Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
It thus becomes intelligible that in the arid region a humus-percentage
which under humid conditions would justly be considered entirely
inadequate for the success of normal crops, may nevertheless suffice
even for the more exacting ones. This is more clearly seen on
inspection of the figures in the third column, which represent the
product resulting from the multiplication of the humus-percentage of
the soil into the nitrogen-percentage of its humus; as appears in
comparing the respective averages, or Nos. 1167 and 110 and others. An
additional consideration is the probable greater ease with which the
nitrifying bacteria can act upon a material so rich in nitrogen.
We must not, then, be misled by the smallness of many humus-percentages
in the arid region, into an assumption of a deficiency in the supply of
soil-nitrogen.
_Decrease of Nitrogen-Content in Humus with
Depth._—Since the oxidation of the carbon and hydrogen
in the humus-substance, and the consequent increase of its
relative nitrogen-content, are manifestly dependent upon the
presence of air and heat, it is reasonably to be expected
that the nitrogen-percentage of the humus should decrease
with the depth of the soil. That this is really the case
is plainly shown in the subjoined table, which gives the
humus-percentages and the nitrogen-content of the humus from
the surface foot down to twelve feet, in a soil on the bench
of the Russian River, Cal., which is sub-irrigated, and
liable to more or less rainfall during the summer. It will
be seen that not only does the absolute humus-percentage
decrease quite regularly down to seven feet, at which point
there evidently was at one time a strong root development,
causing a notable increase of the humus-content; from which
again there is a regular decrease down to the twelfth
foot. It will be noted that the nitrogen-percentage in the
humus, while not decreasing with the same regularity as the
humus-content itself, yet exhibits a general recession from
5.30 to 1.15 in the ninth foot, to which direct oxidation
doubtless never penetrates.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account