Abstract

The distribution of 210 Po and 210 Pb (grand daughter–parent) in the dissolved and total (dissolved+particulate) phase of sea water samples has been measured in the upper 500 m at four stations along a western transect in the South-equatorial Atlantic. Such a transect allows one to make inference about the particle-associated scavenging processes in the equatorial versus subtropical regions of the South Atlantic. A common feature of the 210 Po profiles is that the dissolved activities in the surface waters are about one-third of the equilibrium concentrations, suggesting weeks to a month removal times of 210 Po by adsorption on settling particles. The mean dissolved 210 Po / 210 Pb activity ratios in the equatorial and South Atlantic are 0.27 and 0.39, respectively, representing a pronounced disequilibrium in surface waters. The box-model calculation yields a residence time of about 73 and 130 days for dissolved 210 Po in the surface water at the equatorial and southern sites, respectively. The gross deficiency of 210 Po extends throughout the upper 500 m; however, the 210 Po residence time in the intermediate depths is longer than that in surface water. The observed 210 Po – 210 Pb disequilibrium has been examined with respect to POC concentration, which yields a significant positive correlation ( r 2=0.61), suggesting that the 210 Po deficiency is mainly associated with biological removal. The 210 Pb distribution shows distinctively higher concentrations in the equatorial surface waters (19–22 dpm/100 l), suggesting an enhanced atmospheric flux of 210 Pb . The residence time of dissolved 210 Pb (400–780 days), with respect to atmospheric input, is longer than dissolved 210 Po and 234 Th residence times, and also shows a latitudinal decrease toward the equator in the surface ocean. The shorter residence time in the surface equatorial ocean (0–20 m) seems associated with higher productivity and more rapid particulate scavenging.

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