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Heat Transfer Overview

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Presentation on theme: "Heat Transfer Overview"— Presentation transcript:

1 Heat Transfer Overview

2 How Do We Define Heat Transfer?
Energy in transit due to a temperature difference Electrical analogy Concerned with time rate of change In this we’ll calculate things such as What rate of heat transfer will occur in a certain situation? What temperatures can we expect? How long will it take to heat/cool something? What are some specific applications?

3 Examples of Where You May Use Heat Transfer in Industry
Estimating the temperature of components on a circuit board to determine if failure rates are acceptable and then designing the cooling system Choosing a heat sink and fan that will cool a transistor appropriately Determining the orientation and size of solar panels needed to power a micro-satellite Designing the cooling system for an ice-hockey table Choosing the type and size of heat exchanger to be used to heat a chemical used in semi-conductor manufacturing

4 More Examples… Choosing the type and size of radiator needed for a new type of automobile Calculating the optimal amount of insulation to be placed on a steam pipe to reduce heating costs Determining how much power must be applied to an antennae on an airplane to keep water from freezing on it Designing a quick-freezing system for a meat distributor to seal in flavor and juices Calculating heat losses and gains from a building to size their heating and air conditioning systems

5 Types of Heat Transfer Conduction: due to interaction between particles; usually through a solid Convection: gas to solid (or vice versa) Includes both conduction between particles and advection (heat transfer due to mixing) Radiation: radiated energy (no medium needed)

6 Why not just use computer programs? Why take a class?
How will you set up the model? What boundary and initial conditions? Are the simplifications chosen OK? 3-D convection at moderate/high velocities is impossible to solve without significant simplifications How will you interpret the results? Are the results accurate?

7 Conduction Energy transfer from more to less energetic particles due to particle interactions – diffusion of energy due to molecular activity Examples Usually involves solids Rate = f( ) What is the driving potential?

8 Fourier’s Law of Heat Conduction
k=thermal conductivity (W/m°C or Btu/h ft °F) -- a measure of how fast heat flows through a material -- k(T), but we usually use the value at the average temperature q can have x, y, and z components; it’s a vector quantity

9 Special Case If T(x) is linear, Fourier’s Law for the 1-D case becomes
When will this happen? Example

10 Conduction Definitions
Heat capacity = rcp (J/m3°C) Amount of heat needed to raise a unit volume of material one degree Thermal diffusivity = a = k/rcp (m2/s) How fast heat diffuses through a material

11 Convection Energy transfer due to both Convection=diffusion+advection
molecular motion (diffusion, like conduction) and bulk motion of fluid (motion of gas or liquid) Advection Convection=diffusion+advection Three kinds Forced convection – external fluid motion Natural (free) convection – motion due to buoyancy effects Latent heat exchange – due to phase change – condensation, boiling (covered in ME 211 but not ME 114)

12 Newton’s Law of Cooling
h=heat transfer coefficient (W/m2°C) Ts=solid surface temperature T =temperature of fluid far from surface h=f( )

13 Boundary Layer

14 Example A 0.4 cm x 2 cm computer chip must dissipate 5 W of heat. Air with a heat transfer coefficient of 80 W/m2K and a temperature of 20°C blows over the chip. The chip is in danger of overheating if it reaches 90°C. Is the chip in danger? Should you attach a heat sink?

15 Thermal Radiation Emitted by all matter above 0 Kelvin
Due to changes in electron configurations Requires no medium Emissive power of a blackbody (ideal radiator) Ts=surface temp in Kelvin s=Stefan-Boltzmann Constant 5.67x10-8 W/m2K4

16 Thermal Radiation, Cont.
e=emissivity: how efficiently a surface emits compared to a blackbody a=absorptivity: percent of incident flux absorbed e,a =f(temp, wavelength, surface condition)

17 Thermal Radiation, cont.
Special case: e=a if surface temperatures of all surfaces in an enclosure are close Special case: surface completely surrounded by another isothermal surface, no intervening medium

18 Total Heat Transfer Only conduction, convection, or radiation can occur or else a combination can occur simultaneously Qconv+Qrad or Qcond+Qrad


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