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连云港田湾附近海域放射性核素扩散迁移研究

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基于有限体积海岸海洋模型(FVCOM),进行连云港田湾附近海域三维潮汐潮流数值模拟,并使用示踪剂模块和拉格朗日模块分析海域中放射性核素扩散迁移特性。研究结果表明:模拟结果与观测资料吻合度较高;海域潮汐类型为规则半日潮,模拟和观测的潮位平均误差的绝对值小于0。2 m;流速平均误差的绝对值小于0。02 m/s,最大误差在0。22 m/s左右,流向平均误差的绝对值小于7°,最大误差小于36°;受潮流和季风等的影响,放射性核素在初始时刻紧贴岸线呈现向北迁移,随着时间延长,出现回旋和逆向运动等多种现象;放射性核素扩散迁移到黄海和东海北部需要相对较长时间,对局部海域影响较大,而对黄海和东海北部海域影响相对较小。
Study on the diffusion and migration of radioactive nuclides in the sea area near Tianwan Bay,Lianyungang
A three-dimensional tidal current numerical simulation was conducted in the sea area near Tianwan Bay,Lianyungang using the finite volume coastal ocean model(FVCOM).Additionally,tracer and Lagrange modules were employed to investigate the characteristics of radioactive nuclide diffusion and migration,revealing the following findings:the simulation results exhibited a high level of agreement with observational data;the tidal regime in the study area was characterized as regular semidiurnal tides,with absolute value of average error of tide levels below 0.2 m;the absolute value of average error of velocity was below 0.02 m/s,with maximum error of about 0.22 m/s;absolute value of average error of flow direction was below 7°,with the maximum error below 36°.Influenced by tidal currents and seasonal monsoons,radioactive nuclides initially exhibited a northward migration trend,closely following the coastline at the beginning.Over time,various movement patterns,including recirculation and southward migration,emerged.The diffusion and migration of radioactive nuclides from their initial placement locations to the Yellow Sea and the northern East China Sea took a relatively long time,significantly impacting local coastal areas while having a lesser effect on the broader regions of the Yellow Sea and the northern East China Sea.

FVCOMradioactive nuclidediffusionmigration

张治钟、张江梅、张扬鑫、席发元

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西南科技大学国防科技学院,四川 绵阳 621010

国家原子能机构核环境安全技术创新中心,四川 绵阳 621010

西南科技大学信息工程学院,四川 绵阳 621010

有限体积海岸海洋模型 放射性核素 扩散 迁移

国防基础科研项目国防基础科研项目

JCKY2020404C004JCKY2022404C005

2024

环境污染与防治
浙江省环境保护科学设计研究院

环境污染与防治

CSTPCD北大核心
影响因子:0.79
ISSN:1001-3865
年,卷(期):2024.46(10)