Copper and Zinc Speciation in the Solution of a SoilSludge Mixture
R. Vulkan*,a,
U. Mingelgrinb,
J. Ben-Ashera and
H. Frenkelc
a The Wyler Department of Dryland Agriculture, The Jacob Blaustein Institute for Desert Research, Ben-Gurion University, Sede Boqer Campus 84990, Israel
b Institute of Soils, Water and Environmental Sciences, The Volcani Center, ARO, P.O.B. 6, Bet Dagan 50250, Israel
c Institute of Soils, Water and Environmental Sciences, The Volcani Center, ARO, P.O.B. 6, Bet Dagan 50250, Israel

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Fig. 1. Gel chromatogram of the aqueous extract of the sludge (2:25 sludge to water ratio). (A) Dissolved organic carbon (DOC) and Cu concentrations in leachates of the gel column as a function of the inverse logarithmic function of the molecular weight (Kav). (B) Molecular weight as a function of Kav.
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Fig. 2. Concentration of Cu (A) and dissolved organic carbon (DOC) (B) in effluents from gel chromatography columns. Samples of 2 mL sludge extract (sludge to water ratio 2:25) or of dilutions of that extract to ratios of 1:50 and 1:100 sludge to water, respectively, were applied to the column in each run.
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Fig. 3. Effect of incubation time on the molecular weight (MW) distribution of dissolved organic carbon (DOC) species in a 1:1 water extract of soil loaded with 20% sludge. Kav is the inverse logarithmic function of the molecular weight.
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Fig. 4. Effect of incubation time on the molecular weight (MW) distribution of Cu species in a 1:1 water extract of soil loaded with 20% sludge. Kav is the inverse logarithmic function of the molecular weight.
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Fig. 5. Effect of incubation time on the distribution of Cu species according to their charge in a water extract of the sewage sludge.
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Fig. 6. Effect of incubation time on the distribution of Zn species according to their charge in a water extract of the sewage sludge.
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Copyright © 2002 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.