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HAL Id: jpa-00246295

https://hal.archives-ouvertes.fr/jpa-00246295

Submitted on 1 Jan 1990

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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�

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Dipartimento

di

Energetica,

Università

degli

Studi di

L’Aquila,

Località Monteluco di Roio - Roio

Poggio - L’Aquila, Italy

(Received

30

April

1990, revised 9

August

1990,

accepted

7

September 1990)

Résumé. 2014 On a

développé

un

appareil

pour la mesure en continu de la concentration du radon dans l’air. Le fonctionnement se base sur la capture

électrostatique

des

produits

de

222Rn (ou 220Rn)

et sur l’observation de la

désintégration

03B1 du

218Po

et

214Po (ou 212Bi

et

212Po

pour

220Rn). L’appareil

se montre

particulièrement 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 operates

by electrostatically collecting

the

daughter products

of

222Rn (or

220Rn)

and

observing

the 03B1

decay

events from

218Po

and

214Po (or 212Bi

and

212Po

for

220Rn).

The detector is

particularly

well suited for routine measurements in enclosed environments such as residences and other

buildings.

Introduction.

For a

long

time radon emanation in the earth and in the

atmosphere

has been the

subject

of numerous

studies, but, only recently,

the presence of radon in air is considered with

increasing attention ;

in fact

owing

to the restricted

exchange

of air in closed environments the gas may achieve levels

dangerous

for human health.

222Rn,

an inert gas, is

part

of the

238U decay

series.

Its immediate

parent, 226Ra,

is an

ubiquitous

con-

stituent of crustal or subcrustal

materials,

and is found in soils and in

building

materials

having

rock-

and soil-based

components.

When the

alpha-decay

of

226Ra produces 222Rn,

the

newly

formed nucleus

assumes the

properties

of a gas. Radon gas,

escaping

from the

ground

and

building materials,

may enter the houses

through cracks, drains,

basements.

220Rn (thoron)

may also be

present

in indoor air

but,

in

general,

its concentration is limited

by

relative

short

(55 s)

half-life

[1, 2].

These radon

(or thoron) decay products

are

chemically

active and can attach to

surfaces,

such as

room

walls,

airborne

particles,

or upon

inhalation, lung

tissue. This latter process is

primarily

respon-

sible for the health effects associated with radon.

The need to measure radon at low levels for

extended

periods

with low

maintenance, requires

the

development

of a

special

detector.

In this work we

present

an automated instrument for

measuring daily

fluctuations of

222Rn (or 22oRn)

concentration inside closed environments. Some

experimental

tests in different sites have been ef- fected.

The measurement process.

Short-lived radioactive

daughter products

of

222Rn

and

22oRn,

obtained

by

a

decay

of their

respective parents,

behave as small

positive

ions

(by

the

stripping

of orbital electrons due to

a-particles

emission

and/or

to atomic recoil

mechanisms).

Also

22 2Rn

and

22oRn

progeny obtained

by /3

emission is

preferentially

formed in a

positively charged

state.

However, 222Rn (and 22oRn)

progeny may be also

found in a

negatively charged

or

electrically

neutral

state, but this progeny constitutes a

relatively

small

fraction of the total

[3-7].

The fact that

222Rn

and

22oRn

progeny is

initially

formed in an

electrically charged

state

suggests

the

possibility

of

using

electrostatic collection of the

charged decay products

for a measurement tech-

nique.

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/rphysap:0199000250120125900

(3)

1260

Fig.

1. - Basic architecture of the

sampler.

The

figure

1 shows the basic architecture of the instrument.

The

sampler

of radon consists of a

hemisphere

(~ 4 dm3)

covered with 2.5 cm of open-pore

polyurethane

foam.

The

hemisphere

is connected to - 3 500

[V]

with

respect

to a

commercially

available silicon diffused

junction

detector

(EG

& G ORTEC Model N R-

024-450-100)

located at the centre of the

hemisphere.

Radon,

but not its

daughters,

diffuses

through

the

porous foam filter and enters a sensitive volume.

