To re-run the movie click here.

If there is more heat in one place than another, then the heat can be transferred by one of three mechanisms:

- Radiation - the energy is carried by photons. In
*black body radiation*, the color of the photon emitted is related to the temperature of the body; the hotter the body, the bluer the light. - Conduction - the heat
*propagates*through a chunk of matter in much the same way that an ink stain moves through shirt. The farther the heat moves, the smaller the change in temperature. - Convection - conditions are right for part of the matter to move from the hot region to the cold, taking the heat with it.

Lord Rayleigh was the first to correctly describe the conditions that lead to convection as a single number which now bears his name: . The various factors of the Rayleigh number either make it easier for convection to occur or make it more difficult. Rayleigh found that, if the Rayleigh number was greater than ~1,500, then convection would occur spontaneously.

Factors that aid convection:

is the linear coefficient of thermal expansion of
the material; as the material heats, it expands and becomes less dense,
increasing the buoyancy. is typically about 2 x
10^{-5} K^{-1}. *g*
is the gravity, and is what drives the process.
is the difference in temperature between the top of the convecting
layer and the bottom; obviously, the higher the difference in
temperature, the more vigorous the convection.

Factors that retard convection:

is the thermal diffusivity of the material; together with *k* (the thermal conductivity), it
measures how easy it is to move the heat by conduction. is typically about 10^{-6}
m^{2}s^{-1}; *k* is
on the order of 2 Wm^{-1}
K^{-1}. is the viscosity,
and measures how difficult it is for the fluid to deform. For rocks,
is about 10^{16}
m^{2}s^{-1}.

When we apply these values to the Earth's mantle, we get a value of about 1,000,000 - well in excess of that needed for convection. Even if we assume two layered convection and vastly smaller internal heat production, the Rayleigh number is still great enough to drive convection.

**To demonstrate convection in class, you will need:**

(There are a wide range of substitutes for the water with mica flakes. We have used clear broth with noodles, miso soup, and Orbitz_{tm} soda. Be creative!)

**Before the demonstration:** .

Place the fluid into the jars, and place the jars on the hot plate.
Check to make certain that the outlet has power.

1. Plug the hot plate in and turn it on. Write the equation for the Rayleigh number on the board.

2. Discuss the effect of each factor in the equation; we find it useful to divide the equation into the terms that help convection and those that retard it.

3. With luck and a bit of timing, the liquid should start convecting just about the time you finish discussing the various factors.

4. Examine the jar with the lid. Why is it not convecting?

**For Discussion:**

Does the interior of the Moon convect? (Remember that the Moon has a
lithosphere that is 1000 km thick and that it is made up of rocks that
are similar to those on the earth.) How about the interior of the
asteroid Ceres? (Radius: 466 km)

This page designed by John DeLaughter jed@earth.northwestern.edu Update: Jan 20 1998