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Effects of Organic Amendments on the Reduction and Phytoavailability of Chromate in Mineral Soil

N. S. Bolan*,a, D. C. Adrianob, R. Natesana and B.-J. Koob

a Soil & Earth Science Group, Massey Univ., Palmerston North, New Zealand
b Savannah River Ecology Laboratory, Drawer E, Aiken, SC 29802



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Fig. 1. Amounts of Cr(VI) reduced during the incubation of Cr(VI) with the unamended and amended soils (•, soil; {blacktriangleup}, soil + horse manure; {diamondsuit}, soil + farm yard manure; {Delta}, soil + fish manure; {circ}, soil + spent mushroom; {square}, soil + pig manure; {blacksquare}, soil + poultry manure; {diamond}, soil + biosolid compost). Fitted curves are shown as solid lines.

 


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Fig. 2. Relationship between Cr(VI) reduction and (a) easily oxidizable organic carbon and (b) dissolved organic carbon in the unamended and amended soils.

 


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Fig. 3. Relationships between (a) Cr(VI) reduction and pH of the unamended and amended soils and (b) theoretical and measured amounts of protons consumed during Cr(VI) reduction.

 


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Fig. 4. (a) Dry matter yield of mustard plants and (b) the concentration of total Cr in plant tissue at various levels (g organic carbon kg-1 soil) of biosolid compost addition (•, 0; {blacktriangleup}, 25; {diamond}, 50; {diamondsuit}, 100).

 


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Fig. 5. Relationships between dry matter yield and (a) soil solution Cr(VI) concentration and (b) plant tissue total Cr concentration.

 





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