Sources, transport, and migration of 129I in the northern South China Sea
摘要
Rapid increased nuclear power plants along the cost in China, as well as intensive nuclear activities over the world has raised a big concern on the marine environmental safety. The distribution patterns and transport pathways of artificial radionuclides in the marginal seas of China is important for mitigating impact of radioactive pollution discharged to the seas. 129I is an excellent tracer for investigating the transport and diffusion of water-soluble radioactive pollutants in the marginal seas because of its long half-life, high solubility in seawater and conservative feature in the ocean. In this work, seawater samples were collected from surface and different depth in the stations in the northern South China Sea (NSCS) and analyzed for 129I and 127I using a sensitive analytical method established in our laboratory. The level and distribution of 129I in this region were obtained, and the sources, transport and migration of 129I in the NSCS were investigated. It was revealed that terrestrial input via rivers is the primary source of significantly higher 129I levels in the Pearl River estuary (with 129I/127I atomic ratios from 6.0×10−11 to 38×10−11, compared to (4.0–6.6)×10−11 in surface seawater in the open sea in this region). While, the level of stable iodine isotope (127I) was significantly lower in the estuary area compared to the open sea. The atomic ratios of 129I/127I peaked in the subsurface layer in the open sea in the NSCS. By estimating the distribution of 129I inventory in this sea area, the contributions of different input modes in this region were assessed to be in a order of the ocean current input>river input>direct atmospheric fallout. These results are useful for predicting the diffusion pathways and impacts of nuclear pollution in the event of accidents in marginal seas and for assessing environmental radiation safety.