Friday, March 30, 2012

Oceanography Enters the Iron Age




This is an important discovery along with our understanding of the limiting nature of iron content in terms of surface water productivity.  What it suggests to me is that there is a need to determine an appropriate methodology that successfully releases iron into surface waters and we need to be a little clever about it all.

One way may be to mandate a iron rich mineral as plastic fillers so that bio-degradation is both accelerated and significant in providing the nutrient.  Otherwise, we need to be able to introduce iron onto surface waters in such a way that they stay suspended until released.  There may be mineral forms that will meet this need.  We need to look. 

Fine grinding will produce such particles of even generally heavy product.  Once put in the water, they can linger and provide the necessary nutrients.  All this is done by the mining industry as a matter of course.  Plenty of minerals have iron in some form or the other and in time the oxygen will oxidize out.  None of them have ever been mined for their iron or ever will be.  The issue is to make it fine enough to rust out the iron fairly quickly.

Nature does this for us at times by blowing dust storms out to sea.  Maybe the simple answer is to load desert sand on a ship as ballast and proceed to jump it as the ship transits.

Oceanography enters the Iron Age


Mar 27, 2012

For many years scientists have known that iron is often associated with organic carbon in sediment but did not know why. Now researchers from Canada have found that just over 20% of the organic carbon in sediments is directly bound to reactive iron phases.

They estimate that worldwide 19–45 Gigatonnes of organic carbon are locked up in surface marine sediments in this way. Because reactive iron phases are metastable over long time periods, the sediments could be an efficient "rusty sink" for organic carbon.

"Burial in sediments is the only long-term sink of organic carbon on the planet, on geological timescales," Yves Gélinas of Concordia University told environmentalresearchweb. "Yet only a tiny fraction of organic carbon – about 0.3% – produced in the surface waters through photosynthesis eventually reaches the seafloor and is preserved in sediments. The rest is degraded in the water column and at the surface of the sediment."

The most widely accepted explanation for the tiny proportion of organic carbon preserved, says Gélinas, is that it's protected by sorption on clay mineral surfaces in the water column and in sediments.

"Our work shows that iron oxides are also very important, which is totally new," he added. "Why does it matter? Simply because iron oxides are not stable in anoxic [no-oxygen] environments (they form only in oxic settings), while clay minerals are stable whatever the redox conditions of the system."

The expansion of oceanic "dead zones" – regions where oxygen levels are too low to sustain life – could eventually affect this iron complexation mechanism for preserving organic carbon. According to Gélinas, this will "create a positive feedback mechanism fuelling greater oxygen consumption" as more organic matter will be degraded in the water column or at the surface of the sediments, using additional oxygen and so contributing to the expansion of dead zones.

"Iron has become a very popular research topic in chemical oceanography since the discovery that it is a limiting nutrient for primary productivity in large areas of the ocean," said Gélinas. "We show for the first time that iron also plays an important role in organic carbon preservation. We are definitely in the Iron Age of oceanography."

Gélinas and colleagues from Concordia University and McGill University tested sediments from around the world sampled from freshwaters, estuaries, river deltas, continental margins and the deep sea, using an iron reduction method previously used in soils.
"We now better understand the controls on organic matter preservation in sediments through its stabilization by iron complexation," said Gélinas. "[This] means that we can do a better job building models representing carbon preservation and cycling in marine environments. It also means better prediction of the evolution of the organic carbon preservation function in these models as bottom-water dissolved oxygen concentrations keep decreasing."

Now Gélinas says the team plans to get a clearer idea of the types of chemical bonds that link iron and organic matter, and how changes in local redox conditions affect their relative proportions in sinking particulates and sediments.

"We have recently obtained Synchrotron X-Ray beam time at the Brookhaven National Light Source Laboratory (NLSL) in Long Island, US, and acquired a very promising first set of data showing that our working hypothesis – that iron complexation to organic carbon plays a much greater than anticipated role in preserving a large fraction of organic carbon in sediments – is correct," he said. "We have applied for more beam time at the NSLS and at the Canadian Light Source Synchrotron in Saskatchewan to pursue this work."

The team would also like to estimate the importance of the mechanism in the stabilization of soil organic carbon.

About the author

Liz Kalaugher is editor of environmentalresearchweb.

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