The atmosphere is relatively small compared to our planet.
If the Earth were the size of a basketball the thickness of the first 60,000
feet of atmosphere would be about seven tenths of one millimeter thick. That is
about the thickness of 4 pieces of common copy paper. (Using 6371 Km for Earths
Radius, .125 meters for the radius of a basketball, and .000097 meters for
thickness of the paper.)
Oxygen is the most abundant element on our planet but most
of it is chemically bound in forms that make it unusable for common fuel
combustion or respiration. Although some of the CO2 we produce when combusting
fuels may be recycled through photosynthesis, the other oxides that make up the
ash and other released gases are not.
For many years I have wondered by what means the O2 level in
our atmosphere is maintained; wondering how natural oxygenic photosynthesis
could possibly keep pace with man's intensive use of atmospheric O2.
Last night I was digging through an old box and found a copy
of EOS Volume 92 Number 46 15 November 2011. The article "Ocean
Deoxygenation Past, Present, and Future "- a report sponsored by the NASA
Astrobiology Institute. It began - "To a first order - the oxygen content of the
ocean interior is determined by the influx of gas across the air-surface (i.e.
ventilation) and consumption due primarily to microbial respiration."
Recalling things I learnt in college chemistry brought me to
the conclusion that as the O2 concentration of the atmosphere decreased the dissolved
O2 in the oceans would tend to move out of the ocean and into the atmosphere. The
rate of this process depending on temperature, pressure, concentration gradient,
and the amount of "mixing" that occurs at the ocean- air interface.
The questions I want to ask:
Is it possible that atmospheric O2 concentrations are not
being maintained by natural photosynthesis but by the transfer of O2 stored as solute in
the oceans?
Is the O2 flux through the air - ocean interface a net outflow
from the ocean at a rate greater than the rate of oxygen entering into solution
through oxygenic photosynthesis of ocean plants?
Is there a finite limit to free O2 availability?
Is it possible that human kind could be depleting the supply
of unbound O2?
When we deplete atmospheric O2
are we also depleting the O2 in the oceans?
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