Abstract
96 aerosol samples were collected in north China and analyzed by gamma spectrometry. The activity concentrations of Pb-210 ranged from 97 to 27,955 μBq/m3, with average of 879, 3389 and 813 μBq/m3 in Beijing, Changbai and Hunchun, respectively. Annual effective dose for inhabitants due inhalation varied from 0.68 to 5.94 μSv. There was a positive correlation between Pb-210 and PM2.5 in Beijing. Seasonal variation of Pb-210 concentration was observed in Changbai and Hunchun. Analysis of their correlation with meteorological parameters could help to assess the effects of present pollutant emission and provide scientific support for prevention strategy.
Similar content being viewed by others
Explore related subjects
Discover the latest articles, news and stories from top researchers in related subjects.Avoid common mistakes on your manuscript.
Introduction
Lead is a heavy metal, which mainly accumulates in human bones after uptake through the diet and inhalation. Lead-210, with a half-life of 22.3 years, is an important radioisotope of lead and regards as a high-toxicity radionuclide because of its chemical and radiological effect. Pb-210 in the air mainly originates from the decay of Rn-222 which is emitted from the earth to the atmosphere as gas. The constant releases of Rn-222 from the earth causes constant Pb-210 level in the air. The particle containing Pb-210 deposited on earth was therefore widely used as a chronology tool for dating of sediment. However, increasing human activities, such as mining, fuel burning and coal heating significantly increases the Pb-210 level in the air, because large amount of Pb-210 associated to particles and Rn-222 in gas form were released to the air during combustion in these processes [1, 2]. Lacking of fly ash removal systems in the factories where coal was used as a fuel or the coal is directly for domestic heating further increase the emission of Pb-210 into the air [3]. The Pb-210 in the air would finally enter human body through food chain and inhalation, which cause an exposure of Pb-210. Pb-210 is a beta emitter that decays into toxic alpha emitting Po-210 and beta emitting Bi-210 (1162 keV), which consequently cause a high radiation toxicity and possible health risk to humans. IAEA and WHO have developed operational intervention levels (OILs) and guidance levels regarding the activity concentration of Pb-210 in food and water, which is 2.0 Bq/kg and 0.1 Bq/L, respectively [4, 5]. OILs of Pb-210 in food given by IAEA safety standards is based on assumption of equilibrium radioactive chains with Bi-210, Po-210.
There are many large-scale coal-fired power plants and several smaller local power plants usually with insufficient fly ash removal systems in China [6]. In addition, air pollution including air particles (e.g. PM2.5, PM10) has become one of the most serious environmental problems in large part of China [7,8,9,10]. However, there is limited investigation on level of air Pb-210 in China. Meanwhile, its variation with season, location and PM2.5, the major driving and control parameters on the level of air Pb-210 and its variation are still unclear. This work aims to measure Pb-210 concentrations in the air at three locations, Beijing, Changbai and Hunchun, with a different human activities in north China, and to investigate the controlling parameters influcing the Pb-210 level in the air.
Experimental
Equipment and sampling
Aerosol samples were collected at the roof of building in each investigated site through portable Staplex TF1A type (Clover company, USA) high-volume air sampler, the maximum sampling flow rate is 2 m3/min, the 3M E853:5379 model aerosol membrane with size of BMF 20 g/m2 (Whatman Company, UK) were used as filter when collect particles in the air. Collection efficiency of the membrane was larger than 90% for size of particles great than 0.2 μm. Angle of each sampler was properly arranged during sampling in order to avoid the gas discharge influence from each other of the sampler [11]. In this work, three sites were selected that stand for different scales of location in north of China, they are Beijing, Changbai and Hunchun. For the size of three cities, it is high connected with population. Beijing, capital of China with populations of more than 20 million and number of cars more than 5 million, is one of the largest cities in China. Changbai is a county, stand for the medium scale, with populations of 86,300 while Hunchun, the sampling site is located in a small town, with populations around 5000 and the number of cars is not much. The locations of sampling sites are showed in Fig. 1.
