Special Issue on 2019 Asian Aerosol Conference (AAC)

Guoqing Liu This email address is being protected from spambots. You need JavaScript enabled to view it.1, Jiabao Wu1, Yong Li1, Lingling Su2, Minxia Ding3

Department of Nuclear Science and Technology, College of Physics and Opotoelectronic Engineering, Shenzhen University, Shenzhen 518060, China
Center for Advanced Materials Diagnostic Technology, Shenzhen Technology University, Shenzhen 518118, China
Shenzhen Environmental Monitoring Center, Shenzhen 518049, China


Received: November 5, 2019
Revised: February 24, 2020
Accepted: February 27, 2020

 Copyright The Author(s). This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are cited.

Download Citation: ||https://doi.org/10.4209/aaqr.2019.11.0560  

Cite this article:

Liu, G., Wu, J., Li, Y., Su, L. and Ding, M. (2020). Temporal Variations of 7Be and 210Pb Activity Concentrations in the Atmosphere and Aerosol Deposition Velocity in Shenzhen, South China. Aerosol Air Qual. Res. 20: 1607–1617. https://doi.org/10.4209/aaqr.2019.11.0560


  • 7Be and 210Pb in aerosols and deposition fluxes were measured for a whole year.
  • Temporal trends of 7Be and 210Pb in aerosols and deposition fluxes were studied.
  • Factors controlling 7Be and 210Pb in aerosols and deposition fluxes were evaluated.
  • The deposition velocity of aerosols were calculated using 7Be and 210Pb.


Naturally occurring beryllium-7 (7Be) and lead-210 (210Pb) serve as powerful tracers in atmospheric studies. In this study, 7Be and 210Pb were simultaneously measured in atmospheric aerosols and deposition samples for an entire year (from January to December 2017) in Shenzhen, South China. The activity concentrations of the airborne 7Be and 210Pb ranged from 0.33 to 9.42 mBq m–3 (averaging 3.23 mBq m–3) and from 0.59 to 4.72 mBq m–3 (averaging 1.58 mBq m–3), respectively, and were observed to be high during the winter but low during the summer. Moreover, the relatively high 210Pb concentration was probably due to the elevated level of radon in this region’s soil. The deposition fluxes of the 7Be and 210Pb were found to range from 0.25 to 3.04 Bq m–2 day–1 (averaging 1.57 Bq m–2 day–1) and from 0.34 to 1.31 Bq m–2 day–1 (averaging 0.73 Bq m–2 day–1), respectively. The temporal trends of these fluxes were largely influenced by rainfall and the origin and pathway of air masses, as well as by atmospheric circulation. Based on their concentrations in the aerosols and their deposition fluxes, the average deposition velocities of 7Be and 210Pb were calculated to be 0.83 and 0.62 cm s–1, respectively. The deposition velocities of both radionuclides correlated well with the amount of rainfall, indicating that precipitation plays a crucial role in removing 7Be and 210Pb from the air. The activity size distributions of these nuclides combined with the characteristic meteorological conditions in this region resulted in high deposition velocities during summer and low ones during winter.

Keywords: 7Be and 210Pb; Activity concentrations; Deposition fluxes; Deposition velocity of aerosols; Shenzhen.


Airborne particles (aerosols) have become the major air pollutant in Chinese megacities (Liu et al., 2014). As long as these particles are formed or injected into the atmosphere, they tend to get involved in physical and chemical processes in the atmosphere (Ahmed et al., 2004) and ultimately sink into the terrestrial environment through dry and wet deposition. Atmospheric particles are considered the main carriers of airborne pollutants and play a crucial role both in air quality and deposition fluxes of pollutants to the earth’s surface, which pose a negative effect on the ecological system and human health (Chameides et al., 1999; Yadav et al., 2003). To determine the transport pathway of these pollutants and to assess their environmental impact, it is essential to understand the dynamics of these airborne particles. The naturally occurring beryllium-7 (7Be) and lead-210 (210Pb) serve as powerful tracers for atmospheric studies that include (i) air mass exchange between the stratosphere and troposphere, (ii) residence times of atmospheric aerosols, (iii) washout ratios and deposition velocity of aerosols, and (iv) source tracking of oceanic and continental air masses (Baskaran, 2011).

7Be (T1/2 = 53.3 days) is a cosmogenic radionuclide produced by the reaction of cosmic rays with oxygen and nitrogen atoms in the stratosphere and upper troposphere (Alonso-Hernández et al., 2014); the production rate of 7Be on the earth’s surface for a given latitude is independent of longitude (McNeary and Baskaran, 2003). Generally, the airborne concentration of 7Be increases with altitude and is sensitive to meteorological conditions, such as temperature and precipitation (Gai et al., 2015). A high 7Be concentration in ambient air would indicate a large input from the upper atmosphere (Dueñas et al., 2011a). At mid-latitude, the specific concentrations of 7Be exhibit high values in spring, owing to the seasonal contraction of tropopause, which results in the enhancement of air exchange between the stratosphere and troposphere (Ali et al., 2011; Gai et al., 2015). 210Pb (T1/2 = 22.3 years) is a naturally occurring radionuclide, originating from the decay of 222Rn (T1/2 = 3.8 days). Because 222Rn is mainly emanated from the earth’s surface, 210Pb is considered a tracer of continental air masses (Baskaran, 2011). Once produced, 7Be and 210Pb instantaneously and irreversibly attach themselves mainly to fine particulates and are removed from air through radioactive decay, dry and wet deposition (Ali et al., 2011). Because of distinctly different sources, combined measurements of 7Be and 210Pb provide a powerful tool to study the mechanisms of atmospheric processes. Furthermore, knowledge of these nuclides can help us understand the behavior of other similar contaminants in the air (McNeary and Baskaran, 2003).

