Radon becomes hazardous when it enters homes and becomes
trapped in poorly ventilated or well-insulated areas. Radon moves
up through the soil and moves toward places with greater permeability.
Home foundations are often built with a very porous and
permeable gravel envelope surrounding the foundation, to allow for
water drainage. This also has the effect of focusing radon movement,
bringing it close to the foundation, where the radon may
enter through small cracks in the concrete, seams, spaces around
pipes, sumps, and other openings, as well as through the concrete
which may be moderately porous. Most modern homes intake less
than one percent of their air from the soil. Some homes, however,
particularly older homes with cracked or poorly sealed foundations,
low air pressure, and other entry points for radon, may intake as
much as 20 percent of their internal air from the soil. These homes
tend to have the highest concentrations of radon.
Radon can also enter the home and body through the groundwater.
Homes that rely on well water may be taking in water with
high concentrations of dissolved radon. This radon can then be
ingested, or it can be released from the water by agitation in the
home. Radon is released from high-radon water by simple activities
such as taking showers, washing dishes, or running faucets. Radon
can also come from some municipal water supplies, such as those
supplied by small towns that rely on well fields that take the
groundwater and distribute it to homes without providing a reservoir
for the water to linger in while the radon decays to the atmosphere.
Most larger cities, however, rely on reservoirs and surface
water supplies, where the radon has had a chance to escape
before being used by unsuspecting homeowners.
A greater understanding of the radon hazard risk in an area
can be obtained through mapping the potential radon concentrations
in an area. This can be done at many scales of observation.
Radon concentrations can also be measured locally to learn what
kinds of mitigation are necessary to reduce the health risks posed
by this poisonous gas.
The broadest sense of risk can be obtained by examining
regional geologic maps and determining whether or not an area is
located above potential high-uranium content rocks such as granites,
shales, and rhyolites. These maps are available through the
U.S. Geological Survey and many state geological surveys. The U.S.
Department of Energy has flown airplanes with radiation detectors
across the country and produced maps that show the measured
surface radioactivity on a regional scale. These maps give a very
good indication of the amount of background uranium concentration
in an area and thus are related to the potential risk for radon gas.
More detailed information is needed by local governments,
businesses, and homeowners to assess whether or not they need to
invest in radon remediation equipment. Geologists and environmental
scientists are able to measure local soil radon gas levels using a variety
of techniques, typically involving placing a pipe into the ground
and sucking out the soil air for measurement. Other devices may be
buried in the soil to more passively measure the formation of the damage
produced by alpha particle emission. With such information, the
radon concentrations in certain soil types can be established. This
information can be integrated with soil characteristic maps produced
by the U.S. Department of Agriculture and state and county officials,
to make more regional maps of potential radon hazards and risks.
Most homeowners must resort to private measurements of
radon concentrations in their homes using commercial devices that
detect radon or measure the damage from alpha particle emission.
The measurement of radon levels in homes has become a standard
part of home sales transactions, so more data and awareness of
the problem has risen in the past 10 years. If your home or business
does have a radon problem, an engineer or contractor can simply
and cheaply (typically less than a thousand dollars for an average
home) design and build a ventilation system that can remove the
harmful radon gas, making the air safe to breathe.
impermeable soils and bedrock are unlikely to concentrate
radon beyond their natural background levels.
See also RADIOACTIVE DECAY.
rain See PRECIPITATION.














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