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Published online 1 May 2008
Published in Soil Sci Soc Am J 72:586-594 (2008)
DOI: 10.2136/sssaj2007.0030
© 2008 Soil Science Society of America
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Fractional Availability of Smectite Surfaces in Soils for Adsorption of Nitroaromatic Compounds in Relation to Soil and Solute Properties

Simone M. Charles, Brian J. Teppen, Hui Li and Stephen A. Boyd*

Department of Crop and Soil Sciences, Michigan State Univ., East Lansing, MI 48824


Figure 1
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Fig. 1. Sorption isotherms of p-nitrocyanobenzene (p-NCB), 2,4-dinitrotoluene (DNT), and 1,4-dinitrobenzene (DNB) by K+– and Mg2+–saturated Webster A horizon soil (WA) and Webster A horizon soil from which soil organic matter was removed (WAO).

 

Figure 2
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Fig. 2. Sorption isotherms of p-nitrocyanobenzene (p-NCB), 2,4-dinitrotoluene (DNT), and 1,4-dinitrobenzene (DNB) by K+– and Mg2+–saturated Webster B horizon soil (WB) and Webster B horizon soil from which soil organic matter was removed (WBO).

 

Figure 3
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Fig. 3. Sorption isotherms of p-nitrocyanobenzene (p-NCB), 2,4-dinitrotoluene (DNT), and 1,4-dinitrobenzene (DNB) by K+– and Mg2+–saturated Clarion A horizon soil (CLA) and Clarion A horizon soil from which soil organic matter was removed (CAO).

 

Figure 4
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Fig. 4. Sorption isotherms of p-nitrocyanobenzene (NCB), 2,4-dinitrotoluene (DNT), and 1,4-dinitrobenzene (DNB) by K+– and Mg2+–saturated Clarion B horizon soil (CLB) and Clarion B horizon soil from which soil organic matter was removed (CBO).

 

Figure 5
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Fig. 5. Sorption isotherms of p-nitrocyanobenzene (p-NCB), 2,4-dinitrotoluene (2,4-DNT), and 1,4-dinitrobenzene (1,4-DNB) by K+–beidellite. Isotherms with different letters are statistically different at {alpha} = 0.05.

 

Figure 6
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Fig. 6. Sorption isotherms of 1,3,5-trinitrobenzene (TNB) by K+– and Mg2+–saturated Webster B horizon soil (WB) and Webster B horizon soil from which soil organic matter was removed (WBO).

 





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