源对自己和他人造成任何形式的伤害或损失。
    5. 本站所有资源如无特殊说明,都需要本地电脑安装OFFICE2007及以上版本和PDF阅读器,压缩文件请下载最新的WinRAR软件解压。
    配套讲稿:

    如PPT文件的首页显示word图标,表示该PPT已包含配套word讲稿。双击word图标可打开word文档。

    特殊限制:

    部分文档作品中含有的国旗、国徽等图片,仅作为作品整体效果示例展示,禁止商用。设计者仅对作品中独创性部分享有著作权。

    关 键  词:
    流体力学 传热 课件 Heterogeneous Flow and Separation
    资源描述:

    1、3.Heterogeneous Flow and Separation 3.1 Flow Past Immersed ObjectsDefinition of Drag Coefficient for Flow Past Immersed Objects 1.Introduction and types of drag The flow of fluids outside immersed bodies appears in many chemical engineering applications and other processing applications.For example

    2、settling,drying and filtration,and so on.2.Drag coefficient Correlations of the geometry and flow characteristics for solid objects suspended in fluid are similar in concept and form to the friction factor-Reynolds number correlation given for flow inside conduits.In flow through pipes,the friction

    3、factor was defined as the ratio of the drag force per unit area to the product of fluid density and velocity head.220 220 For flow past immersed objects the drag coefficient is obtained by substituting CD for the friction factor Kf in equation(1.4-32)2222uCuKpDff3.1-1 therefore2/2uCAFpDDfThe Reynold

    4、s number for a particle in a fluid is defined as0ReuDpFrom dimensional analysis,the drag coefficient of a smooth solid in an incompressible fluid depends upon a Reynolds number and the necessary shape ratios.For a given shape(Re)DC3.1-2 Drag coefficients of typical shapes For each particular shape o

    5、f object and orientation of the object with respect to the direction of flow,a different relation of CD versus Re exists.Correlations of drag coefficient versus Reynolds number are shown in figure.These curves have been determined experimentally.However,in the laminar region for low Reynolds numbers

    6、,less than about 1.0,the experimental drag force for a sphere is the same as the theoretical Stokes law equation as follows:03uDFpD03uDFpDpDDuF033.1-3 Combining Eqs.(3.1-1)and(3.1-3)and solving for CD,the drag coefficient predicted by Stokes law isRe24242/020uDuAFCpD3.1-4 The variation of CD with Re

    7、 is quite complicated because of the interaction of the factors that control skin drag and form drag.For a sphere,as the Reynolds number is increased beyond the Stokes law range,separation occurs and a wake is formed.Further increases in Re cause shifts in the separation point.At about Re=3105 the s

    8、udden drop in CD is the result of the boundary layer becoming completely turbulent and the point of separation moving downstream.In the region of Re about 1103 to 2105,the drag coefficient is approximately constant for each shape and CD=0.44 for a sphere.3.1.2 Flow through Beds of Solids 1.Introduct

    9、ion A system of considerable importance in chemical and other process engineering fields is the packed bed,which is used for a fixed-bed catalytic reactor,adsorption of a solute,absorption,filter bed,and so on In the theoretical approach used,the packed column is regarded as a bundle of crooked tube

    10、s of varying cross-sectional area.The theory developed in Chapter 1 for single straight tubes is used to develop the results for the bundle of crooked tubes.2.Laminar flow in packed beds Certain geometric relations for particles in packed beds are used in the derivations for flow.The void fraction i

    11、n a packed bed is defined as The specific surface of a particle av is defined asppvSaFor a spherical particle,pvDa62ppDS36ppDv)1(6)1(pvDaawhere a is the ratio of total surface area in the bed to total volume of bed(void volume plus particle volume)Since(1-)is the volume fraction of particles in the

    12、bedThe average interstitial velocity in the bed is u and is related to the superficial velocity u based on the cross section of the empty container by uu 3.1-9 To determine the equivalent channel diameter De,the surface area for n parallel channels of length L is set equal to the surface-volume rati

    13、o times the particle volume S0L(1-).pveDLSaLSLDn6)1()1(003.1-6 where S0 is the cross-sectional area of the bedThe void volume in the bed is the same as the total volume of the n channelsLDnLSe2043.1-7Combining Eqs.(3.1-6)and (3.1-7)gives an equation for De132peDD3.1-8 For flow at very low Reynolds n