In each investigated site, aerosol samples were collected at the roof of building. These buildings are around 10–15 m high, usually is a fifth to sixth floor. The sampling site in Beijing is on the roof of sixth floor building, the sampling site in Changbai and Hunchun is on the roof sixth and fifth floor building, respectively. Height of the sampling locations was set similar when possible obtained. During this work, parallel samplings were carried out at the same location.
The meteorological conditions such as temperature, humidity and air pressure were recorded during each sampling procedure. The flow rates of about 1.5–2 m3/min were also recorded at the beginning and end of the sampling, respectively, then the volume of the air samples were calculated according to recorded data and recommended methods [11]. Sampling usually started at 8:00 am and lasted nearly 24 h, in general the total volume of the air for each sample is 2000–3000 m3. Two 3M type filters which collected the atmospheric aerosol particles were folded and placed in the mold of stainless steel, then compressed into a 50 mm-in-diameter and 4.5 mm-in-thickness disc by hydraulics, the samples were then transferred to cylindrical polyethylene beakers (dia. 75 mm × ht. 35 mm) and sealed until measurement.
Measurement of radionuclide using gamma spectrometry
A gamma spectrometry consisting of a broad-energy High Purity Germanium (HPGe) type detector named BE5030 (CANBERRA®) shielded in a lead chamber was used for measurement of Pb-210 in aerosol samples, the system has a relative efficiency of 50.5%, and a resolution of 1.88 keV for the 1332 keV Co-60 peak. The measured background in 20–2000 keV is 53 count/min. Software Genie 2000® was used for spectral acquisition and analysis. Activity concentration of Pb-210 in the aerosol was calculated by formula (1):
where S means total net peak area counted by 46.5 keV γ-ray derived from Pb-210, expressed in count/s, R the correction coefficient for radioactive decay, f the emission probability of 46.5 keV γ rays derived from Pb-210, which is 4.25% [12], V means the total volume of each collected outdoor air sample, expressed in m3, \(\xi\) the collection efficiency of air filter membrane, amount to 90%, ε means the gamma spectrometry detection efficiency of 46.5 keV γ-ray derived from Pb-210.
The efficiency for the HPGe gamma spectrometry had been previously calibrated by using a set of mixed nuclides standards filter (identification code: X13598) which is traceable to NPL (National Physical Laboratory, UK). Efficiency calibration of the spectrometer was carried out according to standards [11, 13, 14]. Self-attenuation factor of 46.5 keV γ-ray depending on the density and composition of sample has been established in the laboratory, and used for correct the counting efficiency of the samples. Each samples was normally measured for 24 h. Energy drift of the spectrometers was checked every day and found that no significant shift was observed. For quality control, an intercomparison of γ-spectrometry measurement and analysis was organized by the framework of the minutes on technical cooperation of National Institute for Radiological Protection, Chinese Center for Disease Control and Prevention (NIRP, China CDC), Radiation Monitoring Technical Center of Ministry of Environmental Protection (RMTC) and Japan Chemical Analysis Center (JCAC). Our laboratory periodically participates in the intercomparison exercises for many times [15, 16]. The results of participation in these intercomparison exercises generally resulted in Z-scores less than 2, a Z-score equal to or less than 2 indicates that the measurement is satisfactory.
During sampling days, the data of Air Quality Index (AQI), PM2.5 and PM10 concentration were obtained from local metrological reports [17,18,19]. Statistical Analysis System (SAS) 9.3 was applied for data analysis, and the correlation was considered to be significant at P value less than 0.05.
Results and discussion
The samples from Changbai and Hunchun were collected only at January and September in the period of 2016–2017, which aims to estimate the seasonal and regional difference of the two sites. The samples from Beijing were collected in the period of March to May in 2015, when the haze was the heaviest during the whole year of Beijing.
