In pictures, the Arctic appears pristine and timeless with its barren
lands and icy landscape. In reality, the area is rapidly changing.
Scientists are working to understand the chemistry behind these changes
to better predict what could happen to the region in the future. One
team reports in ACS’ Journal of Physical Chemistry A that sea salt could play a larger role in the formation of local atmospheric pollutants than previously thought.
The
Arctic’s wintertime ice hit a record low this year, and its air is
warming, according to NASA. Previous research has shown that pollutants,
including gaseous nitrogen oxides and ozone, have at times been
recorded at levels similar to those one would see in more populated
areas. Nitrogen oxides are air pollutants that, in sunlight, lead to the
formation of ozone, the main component in smog normally associated with
cities. The gases can be processed in the atmosphere and be deposited
on Earth as nitrates, which can get trapped in snow. In sunlight, snow
can act as a reactor in which nitrates may be transformed back to
nitrogen oxide gases. In the Arctic, sea ice and snow contain salt and
other impurities that can possibly alter the efficiency of this process.
James Donaldson, Karen Morenz and colleagues took a closer look at how
salt and nitrate content in snow could affect the levels of nitrogen
oxides in the air during sunny conditions.
The researchers tested
lab-made snow containing nitrate alone or nitrate and salt. They found
that under simulated sunlight, about 40 to 90 percent more nitrogen
dioxide (NO2) was reformed from the snow with low levels of salt at
environmentally relevant concentrations than snow with no salt.
Researchers observed the greatest effect when they used realistic sea
salt in the experiment. The results suggest that sea ice and salty snow,
which previously have not been considered as factors in the balance of
ozone-forming chemicals in the atmosphere, should be a part of future
models.
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