To date, extensive studies on 7Be and 210Pb in atmospheric deposition as well as in aerosols have been conducted worldwide (Ioannidou et al., 2005; Alonso-Hernández et al., 2014; Du et al., 2015; Gai et al., 2015; Grossi et al., 2016; Chham et al., 2017; Dueñas et al., 2017). However, combined measurements of 7Be and 210Pb in aerosols and in bulk fallout are still limited. Located at the eastern side of the Pearl River Delta (PRD) region in Guangdong Province, South China, Shenzhen is a demonstration/pilot zone for socialism with Chinese characteristics, with an area of 2,021 km2 and a population approaching 20 million (Liu et al., 2015). During the past three decades, Shenzhen has made rapid economic progress and has become one of the most important industrial and economic centers in China. The rapid urbanization and industrial development in Shenzhen and the PRD region have placed considerable pressure on the environment. Many studies have been conducted on air pollution in the PRD region, mostly focused on atmospheric particulate matter, heavy metals, and organic pollutants (Liu et al., 2014). However, few studies have been conducted on the atmospheric radiotracers (e.g., 7Be and 210Pb) in this region; these studies can provide insights into the mechanism of various atmospheric processes. Shenzhen features a subtropical monsoon climate, with oceanic monsoon prevailing in summer and continental monsoon prevailing in winter. The coastal or continental air masses carry the long-range-transported air pollutants to this region, particularly in winter seasons. Shenzhen thus serves as an ideal region for studying air mass transfer in the subtropical monsoon climate region.

The objectives of the current study were as follows: (1) to determine the temporal variations of 7Be and 210Pb in atmospheric aerosols in Shenzhen; (2) to study the seasonal deposition fluxes of 7Be and 210Pb in this region; (3) to investigate factors controlling 7Be and 210Pb in aerosols and deposition fluxes; and (4) to evaluate the deposition velocity of aerosols using 7Be and 210Pb.


Sampling and Preparation

Air sampling was performed in Shenzhen University (Fig. 1), which is located in the Nantou Peninsula of Shenzhen city. The roof of the experimental building at Shenzhen University (22.5°N, 113.9°E) was selected as the sampling site. From January to December 2017, atmospheric deposition (wet + dry) samples were collected at monthly intervals by using a stainless container (0.55-m diameter and 0.6-m height). At the end of each collection, bulk fallout samples were transferred to a pre-cleaned polyethylene vessel, the container was washed with 0.2 M HCl and Milli-Q water to remove 7Be and 210Pb that are possibly adsorbed on the wall, and the combined solution was adjusted to pH 2.0 with 6 M HCl. 7Be and 210Pb were obtained through chemical co-precipitation as described by Du et al. (2008). A known amount of Fe3+ carrier was added to the solution, and after 24 h, the solution was adjusted to pH 8.5 with NH4OH for Fe(OH)3 precipitation. The precipitate was then centrifuged and transferred into a cylindrical polyethylene container (7.5 cm × 7.0 cm) for gamma-ray measurement after drying. 

Fig. 1. Sampling location in Shenzhen, South China.

Concurrently, atmospheric aerosol samples were collected once per week using a high-volume air sampler following the procedure described in our previous work (Liu et al., 2010). The sampling flow rate was 1.05 m3 min–1, and the sampling time for each sample was 24 h; suspended particulates were retained on a Whatman glass microfiber filter (GFF; grade GF/A, 20.3 cm × 25.4 cm). After each sampling, filters were folded and pressed into a cylindrical polyethylene container (7.5 cm × 7.0 cm) so that all samples had the same irradiation geometry.

Analytical Methods

The activity concentrations of 7Be and 210Pb were determined through gamma spectrometry; the methodology was described in Liu et al. (2015). Briefly, the gamma spectrometer was equipped with an HPGe detector (GEM-C5970; ORTEC, USA), with an energy resolution of 1.8 keV at the 1.332 MeV of 60Co and the relative efficiency of 38%. The detector was enclosed in a cylindrical lead shield with 10-cm thickness and 38-cm height. The counting efficiencies of 7Be and 210Pb in filter and deposition samples were calibrated by an aerosol reference material (QRJH1204, containing 152Eu and 137Cs) and a soil reference material (7NTR141201, containing 238U, 235U, 226Ra, 232Th, 40K, 241Am, 137Cs and 60Co), respectively. The efficiency curves were constructed based on the full-energy peak efficiencies of these calibrated radionuclides in a cylindrical geometry (Ø 75 mm × 70 mm). According to the sample-to-detector geometry, the true coincidence summing effect for the efficiency calibration with 152Eu was small and could be neglected. 7Be activity was determined through its 477.6 keV gamma-ray (yield 10.12%), and 210Pb content through its 46.5 keV gamma-ray (yield 4.25%). The counting time was set as 24 h for all the samples. The GammaVision 32 software was used for the data analysis.

