Message Board

Respected readers, authors and reviewers, you can add comments to this page on any questions about the contribution, review, editing and publication of this journal. We will give you an answer as soon as possible. Thank you for your support!

Full name
E-mail
Phone number
Title
Message
Verification Code
Turn off MathJax
Article Contents
Zhou Wenqing,Zhong Qiangqiang,Zhou Yuehua, et al. Biogeochemical behaviors of 210Po, 210Bi, and 210Pb in the East China Sea close to the Changjiang Estuary during a spring red tide event[J]. Haiyang Xuebao,2025, 47(x):1–11 doi: 10.12284/hyxb2024-00
Citation: Zhou Wenqing,Zhong Qiangqiang,Zhou Yuehua, et al. Biogeochemical behaviors of 210Po, 210Bi, and 210Pb in the East China Sea close to the Changjiang Estuary during a spring red tide event[J]. Haiyang Xuebao,2025, 47(x):1–11 doi: 10.12284/hyxb2024-00

Biogeochemical behaviors of 210Po, 210Bi, and 210Pb in the East China Sea close to the Changjiang Estuary during a spring red tide event

doi: 10.12284/hyxb2024-00
  • Received Date: 2024-04-03
  • Rev Recd Date: 2024-10-29
  • Available Online: 2025-02-20
  • The 210Bi-210Pb radionuclide pair is considered to be a new radiotracer for particulate carbon dynamics. Due to the very short half-life of 210Bi and the difficulty of determination, we have very few knowledge about the biogeochemical behavior of 210Bi in the ocean and whether there is a 210Bi-210Pb activity disequilibrium. This paper reported the observation results of dissolved and particulate 210Po, 210Bi, and 210Pb and their activity ratios in seawaters in the East China Sea close to the Changjiang Estuary during a red tide event on the spring scientific cruise from May 5 to 15, 2017. The results showed that the 210Po/210Pb activity ratio varied from 0.20 to 2.08, with an average of 0.82±0.58 (n=15) and the 210Bi/210Pb activity ratio changed between 0.31 and 3.72, showing an average of 1.38±0.79 (n=15). This phenomenon indicates that the activity disequilibrium of 210Po-210Pb and 210Bi-210Pb was ubiquitous in the seawater. More specifically, there is an obvious 210Po and 210Bi excess relative to 210Pb in deep seawater, which implied that 210Po and 210Bi might be released from sinking particles in the middle and deep layer of water column. By calculating the distribution coefficients and fractionation factors of 210Po, 210Bi, and 210Pb, it was found that suspended particles in seawater tended to preferentially scavenge and remove 210Po and 210Bi, comparing with 210Pb. Similar to 210Po, 210Bi showed a stronger particle affinity for marine suspended particles than 210Pb, and the increase of phytoplankton biomass can promote the fractionation behavior between 210Bi and 210Pb, supporting the idea that 210Bi-210Pb can be used to trace particle processes in the ocean.
  • loading
  • [1]
    Liu Qian, Guo Xianghui, Yin Zhiqiang, et al. Carbon fluxes in the China Seas: an overview and perspective[J]. Science China Earth Sciences, 2018, 61(11): 1564−1582. doi: 10.1007/s11430-017-9267-4
    [2]
    Zhou Kuanbo, Dai Minhan, Maiti K, et al. Impact of physical and biogeochemical forcing on particle export in the South China Sea[J]. Progress in Oceanography, 2020, 187: 102403. doi: 10.1016/j.pocean.2020.102403
    [3]
    Fowler S W, Teyssie J L, Church T M. Scavenging and retention of bismuth by marine plankton and biogenic particles[J]. Limnology and Oceanography, 2010, 55(3): 1093−1104. doi: 10.4319/lo.2010.55.3.1093
    [4]
    Wang Jinlong, Zhong Qiangqiang, Baskaran M, et al. Investigations on the time-series partitioning of 210Pb, 207Bi and 210Po between marine particles and solution under different salinity and pH conditions[J]. Chemical Geology, 2019, 528: 119275. doi: 10.1016/j.chemgeo.2019.119275
    [5]
    Yang Weifeng, Tian Jie, Chen Min, et al. A new radiotracer for particulate carbon dynamics: examination of 210Bi-210Pb in seawater[J]. Geochemistry, Geophysics, Geosystems, 2022, 23(12): e2022GC010656. doi: 10.1029/2022GC010656
    [6]
    刘新成, 沈焕庭, 黄清辉. 长江入河口区生源要素的浓度变化及通量估算[J]. 海洋与湖沼, 2002, 33(3): 332−340. doi: 10.3321/j.issn:0029-814X.2002.03.014

    Liu Xincheng, Shen Huanting, Huang Qinghui. Concentration variation and flux estimation of dissolved inorganic nutrient from the Changjiang River into its estuary[J]. Oceanologia et Limnologia Sinica, 2002, 33(3): 332−340. doi: 10.3321/j.issn:0029-814X.2002.03.014
    [7]
    Zhu Jianrong, Wang Jinhui, Shen Huanting, et al. Observation and analysis of the diluted water and red tide in the sea off the Changjiang River mouth in middle and late June 2003[J]. Chinese Science Bulletin, 2005, 50(3): 240−247. doi: 10.1007/BF02897534
    [8]
    周名江, 颜天, 邹景忠. 长江口邻近海域赤潮发生区基本特征初探[J]. 应用生态学报, 2003, 14(7): 1031−1038. doi: 10.3321/j.issn:1001-9332.2003.07.001

    Zhou Mingjiang, Yan Tian, Zou Jingzhong. Preliminary analysis of the characteristics of red tide areas in Changjiang River estuary and its adjacent sea[J]. Chinese Journal of Applied Ecology, 2003, 14(7): 1031−1038. doi: 10.3321/j.issn:1001-9332.2003.07.001
    [9]
    于仁成, 张清春, 孔凡洲, 等. 长江口及其邻近海域有害藻华的发生情况、危害效应与演变趋势[J]. 海洋与湖沼, 2017, 48(6): 1178−1186.

