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Title: Metal enrichment processes in the marine environment

Thesis/Dissertation ·
OSTI ID:6851713

This study discusses metal enrichment in oceanic sediments resulting from remobilization, scavenging, pollution and hydrothermal inputs in the Mississippi River-Gulf of Mexico and Mid-Atlantic Ridge at 26/sup 0/N. Suspended particles collected from the Mississippi River during mean water and suspended-sediment discharge have metal concentrations which vary by <5% for Al, Cd, Cu, Fe, Pb, and Zn and approx.10% for Mn. The massive sediment load carried by the Mississippi River is rapidly deposited on the Mississippi Delta in the Gulf of Mexico. Aluminum and Fe concentrations in Mississippi Delta sediments are similar to those of average Mississippi River suspended matter throughout the delta. In contrast, the Cu/Al ratio in surficial sediments (0-1 cm) decreases from 4.1 x 10/sup -4/ for average suspended matter to 2.7 x 10/sup -4/ about 45 km from the mouth of Southwest Pass. Copper lost from delta sediments can be traced to the deep Gulf of Mexico where concentrations average 50-70 ..mu..g g/sup -1/ compared with 33 ..mu..g g/sup -1/ for Mississippi River suspended matter. The observed increase in offshore sediments in linked to scavenging of Cu by particles. A similar scenario can be presented for Mn.

Research Organization:
Florida Inst. of Tech., Melbourne (USA)
OSTI ID:
6851713
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English