Th-234 and Be-7 as tracers for the sources of particles to the turbidity maximum of the Hudson River estuary

The natural radionuclides Th-234 (half-life=24.1 days) and Be-7 (half-life= 53.3 days) were measured in suspended particles of the turbidity maximum zo ne of the lower Hudson River estuary during several tidal cycles in August 1995 in an effort to understand the dynamics and sources of particles to th is zone. The relatively short half-lives and high particle reactivity of Th -234 and Be-7, coupled with the spatially variable production of Th-234 (fr om U-238, which varies conservatively with salinity in the Hudson), make th ese radionuclides useful tracers of particle dynamics. The activity ratio o f Th-234(xs)/Be-7 reduces the effects of particle type, concentration and s ize on the individual activities and serves as an indicator of where in the estuary the particles were labelled with these radionuclides. Detailed sam pling at three stations in the turbidity maximum during the course of a tid al cycle shows an average Th-234(xs)/Be-7 activity ratio of 1.9 +/- 0.7. Co mparable T-234(xs)/Be-7 ratios in suspended particles from surface and bott om water with different salinities indicate that particles are mixed throug hout the water column. Comparison of observed Th-234(xs)/Be-7 activity rati os with those calculated from models assuming that local processes dominate the tracer distributions suggests that particle residence times are short. However, the observed ratios are greater on average than those calculated, indicating the import of particles with higher ratios from the more saline reaches of the estuary. Estimates of the particle fluxes necessary to acco unt for the observed Th-234/Be-7 activity ratios suggest that about 30% of the flux could arise from advective transport of particles into the turbidi ty maximum zone in association with the tidal circulation and the remainder is supplied from local resuspension. A sensitivity analysis shows that the se estimates are dependent on the activity ratio in the suspended sediment reservoir and fluxes of radionuclides supplied by local resuspension. Varia bility in these factors gives rise to estimates of the advected flux that c an vary hom 24% to 59%. (C) 1999 Academic Press.