The Richfield recorder. (Richfield, Idaho) 1909-1931, 1911-12-14

] ~ kNA0 49,
short time at my disposal | hope to
open up a line Of thought which viii
help some of you in your work; for,
after all, each of your individual
problems must be solved by your
selves.
The amo mt of plant growth is de-
pendent in a decided measure upon
the amount of moisture, within GER
tain limits, in the soil. The supply
ing and maintaining of this moisture
in an amour which will bring the
greatest return is. then, u problem.
The water found in soils is of three
kinds:
First. Free water or the water
found between the soil particles Of
a saturated soil.
Second. Capillary water or that
which is held in a thin film around
each of the soil particles of a moist
but not saturated soil. This is the
water used by the plant in it's growth.
Third. Microscopic water which is
the water held by the soil but which,
in all probability is not used by the
plant.
Only aqueo S or water plants can
grow in a soil containing free water.
Hence our problem is confined to the
regulation of the capillary water n
ly, and to the conditions which gov
ern plant growth. There are three
ways by which soil moisture can es-
cape:
First. By sinking into deep soils
out of reach of the plant roots, and
escaping by under drainage.
Second BY e%vaporating from the
surface.
Third. By passing through the
plant itself in a process known as
Transportation.
Each of these losses a be gov
erned to a certain extent. The first
by making lighter applications of
water at each irrigation. The sec
ond, or surface evaporation, can be
checked by %cultivating the surface
sufficient to form a dust mulch, thus
closing up the openings of the ca
pillary tubes which form when the
surface soil begins to dry out. And
the third o. Transportation can be
checked by the addition of soil fer
tility or by ordinary cultivation.
Thus, the last two can be governed
by the simple operation of stirring
the surface after an irrigation.
The thought is prevalent among
farmers hat a certain amount of
water must be used by a plant in or
der to produce a certain weight of
dry matter. AS early as 1899 Wood
ward found that it required less wa
ter to produce a pound of dry matter
in a plant growing in a rich soil
where the plant food was evenly
balanced, than in one of opposite ma
ture. Later, in 1878, a German in
vestigator found that the yield of
dry matter was greatest where trans
piration was least. He also found
that the enriching of the soil ena-
bled the plant to produce dry matter
with less water.
Now the question may arise in
your minds: Why should cultivation
decrease the amount of water actual
Iy used by the plant? Cultivation
permits the air and sunshine to enter
the soil more readily, causing a con-
sequent liberation of plant food,
which is equivalent in effect to the
addition of the food artificially.
That cultivation actually decreases :
he amount of water used by the
is shown in the results of ex-
yClinACIlS OOu0uILGu dL4iHt. ildu .tN-i
pertinent station in the vegetation =
Certain tanks were planted
o corn. An equal number of tanks
containing the same kinds Of soil ,
we're left bare for a check on the
evaporation from the surface. For
weight hours after each irrigation
then every week, half the sur
aces were cultivated while the other
49, . T-rA - r-rr a.
.hOws the results.
TABLE No. l..
Cultivation VS.. Transportation