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Behavior of Atmospheric ²¹⁰Pb Concentrations and Their Correlations with Meteorological Parameters in Abidjan

Gbalé G. K. Jean-Christophe*, Adon A. Marcellin, Koua A. Antonin

Laboratory of Material Sciences, Environment, and Solar Energy, University Félix Houphouet-Boigny, Abidjan, Côte d’Ivoire

Abstract: Monitoring of radionuclides in aerosols is essential for understanding the factors influencing temporal variations in atmospheric deposition of elements such as ²¹⁰Pb, which is frequently used as a tracer in atmospheric studies. However, long-term monitoring remains limited. Very few studies on air radioactivity are available in Africa and particularly in Côte d'Ivoire. In this study, we measured the radioactivity of ²¹⁰Pb in surface aerosols collected on a weekly basis in the city of Abidjan in south−eastern Côte d'Ivoire from March 2022 to February 2023, using HPGe gamma spectrometry. The mean activity of ²¹⁰Pb was 0.78 ± 0.2 mBq/m³. This activity concentration showed strong seasonal variations, with maximum concentrations recorded during the dry seasons and minimum in the rainy seasons. Statistically significant correlations were observed between ²¹⁰Pb concentration and temperature (r = 0.47; p-value = 0.02), as well as a negative correlation with precipitation (r= -0.48; p-value = 0.02). A statistical test comparing the data obtained in the present work with some bibliographic values of ²¹⁰Pb in aerosols showed that our level of activity concentration is statistically identical to the other previous studies carried out in the world. The active dependence of ²¹⁰Pb with temperature and precipitation was investigated through simple linear regression analysis. Model evaluation and comparison functions were also used. Overall, this study provides an understanding of the behavior, correlations and variability of observed ²¹⁰Pb concentrations influenced by atmospheric conditions in our study area.

Keywords: ²¹⁰Pb, Aerosol, Coastal city, Environmental radioactivity

Received March 08, 2024; Revised April 09, 2024; Accepted April 16, 2024

Citation: Gbalé G. K. Jean-Christophe, Adon A. Marcellin, Koua A. Antonin, Behavior of Atmospheric ²¹⁰Pb Concentrations and Their Correlations with Meteorological Parameters in Abidjan. International Journal of Physics, 12 (2). 77-82. January 2024. doi:10.12691/ijp-12-2-3

1. Introduction

It is generally accepted that our environment, including the atmosphere, is slightly radioactive. The atmosphere is also a very efficient medium for the transfer of natural and man-made radionuclides, including some harmful substances in air, from one place to another. ²¹⁰Pb is a naturally occurring radionuclide produced by the decay of ²²²Rn, which in turn is derived from the ²³⁸U decay chain. Together with other descendants of ²²²Rn (T1/2 = 3.82 d), this radionuclide has a significant impact on the effective dose of ionizing radiation received by humans by inhalation and ingestion [1]. However, it is important to note that the presence of ²¹⁰Pb in atmospheric air is often associated with other factors, such as emissions from factories or human activities, in addition to natural sources. The concentration of ²¹⁰Pb in air can vary depending on these factors, but it is generally present at relatively low levels and can be used as an indicator for scientific research and air quality monitoring. The global inventory of measured ²¹⁰Pb deposition flux is estimated to be about 3.77 × 10¹⁶ Bq/y, i.e., 3.8 × 10²⁵ atoms/y, which agrees well with the global emission flux inventory of 4.65×10²⁵ atoms/y (deduced from the activity flux: 9.79 × 10¹⁹ Bq/y) for ²²²Rn [2,3]. The atmospheric residence time of ²¹⁰Pb in the atmosphere is usually estimated using the activity ratios of its progeny ²¹⁰Bi and ²¹⁰Po [3,4]. Once ²¹⁰Pb is formed, it rapidly associates primarily with submicron aerosol particles that contribute significantly to the formation and growth of aerosols in accumulation mode, characterized by a diameter ranging from 0.07 to 2 µm, which represent an important reservoir of air pollutants. Then the fate of ²¹⁰Pb is thus closely linked to that of carrier aerosols [5]. Studies by [5,6,7] revealed that long-lived ²¹⁰Pb is almost entirely absorbed by aerosol particles in accumulation mode, with an average activity median aerodynamic diameter (AMAD) particle size of 0.55 µm. These aerosols containing radionuclides are then removed from the atmosphere by dry and wet deposition processes, the latter being the predominant mechanism for the removal of these radionuclides from the atmosphere. Long-term measurements of these radionuclides provide valuable information on atmospheric processes, with ²¹⁰Pb serving as a tracer for different aerosol species [8]. With its full energy gamma peak of 46.5 keV, ²¹⁰Pb is easily detectable by non-destructive gamma spectrometry when collected in the air on an aerosol filter. Given the large regional and temporal variations of ²¹⁰Pb, it is important to assess these variations in different geographical contexts. This will also be very useful for specific tracer applications in regional studies, such as atmospheric mixing and transport. In Africa and especially in its tropical zone, there is insufficient data on measurements of ²¹⁰Pb in air at ground level. The present study was undertaken with PM2.5 airborne as ²¹⁰Pb is associated with fine particles. Moreover, Huang et al. found that PM2.5 can explain more than 50% of the variation in ²¹⁰Pb in aerosols [9]. The main objective of this study is providing more in-depth information on the factors responsible for temporal variations in concentrations.

