Mm. Sarin et al., Po-210 and Pb-210 in the South-equatorial Atlantic: distribution and disequilibrium in the upper 500 m, DEEP-SEA II, 46(5), 1999, pp. 907-917
Citations number
14
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
The distribution of Po-210 and Pb-210 (grand daughter-parent) in the dissol
ved 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 t
he 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 Po-210
profiles is that the dissolved activities in the surface waters are about o
ne-third of the equilibrium concentrations, suggesting weeks to a month rem
oval times of Po-210 by adsorption on settling particles. The mean dissolve
d Po-210/Pb-210 activity ratios in the equatorial and South Atlantic are 0.
27 and 0.39, respectively, representing a pronounced disequilibrium in surf
ace waters. The box-model calculation yields a residence time of about 73 a
nd 130 days for dissolved Po-210 in the surface water at the equatorial and
southern sites, respectively. The gross deficiency of Po-210 extends throu
ghout the upper 500 m; however, the Po-210 residence time in the intermedia
te depths is longer than that in surface water. The observed Po-210-Pb-210
disequilibrium has been examined with respect to POC concentration, which y
ields a significant positive correlation (r(2) = 0.61), suggesting that the
Po-210 deficiency is mainly associated with biological removal.
The Pb-210 distribution shows distinctively higher concentrations in the eq
uatorial surface waters (19-22 dpm/1001), suggesting an enhanced atmospheri
c flux of Pb-210. Th, residence time of dissolved Pb-210 (400-780 days), wi
th respect to atmospheric input, is longer than dissolved Po-210 and Th-234
residence times, and also shows a latitudinal decrease toward the equator
in the surface ocean. The shorter residence time in the surface equatorial
ocean (0-20m) seems associated with higher productivity and more rapid part
iculate scavenging. (C) 1999 Elsevier Science Ltd. All rights reserved.