The properties of the litter significantly change with the distance fr
om the tree trunk to the ''clearing'' of the parcella. Its thickness a
nd weight decrease, and the share of the ''active'' fraction of litter
fall increases. Conditions for more complete humification are formed.
Ash content and P and K supplies increase, but supplies of N, Ca, and
Mg decrease. The transect method makes it possible to account efficien
tly for these peculiarities and to obtain representative data on the c
omposition and features of the litter.