More specifically, this study aims to:

- investigate the temporal variations of ²¹⁰Pb in the study site environment;

- investigate the correlation of ²¹⁰Pb concentrations with local climatic conditions;

create a model that takes into account the meteorological conditions in order to predict the behavior of ²¹⁰Pb concentrations.

2. Material and Methods

2.1. Study Area

Samples of aerosol particles in air were taken at a height of 15 m above the ground to minimize the number of dust particles entering the sampler. The sampling station was located at the Faculty of Sciences and Technology of the University Félix Houphouët−Boigny (located at longitude “3°58' 57''” West−“5°21'23''” North) (Figure 1) in the commune of Cocody in the city of Abidjan. Abidjan is the economic capital of Côte d’Ivoire and is located in the south-east at the edge of the Gulf of Guinea at an altitude of 18 m above sea level. Côte d'Ivoire is the transition zone between the humid equatorial climate and the dry tropical climate, which allows the country to be divided into two main zones: the south and the north. The difference between these two zones lies in the humidity level, which can sometimes be around 100 % in the south and as low as 20 % in the north during harmattan weather (cool, dry wind from the Sahara). In the south, below Yamoussoukro, the political capital of Côte d’Ivoire, the climate is equatorial and therefore very humid. This climate zone is characterized by high rainfall and temperatures around 30°C. The north is dominated by the tropical climate of the savannahs with average temperatures ranging from 28° to 37° Celsius. This climatic region also experiences a great rainy season and a great dry season [10].

In the south, there are four seasons:

- the long rainy season: from April to mid-July, with frequent rainfall and numerous storms;

- the short dry season: from mid-July to September, when the sky remains open;

- the short rainy season: from September to November, with some light rainfall;

- the long dry season: from December to March, marked by the northern trade winds (harmattan).

Meteorological data, including rainfall, air temperature, wind speed, and direction, were obtained on site by a wireless VANTAGE PRO 2 weather station.

