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北部湾沉积物中放射性核素的分布特征与控制因素
引用本文:林武辉,冯禹,余克服,蓝文陆,莫珍妮,宁秋云,冯亮亮,何贤文. 北部湾沉积物中放射性核素的分布特征与控制因素[J]. 海洋学报, 2020, 42(2): 143-154. DOI: 10.3969/j.issn.0253-4193.2020.02.015
作者姓名:林武辉  冯禹  余克服  蓝文陆  莫珍妮  宁秋云  冯亮亮  何贤文
作者单位:1.广西大学 海洋学院,广西 南宁 530004
基金项目:国家自然科学基金(91428203,41906043);广西“珊瑚礁资源与环境”八桂学者项目(2014BGXZGX03);广西自然科学基金(2017GXNSFBA198096,2019GXNSFAA185006);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(GCMAC1606)。
摘    要:北部湾是我国大西南地区重要的海上通道,也是我国重要的渔场之一。本研究利用高纯锗γ谱仪系统分析北部湾表层和柱状沉积物中4种最主要的天然放射性核素(238U、226Ra、228Ra、40K)含量和分布特征。结果显示,北部湾沉积物中放射性核素含量低于我国大部分海域的结果,高于珊瑚礁区的极低放射性水平的结果。北部湾沉积物中4种核素都存在"蝴蝶"状空间分布特征,该特征主要源于沉积物粒径的非线性调控,且与沉积物总有机碳浓度存在正相关。此外,利用Mn和210Pb所指示的氧化还原状态和物理/生物扰动过程也可以对柱状沉积物中氧化还原敏感型核素(比如,238U)分布产生一定的影响。本文从232Th/238U、40K/238U、226Ra/238U活度比值角度,发现北部湾沉积物具有典型的陆源沉积物特征,且显著不同于南海珊瑚礁区中生源沉积物特征。本研...

关 键 词:放射性核素  核电站  氧化还原敏感型元素  地球化学指标  沉积
收稿时间:2019-04-25
修稿时间:2019-07-03

Characteristics of radionuclides in sediments collected from the Beibu Gulf and influence factors
Lin Wuhui,Feng Yu,Yu Kefu,Lan Wenlu,Mo Zhenni,Ning Qiuyun,Feng Liangliang and He Xianwen. Characteristics of radionuclides in sediments collected from the Beibu Gulf and influence factors[J]. Acta Oceanologica Sinica (in Chinese), 2020, 42(2): 143-154. DOI: 10.3969/j.issn.0253-4193.2020.02.015
Authors:Lin Wuhui  Feng Yu  Yu Kefu  Lan Wenlu  Mo Zhenni  Ning Qiuyun  Feng Liangliang  He Xianwen
Affiliation:1.School of Marine Sciences, Guangxi University, Nanning 530004, China2.Guangxi Laboratory on the Study of Coral Reefs in the South China Sea, Guangxi University, Nanning 530004, China3.Marine Environmental Monitoring Center of Guangxi, Beihai 536000, China4.Guangxi Academy of Oceanography, Nanning 530022, China5.Radiation-Environment Management and Monitoring Station of Guangxi Zhuang Autonomous Region, Nanning 530222, China
Abstract:The Beibu Gulf is not only a key sea passage in the southwestern China but also one of important fishing grounds in the South China Sea (SCS). In this study, naturally occurring radionuclides (238U, 226Ra, 228Ra, and 40K) in surface sediments and sediment cores of the Beibu Gulf were comprehensively analyzed using high purity germanium (HPGe) γ spectrometry. Our results indicated that radioactivity level of sediments in the Beibu Gulf was lower than that in most of China's seas and was higher than the extremely low radioactivity level of sediments in coral reefs. All nuclides in surface sediments of the Beibu Gulf had a spatial distribution of “butterfly pattern”, attributing to the non-linear regulation of sediment grain size and positive role of total organic carbon in sediment. Additionally, redox state and physical/biological disturbance derived from the proxies of Mn and 210Pb could also affect vertical distribution of redox-sensitive nuclide (eg, 238U) in sediment cores. On the basis of the 232Th/238U, 40K/238U, and 226Ra/238U activity ratio, we found that sediments of the Beibu Gulf had terrigenous characteristics, which were significantly different from biogenic sediments in coral reefs. Our study provided radioactivity level in the Beibu Gulf under the background of the rapid development of nuclear power plant, revealed the "butterfly pattern" of radionuclides and their influence factors, and explored the feasibility of novel geochemical proxies based on radionuclides in marine sedimentation.
Keywords:radionuclide  nuclear power plant  redox-sensitive element  geochemical proxy  sedimentation
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