Monday, February 8, 2016

Carbon Sequestration part II



Overall summary:

There are many ideas for sequestering carbon, these include storing it in geological formations, pumping it into the ocean (liquid CO2 is denser than water), injecting it into the seabed, transforming it into thermodynamically stable minerals, or doing an ‘active earth intervention’ such as iron fertilization.  Dr. Watson talked us through the pros and cons of these methods, their viability, and his opinion.    Dr. Watson’s message was similar to Dr. Katz’s – the earth will survive a very high amount of atmospheric carbon, but it’s doubtful that the current number of  humans can.



Terms

  • Iron Fertilization-  Spreading iron into the ocean to increase the population of phytoplankton Phytoplankton blooms remove CO2 through photosynthesis. This has been tried on the small scale, but like any ‘active earth intervention’ or ‘geoengineering attempt’, people are reluctant to try to actively change the environment dramatically to correct for how we already dramatically changed the environment. Prevention seems like a safer approach. Nonetheless we may eventually need this type of interaction. Other ideas such as using space mirrors to reflect sunlight or putting an anti-greenhouse gas in the atmosphere have also been proposed
  • Acidification-   Increased CO2 levels in the ocean will increase the level of acidity, possibly harming wildlife.  Much aquatic life relies on CaCO3 (mollusks, coral, etc.) and higher acidity dissolves this. 
  • GeologicalCO2 injection-  Injecting CO2 into areas below the earth, sequestering the CO2 into the pockets vacated by oil drilling. (Long Term Storage)
  • Sub-Oceanic Sequestering- Pumping liquid CO2 to the bottom of the ocean, where it will settle to the bottom and stay in relative storage, like a giant lake. There are concerns about this because of ocean acidification, and stability of these giant lakes of CO2
  • Sub-sediment storage – pump CO2 below seafloor making CO2 hydrate.    This seems likely to have the least environmental impact, but issues come up such as who owns the ocean, who funds this, can we really know the long term environmental impact?
  • Geothermal gradient  - the temperature of the earth increases dramatically as we go down through the crust. The center of the earth is as hot as the surface of the sun.  At high pressure CO2 is liquid



Eco and Gov

  • There are economic costs to all of these solutions, but almost no short term return.
  • This is an international problem, so it’s not easy to assign or accept responsibility – fiscally or otherwise
  • To be successful, there needs to be huge government initiative and funding. 
  • Reusing spent oil wells to pump the liquid CO2 into deep cavities



Connections

  • Mimi Katz-Environmental
  • Dr. Borton-solar
  • Dr. Borton-Environmental

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