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So if we could store it and transport it to high altitude and release
it.... assuming in sufficient quantities, it might do some good?
What about something to bind those Cl atoms at altitude? Could we send
up sugar and have it come back down as Splenda? (I'm kidding here).
Nathan Leigh wrote:
Christian M. Cepel wrote:
Assuming that the depletion of O3 is one of the biggest worry of
those with environmental concerns, and that H2 is the fuel of the
future and that nobody has any issue with that being sourced from
seawater, if there any reason why the conversion of H2O to H2 could
not be made to produce O3 instead of O2 and increase the Ozone
content of our atmosphere? Can producing O3 help patch the hole, or
has that become passe with more concentration on the buildup of
greenhouse gases? The keyword for the first 2/3rds of my life was
Chloro Flouro Hydrocarbons (Spelling?), and now that we've got
Styrofoam all but eliminated, and aerosol propellants replaced and
CFC compressor coolant gases replaced, I've heard nothing in the line
of positive "Yeah! we wiped out that piece of the equation." Anyone
know what the deal is in layman's terms?
Ozone at high altitude absorbs ultraviolet light, keeping much of it
from reaching earth's surface and causing more sunburns and skin
cancers. (The upside of more ground-level UV would be a booming
market in sunglasses for those UV-seeing insects...) Ozone at low
altitudes helps form smog and, in sufficient concentrations, is
actually toxic.
For the marvelous self-healing ozone layer, I think the ounce of
prevention beats the pound of cure.
<chemistry>
Ozone is produced at high altitudes when molecular oxygen (O2) absorbs
UV light - the O2 splits into 2 (highly reactive) oxygen atoms, each
of which can cozy up to a molecule of oxygen to produce O3. O3 can
absorb UV light also, splitting into O2 and an oxygen atom - so the
process is cyclic.
CFCs ("f-l-u-o-r-o", as a high school chem teacher beat it into our
heads many years ago) that reach the upper fringes of the atmosphere
will absorb UV light, producing atomic chlorine which reacts
repeatedly with ozone and atomic oxygen to produce molecular oxygen
(also cyclic, but the products are O2 and that voracious chlorine atom).
Ozone absorbs certain wavelengths of UV light that oxygen does not, so
O3 plays a crucial role in keeping light of those wavelengths from
frying us.
</chemistry>
Nathan
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