A. Miltner et al., SOIL ORGANIC-MATTER COMPOSITION IN 3 HUMUS PROFILES OF THE WESTERN TAURUS, TURKEY, AS REVEALED BY WET CHEMISTRY AND CP MAS C-13 NMR-SPECTROSCOPY/, Zeitschrift fur Pflanzenernahrung und Bodenkunde, 159(3), 1996, pp. 257-262
In this study three soil profiles located in the Western Taurus (Turke
y) at different altitudes (10, 1900, and 3080 m a.s.l.) were compared
with respect to their soil organic matter characteristics. The soil sa
mple were fractionated by density to plant residues, slightly altered
plant material,organo-mineral complexes, and organic-free minerals. Bu
lk samples and fractions were analyzed for C and N, the bulk samples a
dditionally for total sugars, lignin signature, and bulk soil organic
matter composition by CP/MAS C-13 NMR spectroscopy. The first step of
litter decomposition and humification is a very strong degradation of
polyaccharides without the loss of O-alkyl structures. This process is
slowing down very fast and the polysaccharides are stabilized. Lignin
is decomposed as fast or even faster than polysaccharides. The data o
btained by wet-chemical analysis and by NMR spectroscopy are not or on
ly weakly correlated to each other. This leads to the conclusion that
the two types of methods give complementary rather than equivalent inf
ormation. For the study of soil organic matter it is important to comb
ine different methods and to draw the advantages of either type.