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Title: Vertical transport processes of an acid-iron waste in a MERL stratified mesocosm

Journal Article · · Environ. Sci. Technol.; (United States)
DOI:https://doi.org/10.1021/es00143a007· OSTI ID:6128244

The vertical transport of the Fe particles formed after an acid-Fe waste mixes with seawater and the impact of the waste on the trace metal composition of seawater were examined in a stratified tank (2 m diameter and 5 m deep) at the MERL facility of the University of Rhode Island. Two acid-Fe waste additions were made to one of the stratified tanks at concentrations comparable to those observed after the initial dispersion of the waste in the ocean (10/sup 5/ dilution); a second stratified tank was maintained as a control. The removal of the Fe waste from the water column was due to settling of the Fe particles through the pycnocline; biological transport of the Fe particles was not an important removal mechanism. The kinetic behavior of the Fe particles was different after the two waste additions; gravitational settling was the rate-limiting step after the first addition, whereas flocculation was the rate-limiting step after the second waste addition. The first acid-Fe waste addition apparently altered the properties of the seawater, possibly stripping organic substances from the water column. This alteration in the characteristics of seawater changed the distribution of Pb and V between the dissolved and particulate forms. Both Pb and V showed a strong correlation with Fe, suggesting scavenging of these metals by the Fe particles. Cu and Cd show remarkable independence from the behavior of Fe. 18 references, 6 figures, 5 tables.

Research Organization:
Univ. of Rhode Island, Kingston
OSTI ID:
6128244
Journal Information:
Environ. Sci. Technol.; (United States), Vol. 20:1
Country of Publication:
United States
Language:
English