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- W2039748488 abstract "The first224Ra (t1/2 = 3.64days) measurements from mixing zones of estuarine systems are presented for the Pee Dee River-Winyah Bay and Delaware Bay Estuaries. High-resolution gamma-ray spectrometry was used to determine224Ra,228Ra (t1/2 = 5.7years), and226Ra (t1/2 = 1622years) activity ratios. Desorption and diffusion from suspended and bottom sediments contributes to the non-conservative increases of the three isotopes in each systems. In Delaware Bay224Ra concentrations were nearly constant over the 2.5‰ to 15‰ salinity range where two turbidity maximum zones are located.228Th scavenging onto the suspended particles in the turbid zones may supply a regenerative source of224Ra in this system. Samples collected on the ebb and flood tide from a salt marsh along Delaware Bay have a 5-fold increase in224Ra from flood to ebb and 3- and 2-fold increases for228Ra and226Ra respectively, indicating salt marshes are another source of radium to estuarine waters." @default.
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- W2039748488 date "1983-09-01" @default.
- W2039748488 modified "2023-10-14" @default.
- W2039748488 title "224Ra,228Ra, and226Ra in Winyah Bay and Delaware Bay" @default.
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- W2039748488 doi "https://doi.org/10.1016/0012-821x(83)90103-6" @default.
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