Temperature Regime of Chernozems of Southern and Meadow-Chernozem Soils of the Ishim Steppe
Yu. V. Kravtsov
Abstract
The temperature regime of chernozems of southern and meadow-chernozem soils of the Ishim steppes characterized by an increased (to the level of the lowest moisture capacity) moisture of subsoil layer depending little on the ground water level and an absolute dominance of absorbed hardly movable humidity has been studied