The activity concentrations (C) of 7Be and 210Pb were calculated as follows:


where Ns and Nb are the counting rates (in s–1) of the sample and background, respectively; ε is the characteristic peak efficiency; δ is the branching ratio; and V is the sample volume of aerosol (in m3). The total deposition fluxes (F) of 7Be and 210Pb were determined as follows:

where ABe/Pb is the total activity of 7Be and 210Pb (in Bq) deposited in the collector; S is the total surface area of the collector (in m2); and T is the sampling duration (in days). The final activity of 7Be was radioactive decay corrected for the time interval between the sampling and measurement, whereas it was not performed for 210Pb due to its relatively long half-life.


Be and 210Pb activity Concentration in the Air

During the sampling period from January to December 2017, the weekly activity concentration of 7Be was in the range of 0.33–9.42 mBq m–3, with an annual average of 3.23 mBq m–3. These values were comparable with those obtained from near-surface atmospheric aerosols reported in low-latitude regions, such as Guangzhou, China (2.59 mBq m–3; Pan et al., 2011), but lower than those reported from mid-latitude regions such as Beijing, China (8.39 mBq m–3; Tan et al., 2013); Malaga, Spain (4.6 mBq m–3; Dueñas et al., 2011b); Detroit, Michigan (4.8 mBq m–3; McNeary and Baskaran, 2003); and Brindisi, Italy (5.4 mBq m–3; Hernández-Ceballos et al., 2015). The activity concentration of 210Pb was in the range of 0.59–4.72 mBq m–3, with an annual average of 1.58 mBq m–3. These values were similar to those reported in the northern cities of China (Li et al., 2013) but higher than in Kumamoto, Japan (0.89 mBq m–3; Momoshima et al., 2006); Malaga, Spain (0.58 mBq m–3; Dueñas et al., 2011b); and Detroit, Michigan (1.15 mBq m–3; McNeary and Baskaran, 2003). China is the largest coal producer and consumer in the world. During coal combustion, 210Pb can be released as fly ash from a coal-fired power plant (Liu et al., 2015), which in turn increases the 210Pb concentration in ambient air. On the other hand, Shenzhen city is a high-radiation background region in China; the soil gas radon concentration was nearly seven times the country’s average (Wang et al., 2006; Liu et al., 2015), which may have contributed to a high 210Pb concentration in this region.

Fig. 2 shows the monthly 7Be and 210Pb activity concentrations and precipitation in the study period. As shown in the figure, the activity concentrations of both 7Be and 210Pb showed seasonal variation; they were high in winter and low in summer, similar to those reported in Kumamoto, Japan (Momoshima et al., 2006), and Qingdao, China (Yang et al., 2013). Shenzhen is located in subtropical monsoon regions, which is wet and hot in summer and dry and cool in winter. During the rainy season, precipitation scavenging causes the aerosol concentration to decrease, thus reducing the attachment medium for 7Be and 210Pb in the air (Yang et al., 2013). On the other hand, maritime air masses that come from the Pacific Ocean usually contain less 7Be and 210Pb, which may also be responsible for the low 7Be and 210Pb in summer. During the dry winter season, the northeast monsoon that originates from Mongolia and southeastern Siberia carries continental air masses to South China; the long-range-transported 210Pb from North China may have led to the increased 210Pb concentration in winter. The production rate of 7Be is latitude dependent, and high 7Be concentrations in aerosols have been reported in northern China (Yang et al., 2013; Gai et al., 2015). The air masses coming from these mid-latitude regions (enriched in 7Be) may have contributed to the high level of 7Be in winter when northeast monsoon prevailing. Many studies have indicated that at mid-latitude regions, an enhanced air exchange occurs between the stratosphere and troposphere in spring (Pan et al., 2011); stratospheric air intrusion may have brought large amounts of 7Be in March in this region. 

Fig. 2. Seasonal variations of 7Be and 210Pb concentrations in the air and precipitation.Fig. 2. Seasonal variations of 7Be and 210Pb concentrations in the air and precipitation.

Deposition Fluxes of 7Be and 210Pb

The monthly bulk deposition fluxes of 7Be and 210Pb along with the precipitation amount are shown in Fig. 3. The deposition fluxes of 7Be and 210Pb were in the range of 0.25–3.04 Bq m–2 day–1 and 0.34–1.31 Bq m–2 day–1, with an annual average of 1.57 and 0.73 Bq m–2 day–1, respectively. The deposition fluxes of 7Be and 210Pb showed seasonal variations; high deposition fluxes were observed in spring (March) for 7Be and autumn (August and September) for both 7Be and 210Pb. The study of Mcneary and Baskaran (2003) indicated that the deposition fluxes of 7Be and 210Pb on the earth’s surface are largely influenced by latitude (for 7Be), longitude (for 210Pb), and local meteorological conditions. By comparison, the deposition fluxes of 7Be in Shenzhen fall in the range of those reported in other regions of China (Yi et al., 2007; Du et al., 2008; Zhang et al., 2013; Gai et al., 2015); Cienfuegos in Cuba (Alonso-Hernández et al., 2014); Geneva, Switzerland (Caillet et al., 2001); Spain (Dueñas et al., 2017); and Detroit, USA (McNeary and Baskaran, 2003). Table 1 summarizes the deposition fluxes of 7Be and 210Pb in 18 stations around the world in the order of latitude. As seen from Table 1, the deposition fluxes of 7Be showed an increasing trend with latitude (from 22.2°N to 46.2°N) and were the highest in the mid-latitude regions, reflecting the well-known latitudinal dependence of atmospheric deposition fluxes of 7Be, as have been observed in some regions (Du et al., 2015; Gai et al., 2015; Hernandez-Ceballos et al., 2015). However, further studies of bulk deposition of 7Be are still needed, especially in the southern hemisphere regions. For 210Pb, its deposition fluxes at our site were comparable to the global average value (0.53 Bq m–2 day–1) for latitude between 20°N and 30°N (Baskaran, 2011) but lower than those reported in Shanghai, China (1.31 Bq m–2 day–1; Du et al., 2008), and higher than Cienfuegos, Cuba, where a value of 0.13 Bq m–2 day–1 was reported (Alonso-Hernández et al., 2014), owing to the significant input of marine air in this place. 

