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Iron oxide forms and heavy metal transformations in sulfaquepts in Baltimore Harbor dredged materials

Thesis/Dissertation ·
OSTI ID:6653723
In contract to many soils, acid ammonium oxalate extractable Fe (Fe{sub o}) was commonly greater than dithionite extractable Fe (Fe{sub d}) in samples of these soils. Apparently as a result of lateral Fe movement, the upper part of one profile contained up to 165 g/kg of total Fe and 122 g/kg of oxalate extractable Fe. Experiments showed that the high Fe{sub o}/Fe{sub d} ratios in these soils may be related to their high organic matter and ferrous-Fe contents as well as to poor crystallinity of Fe oxides and extraction of jarositic Fe of the oxidized zone and Fe monosulfides from reduced zone samples by oxalate with these soils. An incubation experiment was conducted to identify effects of temperature, shaking conditions, and time on the extractability of Fe, Mn, Zn, Cu, Cr, Ni, Pb, and Cd forms in samples from oxidized and reduced zones of the higher elevation profile. Sequential extractions of water (soluble), DTPA (exchangeable and organically complexes), acid ammonium oxalate (Fe oxide associated), and H{sub 2}O{sub 2} (sulfide-bound) were used. As evidence by slight decrease in pH with time and shaking and the presence of some H{sub 2}O{sub 2} extractable metals, the oxidized zone apparently still contains some sulfide-bound metals. Water soluble contents of Mn, Cr, Ni, Pb, and Cd of shaken-reduced zone samples increased with time. Water soluble Mn and Cd in these samples increased from 54 and 0.010 mg/kg to 654 and 0.127 mg/kg, respectively, when they were incubated at 32 C for 7 weeks. Sulfide-bound metals of reduced zone samples transformed to mobile and Fe oxide associated forms with shaking and time. Sulfide-bound Mn under these conditions converted mainly to mobile forms and partly to Fe oxide associated forms.
Research Organization:
Maryland Univ., College Park, MD (USA)
OSTI ID:
6653723
Country of Publication:
United States
Language:
English