The input and decomposition of plant remains in agroecosystems have been st
udied in the Krasnoyarsk region, Central Siberia. The annual input of plant
remains into the plow layer of chernozems varies from 3 to 8 t/ha under ce
real crops (wheat) and from 8 to 15 t/ha under perennial grasses. From 15 t
o 55% of this amount gets into the soil during the growing season before ha
rvest. The synthesis of new humic substances compensates for nitrogen uptak
e by plants from labile organic compounds and ensures the accumulation of n
itrogen in the humus pool of soils.