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DIVISION S-2 - SOIL CHEMISTRY

Nature of Clay-Humic Complexes in an Agricultural Soil

I. Chemical, Biochemical, and Spectroscopic Analyses

^a USDA-ARS, National Soil Tilth Lab., 2150 Pammel Drive, Ames, IA 50011
^b USDA-ARS, Southwest Watershed Research Center, 2000 E. Allen Road, Tucson, AZ 85719-1596
^c Dep. of Plant and Soil Sciences, Mississippi State Univ., P.O. Box 9555, Mississippi State, MS 39762

* Corresponding author (laird{at}nstl.gov)

Soil management systems that encourage the formation and stabilization of recalcitrant clay–humic complexes will have the greatest long-term impact on C sequestration and soil quality. The objective of this study was to determine the relationship between the chemical, biochemical, and spectroscopic characteristics of humic substances and clay mineralogy. Clay–humic complexes were separated from the Ap horizon of a Webster soil (fine-loamy, mixed, superactive Typic Endoaquoll) by an invasive sonication–centrifugation technique. The samples were analyzed for mineralogy by XRD (x-ray diffraction), chemical composition by inductively coupled plasma-atomic emission spectorscopy (ICP-AES), C and N by thermal combustion, C chemistry by solid state ¹³C magic angle spinning-nuclear magnetic resonance spectroscopy (MAS-NMR) and both gas chromatography (GC) and high performance liquid chromatography (HPLC) analyses of extractable organic compounds. The coarse, medium, and fine clay fractions are dominated by quartz, a low-charged interstratified phase, and smectite, respectively. Extractable organic compounds, 30 to 52% of the total C, are dominated by basic amino acids and polyunsaturated fatty acids. Less than 3% of the extractable C is monosaccharides and amino sugars and only trace levels of phenolic acids were found. The C/N ratios of humic substances associated with the coarse, medium, and fine clay fractions are 17, 10, and 10, respectively. The coarse clay fraction has stronger carboxyl and O-alkyl ¹³C-NMR peaks and lower levels of extractable amino acids, fatty acids, monosaccharides, and amino sugars than humics associated with the fine clay fraction. The results indicate that the biochemistry of the clay–humic complexes differs substantially from that of whole soils and that soil clay mineralogy strongly influences humification.

Abbreviations: CEC, cation-exchange capacity • FAME, methylated fatty acids • GC, gas chromatography • HPLC, high performance liquid chromatography • ICP-AES, inductively coupled plasma-atomic emission spectroscopy • MAS-NMR, magic angle spinning-nuclear magnetic resonance spectroscopy • OC, organic C • OM, organic matter • XRD, x-ray diffraction

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