Transcript Document

Project PRISE
Connie Walker, National Optical Astronomy Observatory
Convection
• Perhaps the first thing that most people say is "heat
rises". While not wrong, what you should say is "hot
air rises" or "hot water rises".
• Anything fluid - that is a gas or a liquid - will tend to
change density with changes in temperature.
• For example, if heated, air decreases in density. The
surrounding air is cooler and denser. This makes it
heavier, so it falls beneath the hot air, forcing it
upwards. This is convection.
Convection in rooms
• Radiators heat rooms in some houses. This is a bad name
for them - as they give off heat mainly by convection!
• The convector heater warms the air in contact with it. This
becomes less dense, and rises.
• The ceiling forces this air to circulate as shown, warming
the air around it.
• Finally, when the air has cooled, it falls downwards,
completing the cycle.
Convection in rooms
• Radiators heat rooms in some houses. This is a bad name
for them - as they give off heat mainly by convection!
• The convector heater warms the air in contact with it. This
becomes less dense, and rises.
• The ceiling forces this air to circulate as shown, warming
the air around it.
• Finally, when the air has cooled, it falls downwards,
completing the cycle.
Convection in rooms
• Radiators heat rooms in some houses. This is a bad name
for them - as they give off heat mainly by convection!
• The convector heater warms the air in contact with it. This
becomes less dense, and rises.
• The ceiling forces this air to circulate as shown, warming
the air around it.
• Finally, when the air has cooled, it falls downwards,
completing the cycle.
Convection in rooms
• Radiators heat rooms in some houses. This is a bad name
for them - as they give off heat mainly by convection!
• The convector heater warms the air in contact with it. This
becomes less dense, and rises.
• The ceiling forces this air to circulate as shown, warming
the air around it.
• Finally, when the air has cooled, it falls downwards,
completing the cycle
a convection “current”!
Convection Everywhere
• Convection currents occurs wherever fluids are being
heated. Here are some more examples:
Water in kettles
Soup in saucepans
Water in a hot water tank
• Convection even occurs in the Sun!
QuickTime™ and a
YUV420 codec decompressor
are needed to see this picture.
Convection Currents in the Sun
QuickTime™ and a
YUV420 codec decompressor
are needed to see this picture.
Clouds & Convection
• Pyrocumulus clouds
http://www.youtube.com/watch?v=czYzu3OIjmY
• Cumulus buildup over the San Francisco Peaks
http://www.youtube.com/watch?v=WUkbd_omElE
Convection in Our
Atmosphere and Oceans
• Weather forecasters show how convection currents
are formed when warm and cold air masses meet in
the atmosphere.
• Convection currents are responsible for warm water
currents that occur in oceans.
• This activity demonstrates convection currents in a
very colorful way:
• http://wm.kusa.gannett.edgestreams.net/news/114295
2694628-03-21-06-spangler-inversion.wmv
Convection in a Liquid
• Energy can be transported through a fluid (liquid or
gas) by convection currents..
• The temperature of the water near the flame
increases. This water expands and so its density is
less than the water surrounding it. The higher
temperature water therefore "floats" upwards
transferring energy through the liquid.
Pie-Pan Convection
• Fill the pie-pan between 1/2 to 3/4
full with tap water and squeeze in
about 2 tablespoons of hand soap.
•
Gently stir the soap and water; try
not to create bubbles. Stir until the
soap is mixed throughout the
solution.
•
To see convection currents and
fluid flow more easily, darken the
soapy solution by adding a few
drops of dye.
Liquid hand soap or shampoo with a pearly or metallic appearance and glycol
stearate, glycol distearate or glycerolstearate. (Softsoap & Walgreen's Liquid Soap)
Convection in a Fishtank
• Add a few drops of red and
blue food coloring to a fishtank
of water that is sitting on a
bowl of ice at one end of it & a
bowl of hot water at the other.
• After only a few minutes the
warmer, therefore less dense,
red water rises above the
colder, & denser, blue water.
• This is a perfect illustration of
what happens when a warm
front meets a cold front.
Convection Experiments
Convection Currents Experiment in water:
http://www.youtube.com/watch?v=nD5NHjdxRlY
Convection Currents Experiment in air:
http://www.youtube.com/watch?v=pivQmIR7nDw
Lava Tube:
http://www.youtube.com/watch?v=vQucpUWV1HM or
http://www.youtube.com/watch?v=vQucpUWV1HM
How to make a lava tube:
http://www.youtube.com/watch?v=GAJG8jh2SJA
Teaching Tips
• Establish that convection is the primary method of
heat transfer in fluids, both liquids and gases.
• Ask students to give examples of where convection
currents might be found, and why.
• If the older students have studied plate tectonics,
prompt them to recall convection currents in the
Earth's mantle.
Convection Summary
• Convection occurs in gases and liquids. Hot fluids
rise, cold fluids fall.
• Convection currents occur because heat is lost from
the rising fluid, cooling it down.
• The whole fluid will rise in temperature as a result of
mixing caused by convection currents.
The END
(for now)