Assessment of 210Po, 210Bi and 210Pb in aerosols and their deposition fluxes in the nearshore region of the East China Sea
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摘要: 大气210Po、210Bi和210Pb的沉降通量是海洋中核素示踪颗粒物动力学过程（颗粒有机碳输出、颗粒物输运）的基础参数，为揭示我国近海地区210Po、210Bi和210Pb活度浓度的时空变化规律并估算其沉降入海通量，本文于2016年9月至2017年2月和2021年9-12月分别对上海及厦门地区近地表大气气溶胶中210Po、210Pb和210Bi的活度浓度进行了连续观测；基于210Po/210Pb和210Bi/210Pb两种示踪法计算了气溶胶颗粒物的滞留时间，并利用一维简单气溶胶沉降速率模型估算了3种核素以大气沉降方式输入东海的通量。结果显示，2016年上海秋冬两季210Po、210Bi、210Pb 3种核素活度浓度的变化范围分别为0.11～1.27 mBq/m3、0.45～1.83 mBq/m3和1.12～6.10 mBq/m3；2021年秋季厦门210Po、210Bi、210Pb 3种核素活度浓度的变化范围分别为0.05～0.85 mBq/m3、0.61～2.42 mBq/m3、0.18～1.32 mBq/m3，上海近地表气溶胶中3种核素的活度浓度秋季平均值比厦门地区高。利用210Po-210Pb和210Bi-210Pb活度比计算得到上海和厦门近地面大气的气溶胶滞留时间存在显著差异，基于210Po-210Pb计算上海气溶胶滞留时间均值为（94 ± 54）d，基于210Po-210Pb计算上海气溶胶滞留时间均值为（6.4 ± 4.8）d，造成这种差异的原因很可能是由于两种示踪法本身具有的系统性差异。本文基于一维简易气溶胶沉降速率模型估算了上海地区的210Pb、210Bi和210Po的大气沉降入东海的通量，其在秋季期间的变化范围分别为0.1～26.35 Bq/(m2·d)、0.04～7.91 Bq/(m2·d)和0.01～5.49 Bq/(m2·d)。基于模型估算的210Po、210Bi和210Pb沉降通量与研究区域的实际观测值接近一致，表明利用一维简易气溶胶沉降速率模型间接估算法在替代观测站直测核素的沉降入海通量方面具有一定可行性。Abstract: The deposition fluxes of 210Po, 210Bi and 210Pb in atmosphere are the basis for the application of radionuclide tracing in the ocean. In order to reveal the spatio-temporal variation of the activity of 210Po, 210Bi and 210Pb in nearshore areas and estimate their deposition fluxes into the sea, In this paper, sampling observation and analysis of two typical areas near the East China Sea in Shanghai and Xiamen in different periods are carried out.A time series study was conducted on the activity of 210Po, 210Pb and 210Bi in Shanghai and Xiamen from September 2016 to February 2017 and from September to December 2021, respectively. The residence time of particulate matter was calculated based on 210Po/210Pb and 210Bi/210Pb. Deposition fluxes of three nuclides were also estimated. This paper reported the activity of 210Po, 210Bi and 210Pb in Shanghai in autumn and winter of 2016.The activity ranges of 210Po, 210Pb and 210Bi were 0.11-1.27 mBq/m3, 0.45-1.83 mBq/m3 and 1.12-6.10 mBq/m3, respectively. In the fall of 2021, the activity ranges of 210Po, 210Bi and 210Pb in Xiamen were 0.05-0.85mBq/m3, 0.61-2.42mBq/m3 and 0.18-1.32mBq/m3, respectively.The activity of each nuclide in Shanghai was higher than that in Xiamen. The aerosol residence time (τPo-Pb) over Shanghai and Xiamen are 28-202d and 19-355d, respectively. In this paper, based on a one-dimensional simple aerosol deposition rate model, the atmospheric deposition fluxes of 210Pb, 210Bi and 210Po over Shanghai area into the East China Sea are estimated, and their variation ranges are 0.1-26.35Bq /m2/d, 0.04-7.91Bq /m2/d and 0.01-5.49 Bq /m2/d, respectively. The sedimentation fluxes of 210Po, 210Bi and 210Pb estimated based on the model are close to the actual observed values in the study area during the same period in winter within a certain range. The feasibility of estimating the deposition flux of nuclide into the sea with a simple one dimensional aerosol deposition rate model is verified.
