Distribution and flux of 226Ra and 228Ra in the Amazon River estuary.

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Abstract

Measurements show that desorption from river-borne suspended particulate matter in the estuary increases the riverine flux of both isotopes to the ocean by a factor of approximately 5 over the flux attributable to radium dissolved in the river water alone. -from Authors

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Key, R. M., Stallard, R. F., Moore, W. S., & Sarmiento, J. L. (1985). Distribution and flux of 226Ra and 228Ra in the Amazon River estuary. Journal of Geophysical Research, 90(C4), 6995–7004. https://doi.org/10.1029/JC090iC04p06995

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