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L 18 Thermodynamics [3]

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L 18 Thermodynamics [3] Heat transfer convection conduction radiation emitters of radiation seeing behind closed doors Greenhouse effect Heat Capacity – PowerPoint PPT presentation

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Title: L 18 Thermodynamics [3]


1
L 18 Thermodynamics 3
  • Heat transfer
  • convection
  • conduction
  • radiation
  • emitters of radiation
  • seeing behind closed doors
  • Greenhouse effect
  • Heat Capacity
  • How to boil water

2
Heat flow
  • HEAT ? the energy that flows from one system to
    another because of temperature differences.
  • But how does it flow? Three ways
  • convection
  • conduction
  • radiation

3
Convection
  • heat is carried from place to place by the bulk
    movement of either liquids or gases
  • does not apply to solids
  • when water is boiled, hot liquid rises and mixes
    with cooler liquid, thus the heat is transferred
  • Hot air rises
  • want heat into lower level of house (winter)
  • cooled air into upper levels (summer)

4
Conduction
  • heat is transferred directly through a material,
    with no bulk movement of stuff
  • only energy moves

iron is a particularly poor conductor of heat
5
heat conduction
Cross sectional area A
L
HOT
COLD
Heat Flow
Heat Flow rate depends on A / L
6
Thermal Conductivity
Material Thermalconductivity
Copper 400
Silver 420
Steel (stain.) 14
wood 0.15
glass 0.8
wool 0.04
Goose down 0.025
styrofoam 0.01
  • The effectiveness of a material in conducting
    heat is characterized by a parameter called the
    thermal conductivity
  • there are good thermal conductors
  • (metals) and poor ones (insulators)

7
Grandmas silver spoons
8
? radiation
Heat as moving light
  • Radiation is the heat transfer by electromagnetic
    waves thermal light waves - invisible to the
    eyes
  • thermal radiation is a small part of the
    electromagnetic spectrum waves are
    characterized by their frequency or wavelength
  • different colors in the visible correspond to
    different wavelengths from red to blue

9
electromagnetic spectrum
thermal radiation
microwaves, cell phones
TV
radio waves
x-rays
visible
10
visible electromagnetic waves LIGHT
shorter wavelength ? more energy
visible light
thermal radiation
UV radiation produces sunburn
11
Thermal Radiation
  • The warmth you feel from the sun is the suns
    thermal radiation
  • It travels through the vacuum of space to reach
    earth, no material is necessary (takes 8 minutes)
  • you can feel its effects even though you cannot
    see the radiation.
  • you can feel the thermal radiation from a
    fireplace

12
What produces thermal radiation?
  • all objects whose temperature is above absolute
    zero emit thermal radiation
  • The hotter the object, the more radiation it
    emits, the amount of radiation is T4
  • We all continuously emit thermal radiation
  • We also absorb it from objects and people around
    us
  • If we just emitted radiation we would eventually
    cool to absolute zero!

13
Emission and Absorption are balanced
14
Thermal radiation spectrum
  • The intensity of radiation increases with
    temperature
  • the color shifts toward the blue at higher
    temperatures
  • The UV radiation from the sun is just beyond the
    violet

15
sources of thermal radiation
  • the incandescent light bulb ( the ones that have
    a filament) are sources of both visible light and
    heat.
  • when electricity flows through a wire it gets
    hot.
  • it emits radiation even though you cant see it
  • as it gets hotter it glows red then orange then
    white

tungsten filament, can get very hot and not melt
evacuated glass bulb
16
Radiation emitted by hot objects
  • The hotter they are, the more they emit
  • the efficiency with which an object emits thermal
    radiation is characterized be a parameter called
    its emissive ? e
  • e is a number between 0 and 1
  • a good emitter has an e close to 1
  • a poor emitter has an e close to 0

17
good emitters are good absorbers
  • an object that is a good emitter is also a good
    absorber of thermal radiation
  • a poor emitter is also a poor absorber
  • generally dark, dull objects are the best
    emitters/absorbers
  • shinny objects are poor emitters/absorbers
  • If you do not want the edges of your pie to burn,
    you wrap it in aluminum foil

18
good/bad emitters-Leslies cube
infrared radiation sensor
copper cube filled with hot water
this side is painted black
19
Practical considerations
  • wear light clothing in summer ? light clothing
    absorbs less sunlight
  • cover all body parts in winter ? warm body parts
    (like your head) emit radiation

20
thermal radiation
  • all objects that are at a temperature above
    absolute zero emit thermal radiation (waves)
  • the higher the temp, the more they emit
  • the color (wavelength) of the emitted waves goes
    from red?orange?yellow? blue as the temperature
    increases

21
seeing behind closed doors
we can see behind closed doors because of the
heat signature left by warm objects on walls
Infrared sensors can pick up temp- erature
differences of 0.05 degrees C.
22
The Greenhouse effect
Suns visible light
infrared radiation is trapped
C O2
EARTH
  • http//earthguide.ucsd.edu/earthguide/diagrams/gre
    enhouse/

23
Greenhouse effect
  • the suns visible light can penetrate through the
    atmosphere to the earths surface where it heats
    it
  • the visible light energy is converted to thermal
    light energy
  • the thermal radiation is reflected from CO2 in
    the atmosphere

24
Greenhouse effect
  • concentrations of CO2 have been increasing
  • ? rise in earths temperature
  • same effect occurs in your car during the day.

25
The ozone layer
  • ozone, O3 is a naturally occurring trace element
    in the atmosphere
  • It absorbs solar ultraviolet radiation,
    especially the harmful UV-B rays
  • it is destroyed by Cfcs (chlorofluorocarbons)
  • loss affects us and environment

26
back to some practical topics
27
How do I boil water?
  • How much heat does it take to boil water?
  • Simpler question ? how much heat is required to
    raise the temperature of water by so many
    degrees?
  • The answer depends on how much water you have and
    how hot you want to get it
  • The answer would be different for a different
    material, say aluminum.

28
Heat Capacity or specific heat
  • The heat capacity is the amount of heat that is
    required to raise the temperature of 1 g of a
    substance by 1 degree C.
  • it is measured in Calories
  • for water it is 1 cal/g C
  • heat Q m c temp change

hot plate
mass of sample
specific heat
29
Some heat capacities
Substance Specific heat in cal/g C
water 1
Ethyl alcohol 0.58
Steel 0.11
Aluminum 0.215
lead 0.03
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