CHERNOZEMS HUMUS STATE FEATURES DURING FALLOW LAND DEVELOPMENT

Abstract

The purpose of the study is to determine the direction of change in the humus state of fallow soils in the forest-steppe zone when they are re-involved in arable land. The studies were carried out in the Kras-noyarsk forest-steppe during three growing seasons of 2015–2017 when the forb-grass deposit is replaced at the turf stage by agrocenosis of wheat and then by agrocenosis of pea-oat grass mixture. A distinctive feature of the process of involving fallow land in arable land was the chemical treatment of plants before plowing. Research has established that when the fallow is treated with herbicides and subsequent plowing, the sod horizon disappears, the amount of plant residues decreases sharply, the humus horizon differen¬tiates into arable and subarable with different densities, and blocky and dusty aggregates appear. The humus content under the long-term fallow land and during its plowing was high and amounted to 9.4–9.3 %; no decrease in humus was detected in the first two years after plowing, but the enrichment of humus with nitrogen decreased from an average to a very low level. The content of mobile humus in the soil under the long-term fallow land was 951 mg/100 g; when the fallow was plowed, it decreased to 346 mg/100 g. At the same time, the potential emission of carbon dioxide from agrochernozem increa¬sed – from 5.5 to 18.5 mg CO2 /10 g, which had an average inverse relationship with the SpO content (r = 0.56). It has been established that with intensive agrotechnical influence with the use of chemicals to destroy the turf horizon, the share of SPOs from Shumus decreases by more than 2.8 times due to its mineralization.