Slightly or moderately developed soils (Entisols, Inceptisols) prevail because of the erosion and climate. In the more developed soils the organic matter induces a higher evolution of phyllosilicates with a better habitat for plants. Mollisols have a more stable structure, meanwhile mudflow hazard exists for Alfisols on marls and conglomerates.
Genesi e caratteri chimici, mineralogici e strutturali dei suoli marginali dell'Appennino Lucano
ZANINI, Ermanno;BONIFACIO, Eleonora;Boero, V.
1995-01-01
Abstract
Slightly or moderately developed soils (Entisols, Inceptisols) prevail because of the erosion and climate. In the more developed soils the organic matter induces a higher evolution of phyllosilicates with a better habitat for plants. Mollisols have a more stable structure, meanwhile mudflow hazard exists for Alfisols on marls and conglomerates.
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