SSSAJ Journal of Natural Resources and Life Sciences Education
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Published online 11 September 2009
Published in Soil Sci Soc Am J 73:1831-1842 (2009)
DOI: 10.2136/sssaj2008.0254
© 2009 Soil Science Society of America
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SOIL CHEMISTRY

Soil Properties Controlling the Adsorption of Dissolved Organic Carbon to Mineral Soils

D. N. Kothawalaa,*, T. R. Moorea and W. H. Hendershotb

a Dep. of Geography and Global Environmental & Climate Change Center (GEC3), McGill Univ., 805 Sherbrooke St. West, Montréal, QC, H3A 2K6 Canada
b Dep. of Natural Resource Sciences, Macdonald Campus, McGill Univ., 21, 111 Lakeshore Rd., Ste-Anne-de-Bellevue, Montréal, QC, Canada

* Corresponding author (dollykothawala{at}trentu.ca).

Dissolved organic C (DOC) is the most reactive and mobile component of soil C and can be retained within mineral soils by adsorption. We determined the adsorption characteristics for 52 mineral soil samples from 17 temperate and boreal soil profiles, using a modified Langmuir equation. The DOC solution used for batch experiments was derived from the organic horizons of a Spodosol. We analyzed the extent to which soil properties, such as the sum of poorly crystalline Fe and Al (Fepc + Alpc), texture, and soil C, are related to DOC adsorption to mineral soils. Sorption characteristics including the maximum adsorption capacity (Qmax), and the null point (np), where adsorption equals desorption, were best explained by Fepc + Alpc (R2 = 0.55 and 0.28, respectively). The Alpc exerted a stronger influence than Fepc on Qmax. A simple method for estimating Qmax was developed whereby the change in pOH after treatment with NaF is well correlated to Fepc + Alpc (R2 = 0.71, P < 0.0001) and Qmax (R2 = 0.50, P < 0.0001). The influence of clay content on Qmax was of secondary importance and was largely masked by the dominant influence of Fepc + Alpc. Soil C did not have any influence on Qmax, but a slight negative influence on np. The B horizons of Spodosols and volcanic soils had the greatest Qmax, while large levels of soil C in Spodosols produced a high desorption potential. Results from this study emphasize the importance of considering the adsorption potential in conjunction with the desorption potential for better prediction of changes to the size of mineral soil C pools and DOC export to aquatic systems.

Abbreviations: Alo, oxalate-extractable aluminum • Alp, pyrophosphate-extractable aluminum • Alpc, poorly crystalline aluminum • Cp, pyrophosphate-extractable carbon • DOC, dissolved organic carbon • ECEC, effective cation exchange capacity • Fecry, crystalline iron • Fed, dithionite-extractable iron • Feo, oxalate-extractable iron • Fep, pyrophosphate-extractable iron • Fepc, poorly crystalline iron • IM, initial mass • SMR, stepwise multiple regression







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