Characteristics of soil organic matter (SOM) extracted using base with subsequent pH lowering and sequential pH extraction

Humic substances from eight soils of varying properties were extracted by two different methods: (1) the traditional NaOH-extraction with subsequent acidification to different pH (∼1 to ∼12) and sequential extractions using 0.01 M NaNO3 at incremental pH (∼1 to ∼11). Cumulative organic matter (OM) in the sequential extractions showed properties that were consistent with NaOH-extracted OM. The release of Al and Fe in the sequential extractions was closely related with the release of organic carbon (OC). The ratio of OC associated with humic acid (HA) and fulvic acid (FA) (the HA : FA ratio) varied widely among the soils indicating heterogeneity in their OM composition. However, a significant correlation between this HA : FA ratio and the NaOH extractable %OC content of the soils is indicative of the possible relationship between them. Between pH 5 and 7, which is a typical soil solution pH, a significant amount of HA-associated OC was soluble. In modeling metal speciation in soil solutions, it has been assumed that all dissolved organic carbon (DOC) that is active toward metal binding is associated with FA. The results of this study indicate that the validity of these assumptions based on model sensitivity alone is questionable.