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Key words:
- Nearshore region of the East China Sea /
- 210Po /
- 210Bi /
- 210Pb /
- Residence Time /
- Deposition Flux
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图 1 气溶胶中210Po和210Bi活度的联合分析流程
Fig. 1 Joint analysis of 210Po and 210Bi activity in aerosols
图 2 东海近岸（a）上海和（b）厦门地区气溶胶中210Po、210Bi和210Pb活度浓度随时间的变化关系
Fig. 2 Relationship of activities of 210Po, 210Bi and 210Pb in aerosols over Shanghai (a) and Xiamen (b) over the East China Sea with time
图 3 全球各采样站位秋冬季近地面气溶胶中210Po、210Bi和210Pb活度浓度分布
Fig. 3 Distribution of 210Po,210Bi,210Pb activity concentrations in near ground aerosols of global observation station during autumn and winter season
图 4 基于210Bi/210Pb和210Po/210Pb活度比估算的上海地区大气气溶胶颗粒物滞留时间（a）和基于210Po/210Pb活度比估算的厦门大气气溶胶颗粒物的滞留时间（b）
Fig. 4 Based on the activity ratios of 210Bi/210Pb and 210Po/210Pb, the residence times of atmospheric aerosol particles over (a) Shanghai and (b) Xiamen are estimated
图 5 210Pb沉降入海通量实测值与模拟值（当Vd =（1.0 ± 0.1）cm/s时进行模拟）趋势
Fig. 5 The trend diagram of the measured and simulated flux of 210Pb deposition into the sea (simulated when Vd =（1.0 ± 0.1）cm/s)
表 1 东海近岸近地面大气气溶胶中210Po、210Bi和210Pb的活度浓度及活度比
Tab. 1 Activities and activity ratios of 210Po, 210Bi and 210Pb in near-surface atmospheric aerosols over the East China Sea
东海近岸 样品名 采样时间 体积 TSP 210Po 210Bi 210Pb 210Po/210Pb 210Bi/210Pb m3 μg/m3 mBq/m3 mBq/m3 mBq/m3 上海地区 201609-SHA 2016年9月22-23日 1 642 170 0.92 ± 0.08 NA 3.23 ± 0.25* 0.28 ± 0.03 NA 201610-SHA 2016年10月17-18日 2 206 105 0.58 ± 0.03 0.62 ± 0.02 1.41 ± 0.14* 0.41 ± 0.05 0.44 ± 0.02 201611-SHA-1 2016年11月5-6日 2 571 137 0.59 ± 0.04 0.95 ± 0.03 2.00 ± 0.16* 0.30 ± 0.03 0.48 ± 0.02 201611-SHA-2 2016年11月14-15日 2 307 152 1.27 ± 0.10 1.83 ± 0.12 2.61 ± 0.18* 0.49 ± 0.05 0.70 ± 0.05 201611-SHA-3 2016年11月19-20日 1 462 251 0.83 ± 0.05 1.47 ± 0.07 2.75 ± 0.22* 0.30 ± 0.03 0.53 ± 0.03 201612-SHA-1 2016年12月5-6日 1 320 303 0.66 ± 0.09 NA 2.56 ± 0.18* 0.26 ± 0.04 NA 201612-SHA-2 2016年12月23-24日 1 440 316 0.77 ± 0.05 0.51 ± 0.03 6.10 ± 0.53* 0.13 ± 0.01 0.08 ± 0.01 201701-SHA-1 2017年1月3-4日 1 264 84 0.42 ± 0.03 0.59 ± 0.02 1.89 ± 0.15* 0.22 ± 0.02 0.31 ± 0.02 201701-SHA-2 2017年1月12-13日 1 200 101 0.16 ± 0.01 0.45 ± 0.03 1.40 ± 0.12* 0.11 ± 0.01 0.32 ± 0.03 201702-SHA 2017年2月23-24日 1 333 77 0.11 ± 0.01 NA 1.12 ± 0.10* 0.10 ± 0.01 NA 厦门地区 21XMA-1 2021年9月27-28日 1133 69 0.85 ± 0.04 2.52 ± 0.11 1.32 ± 0.10 0.78 ± 0.06 1.96 ± 0.18 21XMA-2 2021年10月2-3日 1 121 51 0.14 ± 0.01 1.29 ± 0.07 0.80 ± 0.06 0.19 ± 0.02 1.30 ± 0.12 21XMA-3 2021年10月5-6日 1 175 68 0.21 ± 0.01 0.83 ± 0.04 