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Changes in Partitioning of Cadmium-109 and Zinc-65 in Soil as Affected by Organic Matter Addition and Temperature

Å.R. Almåsa, B. Salbub and B.R. Singha

a Agricultural University of Norway, Department of Soil and Water Sciences, Post Box 5028, 1432 Aas, Norway
b Agricultural University of Norway, Department of Chemistry and Biotechnology, Post Box 5026, 1432 Aas, Norway



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  		Fig. 1 Distribution of 109Cd and 65Zn in the three-component soil-soil water system model

 


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  		Fig. 2 The observed (symbols) and calculated (lines) distribution of 109Cd with time among the water-soluble, reversibly sorbed, and irreversibly sorbed fractions as affected by temperature (9 and 21°C) and the addition of organic matter (OM) (4%). Each symbol represents the mean of

 


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  		Fig. 3 The observed (symbols) and calculated (lines) distribution of 65Zn with time among the water-soluble, reversibly sorbed, and irreversibly sorbed fractions as affected by temperature (9 and 21°C) and the addition of organic matter (OM) (4%). Each symbol represents the mean of

 


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  		Fig. 4 Effects of temperature and organic matter addition (OM) on the time-dependent distribution coefficient Ki (L kg-1) for 109Cd and 65Zn

 




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