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34
HOW DID WIND AFFECT THE RADON ENTRY INTO SEVEN DETACHED HOUSES
T. Keskikuru 1 , H. Kokotti 1 , S. Lammi 2 and P. Kalliokoski 1
University of Kuopio 1 , Department of Environmental Sciences 2 , Department
of Computer Science
and Applied Mathematics
P.O.BOX 1627, FIN-70211 KUOPIO, FINLAND
The wind speed and wind direction affected concentration of indoor radon
in seven houses, which are
located in three region of southern Finland. In the case of houses (B
- F) which are built on upper
slope of a permeable esker, according to the analysis of covariance the
highest concentration of indoor
radon, 20 - 33% over grand mean, was observed when wind (v.... 0.4 m.s
-1 ) direction was perpendicular
the esker, leading to increasing pressure of soil gas and consequently
to increased radon entry and
concentration. In the same houses the lowest concentration of indoor radon,
22 - 44% under grand
mean, was observed when the wind was blowing parallel from the top of
the esker. In the slab-on-grade
house (A), these factors have unimportant effect on because the house
is located on a gently
sloping rocky surface. Thus, movement of the wind through the top soil
generally has only a limited
effect on pressure conditions in the soil. In this house, the concentration
of indoor radon was highest,
19% over grand mean, in windy conditions when the wind probably induced
transport of containing
radon air from the non-ventilated room to the ventilated living space.
In the crawl-space house (G),
which was built on flat and clayey field, wind speed was not found to
influence the concentration of
indoor radon although the radon concentration was higher, 12% over grand
mean, in the crawl space
when the wind came from shielded directions. In addition, the lowest concentration
of radon in the
crawl space, 13% under grand mean, was observed when the wind blew from
unshielded directions.
Radon concentration in soil in vicinity of the house probably decreased
during these wind directions.
Wind speed affected only slightly the mean value of concentration of radon
in these seven houses
because radon concentration in the groups of the wind speed did not differ
from each other. This study
showed that the effect of the wind speed on the concentration of indoor
radon was difficult to foresee
because the effect of the wind depended strongly on wind direction.
Key Word Index: radon, wind, indoor, soil-gas transport, esker, slab-on
grade, crawl space, basement.
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