0.53 ± 0.04 0.43 ± 0.03 1.36 ± 0.13 21XMA-4 2021年10月10-11日 1 135 42 0.11 ± 0.01 NA NA NA NA 21XMA-5 2021年10月11-12日 1 263 98 0.08 ± 0.02 NA 0.17 ± 0.10 0.54 ± 0.12 NA 21XMA-6 2021年10月16-17日 1 206 80 0.05 ± 0.02 NA 0.26 ± 0.02 0.23 ± 0.07 NA 21XMA-7 2021年10月23-24日 1 222 23 0.09 ± 0.01 NA 0.41 ± 0.04 0.24 ± 0.03 NA 21XMA-8 2021年10月30-31日 1 484 81 0.10 ± 0.02 NA 1.07 ± 0.07 0.1 ± 0.02 NA 21XMA-10 2021年11月13-14日 1 589 56 0.16 ± 0.01 NA 0.93 ± 0.08 0.19 ± 0.02 NA 21XMA-11 2021年11月20-21日 1 520 123 0.13 ± 0.01 NA 0.76 ± 0.05 0.18 ± 0.02 NA 21XMA-12 2021年11月27-28日 1 620 40 0.06 ± 0.01 NA 0.50 ± 0.05 0.13 ± 0.01 NA 注：*气溶胶中210Pb的活度浓度引自文献[17]；NA表示“未获得”。 
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表 2 全球各地区气溶胶中210Po、210Bi和210Pb的活度浓度大小对比
Tab. 2 Comparison of 210Po activity, 210Bi activity and 210Pb activity in aerosols from different regions of the world
地区 海拔/m 年降水量/
mm观测时间 210Pb mBq/m3 210Bi mBq/m3 210Po mBq/m3 文献 范围 平均值 范围 平均值 范围 平均值 上海 ~20 1 260 2016年9月至2017年2月 1.12～6.10 2.51 ± 1.36 0.45～1.83 0.92 ± 0.50 0.11～1.27 0.63 ± 0.33 本文 厦门 ~15 1 464 2021年9-11月 0.17～1.24 0.67 ± 0.05 0.83～2.52 1.55 ± 0.82 0.06～0.97 0.21 ± 0.25 美国底特律 ~15 851 2017年9月至2018年1月 0.18～2.23 0.85 ± 0.49 0.06～0.81 0.35 ± 0.20 0.010～0.096 0.03 ± 0.019 文献[15] 美国橡树岭
国家实验室~25 - 1984年10月至1985年2月 0.14～0.27 0.19 ± 0.08 0.06～0.11 0.008 ± 0.06 - - 文献[22] 葡萄牙里斯本 25 1 000 1986年1月至1989年12月(秋冬季) 0.04～0.42 0.16 ± 0.09 0.01～0.27 0.12 ± 0.07 0.003～0.171 0.024 ± 0.01 文献[21] 印度坎普尔 ~142 810 2007年1月至2009年4月 0.50～4.80 1.80 ± 1.10 - - 0.002～0.28 0.094 文献[23] 美国波克福莱特 近地面 1 119 1996年1-2月 0.82～1.02 0.92 ± 0.10 - - 0.048～0.152 0.100 ± 0.052 文献[24] 伊格尔岛 美国 近地面 - 1996年1-3月 0.22～0.55 0.37 ± 0.12 - - 0.018～0.059 0.037 ± 0.015
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表 3 上海市气溶胶中210Pb的计算沉降入海通量与实测沉降通量及210Po和210Bi的沉降入海通量模拟值
Tab. 3 Calculated and measured deposition fluxes of 210Pb and simulated deposition fluxes of 210Po, 210Bi in aerosols in Shanghai
观测月份 Vd/(cm·s−1) 210Pb模拟值/(Bq·m−2·month−1) 210Pb实测值/(Bq·m−2·month−1) 210Po模拟值/(Bq·m−2·month−1) 210Bi模拟值/(Bq·m−2·month−1) 2016年9月 1.00 ± 0.25* 83.72 ± 20.39 NA 23.85 ± 2.90 NA 2016年10月 0.70 ± 0.18* 25.58 ± 9.13 28.76 ± 3.85 10.52 ± 1.05 11.25 ± 1.02 2016年11月 0.75 ± 0.19* 47.69 ± 11.32 47.67 ± 5.44 17.43 ± 1.93 27.54 ± 2.74 2016年12月 0.60 ± 0.15* 67.34 ± 16.83 69.64 ± 7.73 11.12 ± 1.44 7.93 ± 0.82 2017年1月 0.70 ± 0.28* 29.85 ± 14.07 45.01 ± 5.31 5.26 ± 0.58 9.43 ± 0.92 2017年2月 0.50 ± 0.13* 14.52 ± 3.77 16.11 ± 3.40 1.43 ± 0.18 NA 注：*气溶胶中210Pb沉降速率Vd引自文献[35]；210Pb沉降通量实测值引自文献[38]；NA表示“未获得”。
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