Cornell Nature-Study Leaflets: Being a selection, with revision, from the teachers' leaflets, home nature-study lessons, junior naturalist monthlies and other publications from the College of Agriculture, Cornell University, Ithaca, N.Y., 1896-1904New York State College of Agriculture
History
Cornell Nature-Study Leaflets: Being a selection, with revision, from the teachers' leaflets, home nature-study lessons, junior naturalist monthlies and other publications from the College of Agriculture, Cornell University, Ithaca, N.Y., 1896-1904
New York State College of Agriculture
Natural history; Nature study
If a kernel of corn be placed in the ground in early spring before the
soil has become warm, the seed will not germinate. Abundance of moisture
and oxygen may be present, but the third requisite for germination,
proper temperature, is lacking. The soil is very slow to become warm in
the spring, and this is due to the large amount of water which must be
evaporated. During the winter and spring, the rain and melting snow have
saturated the soil. The under-drainage is deficient so there is no way
for the escape of the surplus water except by evaporation, and
evaporation is a cooling process. A well-drained soil is thus warmer
than a poorly-drained one.
The atmosphere is much quicker to respond to changes in temperature than
is the soil. In the spring, the air becomes warm while the soil
continues cold, and the rains which fall during this time are warmed by
passing through the warm air. Then in sinking through the soil the
rain-water parts with some of its heat which makes the soil warmer.
During mid-summer the soil becomes very warm, and it is not affected by
cool nights, as is the atmosphere. Consequently as a summer rain may be
several degrees cooler than the soil, the water in passing through the
soil takes up some of the heat; thus the soil conditions are made more
favorable for plant growth. Therefore, soil temperature is regulated
somewhat by the rainfall.
_Experiment No. 10._--The color of a soil also affects its temperature,
a dark soil being warmer than a light colored soil. By having
thermometers as a part of the school room equipment, interesting
experiments may be conducted in determining the effect of color and
moisture upon the temperature of soils.
AIR IN THE SOIL.
Although that part of the plant which we can see is entirely surrounded
by air, it is also necessary that the soil be in such a condition that
it can be penetrated by the air. Indeed, growth cannot begin in a soil
from which the air is excluded.
[Illustration: _Fig. 40. The clover roots penetrate the soil deeply._]
_Experiment No. 11._--To prove this, put clay soil in a pot and plant
seeds; then wet the surface of the soil and puddle or pack the clay
while wet and watch for the seeds to germinate and grow. At the same
time put seeds in another pot filled with loose, mellow, moist soil.
Frequently, after the farmer has sown his grain, there comes a heavy,
beating rain, and the surface of the soil becomes so packed that the air
is excluded and the seeds cannot germinate. If plants are grown in pots
and the water is supplied at the top, the soil may become so hard and
compact as to exclude the air and the plants will make a sickly growth.
The surface soil must be kept loose so that the air can penetrate it.
[Illustration: _Fig. 41. After the clover dies the soil is in better
condition for its having lived._]
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