convection, conduction, and radiation heat transfer

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Convection, Conduction, and Radiation Heat Transfer

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Page 1: Convection, Conduction, and Radiation Heat Transfer

Convection, Conduction, and RadiationHeat Transfer

Page 2: Convection, Conduction, and Radiation Heat Transfer

Review of Density Warmer temperatures = less density Cooler temperatures = higher density

Page 3: Convection, Conduction, and Radiation Heat Transfer

Density and MotionHow does this happen?

Look at the example:

If these 2 arrows come together, will they move?

Why or why not?

10 10

No movement!

Page 4: Convection, Conduction, and Radiation Heat Transfer

Density and MotionNow look at this example.

If these 2 arrows came together, what would happen?

10 5

Movement! The values are not equal & the movement will be in the direction of the bigger force

Page 5: Convection, Conduction, and Radiation Heat Transfer

Density Poem“Motion will go from high to low”

Meaning: the molecules will go from where there are a lot to an area where there are few

Equilibrium: when molecules are equal on both sides (no movement!)

Page 6: Convection, Conduction, and Radiation Heat Transfer

Don’t forget! High amount of molecules = cooler

temperatures

Low amount of molecules = warmer temperatures

Page 7: Convection, Conduction, and Radiation Heat Transfer

Motion and atmosphere Cool air sinks (more dense) Warm air rises (less dense)

Motion:Creates a circular motion: heats up goes up, cools off comes down, heats up goes up, cools off comes down

Page 8: Convection, Conduction, and Radiation Heat Transfer

Motion in water Cool water sinks (more dense) Warm water rises (less dense)

Motion:Creates a circular motion: heats up goes up, cools off goes down, heats up goes up, cools off goes down

Page 9: Convection, Conduction, and Radiation Heat Transfer

Motion under the Crust Cool magma sinks (more dense) Warm magma rises (less dense)

Motion:Creates a circular motion: heats up goes up, cools off comes down, heats up goes up, cools off comes down

Page 10: Convection, Conduction, and Radiation Heat Transfer

What causes those fluids to heat up?Radiation (aka a heat source)

Natural Radiation: The Sun, the center of the earth, fire

Artificial Radiation: hot plate, burner on stove, candle

Page 11: Convection, Conduction, and Radiation Heat Transfer

Conduction When the radiation gets transferred to

an object, that is called conduction 2 objects must be in contact with each

other Objects can be as small as electrons

Examples: touching a hot spoon, sitting on leather seats in the summer, feeling the counter when the sun is out

Page 12: Convection, Conduction, and Radiation Heat Transfer

Convection Currents This is the circular movement of the

heat transfer This is an action, a verb, a “doing” Molecules will flow to different levels of

concentrations: from high to low

Page 13: Convection, Conduction, and Radiation Heat Transfer

Which temperature has more molecules in a given space? Cooler/Cold

Cooler temperatures = increased density Think about the molecules packed

together in ice

What type of temperature outside will have greater density: hot weather or cold weather?

Page 14: Convection, Conduction, and Radiation Heat Transfer

Which temperature has less molecules in a given space? Warmer/hot

Increased temperatures = decreased amount of molecules in the same area

Think about how the molecules would look like in a gas all spread out

What type of temperature outside would have lower density: hot weather or cold weather?

Page 15: Convection, Conduction, and Radiation Heat Transfer

Summary of CCR: Radiation: EM radiation from the Sun

heats up the ground or water Conduction: transfer of heat to touching

molecules Convection: the different densities of

temperature create a circular movement: from high to low