HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Related articles in JEQ Similar articles in this journal Similar articles in ISI Web of Science Similar articles in PubMed Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via ISI Web of Science (7) Citing Articles via Google Scholar Google Scholar Articles by Sowder, A. G. Articles by Morris, P. J. Search for Related Content PubMed PubMed Citation Articles by Sowder, A. G. Articles by Morris, P. J. GeoRef GeoRef Citation Agricola Articles by Sowder, A. G. Articles by Morris, P. J. Related Collections Mixed Wastes Radionuclides Heavy Metals

TECHNICAL REPORTS
Heavy Metals in the Environment

Partitioning and Availability of Uranium and Nickel in Contaminated Riparian Sediments

^a Savannah River Ecology Laboratory, The Univ. of Georgia, Drawer E, Aiken, SC 29802
^b Marine Biomedicine and Environmental Sciences, Medical Univ. of South Carolina, Charleston, SC 29425

^* Corresponding author (bertsch{at}srel.edu)

Received for publication March 4, 2002. The effects of iron oxides and organic matter on the partitioning and chemical lability of U and Ni were examined for contaminated riparian sediments from the U.S. Department of Energy's Savannah River Site. In sequential extractions of four sediments that ranged from 12.7 to 82.2 g kg^-1 in organic carbon, U was found almost exclusively in moderately labile fractions (93% in acid-soluble + organically bound). Nickel was distributed across all operationally defined fractions, including substantial amounts in the very labile fractions (4–15% in water-soluble + exchangeable), noncrystalline and crystalline iron oxides (38–49%), and in the nonlabile residual fraction (25–34%). Aqueous U concentrations in 1:1 sediment–water extracts were highly correlated to dissolved organic carbon (DOC) (R² = 0.96; p < 0.0001) and ranged from 29 to 410 µg L^-1. Aqueous concentrations of Ni exceeded U by two to three orders of magnitude (124–2227 µg L^-1) but were not correlated with DOC (R² = 0.04; p = 0.53). Partitioning and solubility trends suggest that Ni availability is controlled primarily by iron-oxide phases, whereas U availability is dominated by naturally occurring organic carbon. Discrete mineral phases were also identified as nonlabile reservoirs of anthropogenic metals. In spite of comparably high sediment concentrations, Ni appears to be significantly more available than U in riparian sediments and therefore warrants greater consideration in terms of environmental consequences (i.e., transport, biological uptake, and toxicity).

Abbreviations: AA, acid-soluble fraction • AO, noncrystalline iron-oxide fraction • CD, crystalline iron-oxide fraction • CN, exchangeable fraction • DW, water-soluble fraction • DOC, dissolved organic carbon • EDX, energy dispersive X-ray • HA, manganese-oxide fraction • HF, residual fraction • PP, organically bound fraction • SEM, scanning electron microscope • SOC, sediment organic carbon • SRS, Savannah River Site

Related articles in JEQ:

This Issue in Journal of Environmental Quality

JEQ 2003 32: 745-750. [Full Text]  

This article has been cited by other articles:

				T. Punshon, A. Lanzirotti, S. Harper, P. M. Bertsch, and J. Burger Distribution and Speciation of Metals in Annual Rings of Black Willow J. Environ. Qual., June 7, 2005; 34(4): 1165 - 1173. [Abstract] [Full Text] [PDF]