    14、umbers,the pressure drop should vary with the first power of the velocity and inversely with the square of the channel size,in accordance with the Hagen-Poiseulli equation for laminar flow in straight tubes.232DuLpThe equations for u(equation 3.1-9)and De(equation 3.1-8)are used in the Hagen-Poiseui

    15、lle equation22229413232pDuDuLpor 322172pDuLp3.1-11 The true L is larger because of the tortuous path.Experimental data give an empirical constant of 150 for 72Equation(3.1-12)is called the Blake-Kozeny equation for laminar flow,void fractions less than 0.5,effective particle diameter Dp,and Rep1000,

    16、the drag coefficient is approximately constant at 0.40 to 0.45,and letspptdgu75.1(3.2-19 )so the equation isCD=0.44Equation(3.2-19)is Newton law and applies only for fairly large particles falling in gases or low-viscosity fluids.Criterion for settling regime To identify the range in which the motio

    17、n of the particle lies,the velocity term is eliminated from Reynolds number by substituting ut from Eq.(3.2-16)to give,for the Stokes law range 2318Repptpgdud(3.2-21 )Re=K3/18.Re1.0,to provide a convenient criterion K,let312ppgdK(3.2-22)Then,from Eq(3.2-21),Re=K3/18.Setting Re=1.0 and solving gives

    18、K=2.6.If the size of the particle is known,K can be calculated from Eq(3.2-22).If K so calculated is less than 2.6,Stokes law applies.Substitution for ut from Eq.(3.2-19)shows that for the Newtons law range Re=1.75K1.5.In the range between Stokes law and Newtons law(2.6K68.9),the terminal velocity i

    19、s calculated from Eq(3.2-13)using a value of CD found by trial from Fig.Setting this equal to 1000 and solving gives K=68.9.Thus if K is greater than 68.9,Newtons law applies.problem1lSettling of a spherical particle in a air is followed Stokes law,if the temperature changes from 25 to 50,the termin

    20、al velocity will();if settling in liquid,the terminal velocity will()vThe terminal velocity is the velocity that the acceleration that a particle moves through the fluid approaches to()problem2lA single spherical particle settling freely in the fluid and it is laminar flow,when the particle diameter

    21、 increases,the terminal velocity u will ;when the viscosity of fluid increases,u will ;if the fluid is a gas,what happens to u if the temperature increase?lAs shown by equations(3.2-16)and(3.2-19),the terminal velocity ut varies with the square of diameter of particle in the()range,whereas in the()r

    22、ange it varies with 0.5 power of the diameter of particle l For a given packed bed,Blake-Kozeny equation indicates that the flow is()to the pressure drop and()proportional to the fluid viscosity.1、试计算直径为30m的球形石英颗粒(其密度为2650kg/m3),在20水中和20常压空气中的自由沉降速度。To calculate the terminal velocity of a spherical

    23、quartz particle,30 m in diameter and 2650kg/m3 in density,settling in the water and the air at the temperature of 20,respectively.m/s1002.81001.11881.9)9982650()1030(18)(43262gdust11038.21001.19981002.810302346ttduRe Solution:d=30m、s=2650kg/m3(1)=1.0110-3Pas and=998kg/m3for water at t=20checkIt is followed stokes low ut=8.0210-4m/sm/s1018.71081.11881.9)21.12650()1030(18)(25262gdust)210(144.01081.121.11018.710304526ttduRe(2)=1.8110-5Pas =1.21kg/m3 for the air at t=20Assuming that the type of flowing is followed stokes lawcheckut=7.1810-2m/s。

    展开阅读全文
    提示  163文库所有资源均是用户自行上传分享,仅供网友学习交流,未经上传用户书面授权,请勿作他用。
    关于本文
    本文标题:流体力学与传热课件Heterogeneous-Flow-and-Separation.ppt
    链接地址:https://www.163wenku.com/p-5145357.html

    Copyright@ 2017-2037 Www.163WenKu.Com  网站版权所有  |  资源地图   
    IPC备案号:蜀ICP备2021032737号  | 川公网安备 51099002000191号


    侵权投诉QQ:3464097650  资料上传QQ:3464097650
       


    【声明】本站为“文档C2C交易模式”,即用户上传的文档直接卖给(下载)用户,本站只是网络空间服务平台,本站所有原创文档下载所得归上传人所有,如您发现上传作品侵犯了您的版权,请立刻联系我们并提供证据,我们将在3个工作日内予以改正。

    163文库