Fig. 3. Monthly deposition fluxes of 7Be and 210Pb, and precipitation.Fig. 3. Monthly deposition fluxes of 7Be and 210Pb, and precipitation. 

Studies have indicated that the atmospheric deposition fluxes of 7Be and 210Pb are strongly correlated with the rainfall amount (Dueñas et al., 2005; Gai et al., 2015; Dueñas et al., 2017). To study the effect of precipitation on the removal of both nuclides in the air, the deposition fluxes of 7Be and 210Pb were plotted against the monthly rainfall amount during the sampling period. As shown in Fig. 4, a positive correlation exists between 7Be and 210Pb deposition fluxes and precipitation (r = 0.58 and r = 0.47, respectively). Furthermore, if we narrow the time scale from August to December instead of the entire year, the coefficients between rainfall and fluxes were 0.98 for 7Be and 0.95 for 210Pb. It is suggested that the removal processes of these two radionuclides from the air are similar, and rainfall is the dominant factor for the scavenging of 7Be and 210Pb in autumn and early winter. In general, the correlation coefficients between precipitation and deposition fluxes of 7Be were higher than that of 210Pb. Moreover, similar results have been observed by other authors at various stations, such as Xiamen (Yi et al., 2007) and Shanghai (Du et al., 2008) in China; Malaga, Spain (Dueñas et al., 2005); Cienfuegos, Cuba (Alonso-Hernández et al., 2014); and Detroit, USA (McNeary and Baskaran, 2003). This may be due to their distinct source; 7Be is a cosmogenic radionuclide, whereas 210Pb is mainly derived through the decay of 222Rn from soil. The inventories of 210Pb in the top soil layer are higher than that of 7Be and are susceptible to the re-suspension process; thus, the dry fallout of 210Pb is expected to be much higher and is less controlled by precipitation compared with 7Be. Although the deposition fluxes of 7Be are mainly controlled by precipitation, its fallout has a certain limit, regardless of the rainfall amount. As shown in Fig. 3, the deposition fluxes of 7Be remained relatively constant from April to July, with which rainfall fluctuated greatly; the maximum monthly precipitation occurred in June (363.6 mm), but the highest deposition fluxes of 7Be were observed in March. Gai et al. (2015) observed a negative correlation between the annual deposition fluxes of 7Be and the average annual precipitation at different latitudes; thus, it is indicated that the fallout of 7Be in certain latitude does not increase with continuing rainfall due to its latitude dependence. 

Fig. 4. Correlation between deposition fluxes of 7Be and 210Pb, and precipitation.Fig. 4. Correlation between deposition fluxes of 7Be and 210Pb, and precipitation.

Wet precipitation, dry deposition, atmospheric circulation, continental or oceanic air masses are considered main factors that influence the deposition fluxes of 7Be and 210Pb. Dry deposition is estimated to contribute to 14% of the global 210Pb fallout (Balkanski et al., 1993), but it could be much higher in semi-arid areas and even more important than wet fallout (Rastogi and Sarin, 2008). As shown in Figs. 2 and 3, the monthly rainfall was low in January and February, whereas the deposition fluxes of 7Be and 210Pb were still relatively high, along with high concentrations of 7Be and 210Pb in the air. It is suggested that dry deposition may play an important role in winter months in this region. In addition to dry and wet deposition, the deposition fluxes of 7Be and 210Pb are also affected by the origin and pathway of air masses as well as atmospheric circulation. During fall when northeast monsoon prevailing, the continental air masses (rich in 7Be and 210Pb) could have led to high deposition fluxes of 7Be and 210Pb in August and September, with plenty of precipitation during these periods. In Shanghai, China, high deposition fluxes of 210Pb were ascribed to storm dust from northern and northwestern China (Du et al., 2008), reflecting the influence of air masses on local 210Pb deposition. During spring, as the mid-latitude troposphere narrows, the enhanced air exchange between the stratosphere and troposphere may have caused the high deposition fluxes of 7Be in March.