2.2. Air Sampling and Determination of ²¹⁰Pb Activity Concentrations

Aerosol samples (particle size ≤ 2.5 μm) were collected by drawing atmospheric air through a glass microfiber filter (GF 10 047) with a diameter of 47 mm using a Sven Leckel low volume air sampler with a flow rate of 3 m³/h for 168 hours. The sampling program was conducted over one year (2022−2023), with two samples per month. A total of 24 samples were taken from the measurement site with a total volume of air sampled of 504 m³ per sample. Aerosol samples were measured with a Canberra GX3018 hyper-pure (50% relative efficiency p-type) germanium detector placed in a 7.5 cm lead-thick enclosure and covered inside with thick copper plates, 10 mm on the side walls and 1 mm on the upper and lower walls. The counting electronics is a Canberra Lynx. The obtained data were analyzed by the Genie 2000 software. The FWHM of the detector was 2.00 keV at 1.33 MeV line of ⁶⁰Co. The active acquisition time of the gamma spectra of the aerosol samples was 86,400 seconds per sample. The concentration activity of ²¹⁰Pb was calculated by spectrum deconvolution of the 46.5 keV peak. A priori measurement of blank filters for aerosol sampling showed the absence of ²¹⁰Pb activity in the filters. The efficiency calibration was carried out with two Bernard Damas standard filters ref C569 of 51 mm diameter, charged, one by a multi-gamma source consisting of 11 radionuclides covering an energy range from 59.6 keV (²⁴¹Am) to 1836 keV (⁸⁸Y) and the other in ¹²⁹I for the energy ray 29.7 keV. A yield transfer to a 47 mm filter was carried out using the Monte Carlo GESPECOR calculation code [11]. The activity concentration of ²¹⁰Pb is determined by the following relationship [3]:

Where N: total counts under the photopeak of ²¹⁰Pb;

t: counting time;

V: volume of air passed through the filter paper (m³);

ɛ: photopeak efficiency for the detector;

BR: branching ratio of the radionuclide of interest (4% for ²¹⁰Pb).

The above formula assumes that the decay during counting is negligible, taking into account that the half-life of ²¹⁰Pb is very large compared to the counting and sampling times. The detection limit for all filters varies from 0.11 to 0.2 Bq. In this study, the statistical analysis of the data, the description of the ²¹⁰Pb activity concentrations, the tests of the linear correlation coefficients and the linear regression models were carried out using the R computational environment and its graphical user interface RStudio [12]. Meteorological data (precipitations, daily temperatures, and relative humidity) to identify possible correlations were collected using the VANTAGE PRO 2 weather station at the sampling site.

Figure 1. Sampling location in Abidjan (Cote d’Ivoire)

3. Results and Discussion

3.1. Meteorological Conditions During the Sampling Period

Average weekly temperatures ranged from 24.61°C to 29.17°C from March 2022 to February 2023. The lowest temperature was recorded in September 2022, while the highest was observed in February 2023, reaching 29.17°C. As far as precipitation is concerned, we recorded a variation ranging from 0 mm to 273 mm in June 2022, this month being characterized as the wettest of the whole year.

3.2. Temporal Variations ²¹⁰Pb Activity

Figure 2. Monthly variation of ²¹⁰Pb activity (mBq/m³) in aerosol

Activity concentrations of ²¹⁰Pb in aerosol filters ranged from 0.24 to 1.5 mBq/m³, with an average of 0.78 ± 0.20 mBq/m³. The lowest concentration was observed in October 2022, while the highest concentrations were recorded from December 2022 to January 2023 (Figure 2). This variability resulted in minimum levels of concentration during high precipitation seasons. The highest values were recorded from December to February and mid-July to September, corresponding to the dry periods of the year.

3.3. The ²¹⁰Pb Activity Concentration Levels in Abidjan

Our mean value (Table 1) fits harmoniously within the range of values recorded by [13], who collected data on activity concentrations of ²¹⁰Pb in ambient air worldwide, observing levels ranging from 0 to 1 mBq/m³. It should be noted that the highest concentrations of ²¹⁰Pb were recorded in subtropical and temperate latitudes of the Northern Hemisphere, a finding supported by sources such as [9,14].

Table 1. Variation in ²¹⁰Pb Activity concentration (mBq/m³) in the surface air around the word

3.4. Study of Distribution of ²¹⁰Pb Activity Concentration

The overall results of the activity concentration of ²¹⁰Pb measured at our site were the subject of an in-depth statistical analysis. The Shapiro−Wilk normality test was used to assess the concentrations obtained from our 24 samples. This test reveals that our data set follows a normal distribution with p = 0.14 > 0.05. This is corroborated by the Kolmogorov−Smirnov test with p = 0.8 > 0.05. These results, which are of high statistical significance, with a 95% confidence interval, confirm the relevance of the mean of 0.78 ± 0.2 mBq/m³ for our dataset. (Table 2) illustrates the statistics of distribution concentrations.

