If the sand is dry, in the daytime just a few inches below the surface it will be much cooler than the daily maximum at the surface. Below about a foot, the sand will be at about the average daily surface temperature.
In the autumn, the temperature of the sand will increase slightly as depth increases, but this effect is very small in the upper few feet. Geothermal heat flux is negligible.
All this is based on the physics of conduction in solids with a daily or annual wave at the surface. All you need to solve the equation is the mean and amplitude at the surface,the period of the wave (one day or one year) and the thermal diffusivity of the sand. Dry sand has a very low diffusivity compared to most soils, so the depth at which the surface cycle peters out is relatively shallow.
Edited by Frozen (06/22/09 05:04 PM)
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