| May
12, 2005
Study Reveals Smog Clearing Properties Of Atmosphere
By Kim McDonald
Chemists at
the University of California, San Diego and Purdue University
have discovered that natural chemical processes in the atmosphere
may be removing smog and other damaging hydrocarbons at a faster
rate than once believed.
In the May 24th issue
of the Proceedings of the National Academy of Sciences,
the scientists report that naturally-occurring atmospheric chemicals
react with sunlight more effectively than scientists previously
thought, breaking down smog and other pollutants after they
absorb energy from sunlight.
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Jamie
Matthews of UCSD with laser apparatus used in study.
Credit: UCSD
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While many molecules
have been known to behave in this way—producing natural
air cleaners called OH radicals—the chemicals the team
studied have for the first time been observed to produce smog-destroying
OH radicals at low ultraviolet wavelengths. This observation
had long eluded scientists primarily because photochemistry
at these wavelengths had been difficult to study. But a sensitive
laser technique allowed the scientists—Amitabha Sinha
and Jamie Matthews of UCSD and Joseph Francisco of Purdue—to
record these reactions for the first time.
“Thanks to an
innovative laser technique that at last allowed us to observe
these chemicals in action, we now theorize that the atmosphere
may produce up to 20 percent more OH radicals from these chemicals
than we once thought,” said Francisco, professor of earth
and atmospheric sciences and chemistry at Purdue. “We
now have a better understanding of an atmospheric process that
could be giving our pollution-weary lungs more breathing room.”
“This study
is important because it shows that the atmosphere could be generating
far more OH radicals than previously thought and accounted for
by current models, which neglect the new chemistry we observe,”
said Sinha, an associate professor of chemistry and biochemistry
at UCSD who headed the research team. “It could imply
that the atmosphere is more effective at breaking down pollution
than models have shown. We hope the results will improve our
understanding of how the atmosphere works.”
Sinha cautioned, however,
that the results do not mean we can now safely ignore atmospheric
pollution.
“This study in
no way implies that we are out of the woods with regard to atmospheric
pollution,” he said. “What it means is that we need
to do a much more careful job with our measurements in order
to accurately account for all sources of OH radicals present
in the air.”
Much of the hydrocarbon
pollutants pumped into the atmosphere by humans result from
burning organic matter such as wood or fossil fuels. The atmosphere
has three main ways to cleanse itself of such pollutants. Two
are relatively direct: water droplets in clouds absorb and rain
them out of the atmosphere or sunlight breaks the molecules
apart.
“The third way
is the one we are concerned with here, the way that involves
breaking these hydrocarbons down chemically,” said Francisco.
“For that, the atmosphere relies on a reactive group of
chemicals called OH radicals that attach themselves to hydrocarbons
and rip them into inert pieces.”
OH radicals arise naturally
from many atmospheric constituents. The effect they have on
pollution has long been factored into models that describe the
atmosphere and attempt to predict how it will react to increasing
quantities of hydrocarbon pollutants, which generate smog. But
these models do not always function well, Francisco said, in
part because OH radicals are in some ways an unknown quantity.
“One of the biggest
questions in our field concerns the amount of OH radicals the
atmosphere holds,” he said. “It’s tough to
get a handle on them because they are so reactive—which
means they vanish fast—and also because we don’t
have complete knowledge of all the sources that produce them
yet.”
The experiments—which
Sinha and Matthews, a graduate student in his laboratory, performed
at UCSD—used a laser technique that allowed the team to
look at the OH radical-producing molecules in a new way. More
precisely, it allowed them to observe a portion of the molecules’
spectrum which had been something of a blind spot for atmospheric
scientists, who often detect chemical reactions by perceiving
the telltale light frequencies that certain reactions are known
to emit or absorb. Many sources of OH radicals strongly absorb
UV light, making them easily detectable. However, the weak absorptions
in the lower region of the ultraviolet spectrum, from wavelengths
of about 360 to 630 nanometers, has been more challenging.
“It’s usually
difficult to monitor what’s going on in that region of
the spectrum because the molecules of interest typically have
weak absorption features there, so they’re tough to see,”
said Sinha. “However, there is a lot of solar radiation
coming down over this wavelength region, so even weak absorptions
become important. The upshot is that a lot of atmospheric models
have ignored these weak absorption features altogether, assuming
that because nothing can be seen using conventional techniques,
nothing must be happening.”
The sensitive laser
technique, called “action spectroscopy,” however,
enabled the team to characterize the minute quantities of radiation
absorbed by a substance called methyl hydroperoxide when it
breaks up in sunlight and forms OH radicals. Methyl hydroperoxide
is one of the substances that can absorb light in the lower
UV spectrum, and the team theorizes that the sensitive laser
technique, called action spectroscopy, could reveal OH radical
production from other chemically related molecules as well.
Francisco, who contributed
to the study’s computations, said he hopes the study also
would encourage other refinements to atmospheric models.
“Models are only
as good as the information we put into them, and we must always
keep a cautious perspective about the results models return,”
he said. “Sometimes things are happening that you can’t
see using standard methods. Now we hope to take this improved
understanding of the atmosphere and include it in future models.
That’s the next step.”
This research was supported
in part by the National Science Foundation.
Comment:
Amitabha Sinha: (858) 534-5593
or Joseph Francisco:
(765) 494-7851
Media Contacts:
Kim McDonald, UCSD (858)
534-7572 or Chad Boutin,
Purdue (765) 494-2081
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