Table 2. statistics of ²¹⁰Pb activity concentrations

We compared our theoretical mean value with averages obtained in other regions of the world (Table 1) using a student test with welch correction. This test with p = 0.30 > 0.05, shows that the activity concentration level of ²¹⁰Pb at our study site is statistically similar to the averages of previous studies conducted worldwide. The confidence interval for the obtained mean value m is defined as follows: [8] with t0.95 = 1 and a standard deviation of 0.20 mBq/m³. Overall, we can statistically state that the activity level in ²¹⁰Pb concentration is between 0.58 and 0.98 mBq/m³. This result is consistent with the range of concentrations obtained in several previous studies.

3.5. Seasonal Variation of ²¹⁰Pb Activity

At the sampling site, ²¹⁰Pb activity concentrations demonstrated seasonal variation, this result is similar to the finding of many previous studies in other coastal regions [3,9,15]. Changes in ²¹⁰Pb activity depend on the rate of local radon emanation, and meteorological parameters, particularly temperature, precipitation, and moisture content of air and soil [16,17]. Our measurement site is located in the intertropical zone of confluence between two air masses, the monsoon (humid) and the boreal hemisphere (dry) [18]. ²¹⁰Pb concentrations are highest during the months of the great dry season (December-March) corresponding to the northern hemisphere winter and lower during the rainy season (April-July) in summer of northern hemisphere climates. These general trends have also been observed by [1,3,5,15,19,20]. During rainy periods, unstable southwesterly (monsoon) oceanic air masses cause vertical developing cloud formations that result in heavy precipitation [18]. The purifying effect of this precipitation on ambient air is responsible for the substantial decrease in aerosol concentrations and thus those of ²¹⁰Pb [3,21]. Studies by [22,23,24] on radioactivity in ambient air noted the same finding. The influence of precipitation on the sweep and removal of ²¹⁰Pb atoms from the air during dry and rainy seasons was studied by one-factor analysis of variance (ANOVA). The result of this statistical test, illustrated in (Figure 3), shows that the average value, 0.98 mBq/m³, of the dry season is statistically different from 0.48 mBq/m³ of the rainy season p-value = 3.20 ×10⁻⁵ < 0.05.

Figure 3. ²¹⁰Pb boxplot activity for dry and rainy season

The leaching of ²¹⁰Pb aerosols by rainwater is supported by the results of numerous studies that have found significant correlations between ²¹⁰Pb deposition fluxes in rainwater and precipitation amounts in Geneva [25] or Taiwan [26]. Dry periods of the year, characterized by the arrival of continental air masses such as the boreal hemisphere trade winds (harmattan) from the northeast, are responsible for a significant increase in ²¹⁰Pb concentrations in the atmosphere [18]. During these periods, tropospheric aerosol particles, carrying ²¹⁰Pb nuclei, from arid areas accumulate in the atmospheric layer. This seasonal behavior of ²¹⁰Pb could be explained by its origin, namely ²²²Rn, which has higher concentrations during dry periods than during the rainy season [27]. In addition, temperature inversion conditions in ambient air may impede vertical mixing of ²²²Rn, contributing to increased concentrations of ²¹⁰Pb atoms at the soil surface [15]. Low rainfall [2] and air mixing characteristics in the upper layers of the atmosphere promote prolonged residence time of aerosols in the atmosphere, resulting in continuous accumulation of ²¹⁰Pb [28]. Figure 4 illustrate the variations in ²¹⁰Pb concentrations as function of rainfall during the sampling period.

