The flux of 226Ra from estuarine and continental shelf sediments

@inproceedings{Li1977TheFO,
  title={The flux of 226Ra from estuarine and continental shelf sediments},
  author={Yuan-hui Li and G. G. Mathieu and Pierre Eginton Biscaye and H. James Simpson},
  year={1977}
}
A pronounced desorption phenomenon of 226 Ra from sediment was observed in the Hudson River estuary. Mass balance calculations indicate that the desorption of 226 Ra from the river-borne sediment in estuarine environment is an important source of 226 Ra to the oceans. 

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