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Rapid determination of radon monitor calibration factors

NUCLEAR ELECTRONICS AND INSTRUMENTATION

Rapid determination of radon monitor calibration factors

Li Zhiqiang
Xiao Detao
Zhao Guizhi
Wu Xijun
Shan Jian
Zhou Qingzhi
He Zhengzhong
Nuclear Science and TechniquesVol.27, No.5Article number 116Published in print 20 Oct 2016Available online 29 Aug 2016
62900

The monitors used to measure radon concentration must be calibrated, and the calibration factor of each measurement cycle should be determined. Thus, the determination time of calibration factors of NRL-II radon monitors should be reduced. In this study, a method is proposed to determine the calibration factors of radon monitors rapidly. In the proposed method, the calibration factor is initially determined in the 60-min measurement cycle; the calibration factor is then identified in the other measurement cycle on the basis of the principle that the calibration factor of the same radon monitor in different measurement cycles is inversely proportional to the number of α particles produced by 218Po decay in this cycle. Results demonstrate that the calculated calibration factor of the different measurement cycles is consistent with the experimental calibration factor. Therefore, this method is reliable and can be used to determine the calibration factor of radon monitors rapidly.

Rapid determinationRadon concentrationAlpha particle numberCalibration factor

1. Introduction

Radon is a known carcinogen that can cause lung cancer. To control health risks, the World Health Organization proposed 100–300 Bq/m3 as a reference range of radon in a residential area; beyond this range, an area is recommended for remediation [1]. As such, a continuous and reliable system of measurement should be developed to evaluate radon pollution in the environment [2,3], to use radon as a tracer in various processes [4-8], such as earthquake prediction [9-11], and to conduct resource surveys [12,13]. Radon concentrations in the environment are generally measured by sampling ambient air, passing the sample through a particulate air filter into a controlled chamber, and detecting the alpha particles emitted from short-lived decay products [14]. However, the recommended limit cannot indicate the changes in radon concentrations because the actual concentrations of this radioactive element in the environment vary greatly; thus, the currently applied methods cannot satisfy the requirement of a rapid and reliable measurement [15].

To detect changes in environmental radon concentration rapidly, researchers applied the electrostatic collection of 218Po, which is the first-generation progeny of 222Rn decay. The alpha particles produced from this decay are identified and counted; radon concentration is then calculated [16]. A NRL-II radon monitor developed by the University of South China is based on the principle of 218Po collection by using an electric field in a semiconductor detector [17,18]; the monitor is used to measure the radon concentration in air by using a cylindrical metal chamber to sample radon gas-containing environmental air actively. With this monitor, measurement cycles of 15, 30, and 60 min can be set to measure radon concentrations selectively.

The monitors used to measure the radon concentration must be calibrated; in radioactivity determination, statistical variation is high; as such, radon concentrations should be repeatedly determined to obtain an accurate calibration factor of each measurement cycle [19]. In this study, an NRL-II radon monitor is developed on the basis of the principle that the calibration factor of the same radon monitor in different measurement cycles is inversely proportional to the number of α particles produced by 218Po decay in this cycle to reduce measurement time; using this monitor, we initially determine the calibration factor in a 60-min measurement cycle and then calculate other degrees of radioactivity. Thus, statistical fluctuation can be reduced by extending the measurement time, and the calibration factor of the proposed radon monitor can be rapidly determined.

2. Methods and materials

2.1 Sampling circuit and collection cell

Figure 1 illustrates the collection cell of the NRL-II radon monitor and the detector assembly. The system comprises a cylindrical stainless-steel vessel, a passivated implanted planar silicon (PIPS) detector, an amplifier circuit, a high-voltage divider, and a feedthrough. A positive high voltage is supplied to the p layer of the PIPS detector and an electric field is produced in the vessel. The positively ionizing daughter nuclei are collected on the detector surface. The energy of α decay is then measured.

Fig. 1.
Schematic of the collection cell of the NRL-II radon monitor.
pic

The stainless-steel vessel exhibits the following dimensions: 11 cm in diameter, 10 cm in height, and 950 ml in volume. The inner portion of the vessel is electropolished to achieve a low-background level. The PIPS detector is electrically isolated from the stainless-steel vessel with an acrylic plate and a ceramic feedthrough. The following parameters are also set: detection area, 314 cm2; sensitive thickness, 500 µm, and leakage current, 50 nA.

