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Release of Natural Organic Matter Sorbed to Oxides and a Subsoil

K. Kaisera and W. Zecha

a Institute of Soil Science and Soil Geography, University of Bayreuth, D-95440 Bayreuth, Germany



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Fig. 1 Sorption of organic carbon (OC) to amorphous Al(OH)3, goethite, and the 3Bw horizon of an Oxyaquic Dystrochrept and the subsequent desorption by a solution of the same inorganic composition as the sorption solutions but without dissolved organic carbon (DOC). Sorption is given as the relationship between added and sorbed OC (initial pH = 4.0; ionic strength = 0.002 M)

 


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Fig. 2 Release of organic carbon (OC) freshly sorbed on amorphous Al(OH)3, goethite, and the 3Bw horizon of an Oxyaquic Dystrochrept by varying concentrations of NaCl (initial pH = 5.4)

 


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Fig. 3 Release of organic carbon (OC) freshly sorbed on amorphous Al(OH)3, goethite, and the 3Bw horizon of an Oxyaquic Dystrochrept by varying concentrations of Na2SO4 and NaH2PO4 (initial pH = 5.2)

 


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Fig. 6 Variation of the zeta potential ({Psi}{zeta}) of amorphous Al(OH)3 and goethite particles with increasing amounts of sorbed NOM (pH = 6.1; ionic strength = 0.002 M)

 


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Fig. 4 Release of organic carbon (OC) freshly sorbed on goethite and the 3Bw horizon of an Oxyaquic Dystrochrept at varying pH values

 


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Fig. 5 Sorption and desorption of organic carbon (OC) on amorphous Al(OH)3, goethite, and the 3Bw horizon of an Oxyaquic Dystrochrept. The sorption is given as the relationship between added and sorbed OC. The bars indicate subsequent desorption by different solutions for each dissolved organic carbon (DOC) addition. As the soil material contained indigenous OC, a line is given showing the course of soil OC content

 


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Fig. 7 Release of organic carbon (OC) sorbed on amorphous Al(OH)3 and goethite by 0.1 M Na2SO4 and 0.1 M NaH2PO4 at different times after the sorption. The time given on the x-axis is the residence time of the OC on the sorbent prior to the desorption. Error bars represent the standard deviation of three replicates

 


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Fig. 8 Sorption and desorption of the hydrophilic and hydrophobic organic carbon (OC) fraction on amorphous Al(OH)3 and goethite. The sorption is displayed as the relationship between added dissolved organic carbon (DOC) and sorbed OC. The bars indicate subsequent desorption by different solutions for each addition

 





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Copyright © 1999 by the Soil Science Society of America.