Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898 — John Shaqi
Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898Various
Science
Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898
Various
Science -- Periodicals; Technology -- Periodicals
Light is the most important of all the external agencies which
influence the vegetal organism, and the sun's rays have been the most
potent force in shaping the development of existent plant forms.
The sunbeam stands in a manifold relation to the plant. First and
foremost, light is the universal source of energy, by the aid of
which the chlorophyll apparatus in green leaves builds up complex
food substances from simple compounds obtained from the soil and air,
a process necessary for the nutrition of the entire living world.
Some obscure organisms, such as the "nitrosomonas," soil bacteria,
are able to accomplish the construction of complex substances, by
means of energy derived from other chemical compounds, which were,
however, formed originally by green plants. These food-building
processes are designated as photosynthesis, chemosynthesis,
electrosynthesis, thermosynthesis, etc., according to the source of
energy used.
By photosynthesis, carbon dioxide from the air and water from the
cell are combined in the green cells of leaves, forming sugar and
possibly other substances. During this process an amount of oxygen
approximately equal to that of the carbon dioxide taken up is
exhaled. It will be of interest to note the relation of the living
world to the atmosphere. Eight hundred to nine hundred grammes of
carbon dioxide are produced in the respiration of a single person
for a day, and the entire product of the human race for this period
is twelve hundred million kilogrammes. In addition, large quantities
of the gas result from the combustion of the four hundred and sixty
millions of kilogrammes of coal and wood burned yearly. The lower
animals, fungi, and green plants themselves contribute an amount
which must bring the total to twice the immense sum named above.
The atmosphere contains three or four hundredths of one per cent of
carbon dioxide, or an amount of about two to three thousand billions
of kilogrammes. No especial variation in this proportion has been
detected since observations upon this point were first made. The
fact that no increase takes place is partly due to the absorption
of the gas by plants, and its replacement by oxygen, and also to
certain geological processes in constant operation. Absorption
takes place at the rate of about two and a half grammes for every
square metre of leaf surface per hour, or about twenty-five to
thirty grammes daily, since the process goes on only in daylight.
It is to be seen that a single human being exhales as much carbon
dioxide as may be removed from the air by thirty or forty square
metres of leaf surface. According to Ebermayer, a hectare (2.47
acres) of forest would use eleven thousand kilogrammes of carbon
dioxide yearly, and the amount used by plants is generally much in
excess of that furnished by the activity of the inhabitants of any
given area. Plants thrive and show increasing vigor as the amount of
carbon dioxide in the air rises until two hundred times the present
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