The

degree

of

passive diffusion

is determined

by

the

differential radon concentration

gradient

inside and

outside the detector.

The diffusion coefficient of radon in our open pore foam is 0.032

[cm2/s] [1, 7] ;

about 30 minutes

are

required

for

establishing (90 %) by passive

diffusion

equilibrium

inside the sensitive volume.

For each

222Rn

atom that

decays

within the sensitive volume is formed a

218Po (RaA) (-

88 % of

the time the RaA is formed as a

positive ion) [7].

The electrostatic field

applied

within the sensitive volume collects the

218Po (positive ions)

on the

surface of the detector. The RaA attached on the surface of the detector

decays

in

214Pb (RaB) by

a

(6.0 Mev)

emission.

Subsequently

RaB

decays

in

214Bi (RaC),

and

214Po (RaC’ ).

The

214Po decays

in

214Pb (RaD) by a (7.69 Mev) emission,

as shown in the scheme of

figure

2a.

Thus,

for each

222Rn

atom that

decays

within the

sensitive

volume,

two a

particles

are

potentially

observed.

When a radiation reacts in the

detector, negative pulses

are

generated.

These

pulses

are

amplified by

the

preamplifier

located at the bottom of the detec-

tor.

The

output pulse

of the

preamplifier

is sent, after

shaping

and

filtering,

to a

Single-Channel Analyzer (SCA).

The SCA

produces

a

logic output pulse (TTL) only

when the

preamplifier output pulse

falls

within the energy window set

by E

and AE control.

Thus a

particular spectral

line may be selected and counted.

The

figure

3 shows the

a-spectrum

observed

by

our instrument and visualized with an external multichannel

analyzer.

There is a difference in the ratio of two

peaks.

The

peak

of the RaA is lower than that one of the RaC’. Since each RaC’ atom is

produced

from a

RaA atom, the lower collection

efficiency

of RaA

indicates a loss

mechanism,

due

probably

to a

recombination of

218Po positively charged.

The exact mechanisms for

218Po

neutralization are not well

known ;

different and even

contradictory

results have been obtained under various

conditions ;

however the neutralization of Polonium - 218 ions is a function of the

physical

and chemical

properties

of the ambient

air,

such as described in literature

[3,

4, 7],

while the collection

efficiency

of RaC’ appears to be unaffected

by

normal fluctuations of relative

(4)

Fig.

2. -

a)

Radio-226

decay

chain, radon

decay chain ; b)

Radio-224

decay

chain, thoron

decay

chain.

humidity.

The

study

of loss mechanisms in different environmental conditions will be

object

of a further

research.

RaA in a

negatively charged

or neutral state is not

collected on the surface of the

detector ;

on the

contrary RaB,

RaC and

RaC’,

which behave as

positive ions,

are collected.

In this way it is

possible

to detect the

decay

of

RaC’ without

detecting

RaA.

For this reason it is used the

peak region

of the

RaC’ for

selecting

the levels of the SCA.

For the

22oRn

measurement we selected the

peak

of the

212Po (ThC’).

The thoron

decay

chain is

shown in

figure

2b.

The instrument may record

simultaneously

the

222Rn

and

220Rn

concentrations

by utilizing

two SCA

(the

levels of two SCA are selected

using

the

peak

region

of the RaC’ and the

ThC’).

(5)

1262

Fig.

3. -

Alpha

spectrum of RaA and RaC’.

The

sampler

is constructed around a

microproces-

sor with a structure suitable for

managing controlling

units and for

doing

arithmetic

operations. Through

a

proper firmware the processor controls all the oper- ations as well as the

measuring procedures

of the

sampler.

A second

microprocessor,

identical to the

first,

is

installed to control the data communications in the air

pollution monitoring

networks.

The two

microprocessors

are connected

by

a Dual

- Port - Random - Access -

Memory.

This

particular

device allows us to obtain an

interchange

of data

without dead time in the measurement

system.

