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Influence of Soil Geochemical and Physical Properties on the Sorption and Bioaccessibility of Chromium(III)

M. A. Stewarta, P. M. Jardine*,a, M. O. Barnettb, T. L. Mehlhorna, L. K. Hydera and L. D. McKayc

a Environ. Sci. Div., Oak Ridge, TN 37831-6038
b Dep. of Civil Engineering, 208 Harbert Engineering Center, Auburn Univ., AL 36849-5337
c Dep. of Geological Sciences, Univ. of Tennessee, Knoxville, TN 37996-1410




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Fig. 1. Percentage Cr(III) bioaccessibility after 1 and 100 d Cr-soil aging for (a) Ulitisols; (b) Alfisols; (c) Inceptisols; (d) Spodosols, Mollisols, Entisols; and (e) Aridisols.

 


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Fig. 2. The observed (data points) and model fitted (grid surface) relationship between the two most significant independent variables (% clay and TIC) and % Cr(III) bioaccessibility using the model: % Cr(III) bioaccessible = 16.02 + (0.426 x % clay) - (9.56 x % TIC) an r2 value of 0.722.

 


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Fig. 3. The observed (data points) and model fitted (grid surface) relationship between the two independent variables (% clay and TOC) and % Cr(III) bioaccessibility using the model: % Cr(III) bioaccessible = 15.54 + (0.408 x % clay) - (3.78 x % TOC) with an r2 value of 0.674.

 





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The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
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Soil Science Society of America Journal
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