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Broadcaster Press 03
October 22, 2013 www.broadcasteronline.com
USD professor researches
dust in China
By Travis Gulbrandson
travis.gulbrandson@plaintalk.net
While most Americans
might not think of China as
being a country where dust
storms take place, the storms
do raise a number of health
and environment concerns
there.
Because of research
performed in part by a
professor from the
University of South Dakota,
more is being learned about
some of China’s biggest
potential dust-emitters.
Mark Sweeney, associate
professor of earth sciences at
USD, spent two and a half
weeks doing research in
China this past summer.
“What I’ve seen so far is
that in many cases, the
amount of dust that’s
emitted by these different
surfaces in China (is) very
similar to what is emitted in
similar surfaces of the
Mojave Desert,” Sweeney
said during a presentation he
gave Oct. 17 as part of Earth
Science Week.
He traveled to China with
Professor Joe Mason of the
University of Wisconsin to
test the idea that sand dunes
could potentially be large
emitters of dust.
“Traditionally, sand
dunes are not considered big
dust-emitters, because
they’re mostly sand and they
contain five percent less of
silt and clay particles,”
Sweeney said.
However, Israeli
researchers now argue that
sand particles can break
apart due to wind and other
environmental factors,
creating dust.
Sweeney, Mason,
graduate and undergraduate
students performed their
research with a Portable InSitu Wind ERosion Lab (PISWERL) on a variety of
terrains in China, from the
Tengger Desert to dried-out
riverbeds.
“(The PI-SWERL)
simulates the wind and it
generates dust, and then you
can measure dust that comes
off of different types of soil
surfaces at different wind
speeds,” Sweeney said.
The PI-SWERL basically
looks like “an inverted soup
pot” with a blade
underneath, he said.
“The blade spins kind of
like a fan at different RPMs,
and when the blade spins,
the PI-SWERL … creates a
wind and gets the little
particles moving,” Sweeney
said. “The reason why people
are interested in this type of
technology is because it is
portable. One person can
operate it. It fits on a baby
carriage, and it has its own
power source, so you can
move it over the terrain and
measure dust in places where
a large wind tunnel could
never go.”
The PI-SWERL then
measures the amount of
dust, and the data is run
through a computer.
“We basically plug the
data into equations and
come up with an emissions
flux, which would be how
many grams of dust come
off of a square meter of
ground per second,” Sweeney
said.
One of the major
research areas was the
Chinese Loess Plateau, which
Sweeney described as “a very
extensive region in central
China that basically contains
a lot of windblown dust.”
“The dust has been
accumulating over millennia,
and it covers … 640,000
square kilometers. It’s an
enormous area,” he said. “In
some cases the dust is over
100 meters thick, so you’ve
got over 300 feet of dust
that’s been accumulating in
some places for 22 million
years. Basically, that makes
China the king of loess
deposits.”
The loess consists mainly
of silt and clay particles,
stacks well and has good
engineering properties.
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Professor Joe Mason of the University of Wisconsin walks down a flight of stairs along
the Chinese Loess Plateau.
“Loess is cohesive enough
that you can carve caves into
it, and people have been
living in caves since about
200 BC,” Sweeney said.
“There are large
metropolises of these cave
houses.”
While all of the data
collected this summer has
not yet been analyzed, that
which has been processed
shows that coppice dunes –
which form around
vegetation – are among the
largest emitters.
Land use practices could
also be a contributing factor,
Sweeney said.
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he was asked by Professor
Huayu Lu of Nanjing
University – who also paid
for the entire trip – to come
to China in the first place.
“The hope is, after I could
show them how useful it
was, that they could buy
their own and I could
potentially come over again
for additional collaborative
research,” he said.
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“Grazing sheep along the
desert margin might
destabilize some of these
areas where you get coppice
dunes forming, (especially) if
you get strong winds
blowing through there,” he
said.
Water shortages also play
a role, he said.
Sweeney said the PISWERL is the main reason
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