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Distribution and budget of (137)Cs in the China Seas

Cesium–137 is one of the most abundant anthropogenic radionuclides released by atmospheric nuclear testing and nuclear accidents, and accordingly it may significantly impact the health of humans and marine environmental eco–systems. Documenting the distribution and inventory of (137)Cs is thus a cru...

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Detalles Bibliográficos
Autores principales: Wu, Junwen, Xiao, Xiyu, Sun, Jiang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7260368/
https://www.ncbi.nlm.nih.gov/pubmed/32472036
http://dx.doi.org/10.1038/s41598-020-65280-x
Descripción
Sumario:Cesium–137 is one of the most abundant anthropogenic radionuclides released by atmospheric nuclear testing and nuclear accidents, and accordingly it may significantly impact the health of humans and marine environmental eco–systems. Documenting the distribution and inventory of (137)Cs is thus a crucial task. In this study, we collected a large number of datasets with field observations of (137)Cs in the China Seas, in order to provide an in–depth understanding of (137)Cs budgets and distributions. The activity and inventory of (137)Cs in China Seas’ sediments showed large spatial variations, related to the (137)Cs source, sedimentation rates and the mineral composition of sediments. The (137)Cs concentration in sediments decreased with distance from the shore, generally tracing the distribution of sedimentation rates. High (137)Cs inventories in the water column indicated a high solubility and long mean residence times. The mean residence times of (137)Cs in the China Seas were determined to be 45.6 ± 3.8 years for the South China Sea (SCS), 36.8 ± 3.1 years for the East China Sea (ECS), and 12.0 ± 1.0 years for the Yellow Sea (YS). A (137)Cs mass balance suggests that oceanic input from the north Pacific is the dominant (137)Cs source to the China Seas, contributing about 96.9% of this substance. Furthermore, the bulk of (137)Cs remains dissolved in the SCS water column, while (137)Cs is mostly deposited to the sediments of the ECS and the YS. This new compilation of the activity level and inventory of (137)Cs help to establish background levels for future (137)Cs studies in the China Seas.