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Automated radon monitoring system for continuous environmental sampling
Domenica Paoletti, Giuseppe Schirripa Spagnolo
To cite this version:
Domenica Paoletti, Giuseppe Schirripa Spagnolo. Automated radon monitoring system for continuous
environmental sampling. Revue de Physique Appliquée, Société française de physique / EDP, 1990,
25 (12), pp.1259-1263. �10.1051/rphysap:0199000250120125900�. �jpa-00246295�
Dipartimento
diEnergetica,
Universitàdegli
Studi diL’Aquila,
Località Monteluco di Roio - RoioPoggio - L’Aquila, Italy
(Received
30April
1990, revised 9August
1990,accepted
7September 1990)
Résumé. 2014 On a
développé
unappareil
pour la mesure en continu de la concentration du radon dans l’air. Le fonctionnement se base sur la captureélectrostatique
desproduits
de222Rn (ou 220Rn)
et sur l’observation de ladésintégration
03B1 du218Po
et214Po (ou 212Bi
et212Po
pour220Rn). L’appareil
se montreparticulièrement indiqué
pour la mesure courante dans des environnements fermés tels que résidences et immeubles.
Abstract. 2014 An automatic instrument for the continuous measurement of radon concentration in air has been
developed.
The system operatesby electrostatically collecting
thedaughter products
of222Rn (or
220Rn)
andobserving
the 03B1decay
events from218Po
and214Po (or 212Bi
and212Po
for220Rn).
The detector isparticularly
well suited for routine measurements in enclosed environments such as residences and otherbuildings.
Introduction.
For a
long
time radon emanation in the earth and in theatmosphere
has been thesubject
of numerousstudies, but, only recently,
the presence of radon in air is considered withincreasing attention ;
in factowing
to the restrictedexchange
of air in closed environments the gas may achieve levelsdangerous
for human health.
222Rn,
an inert gas, ispart
of the238U decay
series.Its immediate
parent, 226Ra,
is anubiquitous
con-stituent of crustal or subcrustal
materials,
and is found in soils and inbuilding
materialshaving
rock-and soil-based
components.
When thealpha-decay
of
226Ra produces 222Rn,
thenewly
formed nucleusassumes the
properties
of a gas. Radon gas,escaping
from the
ground
andbuilding materials,
may enter the housesthrough cracks, drains,
basements.220Rn (thoron)
may also bepresent
in indoor airbut,
in
general,
its concentration is limitedby
relativeshort
(55 s)
half-life[1, 2].
These radon
(or thoron) decay products
arechemically
active and can attach tosurfaces,
such asroom
walls,
airborneparticles,
or uponinhalation, lung
tissue. This latter process isprimarily
respon-sible for the health effects associated with radon.
The need to measure radon at low levels for
extended
periods
with lowmaintenance, requires
the
development
of aspecial
detector.In this work we
present
an automated instrument formeasuring daily
fluctuations of222Rn (or 22oRn)
concentration inside closed environments. Some
experimental
tests in different sites have been ef- fected.The measurement process.
Short-lived radioactive
daughter products
of222Rn
and
22oRn,
obtainedby
adecay
of theirrespective parents,
behave as smallpositive
ions(by
thestripping
of orbital electrons due toa-particles
emission
and/or
to atomic recoilmechanisms).
Also22 2Rn
and22oRn
progeny obtainedby /3
emission ispreferentially
formed in apositively charged
state.However, 222Rn (and 22oRn)
progeny may be alsofound in a
negatively charged
orelectrically
neutralstate, but this progeny constitutes a
relatively
smallfraction of the total
[3-7].
The fact that
222Rn
and22oRn
progeny isinitially
formed in an
electrically charged
statesuggests
thepossibility
ofusing
electrostatic collection of thecharged decay products
for a measurement tech-nique.
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/rphysap:0199000250120125900
1260
Fig.
1. - Basic architecture of thesampler.
