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The Iron Experiments

Richard Barber's Team Goes to the End of the Earth to See if Dust Once Played a Role in Climate Change p.5

  Since much of the carbon fixed in both patches was tracked down to hundreds of meters below the surface, when “extrapolated over large portions of the Southern Ocean” the SOFeX results suggest “that iron fertilization could cause billions of tons of carbon to be removed from the atmosphere each year,” the release adds.

  So does the SOFeX cruise show that there could be an engineered iron solution for contemporary global warming? Barber doesn’t think the sinking carbon was tracked down deep enough to resolve whether lots of it would be stored for long time periods.

   “But the indications that Martin’s Iron Hypothesis is true keep looking better and better,” he says, noting that, at the least, the scientific community no longer tends to believe those who think iron could have such an effect on global climate are “certified lunatics.”

  “Now it’s actually creeping into the textbooks as a given. First you could not get people to believe it, and now you find that people are believing it without being critical enough. It’s an issue in which basic science seems to give a hint of a socially useful thing. We have made enormous progress in understanding this, but we’re not there yet.

  “In some ways I’m sorry that we raised the engineering side of this,” he says about notions of iron-laden vessels rescuing humankind from problems we have caused ourselves by generating so much CO2 to drive our vehicles and run our power plants.

   “It would be a big mistake for us to use it as an excuse for not doing other things we know would work, like becoming more energy efficient or moving to alternative forms of energy,” he muses.

   “It would be simpler for us, as scientists, if the societal application didn’t exist.”

Monte Basgall is a senior writer in Duke’s Office of News and Communications specializing in science.

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photo captions: 1. A stormy day in mid-summer in the Southern Ocean close to the latitude of the Antarctic Circle, between 66 and 67 degrees south; work outside on deck was suspended when it got this rough. Storms were frequent, but short in duration, usually lasting only a few hours. 2. On board the R/V Roger Revelle. 3. The research vessel Revelle seen through the stern A-frame of the research vessel Melville. In the vast and lonely Southern Ocean it was nice to have the company of two of the most capable ships in the U.S. research fleet. 4. Barber at Duke Marine Lab.
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