The Earth as Modified by Human ActionMarsh, George P. (George Perkins)
History
The Earth as Modified by Human Action
Marsh, George P. (George Perkins)
Conservation of natural resources; Human geography; Nature -- Effect of human beings on; Physical geography
These experiments were continued from March to December, inclusive, of
the year 1868. It was found that during those months the evaporation
from a recipient placed on the ground in a plantation of deciduous trees
sixty-two years old, was less than one-fifth of that from a recipient of
like form and dimensions placed in the open country.] drinks up the
rains and melting snows that would otherwise flow rapidly over the
surface and perhaps be conveyed to the distant sea, and then slowly
gives out, by evaporation, infiltration, and percolation, the moisture
thus imbibed. The roots, too, penetrate far below the superficial soil,
conduct water along their surface to the lower depths to which they
reach, and thus by partially draining the superior strata, remove a
certain quantity of moisture out of the reach of evaporation. The Forest
as Organic.
These are the principal modes in which the humidity of the atmosphere is
affected by the forest regarded as lifeless matter. Let us inquire how
its organic processes act upon this meteorological element. The
commonest observation shows that the wood and bark of living trees are
always more or less pervaded with watery and other fluids, one of which,
the sap, is very abundant in trees of deciduous foliage when the buds
begin to swell and the leaves to develop themselves in the spring. This
fluid is drawn principally, if not entirely, from the ground by the
absorbent action of the roots, for though Schacht and some other eminent
botanical physiologists have maintained that water is absorbed by the
leaves and bark of trees, yet most experiments lead to the contrary
result, and it is now generally held that no water is taken in by the
pores of vegetables. Late observations by Cailletet, in France, however,
tend to the establishment of a new doctrine on this subject which solves
many difficulties and will probably be accepted by botanists as
definitive. Cailletet finds that under normal conditions, that is, when
the soil is humid enough to supply sufficient moisture through the
roots, no water is absorbed by the leaves, buds, or bark of plants, but
when the roots are unable to draw from the earth the requisite quantity
of this fluid, the vegetable pores in contact with the atmosphere absorb
it from that source.
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