WASHINGTON July 20, 2004 — The millions of
Americans enjoying beach vacations this summer may not be aware of
it, but the land beneath their feet is breathing.
As tides come and go, the water causes changes in underground air
pressure, forcing air and moisture in and out of the ground along
the shore, Jui J. Jiao of the University of Hong Kong found in
studying coastal areas near his school.
While tidal changes in underground water levels along the shore
were known, changes in air pressure beneath the surface were not as
well recognized, Jiao reports in Geophysical Research Letters.
The inhaling and exhaling isn't something likely to be noticed by
frolicking beachgoers, though Jiao believes organisms living in the
soil should be able to detect it.
"People can feel the process only under very special conditions.
In Hong Kong, people once saw the water bubbles coming out of the
fractures or joints of an asphalt pavement and heard the noise of
the air flow through fractures," he said.
But that was a special case with a rapidly changing tide and air
and water moving through a limited number of underground
pathways.
"Under normal conditions, people usually cannot directly detect
this phenomenon. This is probably a reason why this phenomenon has
not been studied until recently," he said.
Jiao said the breathing causes a constant exchange of air, water
moisture and any pollution that may be present between the soil and
the air.
In addition, the constant changes in pressure beneath the surface
may have an effect on buildings, airport and seaport structures and
coastal highways, which are usually designed to support downward
acting loads.
Since asphalt and building structures can block this air flow,
the coastal breathing may produce repeated cyclical up and down
pressures on these structures.
"It is well known that the strength of materials under cyclic
conditions is significantly lower than for (single direction)
loading," Jiao said via e-mail. "The performance of concrete or
asphalt surface under cyclic loading by tidal-induced air pressure
below the paved ground surface needs to be evaluated."
Douglas L. Inman of the Scripps Institution of Oceanography in La
Jolla, Calif., agreed that the finding "will be very important to
coastal engineers working in areas of reclaimed land where it is
important to avoid having roads and structures pop-up."
Inman, who was not part of Jiao's research team, said that the
breathing may be more common in areas of artificial fill, like Hong
Kong.
"There should be much less 'breathing' along natural coastal
areas except where the ... rock consists of porous limestone or
cobbles," he said.
Jiao and his co-author, Hailong Li of the China University of
Geosciences at Wuhai, found that regular changes in below-ground air
pressure which were most affected by the rising and lowering of the
water table with the tides.
The process, which is lessened when it is raining, is relevant to
coastal areas worldwide, Jiao said.
The research was funded by the Hong Kong Research Grants Council,
the University of Hong Kong and the National Science Foundation of
China.
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