2.2 Principle of measurement

The NRL-II radon monitor was used to measure the radon concentrations. Air is initially sampled at a rate of 2.0 LPM by using a highly efficient filter paper head into the chamber with a DC-pump-controlled MCU at the working Ts. The 3-kV positive high voltage (HV) is turned on. As 222Rn decays, the positive charges of the first-generation progeny of 218 Po are absorbed on the semiconductor surface under the influence of an electrostatic field. As the progeny continuously decays, the energy of the α particles at the collection time TM is determined using the semiconductor detector, and the radon concentration is calculated on the basis of the relationship between the number of α particles and the radon concentration (calibration factor). The 222Rn concentration is calculated through electrostatic collection, as expressed in the following equation:

C222Rn=KηVRΔNP(T), (1)

where C222Rn is the radon concentration that should be measured in a specific environment, R is the correction factor of temperature and humidity [20], η is the detection efficiency, ΔNP is the number of alpha particles after the first-generation progeny 218Po further decays, K is the calibration factor of a radon monitor, and V is the volume of the chamber that should be measured. Equation (1) shows the detection efficiency.

The number of α particles collected by the detectors after 218Po decays is expressed as follows:

ΔNP(T0)=ηVRΔNP(T0). (2)

Thus, Eq. (1) can be rewritten as follows:

C222Rn=KΔNP(T). (3)

If the decay constants and the intensity of 222Rn radioactivity are λR and AR, respectively, the corresponding decay constants and the intensity of 218Po radioactivity are λP and AP, respectively. At time t, the numbers of nuclei in 222Rn and 218Po atoms are NR(t) and NP(t), respectively. Hence, NP(t)=0 when t=0, and

NR(t)=NR(0)eλRt. (4)

The radioactivity of 222Rn is expressed as follows:

AR(t)=λRNR(t)=λRNR(0)eλRt. (5)

The change in the number of nuclei in 218Po atoms per unit time can be calculated from 222Rn on the basis of the rate λRNR(t). However, 218Po can decay into 214Bi, which is expressed as dNP(t)dt:

dNP(t)dt=λRNR(t)λPNP(t). (6)

Substituting Eq. (6) with Eq. (5), we obtain the following expression:

NP(t)=λRλPλRNR(0)(eλRteλPt). (7)

According to Eq. (7), the activity of 218Po can be expressed as follows:

AP(t)=λPNR(t)=λRλPλPλRNR(0)(eλRteλPt). (8)

We can then obtain Eq. (9) from the number of decayed 218Po atoms from Ts to T on the basis of Eq. (8):

ΔNP(T)=0TMλRλPλPλRNR(0)(eλRteλPt). (9)

To simplify Eq. (9), we derive the following equation:

ΔNP(T)=λRλPλPλRNR(0)[1λR(1eλRTM)1λP(1eλPTM)], (10)

where T is the measurement cycle, which includes TS and TM, TS is the sampling time, and TM is the measurement time. If T = 60 min, the calibration factor of the measurement cycle (TM=3300 s) is K0. According to Eq. (3), Eq. (11) is obtained:

K0=C222RnΔNP(T0), (11)

where Kx is the calibration factor of the other measurement cycles on the basis of Eqs. (1) and (9):

Kx=ΔNP(T0)ΔNP(Tx)K0. (12)

Equation (9) can be substituted into Eq. (12) to obtain Eq. (13):

Kx=1λR(1eλRTM0)1λP(1eλPTM0)1λR(1eλRTMx)1λP(1eλPTMx)K0. (13)

Equation (13) shows that the calibration factor of the same radon monitor is associated with measurement cycle and sampling time, but not with collection and detection efficiency. The calibration factor of the radon monitor measured in any cycle at any sampling time can be calculated. The following equation can be used when the same radon monitor is used to experimentally obtain the calibration factor K0, which is 60 min, to rapidly determine the radon concentration. To calculate the calibration factor in different measurement cycles, we set the following parameters: Ts=300 s, λR=2.1×106 s1, and λP=3.7×103 s1; TM is 600 and 1500 s when T and the measurement cycle are 15 and 30 min, respectively. The calibration factors K15 and K30 are expressed as follows:

K15=8.42K0, (14) K30=2.46K0. (15)

Equations (13) and (14) show that a lengthy measurement cycle corresponds to a low calibration factor when the sampling time is fixed.

3. Experimental setup

Our calibration system (Fig. 2) is composed of the standard chamber, manifolds, PQ2000, and three improved NRL-II radon monitors. The calibration factor K is obtained as follows: the three radon monitors and PQ2000 are turned on for 1 h to allow these components to work synchronously. The background count of the radon monitors and air nb is initially determined and the radon-containing air is removed. By this time, ΔNP(T) or the gross count of 218Po α particles radiates in the chamber. The mean value of the radon concentration C222Rn can then be obtained by PQ2000, and the value of the calibration factor K is obtained on the basis of Eq. (11). To maintain a stable C222Rn in the chamber, we use the standard radon chamber with a volume of 25 m3 from the University of South China, and the steam leakage rate of the entire system is <0.10%. The system is also equipped with an air-conditioning unit to regulate temperature and humidity with dynamic stability. The radon concentration of the chamber is set at 2500 Bq m−3 to reduce the influence of errors caused by radioactivity statistics. The stable temperature and humidity are also maintained at 20± 2  °C and 45±5  %, respectively. The detection efficiency η is different when the Ø20-mm detector of the a radon monitor is replaced with Ø30 mm. Moreover, the volume of the collecting cell is changed when the volume of the b radon monitor is adjusted from 950 to 785 ml.

