A new global-scale modeling study that takes into account
nitrogen -- a key nutrient for plants -- estimates that carbon
emissions from human activities on land were 40 percent higher in the
1990s than in studies that did not account for nitrogen.
Researchers at the University of Illinois at Urbana-Champaign and the
University of Bristol Cabot Institute published their findings in the
journal Global Change Biology. The findings will be a part of
the upcoming Fifth Assessment Report from the Intergovernmental Panel on
Climate Change. "One nutrient can make a huge impact on the carbon
cycle and net emissions of the greenhouse gas carbon dioxide," said
study leader Atul Jain, a professor of atmospheric sciences at the U. of
I. "We know that climate is changing, but the question is how much? To
understand that, we have to understand interactive feedback processes --
the interactions of climate with the land, but also interactions
between nutrients within the land."
The carbon cycle is a balance of carbon emissions into the atmosphere
and absorption by oceans and terrestrial ecosystems. Carbon is absorbed
by plants during photosynthesis and by the oceans through sea-air gas
exchange. On the other side of the cycle, carbon is released by burning
fossil fuels and by changes in land use -- deforestation to expand
croplands, for example. While fossil fuel emissions are well-known,
there are large uncertainties in estimated emissions from land use
change.
"When humans disturb the land, the carbon stored in the plants and
the soil goes back into the atmosphere," Jain said. "But when plants
regrow, they absorb carbon through photosynthesis. Absorption or release
of carbon can be enhanced or dampened depending on environmental
conditions, such as climate and nutrient availability."
Nitrogen is an essential mineral nutrient for plants, which means
that plants need it to grow and thrive. In nontropical regions
especially, plant regrowth -- and therefore carbon assimilation by
plants -- is limited by nitrogen availability.
"Most models used to estimate global land use change emissions to
date do not have the capability to model this nitrogen limitation on
plant regrowth following land use change," said Prasanth Meiyappan, a
graduate student who is a co-author of the study. "This means, for
example, they overestimate regrowth and they underestimate net emissions
from the harvest-regrowth cycle in temperate forest plantations."
Jain's team, in collaboration with Joanna House, a researcher at the
University of Bristol's Cabot Institute, concluded that by not
accounting for nitrogen as a limiting nutrient for plant growth, other
models might have underestimated the 1990s carbon emissions from land
use change by 70 percent in nontropical regions and by 40 percent
globally.
"This gross underestimation has great implications for international
policy," House said. "If emissions from land-use change are higher than
we thought, or the land sink (regrowth) is more limited, then future
emissions cuts would have to be deeper to meet the same mitigation
targets." Next, the researchers are investigating the impacts of other
nutrients, such as phosphorus, on the carbon cycle. They also are
estimating the carbon stored in the soil, and how much is released or
absorbed when the soil is perturbed.
"Soil has great potential to sequester carbon," Jain said. "The
question is, how much that's being released is being sequestered in the
soil? We have to understand how human behavior is changing our
environment and interacting with our ecosystems."
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