Distribution of 226Ra and 210Pb in the mixed layer of the western equatorial Pacific Ocean

1997 ◽  
Vol 48 (5) ◽  
pp. 371 ◽  
Author(s):  
Philip H. Towler ◽  
J. David Smith

The residence time of particulate and dissolved 210Pb in the upper layer of the western equatorial Pacific Ocean is examined. Activities of dissolved 226Ra, dissolved and particulate 210Pb, and particulate 210Po were determined to a depth of 300 m in a series of depth profiles collected along a transect across the equator at 155˚E in November 1993. Total 210Pb in the surface water decreased from 2·7 Bq m-3 at 10˚N to 1·8 Bq m-3 at 10˚S. Dissolved 210Pb generally decreased with depth but showed subsurface (100–150 m) maxima at 10˚N and 5˚N. The nutrient concentrations at 300 m were highest at these stations, suggesting some degree of upwelling. Calculations indicate that the residence times of dissolved (<0·45 µm) and particulate (>0·45 µm) 210Pb in the top 300 m were 4·6–9·6 years and 0·15–0·29 year respectively.

2000 ◽  
Vol 51 (7) ◽  
pp. 647 ◽  
Author(s):  
Gillian A. Peck ◽  
J. David Smith

The distribution of the radionuclides 226Ra, 210Pb and 210Po in the dissolved (<0.45 µm) and 210Pb and 210Po in the particulate (>0.45 µm) phases was measured in the upper 300 m of the Bismarck Sea off the Sepik River and along the equator from 143˚E to 152˚E in the western equatorial Pacific Ocean. 210Pb and 210Po occurred principally in the dissolved phase with a 210Po/210Pb ratio <1. Particulate matter had 210Po/210Pb ratios greater than 1.0. Box model calculations yielded an average atmospheric flux of 210Pb of 4.5 mBq cm-2 year-1 to the ocean surface. The average residence times for dissolved 210Po and dissolved 210Pb were 0.27 years and 8.0 years respectively (in the mixed layer) and 1.45 years and 170 years (in the deeper layer). With an average residence time of 0.08 0.03 years, particulate 210Po varied little between the layers. The difference in 210Po and 210Pb residence times reflects the greater particle reactivity of 210Po. The flux of particulate organic carbon was calculated to be 104 21 mg m-2 day-1 from the upper 100 m and 180 22 mg m-2 day-1 from 100–300 m.


Nature ◽  
1986 ◽  
Vol 323 (6088) ◽  
pp. 523-526 ◽  
Author(s):  
G. Meyers ◽  
J. R. Donguy ◽  
R. K. Reed

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