Fig. 2.
NRL-II radon monitor calibration system.
pic

4. Results and discussion

Three measurements are conducted using the three radon monitors with a cycle of 60 min (3600 s). The mean value of the radon concentration of the AlphaGUARD PQ2000Pro (Genitron Instruments GmbH, Germany) is considered the standard concentration of the chamber. Therefore, the average value of the three measurements and the calibration factor of each radon monitor with a cycle of 60 min can be obtained by using Eq. (13). The calibration factor can be obtained from the measurements of the three experiments: K0a=1.62 Bq m3 cpm1, K0b=2.01 Bq m3 cpm1, and K0c=1.57 Bq m3 cpm1. K0a, K0b, and K0c are substituted into Eqs. (14) and (15) to determine the theoretical values of K15 and K30. The measurements are conducted thrice by using the three radon monitors with 15- and 30-min cycles. C222Rn is obtained again, and the mean value of the PQ2000Pro radon concentration is measured as the standard concentration of the chamber. The calibration factor K can be calculated according to Eq. (3). The calculated and measured data are listed in Table 1.

Table 1.
Comparison between theoretical and experimental calibration factors of three NRL-II continuous radon monitors. (*cycles of 60 min of the experimental calibration factor as the standard calibration factor.)
T (min) Number Theoretical Calibration factor (Bq m−3 cpm−1) Experimental calibration factor (Bq m−3 cpm−1) Errors
1 2 3 Average
15 a 13.63 14.35 14.08 13.69 14.04 3.00%
15 b 16.92 17.47 17.85 17.02 17.44 3.07%
15 c 13.22 14.08 13.16 13.79 13.67 3.40%
30 a 3.99 4.01 3.9 4.13 4.01 0.50%
30 b 4.94 5.11 5.08 4.89 5.03 1.82%
30 c 3.86 3.82 3.85 3.97 3.88 0.51%
60* a - 1.64 1.60 1.61 1.62 -
60* b - 1.99 2.15 1.89 2.01 -
60* c - 1.58 1.60 1.53 1.57 -
Show more
* Cycles of 60 min of the experimental calibration factor as the standard calibration factor

Table 1 shows that the experimental calibration factors of the radon monitor are consistent with the theoretical values, and the result is reliable. However, a large difference is observed when the three monitors are used at a measurement cycle of 15 min. Thus, the experimental calibration factors are significantly different from the theoretical calibration factors. Three reasons may contribute to this inaccuracy.

(1) Sufficient time is necessary to turn on high-voltage modules and reach a stable electric field. Using a high-voltage ammeter, we observe that 10 s is required to turn on our high-voltage modules. We then subtract 10 s from TM0 and TMx and substitute the result in Eqs. (14) and (15) to obtain the following:

K15*=8.60K0, (16) K30*=2.47K0. (17)

Thus, we can determine the relationship between the corrected determinations by substituting K0a, K0b, and K0c of each monitor and the experimental calibration factor (Table 2). The corrected and experimental values are consistent with each other (Table 2). However, the b radon monitor exhibits greater inaccuracy than the a and c radon monitors after this correction is performed because the measurement cycle of the b radon monitor is relatively smaller than that of the two other monitors. As a consequence, a larger difference is observed. (2) In time-consuming measurements, the temperature and humidity of the collecting cell cannot be maintained at constant levels. Thus, a slight change can influence the efficiency of 218Po collection and the results. (3) Radioactivity generally fluctuates.

Table 2.
Comparison between the revised theoretical and experimental calibration factors of the three NRL-II continuous radon monitors
T (min) Number Revised theoretical calibration factor(Bq   m−3 cpm−1) Average of experimental calibration factor (Bq m−3 cpm−1) Errors
15 a 13.63 14.04 0.79%
15 b 17.28 17.44 0.92%
15 c 13.50 13.67 1.25%
30 a 4.00 4.01 0.25%
30 b 4.97 5.03 1.20%
3 c 3.88 3.88 0.00%
Show more

Table 2 shows that the revised calibration factors of the different measurement cycles are consistent with the experimental calibration factors. Therefore, the proposed method can be used to determine the calibration factors of radon monitors rapidly and to improve the accuracy of continuous measurements.

5. Conclusions

In this study, a method is proposed to determine the calibration factors of radon monitors rapidly. We initially determine the calibration factor in the 60-min measurement cycle. The calibration factors in the other measurement cycles are then calculated on the basis of the principle that the calibration factor of the same radon monitor in a different measurement cycle is inversely proportional to the number of α particles produced by 218Po decay in the same cycle. The experimental results demonstrate that the calculated calibration factor of the different measurement cycles is consistent with the experimental calibration factor. Therefore, this method can be used to determine the calibration factor of radon monitors rapidly.

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