(5.2)--Chapter 2 Steady-state heat cond传热学传热学传热学.ppt
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1、Chapter 2 Steady-state heat transfer nBasic law of heat conductionFouriers LawnMathematical description of heat conductionnAnalytical solution to typical one-dimensional steady-state heat conductionnHeat conduction through finsnOne-dimensional heat conduction with heat generationResearch method:With
2、 the assumption of continuum,the relationship between heat rate and temperature distribution of objects and other influencing factors is discussed from a macroscopic point of view.In general,most solids,liquids and gases can be considered as continuum.However,when the mean molecule free walk is not
3、negligible compared to the macroscopic size of the object,such as a lean gas whose pressure reduces to a certain extent,it cannot be considered as a continuum.2.1 Basic law of heat coauction1.Temperature field At time,the temperature distribution of all locations in the object is called temperature
4、field of the object at that moment.For steady state problems,temperature field do not change over time.Temperature field is a function of space coordinates and time.nTwo-dimension steady state:nOne-dimension steady state:nZero-dimension steady state:2.Isothermal surface,isotherm1.Isothermal surface:
5、the same moment,the temperature of each point2.Isotherm:the intersection of the isothermal surface and either sidePhotographs taken by infrared cameras,satellite optical remote sensors,etc.3.A point in an object can only have one temperature value at the same time,so the isothermal surfaces(lines)of
6、 different temperatures cannot intersect at the same time.The object studied is a continuum,and the isothermal surface(line)will not terminate inside the object.It can only terminate at the boundary of the object,or the closed surface(line)formed by itself.3.Temperature gradientnDefinition:The chang
7、e rate of temperature in the normal direction of the isothermal surface,nVector,point to the direction of temperature increaseIn a Cartesian coordinate system,temperature gradient can be expressed as:are partial derivatives in the x,y,and z directions;In the normal direction of the isothermal surfac
8、e,the temperature change rate per unit length is the largest.i,j,and k are unit vectors in the x,y,and z directions.Heat FluxThe magnitude and direction of heat flux can be expressed by the heat flux vector q:The direction of the heat flux vector points to the direction of temperature decrease.ntdAd
9、qIn a Cartesian coordinate system,the heat flux vector can be expressed as:qx,qy,qz represent the component of q in three coordinate directionsnFouriers law was obtained by French physicist Fourier in 1822.nGeneral form(i.e.written as heat flux vector)Negative sign indicates the direction of heat tr
10、ansfer is opposite to the temperature gradient4.Fouriers lawnFor isotropic materialIsotropic1.Thermal conductivity is temperature and direction dependent(anisotropic,e.g.wood,fiber,car tires)2.Value:Carbon steel 36.7,Water at 20 0.599Dry air at 20 0.0259 5.Thermal ConductivityAg 427Cu 399Pure metalT
11、hermalInsulationmaterialBuilding materialsAlloyArtificial materialSuper insulationArtificial heat pipeDry airConductivemedium Insulation materialPorous material,filled by air,3.Many materials,with comprehensive processes including heat conduction,convection and radiation,are uniformly expressed by t
12、he thermal conductivity coefficient.At this time,it is called the apparent(converted)thermal conductivity.Such as:light furnace wall(refractory fiber),cotton tire clothing,space clothing,super insulation material.4.Obtained through experiments:non-steady state measurement(quasi steady state);steady
13、state measurement5.Relationship with temperature:In engineering,linear approximations are usually available.Where:is the temperature;is a constant;is the intercept of the extension of the straight line on the ordinate.2.2 Thermal differential equations and conditions1.Statement of problem1.One-dimen
14、sional problem,can directly integrate Fouriers law to obtain heat flux.2.Multidimensional problem:Fouriers law still appliesFouriers law reveals the relationship between temperature gradient and heat flux at each point in continuous temperature field,so when the temperature distribution in the objec
15、t is obtained,the corresponding heat flux distribution can be obtained.3.The thermal differential equation is to reveal the intrinsic relationship between continuous temperature field and space coordinates and time.2.Ideas and principlesTaking a Cartesian coordinate system as an example,a micro-para
16、llel hexahedron is segmented from the object,using:1.Fouriers law2.Energy conservation law(thermal balance principle)establishes thermal differential equation1.Isotropic,homogeneous2.Uniform density,specific heat,independent of temperature(constant properties)3.Assumptions4.Derivation1.Law of conser
17、vation of energy In any time interval:Analogy:Total heat into elementHeat generation of heat sources in elementsIncrease of element energyTotal heat export elementFund from parents and siblingsMy income(scholarship,other income)Total expenditureDeposit increment in hand(+or-)1.Law of conservation of
18、 energy2.Energy increase in element within unit time Specific heat,(The amount of heat required to increase the unit mass by 1)Amount of heat required to increase the unit mass by 1 Amount of heat(internal energy)required for element to rise t per unit time 3.Heat generation of heat source in elemen
19、t within unit time Heat generated by heat source per unit volume per unit time,4.Import heatFouriers lawOn surface at ,temperature gradient is;Thermal conduction area5.export heatTaylor series expansion,take the first two itemsDue toExpressed in Taylor series,omitting high-order small quantities6.fi
20、nishingSubstituting(c)into equation(a):Substituting(d)into equation(c):(2-7)When is temperature dependent,(2-7)is heat transfer differential equation in three-dimensional Cartesian coordinate system with heat generation,non-steady state,and variable thermal conductivity.Can not mention the different
21、ial symbol outside.5.Equation formnIn three-dimensional rectangular coordinate system,heat conduction differential equation with internal heat generation,non-steady and constant thermal conductivity:nor:nwhere the Laplace calculusThermal diffusivity nHeat conduction differential equation for non-ste
22、ady,with no heat generation,and constant thermal conductivity conditions in three-dimensional rectangular coordinate system:Since,then:oror (Laplace equation)nDifferential equation of heat conduction with internal heat generation,non-steady and variable thermal conductivity in cylindrical and spheri
23、cal coordinate system,please see textbook(2-12),(2-13)on p.44.Cylindrical spherical coordinate(r,z)Spherical coordinate(r,,),Heat conductivity is large and heat capacity is small,leads to little heat transfer ,Temperature rises faster,leads to faster heat transfer6.Heat diffusion rate(Temperature co
24、nductivity coefficient)(also a property)From express,means transfer rate of temperaturene.g.:Cu:Air:Wood:nPut a copper-rod and a wood-rod in fire,then hold one end of both rods,copper-rod is hot but wood-rod is not so hot.nOnly in unsteady heat conduction,a shows its effect.7.Definite conditions nFo
25、r any differential equation,it can be solved by mathematical method.But for a specific problem,heat conduction differential equation with general solution is not enough,it must satisfy the special solution of some additional conditions.These additional conditions are mathematically called the defini
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