> I did try to run the following idea past a ocean biogeochemist: Use wind
> power to pump deep (nutrient-rich) water up to the surface, to increase
> primary productivity, potentially burying carbon as detritus and also
> increasing food production. He was full of reasons why it wouldn't work
> (eg if it had a significant effect, there would be the risk of anoxia
> due to the organic fallout, with various unwelcome consequences).

How does the biological pump work without there being anoxia somewhere
I wonder?

You'd think that if there was always enough oxygen, then some
enterprising bugs would fully consume the biomass and thereby all the
CO2 would be released again.

------------------------------

OTEC sounds like it's a very similar idea

http://www.nrel.gov/otec/what.html

-------------------------------

http://www.nrel.gov/otec/what.html

The above is a good and detailed report by the Royal Society, They are
dismissive of lime stone addition, saying too much material would be
required, and don't really discuss other options. They do say though
that there is a large store of calcium carbonate in sediments (30
million Gt of carbon equivalent, for comparison current fossil fuel
emissions are 7 Gt) and that over geologic timescales that should mean
little acidification, but apparently proxy data are too poor and
provide conflicting evidence about the pH of the oceans for periods in
the distant past when CO2 was above 1000 PPM to say much about how
this played out in practise.





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