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Title: Spatial variations of particle scavenging rates within the central and northern Adriatic Sea: use of U--Th disequilibria

Conference ·
OSTI ID:664596

Dissolved and particlulate Thorium-234 ({sup 234}Th) were measured in near surface waters from the Central and Northern Adriatic Sea in order to gain an insight into the intensity and variability of active scavenging and particle removal processes. Dissolved {sup 234}Th to Uranium-238 ({sup 238}U) activity ratios vary from 0.21 to 0.75 and clearly imply that {sup 234}Th is being actively scavenged from sea water on a timescale of <3 months. The scavenging rate of dissolved {sup 234}Th with respect to scavenging onto particles appears to correlate with primary productivity measurements. Scavenging and rapid removal of particulate {sup 234}Th from the water column is best explained by a mechanism of zooplankton grazing and fecal pellet production. At one sight in the Jabuka Pit, particulate {sup 234}Th residence times below the pycnocline are long (30-40 days) suggesting that particles are being more readily recycled at these depths. By comparison, in a seawater profile collected near the Po outflow region, {sup 234}Th is depleted with respect to {sup 238}U through the entire water column. We conclude from this assessment that particles in waters near the Po River outflow will be more efficiently transported to bottom sediments compared with those in deeper waters over the Jabuka Pit.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE Assistant Secretary for Environment, Safety, and Health, Washington, DC (United States)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
664596
Report Number(s):
UCRL-JC-123865-Rev.1; CONF-9604130-; ON: DE98057885; BR: HD2006400
Resource Relation:
Conference: EEC conference on physical and biogeochemical processes of the Adriatic Sea, Ancona (Italy), 23-27 Apr 1996; Other Information: PBD: 1 Apr 1998
Country of Publication:
United States
Language:
English