«We are continuously asked, how
much organic carbon and CO2 do gelatinous plankton sink worldwide, whether their export capacities are similar to phytoplankton and marine snow.
«There's so
much organic carbon trapped in permafrost,» she said, «and we don't really know what's going to happen as the climate warms.»
Not exact matches
«We don't just look at total soil
organic carbon, but also the components of soil that have stable pools of
carbon — humic substances, which gives us a
much more accurate and precise view of the stable, long - term storage of
carbon in the soils.»
Certifications other than
organic don't do
much to reduce
carbon footprint over conventional farming, suggesting that standards need to be modified to encourage footprint - lowering practices.
Tilling results in soil
organic matter being broken down
much more rapidly, and
carbon is lost from the soil into the atmosphere.
The process of making
organic capacitors does release a little
carbon dioxide, but not nearly as
much as would be emitted if you let the same quantity of material burn or decay, says Caroline Burgess Clifford at Penn State University.
Much of that
carbon is frozen
organic matter locked within permafrost.
If the
carbon that makes up
much of the
organic matter remains stored in the soil, then it doesn't get into the atmosphere where it can contribute to climate change.
By comparing the amount of
carbon 13 in the inorganic particles with the absence of
carbon 13 in the
organic matter, scientists can estimate how
much oxygen was present in the atmosphere at that time.
«We need to understand where
carbon goes, how
much of it goes into the
organic matter, how that affects the air - sea exchanges of CO2 and what happens to fossil fuel we have emitted from our tailpipes.»
The resultant clay then washes down to the sea and settles on the bottom, where the clay's chemical properties actively attract
organic carbon and then absorb it,
much like kitty litter.
As these more substantial microbes die, the researchers found they increase the flux of sinking
organic carbon particles by as
much as 35 percent.
But because their roots and soil are regularly washed by tides,
much of this
organic carbon leaches into the ocean.
Researchers led by Thorsten Dittmar of Florida State University in Tallahassee measured how
much mangroves contribute to the
organic carbon...
«These superdeep diamonds contained
much less
carbon - 13, which is most consistent with an origin in the
organic component found in altered oceanic crust.»
Researchers have found that
carbon particles released into the air from burning trees and other
organic matter are
much more likely than previously...
Much of the research has focused on microorganisms capable of immobilizing contaminants, such as uranium, after introducing
organic carbon compounds, such as acetate, lactate and ethanol.
How
much was
organic (bound to
carbon) vs. inorganic arsenic?
We also need to listen to authors such as Heather Rogers, who has undertaken a devastating critique of «ethical consumerism» and today's
much - touted «green» solutions —
carbon offsets,
organic food, biofuels, and eco-friendly cars and homes — in her book, Green Gone Wrong.
There could be a lot of hydrate in Arctic sediments (it's not real well known how
much there is), but there is also lot of
carbon as
organic matter frozen in the permafrost.
David, I havent been keeping up with all the PETM research, but I do recall that individual plankton recovered from Bass River, New Jersey show a single step CIE. Due to the high sedimentation rate of coastal fluvial systems, Bass River sediments are consistent with a
much shorter duration of
organic carbon release during the PETM (estimated as less than 500 years).
Not only are burning trees sending millions of tons of
carbon into the atmosphere, perhaps even worse are the flames consuming peatland, a rich soil - like earth made up of decomposing
organic material that can store as
much as 3,300 tons of
carbon per hectare.
Inthorn contemplates that enhanced and widespread downslope transport of
organic carbon in cloudy water layers may have been
much more vigorous at times when sea level was fluctuating and lower than today.
The
carbon loss occurred first through the removal of the original vegetation, which stored
much carbon in its leaves, stems and trunks; then through the oxidation of
carbon in newly exposed soils; and finally through increased soil erosion, which carried away
much of the
organic - rich sediment during flooding.
To determine how
much carbon is released by erosion, the researchers combined their soil
organic carbon calculations with long - term erosion rates (the region loses a mean of 0.7 meters of coastline per year).
They measured the
organic carbon content of the samples and determined how
much of the soil volume was taken up by large bodies of ground ice.
The researchers estimate that the dissolved
organic carbon released by melting glaciers will be an increase of half as
much again on the current flow − the equivalent of about half the annual flow of dissolved
carbon down the mighty Amazon River.
There are at least ~ 1500 billion tons of
organic carbon in permafrost zone soils, almost twice as
much as currently exists in the atmosphere.
This would mean there is
much more BC in the atmosphere on average (also
organic carbon, etc) than Bond used in their modeling.
Much carbon was sequestered as shells, peat, or other
organic debris.
In fact, 10,000 medium - sized
organic farms can store as
much carbon in the soil as we would save if we took one million cars off the road.
The result is that the plots continue to have similar yields, with the
organic plots performed
much better in terms of building soil
carbon and retaining nitrogen in the soil.
If all farmable fields in the world accumulated as
much carbon as fast as the
organic fields at Rodale Institute, we could store 40 percent of the world's annual global greenhouse gas emissions in the soil.
Meanwhile, according to the American Public Transportation Association, mass transit produces 95 percent less
carbon monoxide, 90 percent less volatile
organic compounds, and about half as
much carbon dioxide as private vehicles.