A total of 96 outdoor air samples were collected. The reported expanded uncertainty of the result was based on a standard uncertainty multiplied by a coverage factor (k = 2), providing a coverage probability of approximately 95%. The uncertainty evaluation was carried out in accordance with the requirements of national standard [11, 13]. Pb-210 concentration changes, correlation between AQI, PM2.5 and PM10 with Pb-210 concentration are illustrated in Figs. 2, 3 and 4 for Beijing, Changbai and Hunchun, respectively. The data of AQI, PM2.5 and PM10 was obtained from the local metrological reports. Statistical results for sampling site of Beijing demonstrated the correlation coefficients between Pb-210 activity concentrations and AQI, Pb-210 activity concentrations and PM2.5, Pb-210 activity concentrations and PM10 were 0.75, 0.80 and 0.64, respectively, and there were statistical significant (P < 0.0001). Seasonal concentration changes of Pb-210 from 2016 to 2017 with the trend of air quality index in Changbai has shown a correlation with the consumption of main fossil fuels (coal and oil) in winter (Fig. 3).
The average values and the sample information were summarized in Table 1. The average Pb-210 activity concentrations in Beijing, Changbai and Hunchun were 879, 3389 and 813 μBq/m3, respectively, with the variation range of 97–27,955 μBq/m3. The average values in winter were 20,403 and 1456 μBq/m3 in Changbai and Hunchun, respectively, while in autumn it were much lower with values of 869 and 701 μBq/m3 in Changbai and Hunchun, respectively. Pb-210 concentrations in Changbai was significantly higher than that in Hunchun in winter (January, P < 0.01), but the difference was insignificant in autumn between two sites (September, P = 0.1498). As we known, the basic source of Pb-210 in air is the decay of Rn-222 escaping from soil, the release of human activities, and the impact of environmental changes. The major difference in two sites is human activities, as there are more populations in Changbai (~ 86,300 persons) than in town of Hunchun (~ 5000 persons). So, difference in winter may be attributed to the more amount use of coal in Changbai for more larger scale of domestic heating in winter because the lowest tempeture is around − 40 °C in winter. Some researchers indicated that the radionuclides concentrations were enhanced by coal combustion [3, 20, 21]. In addition, the sampling sites in Changbai is located in the center of urban district, while the sampling site in Hunchun is located in Jingxin Town, which is approximately 35 km far away from the center urban district,. The air Pb-210 concentrations in winter was significantly higher than that in autumn in both Changbai group (P < 0.01) and Hunchun group (P < 0.01). The measured results in these work are comparable to those reported in Poland [1], Egypt [22] and Germany [23], while is not consistent with literatures reported by Talbi [24].
Series of simple linear correlation analysis were carried out between different sites. It demonstrated that the correlation coefficient between Pb-210 activity concentrations and AQI, Pb-210 activity concentrations and PM2.5, Pb-210 activity concentrations and PM10 were 0.73, 0.76 and 0.70, respectively in Hunchun group, and there were statistical significant (P < 0.01). But there were strong correlations among AQI, PM2.5 and PM10, partial correlation analysis was carried out and the results presented that none of the three pairs had a significant correlation after excluding impact of the other two factors. The same statistical methods were used to analyze the data of Changbai group.
Statistical results of Beijing group demonstrated that the correlation coefficients between Pb-210 activity concentrations and AQI, Pb-210 activity concentrations and PM2.5, Pb-210 activity concentrations and PM10 were 0.75, 0.80 and 0.64, respectively, and they were statistical significant (P < 0.0001). However, partial correlation analysis result presented that only the correlation between Pb-210 activity concentrations and PM2.5 was significant (r* = 0.43, P = 0.0088) after excluding impact of the other two factors. It can be concluded that there was a positive correlation between Pb-210 activity concentrations and PM2.5 (P < 0.01) for Beijing group. It has been reported that lead had been the highest concentration within the heavy metal detected in PM2.5 and showed particle size dependence with lead metals concentrations, which were high in the particle size range of 1.1–4.7 µm [25, 26], which was partial consistent with this study.
