海洋沉积过程的铀系放射性核素示踪技术:物源识别、沉积、再悬浮

林武辉, 余克服, 王英辉, 刘昕明, 陈立奇. 海洋沉积过程的铀系放射性核素示踪技术:物源识别、沉积、再悬浮[J]. 海洋地质与第四纪地质, 2020, 40(1): 60-70. doi: 10.16562/j.cnki.0256-1492.2018092001
引用本文: 林武辉, 余克服, 王英辉, 刘昕明, 陈立奇. 海洋沉积过程的铀系放射性核素示踪技术:物源识别、沉积、再悬浮[J]. 海洋地质与第四纪地质, 2020, 40(1): 60-70. doi: 10.16562/j.cnki.0256-1492.2018092001
LIN Wuhui, YU Kefu, WANG Yinghui, LIU Xinming, CHEN Liqi. Using uranium-series radionuclides as tools for tracing marine sedimentary processes: Source identification, sedimentation rate, and sediment resuspension[J]. Marine Geology & Quaternary Geology, 2020, 40(1): 60-70. doi: 10.16562/j.cnki.0256-1492.2018092001
Citation: LIN Wuhui, YU Kefu, WANG Yinghui, LIU Xinming, CHEN Liqi. Using uranium-series radionuclides as tools for tracing marine sedimentary processes: Source identification, sedimentation rate, and sediment resuspension[J]. Marine Geology & Quaternary Geology, 2020, 40(1): 60-70. doi: 10.16562/j.cnki.0256-1492.2018092001

海洋沉积过程的铀系放射性核素示踪技术:物源识别、沉积、再悬浮

  • 基金项目: 国家重大科学研究计划项目“南海珊瑚礁对多尺度热带海洋环境变化的响应、记录与适应对策研究”(2013CB956102);国家自然科学基金“珊瑚礁千米深钻记录的西沙碳酸盐台地形成演化和环境变迁史”(91428203),“南海造礁珊瑚对海洋人工放射性核素90Sr源汇过程的指示作用研究”(41906043);广西“珊瑚礁资源与环境”八桂学者(2014BGXZGX03);广西自然科学基金面上项目“北部湾海洋沉积物中放射性核素的分布格局和调控机制研究”(2019GXNSFAA185006);国家海洋局海洋-大气化学与全球变化重点实验室开放基金“造礁珊瑚对海水中人工放射性核素90Sr的指示作用研究”(GCMAC1606)
详细信息
    作者简介: 林武辉(1987—),男,博士,主要研究海洋过程的同位素示踪、海洋放射性监测与评价,E-mail: linwuhui8@163.com
    通讯作者: 余克服(1969—),男,教授,主要从事珊瑚礁地质与生态环境研究,E-mail: kefuyu@scsio.ac.cn
  • 中图分类号: P736.21

Using uranium-series radionuclides as tools for tracing marine sedimentary processes: Source identification, sedimentation rate, and sediment resuspension

More Information
  • 放射性核素示踪技术被广泛应用于海洋学研究。海洋沉积物是许多物质的归宿,海洋沉积过程的研究常关注3个关联问题:物质来源、沉积速率、再悬浮过程。针对这3个问题,在南海9个珊瑚礁区、北部湾涠洲岛海域、珠江口、北冰洋、南大洋等多个海区利用典型的铀系放射性核素(210Pb、226Ra、234Th、238U)示踪技术开展海洋沉积过程研究。物源识别方面,研究发现珊瑚礁区沉积物具有极低的226Ra/238U活度比值(<0.1),显著低于其他海区的226Ra/238U活度比值(0.5~1.0),该独特性质可以应用于珊瑚礁区的沉积物/悬浮物来源示踪,是其他传统元素地球化学方法(Al、Ti、稀土元素)的补充。沉积速率方面,基于210Pb的恒定通量恒定沉积速率(Constant Flux Constant Sedimentation Model, CFCS)模式,定量计算了广西涠洲岛珊瑚礁区沉积柱样的沉积速率(3.7±0.6 mm/a),该结果低于中国多个近岸海域的沉积速率(5~96 mm/a)。沉积物再悬浮方面,提出利用“残余234Th”(不同于过剩234Th)示踪海洋沉积物再悬浮过程,并成功应用于北冰洋、南海、南大洋。

  • 加载中
  • 图 1  放射性核素示踪技术在海洋过程研究中的典型应用

    Figure 1. 

    图 2  海洋沉积物采样站位分布和对应的沉积物中226Ra和238U活度

    Figure 2. 

    图 3  广西涠洲岛珊瑚礁区沉积物柱状样的站位图与过剩210Pb活度自然对数计算后的垂直分布

    Figure 3. 

    图 4  北冰洋陆架区(a)、南海珠江口陆架区(b)、南大洋陆架区(c)不同站位的残余234Th(RAP234)剖面图

    Figure 4. 

    图 5  北冰洋SR3站位的海水浊度与残余234Th剖面图对比

    Figure 5. 

    图 6  北冰洋颗粒有机碳(POC)和残余234Th(RAP234)相关性分析

    Figure 6. 

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出版历程
收稿日期:  2018-09-20
修回日期:  2019-01-03
刊出日期:  2020-02-25

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