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Preparing Agriculture for a Changing
World
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Traditional tillage releases CO2 into the atmosphere. But
conservation tillage, like this cotton planted with no-till, can help store
carbon in the soil.
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Decades of tillage have caused soils on American cropland to lose up to half
their virgin organic matter. Much of it may literally be going up in a puff of
gas--as CO2.
"Carbon is the backbone of the organic matter that made our native
prairie soils so black and fertile," says Donald C. Reicosky, an ARS soil
scientist in Morris, Minnesota. "Soil carbon levels have been declining
ever since the first plows tore up prairie land."
The worst of the short-term losses occurs within minutes after the moldboard
plow fractures the soil, forcefully releasing CO2 stored in soil
pores and water. "It's just like opening a bottle of champagne. The gas in
the air space above the liquid is released, and CO2 bubbles out of
solution to establish a new equilibrium in the air," he says.
"The CO2 is a byproduct of microbial feeding on, and the
biological oxidation of, soil organic matter," says Reicosky, who has
measured CO2 losses from soils in Alabama, Texas, and Minnesota. He
gauges the amounts with a clear, plastic chamber equipped with an infrared
CO2 analyzer and carried by a tractor.
Studies by Reicosky and colleagues show that the soil releases as much as
260 pounds of CO2 per acre per hour immediately after tillage. Over
time, even more is lost because of the extra oxygen let in by tillage and the
extra organic matter from crop residues plowed under. "That speeds up
decomposition," notes Reicosky. "You're able to feed more soil
microorganisms faster, and there goes your organic matter."
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Technician Julie Roth prepares samples for soil carbon analysis.
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Not coincidentally, as the amount of soil
carbon has declined, atmospheric CO2 has gone up. The intensive
tillage seen in America's post-World War II farming boom increased the rate at
which soil carbon was converted into CO2, just as the Industrial
Age's coal-burning smokestacks were turning coal carbon into CO2 at
a furious pace.
But if tillage is the cause, it's also the cure, Reicosky says. Crop residue
management and conservation tillage reduced carbon losses by up to four-fifths
in Reicosky's studies. These practices disturb the soil less and conserve
organic matter by leaving dead roots undisturbed and crop residue on the
surface after harvest.
"The trick is to use crop residue management and other soil management
techniques to keep carbon where it belongs," he says. "Let the soil
serve as a storage reservoir, or sink, for excess carbon created from human
activity, ameliorating the potential environmental harm of rising levels of
atmospheric carbon dioxide."
There are estimates that widespread adoption of improved crop residue
management could return soil carbon levels to near those of our native
prairies, storing or sequestering a portion of the carbon released through
worldwide fossil fuel emissions, Reicosky says.
Of course, returning highly erodible cropland to perennial grasses would be
even better, says program leader Mayeux.
"To date, that has been done on 36 million acres (15 million hectares)
of land taken out of production and covered with grass or trees under the
federal Conservation Reserve Program," he says.
"Each year, these CRP soils may be storing almost a third of the 38
million metric tons of carbon released annually into the atmosphere by all
sources related to U.S. agriculture. Most of these lands are dryland farms in
the Great Plains."
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Inside the "sniffing corral" at Watkinsville, Georgia, soil
chemist Ronald Sharpe (left) and soil scientist Lowry Harper check equipment
designed to measure methane concentrations in air.
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Lowry A. Harper, an ARS agricultural microclimatologist in Watkinsville,
Georgia, also measures CO2--not from soil but from animal waste
treatment ponds called lagoons.
He has devised a system for measuring CO2 and other greenhouse
gases with an array of outdoor "sniff," or sampling, tubes connected
to a laser spectrometer or an infrared gas analyzer.
For the lagoons, Harper mounts the sniff tubes on a floating barge to detect
CO2, methane, nitrous oxide, and ammonia emissions. Harper's
research will not only help computer modelers better evaluate the greenhouse
gases emitted from animal waste lagoons, but also establish whether there's
enough methane emitted to make it worthwhile for a farmer to use it as fuel for
an electrical generator.
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Harper uses a land-based version of the sniff
tubes for measuring methane emissions from cattle breath. He uses similar
techniques to detect nitrous oxide on land and has measured significant
emissions where animal wastes have been spread.
Eventually, he and others plan to adapt the equipment to measure gas
emissions from soil, landfills, rice paddies, animal manure, and termite
mounds.
From his tests so far with cattle in Australia, Georgia, and Texas--the
first such outdoor tests in the world--Harper has found that a cow grazing on
pasture can emit more than 8 ounces (230 grams) of methane per day. "That
is somewhat more than estimates from indoor tests of confined animals," he
says. The studies also pointed to a solution: Higher quality diets reduced
methane emissions. Cows fed grain rather than pasture grass emitted only 2.4
ounces (70 grams) per day, about half as much as previous tests indicated.
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This page last updated June 2005.
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