The measured Pb-210 activity concentrations were compared with different studies as listed in Table 2. It showed that most of Pb-210 concentrations in different sites of China were higher than that in districts of other countries, especially in Changbai. Most of these values have exceeded the world average levels that reported by UNSCEAR (500 μBq/m3) [27], indicated there are sources of systemic and regional pollution risks. Therefore, the studies to trace, prevent, and control the source of major pollution must be strengthened.
To evaluate corresponding annual effective dose of Pb-210 due inhalation for inhabitants, the committed effective dose was calculated by formula (2):
where A is the mean values of Pb-210 activity concentration in air of investigated sites, expressed in Bq/m3, T the Pb-210 dose conversion coefficient, expressed in Sv/Bq, dose conversion coefficient of Pb-210 with ages group of 1–2 years old, 2–7 years old, 7–12 years old, 12–17 years old and above 17 years old were 2.90E−06, 1.50E−06, 1.40E−06, 1.30E−06, 9.00E−07 Sv/Bq, respectively [40]. Where b means the respiratory rate, expressed in m3/d [41], d the fraction of time spent outdoors by inhabitants of the considered area corresponds to 0.2, 365 × 0.2 = 73 days, expressed in days [41]. After considering different respiratory rate corresponding different ages group, the committed effective dose attributed to Pb-210 in all sample sites were estimated and presented in Table 3. The results shows that internal dose through inhalation of the above mentioned air was estimated to be 0.68–5.94 μSv. The maximum annual effective dose are nearly 5% of the effective doses from outdoor radon progeny in China, which is 126 μSv [42].
Conclusions
Level of Pb-210 in atmosphere in North China were higher than that a selection of other countries. Based on observation from year of 2015 to 2017, Pb-210 together with comprehensive investigation data of Air Quality Index (AQI), PM2.5 and PM10 concentration were obtained to analysis the correlation and trend of those factors. The average activity concentrations of Pb-210 during the winter season in Changbai and Hunchun were higher than those in autumn. The seasonal variation was statistically significant (t test, 95% CI), which mainly results from the increment of coal combustion in winter. Pb-210 activity concentrations in Changbai were higher than that in Hunchun in winter. The statistical results of the activity concentration in Beijing demonstrated that there was a positive correlation between Pb-210 activity concentrations and PM2.5 (P < 0.01). The developed method and obtained data can be used as a baseline to evaluate air quality, corresponding effective dose from inhalation for inhabitants were evaluated, with maximum effective dose of 4.44 μSv for adult. Distribution analysis of the results could help to assess the effects of historical emission control measurement and provide experience and scientific support for the following air pollutant prevention strategy making in Beijing and other north areas of China.
