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Ocean Carbon Sequestration

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What the increase in atmospheric CO2 has done to ocean chemistry ... CO2 concentration increases more CO2 dissolves into the ocean as carbonic acid ... – PowerPoint PPT presentation

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Title: Ocean Carbon Sequestration


1
Ocean Carbon Sequestration
  • John Nowoslawski
  • Fall 2003

2
Today
  • Basics of CO2 in the atmosphere and how it gets
    into the ocean
  • What the increase in atmospheric CO2 has done to
    ocean chemistry
  • Possibility of the ocean to safely sequester CO2
    from the atmosphere while reversing the negative
    effects on ocean chemistry from increased
    atmospheric CO2
  • Experiments
  • Where it could go

3
Follow the Carbon
4
Carbon in the Ocean
The entire system is in equilibrium
5
Anthropogenic Effects
  • As the atmospheric CO2 concentration increases
    more CO2 dissolves into the ocean as carbonic
    acid
  • The buffer system of the ocean activates in order
    to prevent a large swing in pH
  • CO3-- ions pick up H ions and convert to HCO3-
    ions
  • Bottom Line the pH of the ocean has decreased
    and will continue to decrease. The concentration
    of carbonate ions (CO3--) is decreasing.

6
Solution?
  • Increase the CO3-- concentration. But how?
  • Add CO3-- ions by throwing rocks into the ocean.
  • What will this do?

7
Throwing Stuff into the Ocean
If we add CO3-- ions, the buffer system of the
ocean will pull CO2 out of the atmosphere to make
HCO3- ions to keep the system in equilibrium
8
Throwing Stuff into the Ocean
  • What happened?
  • The dwindling carbonate ion (CO3--) concentration
    has increased.
  • The negative effects from the lowering of the pH
    are reversed
  • The buffer system of the ocean is strengthened
  • The total amount of carbon the ocean can store
    has increased
  • CO2 is naturally pulled out of the atmosphere
    (sequestered) and is in a stable form in one of
    the earths largest carbon sinks.

9
Experiments
  • Made Artificial Seawater in the laboratory
  • Figuring out which minerals dissolve into
    seawater and what problems arise
  • Ocean chemistry is very unstable because the
    upper 100m of the ocean is supersaturated with
    respect to Calcite (CaCO3)
  • Building a dissolution rate calculator
  • Whatever mineral added to the water must dissolve
    in the upper 100m of the ocean, or it is too far
    from the atmosphere to pull out CO2

10
Dissolution Rate Calculator
11
Conclusion
  • It is possible that the addition of alkaline
    minerals will decrease atmospheric CO2
    concentration and safely sequester it while
    having other positive effects on ocean chemistry.
  • Experiments are being performed to determine if
    the dissolution will happen and if the effects
    are beneficial.
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