Figure 4. Evolution of ²¹⁰Pb as a function of rainfall

The process of leaching atmospheric aerosols by precipitation results in a decrease in the activity concentrations of ²¹⁰Pb in surface air. A negative correlation between these two parameters can therefore be expected as shown by the Pearson rank correlation coefficient (Table 3). Correlations between ²¹⁰Pb concentrations and precipitation, temperature and humidity were studied. We obtained the correlation coefficients for these parameters as -0.48, 0.47 and -0.06. Although some authors have observed opposite correlations for temperature and humidity [20], the main factor influencing the decrease remains abundant precipitation, which is negatively correlated with ²¹⁰Pb concentrations [3,5,9,20]. The (Figure 5) highlights a correlation between ²¹⁰Pb concentrations, rainfall, and temperature. More specifically, periods of rainfall between 0 and 50 mm coincide with elevated temperature, indicating simultaneous positive and negative correlation.

3.6. Simple Linears Models

The linear relationship between ²¹⁰Pb and temperature, as predicted by Model 2, was confirmed by the p-value test (p = 1.9 ×10⁻¹⁰ < 0.05), demonstrating the great significance of this relationship. In addition, the percentage variance (r² = 0.83) indicates that 83% of the temporal variability of ²¹⁰Pb is explained by ambient temperature. For the use of precipitation as an explanatory variable for ²¹⁰Pb, the coefficients of Model 1 were found to be largely significant, and this was chosen for statistical reasons (r² = 0.20; p = 4.2 ×10⁻¹⁰ < 0.05) (Table 3). However, the low variance of Model 1 suggests that it would be wise to introduce other explanatory variables (multiple linear regression) into the model to improve its predictive capacity. This paves the way for further modelling of ²¹⁰Pb using nonlinear models with precipitation. The evaluation of the models ends with a residue analysis, which checks whether the fundamental assumptions of the linear model are violated. The Jarque and Bera non-normality test applied to the residuals of models 1 (p = 0.74 > 0.05) and model 2 (p = 0.59 > 0.05) generated p values (p > 0.05), meaning that there is no reason to conclude that the residues do not follow a normal distribution.

Finally, the homoscedasticity test Breusch-Pagan test generated a p-value (p = 0.16 > 0.05; Model 1) and (p = 0.25 > 0.05; Model 2). Therefore, we can conclude that the residuals have minimal variance, which confirms the statistical validity of the different models.

Table 3. Summary of the most significant linear models for ²¹⁰Pb predictions

4. Conclusion

Sampling was conducted twice a month over a one-year period. During this period, the concentration of ²¹⁰Pb ranged from 0.24 to 1.51 mBq/m³, with an annual average of 0.78 mBq/m³. Student's statistical test applied to the data estimated the activity level in ²¹⁰Pb concentration, between 0.56 and 0.98 mBq/m³. These values are consistent with those reported in the scientific literature for this radionuclide. The ²¹⁰Pb activity concentration showed a strong seasonal variation. Indeed, the highest concentrations were observed during the dry seasons of the year. Conversely, rainy seasons have reduced concentrations of aerosols containing the radionuclide ²¹⁰Pb in ambient air. Precipitation, by removing this radionuclide from the atmosphere, plays an essential role in the temporal variation of ²¹⁰Pb, which exhibit a negative correlation with precipitation intensity and a positive correlation with temperature. Therefore, these two parameters play a role in the seasonal variation of ²¹⁰Pb. Several linear prediction models have been developed to try to explain this temporal variation. However, this variability cannot be fully explained by a simple linear equation, which instead requires the use of multiple linear regressions taking into account other meteorological parameters, or even the exploration of nonlinear models.

ACKNOWLEDGEMENT

The authors would like to thank the Institute for Radiation Protection and Nuclear Safety (IRSN), in particular Mr. Kévin Galliez, Head of the PSE-ENV/SAME (Nuclear Measurements Laboratory) laboratory, and Mrs. Monferran Coralie, engineer of the Laboratory of Expertise, Radiochemistry and Analytical Chemistry PSE-ENV/SAME/LERCA of IRSN, for agreeing to analyze the aerosol filters by Gamma Spectrometry.

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