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Can you extract atmospheric CO2 in
order to reduce global warming? If so, how would
you do it?
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Question Date: 2007-10-20 | | Answer 1:
This is an excellent question, and actually
many scientists from both public (government) and
private (for-profit) organizations are working on
this. There are several popular approaches to
removing atmospheric CO2. The most
actively studied one is to fertilize the oceans
with iron, which causes microscopic plants
(phyto-plankton) to grow faster. As they grow,
photosynthesis causes them to remove
CO2 from the air and convert it to
sugars so that they can grow. When they die, we
hope that they fall to the bottom of the ocean and
thus a lot of CO2 is stored in their
dead bodies. The reason that iron works as a
fertilizer is because the oceans are very far from
land where most of the iron is, and the process of
photosynthesis requires iron to make the
chlorophyll molecule work properly. One problem
with this approach is that if something eats the
phytoplankton or bacteria decompose them before
they sink then all that CO2 will be
released (breathed out by respiration) and will
wind up back in the atmosphere. There are two
large private companies trying to develop this,
and it has been tried several times in the
Antarctic and Pacific oceans (where they dump iron
in the ocean over 100's of square miles by boat),
but there are a lot of concerns over how it may
impact the ecosystem in unforeseen ways. This is
also a problem because no country "owns" the
oceans and thus nobody is responsible if something
goes wrong. | | Answer 2:
I searched your question on Google: atmospheric
CO2 extraction And I found there is a
$25 million prize for doing this. Some scientists
published an article about doing it, but the prize
is for removing at least a billion tons of
CO2 per year. Click here:futurepundit | | Answer 3:
IF CO2 is in fact responsible for
global warming (which it probably is, but there is
still some debate), then the answer is yes.
Corporations and governments alike are now working
on developing CO2-sequestration
technologies that will do this, using biological
means. I don't know how they plan to pull this off
- this is an engineering question and I'm not an
engineer. I also don't know how successful they
are going to be: as with any invention, until you
do it you never know if it is in fact possible in
a practical sense or not. | | Answer 4:
It's possible to "scrub" CO2 from
air using several chemicals, usually amine-based
solvents. But these are all expensive. Also,
many of these chemicals require mining or
additional fossil fuels to make them, which defeat
the purpose. An even bigger problem is that we
don't have any good way to *store* the
CO2 after we remove it. Since the world
burns about 1 cubic mile of coal every year, that
means we would need to store 1 cubic mile of solid
carbon, or many times that much gas.
Unfortunately, the most stable, long-lasting,
compact means of storing carbon is... coal. So
the best thing we could ever do for global warming
is to leave the coal (and oil) in the
ground. The best shot we have at
sequestering large amounts of CO2 is to
promote nature to do it for us. Plankton in the
ocean converts CO2 to oxygen, but there
is not enough plankton to compensate all the
CO2 we are producing from fossil fuels.
One proposal is to "fertilize" the ocean with
iron particles which help plankton grow. But it's
not clear whether we can do this on a huge scale,
or whether it would cause other problems. | | Answer 5:
Yes, many scientists think that it might be
possible to extract atmospheric CO2 and
sequester it in some solid form so it no longer
contributes to the greenhouse effect. Probably
the best way to do this is to have plants convert
atmospheric CO2 into plant matter by
photosynthesis (all of the carbon in cellulose,
wood and other plant matter was once atmospheric
CO2). Then you have to make sure the
plant matter doesn't decompose and release the
CO2 back into the atmosphere. For
example, if you grew a tree, cut it down, and then
sank the tree to the bottom of the ocean, all of
the CO2 in the tree would be
sequestered. This would be hard to do with trees,
but some oceanographers think it is possible to do
the same thing with phytoplankton. Phytoplankton
are the microscopic algae that float near the
ocean surface and get their energy from
photosynthesis. In most oceans, the growth of
phytoplankton is limited by the availability of
iron, so if we fertilize the ocean with iron,
phytoplankton growth will 'bloom.' In theory most
of the phytoplankton in the bloom would die and
sink to the bottom of the ocean, taking all of
their carbon with them. However, there are still
some bugs to be worked out in this plan - for one
thing, it would take an unrealistic amount of iron
to really make a dent in atmospheric
CO2 concentrations. An
interesting way of thinking about this problem is
to remember where all of the 'extra'
CO2 in the atmosphere came from in the
first place: fossil fuels. How did all of the
carbon get into fossil fuels? Millions of years
ago, many plants converted CO2 into
plant matter, and that plant matter became
sequestered in the ground and fossilized instead
of decomposing and returning to the atmosphere.
Now we've released much of that CO2 by
burning coal and oil and so forth, so these new
ideas about CO2 sequestration are
really just a way of duplicating the process that
generated fossil fuels. Anyway, like I said,
there are still a lot of problems with the
iron-fertilization plan. So if you can come up
with a better plan that would be pretty helpful! | | Answer 6:
It is certainly possible to extract
CO2 from the atmosphere; however, to do
so in quantities sufficient to make any measurable
change in the content is staggeringly difficult,
simply because of the quantity.Recently (2002),
the amount of CO2 was measured to be
about 0.037% of the atmosphere. Given that normal
air pressure is 14.7pounds/sq. in. or10,500 Kg/sq
m, the mass of the atmosphere is the earths
surface area times the mass of air over each sq.
meter (i.e. the pressure as sea level). This works
out to be: 5.3x10^18 Kg. So the current amount of
CO2is: 2x10^17Kg or 200 trillion metric
tons. The problem of CO2 injection into
the atmosphere is joint among all fossil fuel
burning activities on the planet such as driving,
heating, cooking and power generation. This is why
most efforts have been to limit expansion of such
activities (i.e. the Kyoto accords). On the
other hand, there is the theory that the current
mass fraction of CO2 is limited by
plant growth on land and (mostly) in the oceans
since the current atmospheric makeup seems
strongly affected by the Earth's biomass. However,
the mechanisms behind the current atmosphere are
not completely understood and there is very little
information about the way the biosphere will
change if the mass fraction of CO2 is
changed. It might be that the global warming
question revolves around the behavior of
microscopic plants and bacteria in the oceans.
There is potential for specialized engineered
plankton or bacteria to make differences on this
scale -- but the associated risks enormous as
unforeseen side effects could endanger the
planet's food supply. In general, you must
be careful accepting statements about vast complex
systems where there is a substantial unknown
factor. Scientists cannot isolate the planet to
see what really makes it work -- and while
physical analysis (like the masses above) are
relatively easy to determine, figuring out how the
biological and geological system works and what
will happen due to a hundred years of industrial
dumping of CO2is very difficult.
Recently, there has been substantial evidence for
global warming of the planet -- at least over the
last century. However, beyond that period, the
Earth's mean temperature is not easy to determine
directly, and a century is a very short time
period compared to those processes which we
strongly suspect change the atmospheric
composition and temperature. It is somewhat likely
that the real consequences of CO2
dumping will await further study and interpretation. Click Here to return to the search form.
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