Particulate transport of radionuclides 14C and 55Fe to deep waters in the Pacific Ocean

Lal, D. ; Somayajulu, B. L. K. (1977) Particulate transport of radionuclides 14C and 55Fe to deep waters in the Pacific Ocean Limnology & Oceanography, 22 (1). pp. 55-59. ISSN 0024-3590

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Official URL: http://www.jstor.org/pss/2834870

Abstract

Observations during 1969-1971 indicate that radionuclides 14C and 55Fe in particulates in Pacific Ocean Water 28-31°N, 119-121°W up to depths of 2,500 m were transported from the surface within a short time ( < 10 yr). The mean downward sinking rates for 55Fe and 14C are deduced to be 0.5×10−3 and 2.5×10−3 cm s−1. The appreciably faster transport of 14 C is consistent with the fact that the mean size calculated for biogenic calcareous particles transporting 14C is larger than that for the 55Fe-labeled particles.

Item Type:Article
Source:Copyright of this article belongs to American Society of Limnology and Oceanography.
ID Code:49768
Deposited On:21 Jul 2011 10:17
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