Total Deposition Velocity of Aerosols Using 7Be and 210Pb

Atmospheric deposition is one of the key processes that remove pollutants from air and is considered the major source of nutrients and toxic substances to ecosystems. The deposition velocity of aerosol particles can be used to estimate the deposition fluxes of air pollutants and to assess environmental impact. The total deposition velocity (Vd) of any radionuclide in air can be determined as follows (McNeary et al., 2003; Dueñas et al., 2005):

where F and C are the total deposition flux (wet + dry) and the activity concentration of this radionuclide in aerosols, respectively. In this study, the total deposition velocity of 7Be and 210Pb were calculated as the ratio of the deposition fluxes of 7Be and 210Pb to the monthly average concentrations of 7Be and 210Pb in the air.

7Be and 210Pb serve as good tracers for studying the total deposition velocity of aerosols (McNeary et al., 2003). First, the activity concentrations and deposition fluxes of 7Be and 210Pb in ambient air can be easily determined. Second, the production rates of 7Be and 210Pb at any given site remain constant over a long period. Third, the size distributions of 7Be and 210Pb in aerosols are similar to other atmospheric particulate pollutants; thus, the deposition velocity of 7Be and 210Pb can be used to determine the deposition fluxes of these pollutants to the earth’s surface.

Table 2 presents the monthly average deposition velocity of 7Be and 210Pb, together with the precipitation amount, the number of rainy days, and atmospheric fine particulate matter (PM2.5) during the sampling period. The total deposition velocity of 7Be at our site ranged from 0.04 to 2.06 cm s–1, with an average value of 0.83 cm s–1. The corresponding values for 210Pb varied from 0.09 to 1.24 cm s–1, with an average value of 0.62 cm s–1. Moreover, both 7Be and 210Pb deposition velocity displayed seasonal variations, and they were high in summer and low in winter. Limited data are available on the simultaneously measured deposition velocity for 7Be and 210Pb. Table 3 lists the deposition velocity of 7Be and 210Pb calculated in previous studies. The deposition velocity of 7Be and 210Pb at our site were similar to those reported in Detroit, Michigan (McNeary et al., 2003), and Norfolk, Virginia (Todd et al., 1989). The deposition velocity of 7Be was higher than that of 210Pb, except in a study from Málaga, Spain (Dueñas et al., 2005). Considering 210Pb is mainly derived from the decay of 222Rn, the activity concentration of 210Pb in aerosol near the ground is expected to be high; thus, the total deposition velocity of 210Pb is expected to be low (McNeary et al., 2003). The strong positive correlation (r = 0.80; Fig. 5) between 7Be and 210Pb deposition velocity indicates that, irrespective of the different source, both radiotracers are attached to similar size aerosols and they are removed from the atmosphere by similar mechanisms. 

Fig. 5. Deposition velocity of 7Be versus 210Pb.Fig. 5. Deposition velocity of 7Be versus 210Pb.

The deposition velocity of atmospheric aerosols depends on the particle size and meteorological conditions. 7Be and 210Pb in air are mainly attached to fine particles, and the most likely route for their removal is rainout. For a better understanding of the rainout effect, the deposition velocity of 7Be and 210Pb versus precipitation and the number of rainy days are plotted in Fig. 6. As seen in the figure, both 7Be and 210Pb deposition velocity showed a significant positive correlation with the rainfall amount and the number of rainy days. It is suggested that precipitation is the key factor in affecting the deposition velocity of 7Be and 210Pb and plays a crucial role in removing these radionuclides from air. The deposition velocity of radionuclide is a function of its deposition fluxes and the activity concentration in air. 

Fig. 6. Deposition velocity of 7Be and 210Pb in correlation with precipitation and the number of rainy days.Fig. 6. Deposition velocity of 7Be and 210Pb in correlation with precipitation and the number of rainy days.

Atmospheric fine particulate matter, the transfer medium of particle-active radionuclides, is an important factor in controlling the activity concentration of radionuclides in air, which in turn affect their deposition velocity. As seen in Fig. 7, strong negative correlations were observed between 7Be (r = –0.91) and 210Pb (r = –0.78) deposition velocity, and PM2.5 content in the air. Similar results were reported in Dueñas et al. (2005) and McNeary and Baskaran (2003), with negative correlations observed between the two deposition velocity and total suspended particle (TSP), and weak correlations between 7Be and 210Pb deposition velocity and the particulate matter collected on the filter membranes. Shenzhen features a subtropical monsoon climate; the summer monsoon occurs annually, and typhoons are common in this region. During the rainy season, the lower layer of the atmosphere is rapidly washed and the deposition velocity of 7Be and 210Pb are expected to be high; as seen from Table 2, the deposition velocity of 7Be or 210Pb displayed the highest values in summer, with an average of 1.74 and 1.02 cm s–1, respectively. During the dry winter season, PM2.5 concentrations in air were high (> 30 µg m–3). Considering that 7Be and 210Pb are mainly attached to fine particles (< 1 µm) and are feebly affected by gravitational settling, the dry fallout of 7Be or 210Pb is expected to be low, which results in the low deposition velocity of these radionuclides in winter. 

Fig. 7. Deposition velocity of 7Be and 210Pb in correlation with PM2.5 in the air.Fig. 7. Deposition velocity of 7Be and 210Pb in correlation with PM2.5 in the air.


