CHARACTERIZATION OF SOLID AND DISSOLVED CARBON IN A SPRUCE-FIR SPODOSOL

Organic substances are an integral part of the biogeochemistry of many elements in forest ecosystems. However, our understanding of the comp osition, chemistry, and reactions of these materials are incomplete an d sometimes inconsistent. Therefore, we examined in detail dissolved o rganic carbon (DOC) in forest floor leachates over a two-year period ( 1992-1993), soil C, and DOC adsorption by a mineral soil to determine the relationship between soil solid and solution C characteristics in a spruce-fir ecosystem. The structural composition of DOC, DOC fractio ns (hydrophobic and hydrophilic acids, hydrophilic neutrals), and soil samples from the organic and mineral horizons were also analyzed usin g C-13 nuclear magnetic resonance (NMR) spectroscopy. Total DOC in for est floor leachates ranged from 7.8 to 13.8 mmol L(-1) with an average of 8.6 mmol L(-1). Concentrations were highest in September of both 1 992 and 1993. Fractionation of the forest floor DOC indicated these so lutions contained high organic acid contents that averaged 92% of the total DOC. Hydrophobic acids were also preferentially adsorbed by the B horizon. The C-13 NMR data suggested alkyl, carbohydrate, aromatic, and carboxylic C were the primary constituents for organic and mineral soils, DOC, and DOC fractions. Compositional changes of C were observ ed as aromatic and carbohydrate decreased, whereas alkyl, methoxy, and carbonyl moieties increased with depth. However, C composition change d little among the three organic layers based on the similarity of alk yl/carbohydrates ratios as determined from NMR area integration, sugge sting that in this acid soil, decomposition proceeds rather slowly. Hy drophobic acids contained high contents of aromatic C, whereas hydroph ilic acids were comprised primarily of carboxylic C. Hydrophilic neutr als were rich in carbohydrate C. Results indicated that these DOC frac tions were unaltered during the isolation process. Carboxylic C groups appeared to dissolve easily and were probably the primary contributor to organic acidity in our organic dominate leachates. Results also su ggested that DOC materials adsorbed on the B horizon underwent further biodegradation. Several seasonal patterns of C composition were obser ved in the forest floor leachates and DOC fractions collected between 1992 and 1993. Overall, the evidence from this study suggested that (i ) DOC levels were mainly controlled by biological activity, (ii) fores t floor DOC was comprised primarily of organic acids, (iii) contact of soil leachates with B horizon material affected DOC quantitatively an d qualitatively, (iv) phenolic, carboxylic, and carbonyl C appeared to dissolve readily in the forest Oa horizon, (v) DOC materials adsorbed on the B horizon selectively underwent further decomposition, and (vi ) C composition is a function of the extent of decomposition and DOC f ractions.