References
Dlugosz M, Grabowski P, Bem H (2010) 210Pb and 210Po radionuclides in the urban air of Lodz, Poland. J Radioanal Nucl Chem 283(3):719–725
Weng Y, Chu TC (1992) Concentration of radionuclides of size fractionated fly ash emissions from a thermal power plant using Taiwan coal. J Radiat Res 33:141–150
Asokan P, Saxena M, Asolekar SR (2005) Coal combustion residues—environmental implications and recycling potentials. Resour Conserv Recycl 43(3):239–262
WHO (2017) Guidelines for drinking-water quality, fourth edition incorporating the first addendum. World Health Organization, Geneva
IAEA (2011) Criteria for use in preparedness and response for a nuclear or radiological emergency, General Safety Guide No. GSG-2, IAEA Safety Standards
Chen YL (2011) Research on low emission of electrostatic precipitator (ESP). In: Proceedings of 14th conference of ESP, pp 1–24
Xuexi T, Rujin H, Junji C, Qiang Z, Yafang C, Hang S, Di C, Ulrich P, Thorsten H, Uli D, Guohui L, Douglas RW, Colin DO (2017) Severe pollution in china amplified by atmospheric moisture. Sci Rep 7(1):15760. https://doi.org/10.1038/s41598-017-15909-1
Jianlei L, Yanyun Z, Ying Z, Shuiyuan C, Dongsheng C, Xiurui G, Sha C, Xiaoxin L, Xiaofan X, Haiyan W (2017) Trends of PM2.5 and chemical composition in Beijing, 2000–2015. Aerosol Air Qual Res 17:412–425
Nianliang C, Dawei Z, Yunting L, Xiaoming X, Ziyue C, Fan M, Bingbo G, Bin H (2017) Spatio-temporal variations of PM2.5 concentrations and the evaluation of emission reduction measures during two red air pollution alerts in Beijing. Sci Rep. https://doi.org/10.1038/s41598-017-08895-x
Wenju C, Ke L, Hong L, Huijun W, Lixin W (2017) Weather conditions conducive to Beijing severe haze more frequent under climate change. Nat Clim Change. https://doi.org/10.1038/NCLIMATE3249
Chinese Standards, WS/T 184-1999 (1999) Gamma spectrometry method of analyzing radionuclides in air. Ministry of Health of the People’s Republic of China (in Chinese)
Firestone RB, Shirley VS (1996) Table of isotopes. Wiley, New York
Chinese Standards, GB 11713-2015 (2015) General analytical methods of high-purity germanium gamma spectrometer. Ministry of Health of the People’s Republic of China (in Chinese)
International Atomic Energy Agency (1989) Measurement of radionuclides in food and the environment. Technical report series No. 295. Vienna, IAEA
Fei T, Cuihua X, Qing Z, Jing Z, Qiang Z, Wenhong L, Jianfeng Z, Xu S (2014) A review of nationwide radioactivity comparisons on gamma-ray spectrometry organized by the NIRP, China. Appl Radiat Isot 87:435–438
Qiang Z, Xiaoqiang W, Fei T, Yanqing H, Ikeuchi Yoshihiro, Jia Y, Cuihua X, Jing Z, Li Wenhong, Qing Z, Xu S (2015) Intercomparison of γ-spectrometry analysis of radionuclides between China and Japan in 2012–2013. Appl Radiat Isot 105:244–248
Historical data query of Jilin air quality index. http://www.tianqihoubao.com/lishi/baishan.html. Accessed 8 Jan 2018 (in Chinese)
Historical data query of Jilin air quality index. http://www.tianqihoubao.com/lishi/yanbian.html. Accessed 8 Jan 2018 (in Chinese)
Historical data query of Beijing air quality index. http://www.tianqihoubao.com/lishi/beijing/month/201503.html. Accessed 8 Jan 2018 (in Chinese)
Zeevaert T, Sweeck L, Vanmarcke H (2006) The radiological impact from airborne routine discharges of a modern coal-fired power plant. J Environ Radioact 85(1):1–22
Sahu SK, Tiwari M, Bhangare RC, Pandit GG (2014) Enrichment and particle size dependence of polonium and other naturally occurring radionuclides in coal ash. J Environ Radioact. 138:421–426
Ahmed AA, Mohamed A, Ali AE, Barakat A, Abd El-Hady M, El-Hussein A (2004) Seasonal variations of aerosol residence time in the lower atmospheric boundary layer. J Environ Radioact 77(3):275–283
Winkler R (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(1):57–68
Csanádi Z (2017) Heavy metals in PM2.5 aerosols in urban sites of Győr, Hungary. Urban Civ Eng 11(6):758–761