The
figure
1 shows the basic architecture of the instrument.The
sampler
of radon consists of ahemisphere
(~ 4 dm3)
covered with 2.5 cm of open-porepolyurethane
foam.The
hemisphere
is connected to - 3 500[V]
withrespect
to acommercially
available silicon diffusedjunction
detector(EG
& G ORTEC Model N R-024-450-100)
located at the centre of thehemisphere.
Radon,
but not itsdaughters,
diffusesthrough
theporous foam filter and enters a sensitive volume.
The
degree
ofpassive diffusion
is determinedby
thedifferential radon concentration
gradient
inside andoutside the detector.
The diffusion coefficient of radon in our open pore foam is 0.032
[cm2/s] [1, 7] ;
about 30 minutesare
required
forestablishing (90 %) by passive
diffusion
equilibrium
inside the sensitive volume.For each
222Rn
atom thatdecays
within the sensitive volume is formed a218Po (RaA) (-
88 % ofthe time the RaA is formed as a
positive ion) [7].
The electrostatic field
applied
within the sensitive volume collects the218Po (positive ions)
on thesurface of the detector. The RaA attached on the surface of the detector
decays
in214Pb (RaB) by
a
(6.0 Mev)
emission.Subsequently
RaBdecays
in214Bi (RaC),
and214Po (RaC’ ).
The214Po decays
in214Pb (RaD) by a (7.69 Mev) emission,
as shown in the scheme offigure
2a.Thus,
for each222Rn
atom thatdecays
within thesensitive
volume,
two aparticles
arepotentially
observed.
When a radiation reacts in the
detector, negative pulses
aregenerated.
Thesepulses
areamplified by
the
preamplifier
located at the bottom of the detec-tor.
The
output pulse
of thepreamplifier
is sent, aftershaping
andfiltering,
to aSingle-Channel Analyzer (SCA).
The SCAproduces
alogic output pulse (TTL) only
when thepreamplifier output pulse
fallswithin the energy window set
by E
and AE control.Thus a
particular spectral
line may be selected and counted.The
figure
3 shows thea-spectrum
observedby
our instrument and visualized with an external multichannel
analyzer.
There is a difference in the ratio of two
peaks.
Thepeak
of the RaA is lower than that one of the RaC’. Since each RaC’ atom isproduced
from aRaA atom, the lower collection
efficiency
of RaAindicates a loss
mechanism,
dueprobably
to arecombination of
218Po positively charged.
The exact mechanisms for
218Po
neutralization are not wellknown ;
different and evencontradictory
results have been obtained under various
conditions ;
however the neutralization of Polonium - 218 ions is a function of thephysical
and chemicalproperties
of the ambient
air,
such as described in literature[3,
4, 7],
while the collectionefficiency
of RaC’ appears to be unaffectedby
normal fluctuations of relativeFig.
2. -a)
Radio-226decay
chain, radondecay chain ; b)
Radio-224decay
chain, thorondecay
chain.humidity.
Thestudy
of loss mechanisms in different environmental conditions will beobject
of a furtherresearch.
RaA in a
negatively charged
or neutral state is notcollected on the surface of the
detector ;
on thecontrary RaB,
RaC andRaC’,
which behave aspositive ions,
are collected.In this way it is
possible
to detect thedecay
ofRaC’ without
detecting
RaA.For this reason it is used the
peak region
of theRaC’ for
selecting
the levels of the SCA.For the
22oRn
measurement we selected thepeak
of the
212Po (ThC’).
The thorondecay
chain isshown in
figure
2b.The instrument may record
simultaneously
the222Rn
and220Rn
concentrationsby utilizing
two SCA(the
levels of two SCA are selectedusing
thepeak
region
of the RaC’ and theThC’).
1262
Fig.
3. -Alpha
spectrum of RaA and RaC’.The
sampler
is constructed around amicroproces-
sor with a structure suitable for
managing controlling
units and for
doing
arithmeticoperations. Through
aproper firmware the processor controls all the oper- ations as well as the
measuring procedures
of thesampler.
A second
microprocessor,
identical to thefirst,
isinstalled to control the data communications in the air
pollution monitoring
networks.The two
microprocessors
are connectedby
a Dual- Port - Random - Access -
Memory.
