Sm. Aguilera et al., ORGANIC-MATTER IN VOLCANIC SOILS IN CHILE - CHEMICAL AND BIOCHEMICAL-CHARACTERIZATION, Communications in soil science and plant analysis, 28(11-12), 1997, pp. 899-912
Determinations were made of total soil organic matter (SOM), stable an
d labile organic fractions, biomass carbon (C), and chemical compositi
on of several humus-soil-fractions in chilean volcanic soils, Andosols
and Ultisols. Their physico-chemical Properties and humification degr
ee at different stages in edaphic evolution were also assessed. In add
ition, organic matter models were obtained by chemical and biological
syntheses and the structures and properties of natural and synthetic h
umic materials were compared with SOM. Results indicate that Andosols
have higher SOM levels than Ultisols, but the fraction distribution in
the latter suggests a shift of the more stable fractions to the more
labile ones. Moreover, contents of humines, and humic and fulvic acids
suggest that Chilean volcanic soil SOM is highly humified. On the oth
er hand, among the SOM labile fractions, carbohydrate and biomass are
about 15% of the SOM which are one of the most important fractions in
soil fertility.