Talbi A (2017) Assessment of annual air pollution levels with PM1, PM2.5, PM10 and associated heavy metals in Algiers, Algeria. Environ Pollut 232:252–263
Aryal R (2013) Characteristics of atmospheric particulate matter and metals in industrial sites in Korea. Environ Pollut 2(4):10–21
UNSCEAR (2000) Sources, effects and risk of ionizing radiation, vol 1. United Nations Scientific Committee on the Effects of Atomic Radiation, New York
Isakar K, Kiisk M, Realo E, Suursoo S (2016) Lead-210 in the atmospheric air of North and South Estonia: long-term monitoring and back-trajectory calculations. Proc Estonian Acad Sci 65(4):442
Gordo E, Liger E, Dueñas C, Fernándezc MC, Cañetea S, Pérezd M (2015) Study of 7Be and 210Pb as radiotracers of African intrusions in Malaga (Spain). J Environ Radioact 148:141–153
Baeza A, Rodríguez-Perulero A, Guillén J (2016) Anthropogenic and naturally occurring radionuclide content in near surface air in Cáceres (Spain). J Environ Radioact 165:24–31
Chham E, Piñerogarcía F, Gonzálezrodelas P, Ferro-García MA (2017) Impact of air masses on the distribution of 210Pb in the southeast of Iberian Peninsula air. J Environ Radioact 177:169–183
Tositti L, Brattich E, Cinelli G, Baldacci D (2014) 12 years of 7Be and 210Pb in Mt. Cimone, and their correlation with meteorological parameters. Atmos Environ 87(87):108–122
Ali N, Khan EU, Akhter P, Khattak NU, Khan F, Rana MA (2011) The effect of air mass origin on the ambient concentrations of Be-7 and Pb-210 in Islamabad, Pakistan. J Environ Radioact 102(1):35–42
Pham MK, Betti M, Nies H, Povinec PP (2011) Temporal changes of 7Be, 137Cs and 210Pb activity concentrations in surface air at Monaco and their correlation with meteorological parameters. J Environ Radioact 102(11):1045–1054
Magand O, Ferrari C, Gauchard PA, Amato P, Fain X (2006) Analysis of 7Be and 210Pb air concentrations in Ny-Alesund, Svalbard: CHIMERPOL II project, preliminary results. Memoirs of National Institute of Polar Research Special Issue, vol 59 (Special issue), pp 96–115
Daish SR, Dale AA, Dale CJ, May R (2005) The temporal variations of 7Be, 210Pb and 210Po in air in England. J Environ Radioact 84(3):457–467
Guojiang W, Wei Y, Shilu W, Enyuan W, Fengchang W, Lee SN, Changsheng W, Ronggui H (2005) The high concentration of 210Pb characterized by “U” in the surface air of Qianzhong area. Chin Sci Bull 50(14):1498–1502 (in Chinese)
Jingshun P, Fuping W, Ling C, Xiaona R, Jing Z, Shunping Z, Zhonggang C, Ziqiang P (2017) The preliminary analysis of 210Pb and 210Po activity concentration in main cities of China. Radiat Prot. 37(6):433–437 (in Chinese)
Hongqi S, Yu Z, Aifang D, Zhenfang D (2017) Variation in activity concentration of 210Pb in atmospheric aerosol and its radiation dose assessment in Qingdao. Chin J Radiol Med Prot 37(5):372–375 (in Chinese)
Chinese Standards, GB 18871-2002 (2002) Basic standards for protection against ionizing radiation and for the safety of radiation sources. Ministry of Health of the People’s Republic of China (in Chinese)
Chinese Standards, GB 16148-2009 (2009) specification for assessments of intakes and internal does of radionuclides. Ministry of Health of the People’s Republic of China (in Chinese)
Ziqiang P, Senlin L et al (2011) Radiation level in China. China Atomic Energy Publishing and Media Co., Ltd., Beijing
Acknowledgements
This work was supported by the Support Program of Ministry of Science and Technology (No. 2014FY211000), the National Key Technology R&D Program (No. 2013BAK03B05).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Tuo, F., Pang, C., Wang, W. et al. Level, distribution, variation and sources of Pb-210 in atmosphere in North China. J Radioanal Nucl Chem 318, 1855–1862 (2018). https://doi.org/10.1007/s10967-018-6205-6
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10967-018-6205-6