The atmospheric activity concentrations and bulk deposition fluxes of 7Be and 210Pb were simultaneously measured for a whole year in Shenzhen, South China. Owing to the elevated 222Rn level in this region’s soil, relatively high 210Pb concentrations in the atmospheric aerosols were observed. The activity of both airborne 7Be and 210Pb and the bulk deposition fluxes showed seasonal variations, with higher winter values and lower summer ones. Precipitation and the origin and pathway of air masses, in addition to atmospheric circulation, are considered the primary controlling factors for 7Be and 210Pb’s activity concentrations in the air and their deposition fluxes in the studied region. Using these two radiotracers to calculate the deposition velocity of aerosols, we discovered that the deposition velocities of 7Be and 210Pb were strongly positively correlated with the rainfall amount but negatively correlated with the airborne PM2.5 concentration. Precipitation plays a critical role in removing these radionuclides from the air, and the deposition velocities were high during the summer and low during the winter due to the activity distributions of 7Be and 210Pb and the meteorological conditions in this region.


This work was supported by Shenzhen Science and Technology Innovation Project (No. JCYJ20170818100556755), the Natural Science Foundation of Guangdong Province (No. 2016A030313037), and the National Natural Science Foundation of China (No. 11275130, 41102217). We would like to thank the reviewers for their valuable suggestions to improve the manuscript.


  1. Ahmed, A.A., Mohamed, A., Ali, A.E., Barakat, A., Abd El-Hady, M. and El-Hussein, A. (2004). Seasonal variations of aerosol residence time in the lower atmospheric boundary layer. J. Environ. Radioact. 77: 275–283. [Publisher Site]

  2. Ali, N., Khan, E.U., Akhter, P., Rana, M.A., Rajput, M.U., Khattak, N.U., Malik, F. and Hussain, S. (2011). Wet depositional fluxes of 210Pb- and 7Be-bearing aerosols at two different altitude cities of North Pakistan. Atmos. Environ. 45: 5699–5709. [Publisher Site]

  3. Alonso-Hernández, C.M., Morera-Gómez, Y., Cartasw-Águila, H. and Guillén-Arruebarrena, A. (2014). Atmospheric deposition patterns of 210Pb and 7Be in Cienfuegos, Cuba. J. Environ. Radioact. 138: 149–155. [Publisher Site]

  4. Balkanski, Y.J., Jacon, D.J., Gardner, G.M., Graustein, W.C., and Turekian, K.K. (1993). Transport and residence times of tropospheric aerosols inferred from a global three-dimensional simulation of 210Pb. J. Geophys. Res. 98: 20573–20586. [Publisher Site]

  5. Baskaran, M., Coleman, C.H. and Santschi, P.H. (1993). Atmospheric depositional fluxes of 7Be and 210Pb at Galveston and College Station, Texas. J. Geophys. Res. 98: 20555–20571. [Publisher Site]

  6. Baskaran, M. (2011). Po-210 and Pb-210 as atmospheric tracers and global Pb-210 fallout: A review. J. Environ. Radioact. 102: 500–513. [Publisher Site]

  7. Caillet, S., Arpagaus, P., Monna, F. and Dominik, J. (2001). Factors controlling 7Be and 210Pb atmospheric deposition as revealed by sampling individual rain events in the region of Geneva, Switzerland. J. Environ. Radioact. 53: 241–256. [Publisher Site]

  8. Chameides, W.L., Yu, H., Liu, S.C., Bergin, M., Zhou, X., Mearns, L., Wang, G., Kiang, C.S., Saylor, R.D., Luo, C., Huang, Y., Steiner, A. and Giorgi, F. (1999). Case study of the effects of atmospheric aerosols and regional haze on agriculture: An opportunity to enhance crop yields in China through emission controls? PNAS 96: 13626–13633. [Publisher Site]

  9. Chham, E., Piñero-García, F., González-Rodelas, P. and Ferro-García, M.A. (2017). Impact of air masses on the distribution of 210Pb in the southeast of Iberian Peninsula air. J. Environ. Radioact. 177: 169–183. [Publisher Site]

  10. Crecelius, E.A. (1981). Prediction of marine atmospheric deposition rates using total 7Be deposition velocities. Atmos. Environ. 5: 579–582. [Publisher Site]

  11. Du, J., Zhang, J., Jing, Z. and Wu, Y. (2008). Deposition patterns of atmospheric 7Be and 210Pb in coast of East China Sea, Shanghai, China. Atmos. Environ. 42: 5101–5109. [Publisher Site]

  12. Du, J., Du, J., Baskaran, M., Bi, Q., Huang, D. and Jiang, Y. (2015). Temporal variations of atmospheric depositional fluxes of 7Be and 210Pb over 8 years (2006-2013) at Shanghai, China, and synthesis of global fallout data. J. Geophy. Res. 120: 4323–4339. [Publisher Site]

  13. Dueñas, C., Fernandez, M.C., Carretero, J., Liger, E. and Cañete, S. (2005). Deposition velocities and washout ratios on a coastal site calculated from 7Be and 210Pb measurements. Atmos. Environ. 39: 6897–6908. [Publisher Site]

  14. Dueñas, C., Fernandez, M.C., Carretero, J., Liger, E. and Cañete, S. (2011b). Atmospheric deposition of 7Be at a coastal Mediterranean station. J. Geophysical. Res. 106: 34059–34065. [Publisher Site]

  15. Dueñas, C., Orza, J.A.G., Cabello, M., Fernández, M.C., Cañete, S., Pérez, M. and Gordo, E. (2011b). Air mass origin and its influence on radionuclide activities (7Be and 210Pb) in aerosol particles at a coastal site in the western Mediterranean. Atmos. Res. 101: 205–214. [Publisher Site]