Figure

4 shows the

complete

radon

monitoring system.

Fig.

4. - Continuous environmental

sampling

with radon

monitor. The

sampler

and associated

counting

electronics

are shown at a

monitoring

site.

Measurements.

The instrument was calibrated

by exposing

the

sensitive volume to various known concentrations of

radon, using

the

technique

described in references

[8, 9]

and

observing

the

equilibrium

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 were

made after the instrument underwent extensive field

operation (about

six

months)

in the

gallery

of Gran

Sasso

Laboratory.

The calibration factor remained a constant value of 0.76 counts per minute for a radon concentration of 1

Bq/m3

and the instrument

background is

0.04 counts per hour.

The minimum

significant

measurable

activity [10]

in 60 minutes

counting period,

at the 95 % confi-

dence

level,

is 0.012

Bq/m3.

The response time of the monitor was determined

by observing

the count rate, as radon was

initially injected

into the test chamber. A

steady

state

condition between the radon concentration in the

atmosphere

and the sensitive volume was achieved within 30 minutes. There is a time

lag

between a

change

in the ambient

radon

concentration and the instrument response which is related to the diffusion time and the time necessary for

buildup

of the short-

lived

daughters

on the detector.

Measurements of in door radon concentration

were made in a ventilate room and in the

gallery

of

Gran Sasso

Laboratory (2

000 meters

underground).

The data set demonstrated a difference in the radon concentration between

University of L’Aquila

Lab-

oratory

(Fig. 5a)

and

Gallery of

the Gran Sasso

Laboratory (Fig. 5b).

In the natural

gallery,

where

the

humidity

and

temperature

are constant, the radon emanation shows a

typical regular trend,

while in a residential room of average ventilation the

Fig.

5. -

Daily

variations of radon concentration ob- served at two locations.

(6)

The

system

was

designed

without the use of air

movers or pumps. The unit is unobtrusive and

acceptable

into a

daily

routine without

disrupting

business activities.

We would like to

acknowledge

the S.E.A.

(Strumen-

tazione Elettronica Avanzata Via

Tiburtina,

1010

00156 Roma

Italy)

for

support

in instrument reali- zation.

References

[1]

NERO Jr A. V.,

Controlling

Indoor Air

Pollution,

Sc.

Am. 258

(1988)

24-30.

[2]

SEXTRO R. G.,

Understanding

The

Origin

Of Radon

Indoors-Building

a

predictive capability,

Atmos-

pheric

Environment 21

(1987)

431-438.

[3]

WRENN MCDONAL E., SPITZ H. and COHEN N.,

Design

of a Continuous

Digital-Output

environ-

mental Radon

Monitor,

IEEE Trans. Nucl. Sci.

NS-22

(1975)

757-761.

[4]

NEGRO V. C. and WATNICK S.,

Fungi

2014 A Radon

Measuring

Instrument With Fast

Response,

IEEE Trans. Nucl. Sci. NS-75, N° 1

(February 1978).

[5]

JONASSEN N., The effect of electric fields on

222Rn daughter products

in indoor air, Health

Phys.

45

(1983)

487.

[6]

BIGU J., Effect of Electrical Field on

220Rn Progeny

Concentration, Health

Phys.

49

(September 1985)

512-516.

[7]

CHU Kal-Dee and HOPKE

Philip

K., Neutralization kinetics for

polonium-218,

Environ. Sci.

Technol. 22

(1988)

711-717.

[8]

LUCAS H. F.,

Improved

Low-Level

Alpha-Scintil-

lation Counter for Radon, Rev. Scient. Instrum.

28

(1957)

680-683.

[9]

MASTINO G. G., An emanation

Apparatus

With

Simple Operational

Procedure for Measure of Low Levels of

226Ra,

Health

Phys.

28

(1975)

97-

100.

[10]

ALTSHULER B. and PASTERNACK B., Statistical Measures of the Lower Limit of Detection of A

Radioactivity

Counter, Health

Phys.

9

(1963)

293-298.

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