Thisparticular
device allows us to obtain an
interchange
of datawithout dead time in the measurement
system.
Figure
4 shows thecomplete
radonmonitoring system.
Fig.
4. - Continuous environmentalsampling
with radonmonitor. The
sampler
and associatedcounting
electronicsare shown at a
monitoring
site.Measurements.
The instrument was calibrated
by exposing
thesensitive volume to various known concentrations of
radon, using
thetechnique
described in references[8, 9]
andobserving
theequilibrium
response of the detector. Several exposures to different concen-trations of
222Rn
were made to insure that the detector response is linear with concentration.A calibration and
background
determination weremade after the instrument underwent extensive field
operation (about
sixmonths)
in thegallery
of GranSasso
Laboratory.
The calibration factor remained a constant value of 0.76 counts per minute for a radon concentration of 1
Bq/m3
and the instrumentbackground is
0.04 counts per hour.
The minimum
significant
measurableactivity [10]
in 60 minutes
counting period,
at the 95 % confi-dence
level,
is 0.012Bq/m3.
The response time of the monitor was determined
by observing
the count rate, as radon wasinitially injected
into the test chamber. Asteady
statecondition between the radon concentration in the
atmosphere
and the sensitive volume was achieved within 30 minutes. There is a timelag
between achange
in the ambientradon
concentration and the instrument response which is related to the diffusion time and the time necessary forbuildup
of the short-lived
daughters
on the detector.Measurements of in door radon concentration
were made in a ventilate room and in the
gallery
ofGran Sasso
Laboratory (2
000 metersunderground).
The data set demonstrated a difference in the radon concentration between
University of L’Aquila
Lab-oratory
(Fig. 5a)
andGallery of
the Gran SassoLaboratory (Fig. 5b).
In the naturalgallery,
wherethe
humidity
andtemperature
are constant, the radon emanation shows atypical regular trend,
while in a residential room of average ventilation theFig.
5. -Daily
variations of radon concentration ob- served at two locations.The
system
wasdesigned
without the use of airmovers or pumps. The unit is unobtrusive and
acceptable
into adaily
routine withoutdisrupting
business activities.
We would like to
acknowledge
the S.E.A.(Strumen-
tazione Elettronica Avanzata Via
Tiburtina,
101000156 Roma
Italy)
forsupport
in instrument reali- zation.References
[1]
NERO Jr A. V.,Controlling
Indoor AirPollution,
Sc.Am. 258
(1988)
24-30.[2]
SEXTRO R. G.,Understanding
TheOrigin
Of RadonIndoors-Building
apredictive capability,
Atmos-pheric
Environment 21(1987)
431-438.[3]
WRENN MCDONAL E., SPITZ H. and COHEN N.,Design
of a ContinuousDigital-Output
environ-mental Radon
Monitor,
IEEE Trans. Nucl. Sci.NS-22
(1975)
757-761.[4]
NEGRO V. C. and WATNICK S.,Fungi
2014 A RadonMeasuring
Instrument With FastResponse,
IEEE Trans. Nucl. Sci. NS-75, N° 1
(February 1978).
[5]
JONASSEN N., The effect of electric fields on222Rn daughter products
in indoor air, HealthPhys.
45(1983)
487.[6]
BIGU J., Effect of Electrical Field on220Rn Progeny
Concentration, HealthPhys.
49(September 1985)
512-516.[7]
CHU Kal-Dee and HOPKEPhilip
K., Neutralization kinetics forpolonium-218,
Environ. Sci.Technol. 22
(1988)
711-717.[8]
LUCAS H. F.,Improved
Low-LevelAlpha-Scintil-
lation Counter for Radon, Rev. Scient. Instrum.
28
(1957)
680-683.[9]
MASTINO G. G., An emanationApparatus
WithSimple Operational
Procedure for Measure of Low Levels of226Ra,
HealthPhys.
28(1975)
97-100.
[10]
ALTSHULER B. and PASTERNACK B., Statistical Measures of the Lower Limit of Detection of ARadioactivity
Counter, HealthPhys.
9(1963)
293-298.