    Yu Rencheng, Zhang Qingchun, Kong Fanzhou, et al. Status, impacts and long-term changes of harmful algal blooms in the sea area adjacent to the Changjiang River estuary[J]. Oceanologia et Limnologia Sinica, 2017, 48(6): 1178−1186.
    [10]
    Zhou Zhengxi, Yu Rencheng, Zhou Mingjiang. Seasonal succession of microalgal blooms from diatoms to dinoflagellates in the East China Sea: a numerical simulation study[J]. Ecological Modelling, 2017, 360: 150−162. doi: 10.1016/j.ecolmodel.2017.06.027
    [11]
    赵艳民, 秦延文, 张雷, 等. 基于GIS的近30年长江口及其邻近海域赤潮时空分布特征研究[J]. 海洋科学, 2021, 45(12): 39−46.

    Zhao Yanmin, Qin Yanwen, Zhang Lei, et al. Temporal and spatial distribution of red tides in the Changjiang estuary and in adjacent waters from 1989 to 2019[J]. Marine Sciences, 2021, 45(12): 39−46.
    [12]
    Zhong Qiangqiang, Puigcorbé V, Sanders C, et al. Analysis of 210Po, 210Bi, and 210Pb in atmospheric and oceanic samples by simultaneously auto-plating 210Po and 210Bi onto a nickel disc[J]. Journal of Environmental Radioactivity, 2020, 220-221: 106301. doi: 10.1016/j.jenvrad.2020.106301
    [13]
    Rigaud S, Puigcorbé V, Cámara-Mor P, et al. A methods assessment and recommendations for improving calculations and reducing uncertainties in the determination of 210Po and 210Pb activities in seawater[J]. Limnology and Oceanography: Methods, 2013, 11(10): 561−571. doi: 10.4319/lom.2013.11.561
    [14]
    Baskaran M, Church T, Hong G, et al. Effects of flow rates and composition of the filter, and decay/ingrowth correction factors involved with the determination of in situ particulate 210Po and 210Pb in seawater[J]. Limnology and Oceanography: Methods, 2013, 11(3): 126−138. doi: 10.4319/lom.2013.11.126
    [15]
    Waples J T. Measuring bismuth-210, its parent, and daughter in aquatic systems[J]. Limnology and Oceanography: Methods, 2020, 18(4): 148−162. doi: 10.1002/lom3.10352
    [16]
    钟强强. 核素大气沉降过程及其对上层海洋POC输出通量研究的启示[D]. 上海: 华东师范大学, 2020.

    Zhong Qiangqiang. Atmospheric deposition of radionuclides and its application in POC export fluxes of the upper sea[D]. Shanghai: East China Normal University, 2020.
    [17]
    Waples J T. Bismuth-210, its parent, and daughter and their use as particle tracers in aquatic systems[J]. Marine Chemistry, 2022, 239: 104072. doi: 10.1016/j.marchem.2021.104072
    [18]
    Tateda Y, Carvalho F P, Fowler S W, et al. Fractionation of 210Po and 210Pb in coastal waters of the NW Mediterranean continental margin[J]. Continental Shelf Research, 2003, 23(3/4): 295−316.
    [19]
    Zhong Qiangqiang, Wang Jinlong, Du Jinzhou, et al. The 210Po/210Pb disequilibrium in a spring-blooming marginal sea, the Southern Yellow Sea[J]. Journal of Environmental Radioactivity, 2019, 207: 15−26. doi: 10.1016/j.jenvrad.2019.05.017
    [20]
    Tang Yi, Stewart G, Lam P J, et al. The influence of particle concentration and composition on the fractionation of 210Po and 210Pb along the North Atlantic GEOTRACES transect GA03[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2017, 128: 42−54. doi: 10.1016/j.dsr.2017.09.001
    [21]
    Honeyman B D, Balistrieri L S, Murray J W. Oceanic trace metal scavenging: the importance of particle concentration[J]. Deep Sea Research Part A. Oceanographic Research Papers, 1988, 35(2): 227−246. doi: 10.1016/0198-0149(88)90038-6
    [22]
    Mudbidre R, Baskaran M, Schweitzer L. Investigations of the partitioning and residence times of Po-210 and Pb-210 in a riverine system in Southeast Michigan, USA[J]. Journal of Environmental Radioactivity, 2014, 138: 375−383. doi: 10.1016/j.jenvrad.2014.01.007
    [23]
    Biggin C D, Cook G T, MacKenzie A B, et al. Time-efficient method for the determination of 210Pb, 210Bi, and 210Po activities in seawater using liquid scintillation spectrometry[J]. Analytical Chemistry, 2002, 74(3): 671−677. doi: 10.1021/ac0107599
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(6)  / Tables(3)

    Article views (13) PDF downloads(6) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return