  16. Dueñas, C., Gordo, E., Liger, E., Cabello, M., Cañete, S., Pérez, M. and de la Torre-Luque, P. (2017). 7Be, 210Pb and 40K depositions over 11 years in Málaga. J. Environ. Radioact. 178-179: 325–334. [Publisher Site]

  17. Feely, H.W., Larsen, R.J. and Sanderson, C.G. (1989). Factors that cause seasonal variations in beryllium-7 concentrations in surface air. J. Environ. Radioact. 9: 223–249. [Publisher Site]

  18. Gai, N., Pan, J., Yin, X.C., Zhu, X.H., Yu, H.Q., Li, Y., Tan, K.Y., Jiao, X.C. and Yang, Y.L. (2015). Latitudinal distributions of activities in atmospheric aerosols, deposition fluxes, and soil inventories of 7Be in the East Asian monsoon zone. J. Environ. Radioact. 148: 59–66. [Publisher Site]

  19. Grossi, C., Bellester, J., Serrano, I., Galmarini, S., Camacho, A., Curcoll, R., Morguí, J.A., Rodò, X. and Duch, M.A. (2016). Influence of long-range atmospheric transport pathways and climate teleconnection patterns on the variability of surface 210Pb and 7Be concentrations in southwestern Europe. J. Environ. Radioact. 165: 103–114. [Publisher Site]

  20. Hernandez-Ceballos, M.A., Cinelli, G., Marín Ferrer, M., Tollefsen, T., De Felice, L., Nweke, E., Tognoli, P.V., Vanzo, S. and De Cort, M. (2015). A climatology of 7Be in surface air in European Union. J. Environ. Radioact. 141: 62–70. [Publisher Site]

  21. Hirose, K., Honda, T., Yagishita, S., Igrarshi, Y. and Aoyama, M. (2004). Deposition behaviors of 210Pb, 7Be and thorium isotopes observed in Tsukuba and Nagasaki, Japan. Atmos. Environ. 38: 6601–6608. [Publisher Site]

  22. Ioannidou, A., Manolopoulou, M. and Papastefanou, C. (2005). Temporal changes of 7Be and 210Pb in surface air at temperate latitudes 40°N. Appl. Radiat. Isot. 63: 277–284. [Publisher Site]

  23. Kim, G., Hussain, N., Scudlark, J.R. and Church, T.M. (2000). Factors influencing the atmospheric depositional fluxes of stable Pb, 210Pb and 7Be into Chesapeake Bay. J. Atmos. Chem. 36: 65–79. [Publisher Site]

  24. Kim, S.H., Hong, G.H., Baskaran, M., Par, K.M. and Chang, S.C. (1998). Wet removal of atmospheric 7Be and 2I0Pb at the Korean Yellow Sea coast. Yellow Sea 4: 58–68.

  25. Lal, D. and Peters, B. (1967). Cosmic ray produced radioactivity on the earth. In Kosmische Strahlung II / Cosmic Rays II, Sitte, K. (Ed.), Springer Berlin Heidelberg, Berlin, Heidelberg, pp. 551–612.

  26. Lal, D. (1968). The radioactivity of the atmosphere and hydrosphere. Annu. Rev. Nucl. Sci. 18: 407–435. [Publisher Site]

  27. Lee, C.S.L., Li, X., Zhang, G., Peng, X.Z. and Zhang, L. (2005). Biomonitoring of trace metals in the atmosphere using moss (Hypnum plumaeforme) in the Nanling Mountains and the Pearl River Delta, Southern China. Atmos. Environ. 39: 397–407. [Publisher Site]

  28. Li, J., Pan, J., Wen, F. and Chen, L. (2013). Calculation and analysis of aerosol residence times in atmosphere. Radiat. Prot. Bull. 33: 25–28. (in Chinese with English Abstract)

  29. Liu, G., Tong, Y., Luong, J.H.T., Zhang, H. and Sun, H. (2010). A source study of atmospheric polycyclic aromatic hydrocarbons in Shenzhen, South China. Environ. Monit. Assess. 163: 599–606. [Publisher Site]

  30. Liu, G., Luo, Q., Ding, M. and Feng, J. (2015). Natural radionuclides in soil near a coal-fired power plant in the high background radiation area, South China. Environ. Monit. Assess. 187: 356. [Publisher Site]

  31. Liu, H., Jacob, D.J., Bey, I. and Yantosca, R.M. (2001). Constraints from 210Pb and 7Be on wet deposition and transport in a global three-dimensional chemical tracer model driven by assimilated meteorological fields. J. Geophys. Res. 106: 12109–12128. [Publisher Site]

  32. Liu, J., Li, J., Zhang, Y., Liu, D., Ding, P., Shen, C., Shen, K., He, Q., Ding, X. and Wang, X. (2014). Source apportionment using radiocarbon and organic tracers for PM2.5 carbonaceous aerosols in Guangzhou, South China: Contrasting local-and regional-scale haze events. Environ. Sci. Technol. 48: 12002–12011. [Publisher Site]

  33. McNeary, D. and Baskaran, M. (2003). Depositional characteristics of 7Be and 210Pb in southeastern Michigan. J. Geophys. Res. 108: 4210.[Publisher Site]

