"Iron fertilization" refers to the process of adding iron to the ocean to stimulate the growth of tiny plant-like organisms called phytoplankton. These organisms use carbon dioxide during photosynthesis, helping to reduce it in the atmosphere and potentially mitigating the effects of climate change.
Full definition
With Leinen as its chief scientific officer, Climos sought to perform
ocean iron fertilization experiments and sell carbon credits it could show it earned.
-- Southern Ocean
Iron Fertilization Experiment (SOFeX)-- The basics of the most recent expedition — Penny Chisholm's site, which lists many professional papers — Paul Falkowski's article (PDF document)-- DOE article: Climate Change Scenarios Compel Studies of Ocean Carbon Storage — Government site for carbon sequestration research — An earlier piece Williams wrote on sequestration — Will Ocean Fertilization To Remove Carbon Dioxide from the Atmosphere Work?
For
iron fertilization forcing, we choose temperature − dust relationships from the high southern latitudes, as the Southern Ocean is the main region where this process is relevant.
«I would be reluctant to extrapolate from any one experiment anything having to do with the efficacy of
iron fertilization as a carbon - sequestration strategy,» says Coale.
Other more conventional (if much smaller) scientific tests of
iron fertilization in waters near Antarctica found a mix of results on oceanic carbon dioxide uptake, meaning lots more research needs to be done before anyone can bank on ocean repositories as a significant offset for smokestack carbon dioxide emissions.
GreenSea Venture, the company started by Markels, remains very focused
on iron fertilization as a sequestration strategy.
Scientists often look into Earth's past to better predict its future, and some clues
about iron fertilization come from past ice ages.
«I am disturbed and disappointed as this will make legitimate, transparent [ocean
iron fertilization] experiments more difficult,» Smetacek says.
According to Ingall, removal of iron by diatom - dominated phytoplankton communities may dampen the intended outcome of enhanced carbon uptake
through iron fertilization by reducing the productivity of other phytoplankton, which take up carbon dioxide more efficiently.
Andy: I heard Professor Wally Broecker — a guy who knows a thing or two about the oceans on this planet — say something like «we shouldn't mess with the oceans [by attempting large -
scale iron fertilization] unless we know for sure that it won't have unforeseen ecological effects».
Most likely in response to the recent study published in Nature about
oceanic iron fertilization, The Onion has an issue of American Voices about it.
We deal
with iron fertilization in the context of the Danish Center for Earth System Science (DCESS) model (41) for which reduction of high - latitude new production (relative to that which would occur if phytoplankton there could make full use of all available nutrients) is expressed in terms of an efficiency factor (see equation 19 in ref.
According to the report, «deploying ocean
iron fertilization at climatically relevant levels poses risks that outweigh potential benefits.»
It remains unclear at this point which particular species bloomed as a result of the HSRC iron release but the team is sending out for analysis more than 10,000 water samples, data the HSRC team says it will share as
other iron fertilization experiments have done.
Coale warns that
calling iron fertilization a failed strategy on the basis of an experiment in low - silicon waters is just as unwise as declaring the technique a home run after a successful experiment would have been.
This was the conclusion of a recent analysis of natural
iron fertilization by the Kerguelen Plateau in the Southern Ocean (Blain et al, 2007).
In that project, US entrepreneur Russ George convinced a Haida Nation village to
pursue iron fertilization to boost salmon populations, with the potential to sell carbon credits based on the amount of CO2 that would be sequestered in the ocean.
Sequestering carbon in these parts of the global ocean
via iron fertilization «would require significant ecosystem change,» Trull's paper said.
Based on a century of ocean plankton science and the 10 international experiments on
iron fertilization over the last 15 years we are confident that the scale, methods and technologies of the work we are planning will have positive impacts on all fronts, improving water quality, buffering surface water acidity, recharging the marine food chain, and safely sequestering enormous amounts of CO2 to help slow climate change.
HSRC's George has a long history of attempting to commercialize
such iron fertilization, most notoriously via the company known as Planktos, which went bankrupt in 2008.
Whereas this experiment might shed light on whether or
not iron fertilization can hope to draw down atmospheric levels of CO2, it hardly amounts to a long - term planetary scale change — the definition of geoengineering according to the U.K.'s Royal Society.
«There are plenty of ways to do it wrong, but done right,
[iron fertilization] does actually sequester carbon for hundreds of years in the place that it would ultimately end up anyway,» remarked Andrew Watson, a biogeochemist at the University of East Anglia.
The federal Department of Energy, recently provided with $ 90 million in carbon sequestration research, continues to seek proposals to
study iron fertilization as a carbon dioxide amelioration strategy.
More dust, less sunlight, colder oceans, but more dust means that more dust falls on the oceans, which means the
more iron fertilization of photosynthetic organisms there is, the higher the level of photosynthesis, so the more CO2 is converted into biomass, so more organic carbon falls to the sea bed, so the more atmospheric carbon disappears into the ocean sink, and also the wider the oxic band at the oceans surface and so more methane is oxidized on the way to the surface.
«Determining the local effects of
iron fertilization against the background of natural variations is difficult, and impacts on fisheries, ocean biota and carbon cycling harder still,» wrote members of the In - Situ Iron Studies Consortium — an international group of scientists studying such ocean fertilization — in a letter to the Guardian newspaper, which first reported on the Haida experiment.
«There's not evidence that that region is iron - limited,» argues phytoplankton researcher Maite Maldonado of the University of British Columbia, who sailed on one of the first
experimental iron fertilization cruise in the Southern Ocean in 1999.
(
Iron fertilization enthusiasts focus on the Southern Ocean because other seas have much more natural algae, so growing blooms might just foster growth that would have happened anyway.)
Before the 2004 study, known as EIFEX, the
European Iron Fertilization Experiment, scientists had conducted 11 experiments at sea to explore how trace quantities of iron may encourage the growth of algae.
Wilf Luedke, Canada's chief of salmon stock assessment for the south British Columbia coast, told me he has nothing against careful tests of deep -
sea iron fertilization, but worries that the debate — given the complexity in climate and ocean conditions shaping salmon populations — could distract from more clear - cut, and cheaper, ways to aid salmon, and absorb carbon dioxide, closer to shore.
Iron fertilization just won't cut it, either scientifically or ecologically, she warned, adding that the best solution is simply to stop producing CO2.
Nevertheless, in view of the serious risks we are presently taking with our global climate, I feel that
considering iron fertilization as a possible means for purposeful co2 sequestration can not be entirely dismissed at this point.»
The 2012
iron fertilization generated an algae bloom that fed salmon at the right time to boost the salmon population * the salmon bloom died in days and then fell to the bottom of the ocean taking large amounts of CO2 with them
Phrases with «iron fertilization»