It will be noticed that the temperature of the soils increased until
the early part of the afternoon and after that time they lost heat.

[Illustration: FIG. 31.--SOIL TEMPERATURE EXPERIMENT.
Thermometer in pot of soil.]


HOW SOILS ARE WARMED

=Experiment.=--Hold your hand in bright sunlight or near a warm stove
or radiator. Your hand is warmed by heat radiated from the sun or warm
stove through the air to your body. In the same manner the rays of the
sun heat the surface of the soil.

=Experiment.=--Take the stove poker or any small iron rod and hold one
end of it in the fire or hold one end of a piece of wire in a candle
or lamp flame. The end of the rod or wire will quickly become very hot
and heat will gradually be carried its entire length until it becomes
too hot to hold. This carrying of the heat from particle to particle
through the length of the rod is called heating by conduction. Now
when the warm rays of the sun reach the soil, or a warm wind blows
over it, the surface particles are warmed and then pass the heat on to
the next ones below, and these in turn pass it to others and so on
till the soil becomes heated to a considerable depth by conduction.

A clay soil will absorb heat by conduction faster than a sandy soil
because the particles of the clay lie so close together that the heat
passes more readily from one to another than in the case of the
coarser sand.