  34. Momoshima, N., Nishio, S., Kusano, Y., Fukuda, A. and Ishimoto, A. (2006). Seasonal variations of atmospheric 210Pb and 7Be concentrations at Kumamoto, Japan and their removal from the atmosphere as wet and dry depositions. J. Radioana. Nucl. Chem. 268: 297–304. [Publisher Site]

  35. Olsen, C.R., Larsen, I.L., Lowry, P.D., Cutshall, N.H., Todd, J.F., Wong, G.T.F. and Casey, W.H. (1985). Atmospheric fluxes and marsh-soil inventories of 7Be and 210Pb. J. Geophys. Res. 90: 10487–10495. [Publisher Site]

  36. Pan, J., Yang, Y.L., Zhang, G., Shi, J.L., Zhu, X.H., Li, Y. and Yu, H.Q. (2011). Simultaneous observation of seasonal variations of beryllium-7 and typical POPs in nearsurface atmospheric aerosols in Guangzhou, China. Atmos. Environ. 45: 3371–3380. [Publisher Site]

  37. Rastogi, N. and Sarin, M.M. (2008). Atmospheric 210Pb and 7Be in ambient aerosols over low- and high-altitude sites in semiarid region: Temporal variability and transport processes. J. Geophys. Res. 113: D11103. [Publisher Site]

  38. Renfro, A.A., Cochran, J.K. and Colle, B.A. (2013). Atmospheric fluxes of 7Be and 210Pb on monthly time-scales and during rainfall events at Stony Brook, New York (USA). J. Environ. Radioact. 116: 114–123. [Publisher Site]

  39. Sarri, H.K., Schmidt, S., Castaing, P., Blanc, G., Sautour, B., Masson, O. and Cochran, J.K. (2010). The particulate 7Be/210Pbxs and 234Th/210Pbxs activity ratios as tracers for tidal-to-seasonal particle dynamics in the Gironde Estuary (France): Implications for the budget of particle-associated contaminants. Sci. Total. Environ. 408: 4784–4794. [Publisher Site]

  40. Tan, K.Y., Yang, Y.L., Zhu, X.H., Chen, S., Jiao, X.C., Gai, N. and Huang, Y. (2013). Beryllium-7 in near-surface atmospheric aerosols in mid-latitude (40 degrees N) city Beijing, China. J. Radioanal. Nucl. Chem. 298: 883–891. [Publisher Site]

  41. Todd, J.F., Wong, G.T.F., Olsen, C.R. and Larsen, I.L. (1989). Atmospheric depositional characteristics of beryllium-7 and lead-210 along southeastern Virginia coast. J. Geophy. Res. 94: 11106–11116. [Publisher Site]

  42. Turekian, K.K, Benninger, L.K. and Dion, E.P. (1983). 7Be and 210Pb total deposition fluxes at New Haven Conneticut and at Berbuda. J. Geophy. Res. 88: 5411–5415. [Publisher Site]

  43. Wang, N., Zheng, L., Chu, X., Li, S. and Yuan, S. (2016). The characteristics of radon and thoron concentration from soil gas in Shenzhen City of Southern China. Nukleonika 61: 315–319. [Publisher Site]

  44. Winkler, R. and Rosner, G. (2000). Seasonal and long-term variation of 210Pb concentration in air, atmospheric deposition rate and total deposition velocity in South Germany. Sci. Total Environ. 263: 57–68. [Publisher Site]

  45. Yadav, A.K., Kumar, K., Kasim, A., Singh, M.P., Parida, S.K. and Sharan, M. (2003). Visibility and incidence of respiratory diseases during the 1998 haze episode in Brunei Darussalam. Pure Appl. Geophys. 160: 265–277. [Publisher Site]

  46. Yang, Y., Gai, N., Geng, C., Zhu, X., Li, Y., Xie, Y., Yu, H. and Tan, K. (2013). East Asia monsoon's influence on seasonal changes of beryllium-7 and typical POPs in near-surface atmospheric aerosols in mid-latitude city Qingdao, China. Atmos. Environ. 79: 802–810. [Publisher Site]

  47. Yi, Y., Zhou, P. and Liu, G. (2007). Atmospheric deposition fluxes of 7Be, 210Pb and 210Po at Xiamen, China. J. Radioanal. Nucl. Chem. 273: 157–162. [Publisher Site]

  48. Zhang, F., Zhang, B. and Yang, M. (2013). Beryllium-7 atmospheric deposition and soil inventory on the northern Loess Plateau of China. Atmos. Environ. 77: 178–184. [Publisher Site]

  49. Zhang, L., Yang, W., Chen, M., Wang, Z., Lin, P., Fang, Z., Qiu, Y. and Zheng, M. (2016). Atmospheric deposition of 7Be in the southeast of China A case study in Xiamen. Aerosol Air Qual. Res. 16: 105–113. [Publisher Site]

  50. Zhu, J. and Olsen, C.R. (2009). Beryllium-7 atmospheric deposition and sediment inventories in the Neponset River estuary, Massachusetts, USA. J. Environ. Radioact. 100: 192–197. [Publisher Site]

Aerosol Air Qual. Res. 20 :1607 -1617 . https://doi.org/10.4209/aaqr.2019.11.0560  

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