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RADON MONITORING AT THE JOINT RESEARCH CENTRE ISPRA
S. Verdelocco, D. Walker, P. Turkowsky, and C. Osimani
Joint Research Centre Ispra, Radiation Protection Unit, Via E.
Fermi, 21020 Ispra (Va), Italy
Tel: 00390332786299 Fax: 00390332785184 email: david.walker@jrc.org
The object of this study is to measure radon concentrations, both in the
soil and buildings of the JRC
Ispra, in order to compile a radon map indicating areas with low, medium
and high concentrations.
The monitoring is being performed following the recommendations for the
implementation of Title
VII of the European Basic Safety Standards Directive (BSS) concerning
significant increase in
exposure due to natural radiation sources. For measuring radon both passive
and active methods are
being used. The passive method is a passive track detector in Karlsruhe
beakers. The active instrument
used for indoor measurements is a portable radon monitor Alphaguard
PQ2000. The study is
divided into two parts: soil air measurements and indoor measurements.
For soil air measurements a
geological study of the area was performed in order to identify measurement
sites and understand the
relationship between radon emission and soil type. A thick layer of alluvial
and glacial deposits covers
the JRC area with more than 100 meters thickness in some sites. 38 measurement
sites were chosen to
cover the whole area. The measurements commenced in August 1998 and will
be completed after one
year to take into account seasonal variations, which are critical especially
for outdoor measurements.
The mean concentration measured so far for every site is less than 10000
Bq/m³. For indoor
measurements monitoring in many buildings is being performed both with
active and with passive
methods. The mean concentration measured, with the active monitor, for
all buildings is less than 50
Bq/m³ in both old and new constructions.
The results so far obtained indicate that the JRC territory is not a radon
prone area. The thickness,
composition and low permeability of superficial deposits may be the reason
for low radon
concentrations in this area.
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