The Kenna record. (Kenna, Roosevelt County, N.M.) 190?-1924, 1913-01-10
DEEP FLOWING BIG BENEFIT
Dominant Factor In Carrying MolS
ture Over Winter for the Prodwc-
duetlon Of Good Crop.


It is wonderful how little moisture
penetrates our harder soils IN sum-
mer, no matter how abundant the rain.
fall may be, and even long experience
with such soils hardly prepare one for
their dry condition when one goes
forth to pillow.
The moisture falling so late this
season there has not been so much
evaporation, and in some soils have
observed the downward penetration
has been much greater than with
great deal more precipitation in the
summer months, and it is likely to
endure for some time, giving an OPP
portunity for deep blowing.
1t is not necessary here to urge deep
blowing is suitable to all conditions.
The point is, is it not necessary to
our hard land, especially those to be
dry farmed?
Merely as u matter of carrying over
water in the soil and for the entrance
OF later rains and snow, is 1t not the
one most dominant factor in produc-
Ing crops; Is not the question OF max
ing use Of our denser dry soils one Of
bringing them more to the porous
condition of sander soil, which alb
serbs all the rainfall and great deal
of snow before 1t evaporates in our
warm sun and dry atmosphere?
II the answer is yes, then the i'm.
portance of blowing deeply when con.
ditions are favorable as at present
must not be overlooked unless we
have command of deep tillage tools
and power to operate them, and even
with these a less expensive result will
be claimed than in a dry time.
have not the data and do not know
even that ct exists to show at what
point gravity overcomes the pumping
power of the sun to draw moisture
from the soil, but 1t is at no great depth.
So long Us the soil Is kept stored and
pipes are not formed through which
the water can evaporate. Roughly
speaking should say that when
moisture has descended eight to ten
inches 1t will with any reasonable top
mulch either from good blowing or
cultivation continue in large measure
to descend and that short of six inches
it will be very apt to ascend in vapor
and largely disappear. no matter how
carefully we try to retain the dust
mulch on large tracts of land.
Theoretically the dust mulch will
hold 1t perhaps also in practice 80 long
as no cropping interferes with culti-
walton, but for practical results 1t is
extremely desirable to get the mois-
ture down as far as possible from the
suns attraction, which raises 1t to the
surface to be carried away by winds
and evaporation in an atmosphere
which will with us almost always abb
serb moisture.
This same moisture when 1t has de-
scended to depth of eight to twelve
inches lies as poultice on the sub
soil and softens 1t and descends yet
deeper where in its original state the
subsoil was quite incapable of absorb
ing 1t in the small quantities which
lay on it for only a short time and
thus we get a penetration of moisture
to FIVE, six or more feet, and have &C
complished something permanent
quite different from merely wetting
five or six inches OF top soil by light
blowing.
1t is true that crops will use the
moisture, but its effects on the subsoil
will remain, for 1t has become absorb