ВЛАГООБЕСПЕЧЕННОСТЬ ТРАВЯНИСТОГО ПОКРОВА В УСЛОВИЯХ ДЕНДРАРИЯ И ЕЕ ОСОБЕННОСТИ

Abstract

From the analysis of the actual data, it follows that at the beginning of June 2014, there was a significant moistening of the humus horizon of Chernozem under the grass cover. But at the end of the month, the amount of available moisture decreased sharply and continued to decrease during July and August. This led to a shortage of water reserves, which could only be compensated by irrigation. 2016 was generally wetter, although the moisture content in the upper humus horizon was low when it emerged from winter in may. The drop in humidity in Chernozem continued until mid-June, when the ELVs decreased to unsatisfactory values. Since the end of June, regular precipitation has dramatically increased the available moisture reserves, remaining very good until the end of the growing season. As a result, a significant deficit of productive moisture was observed only in late may and early June. In June 2017, the productive moisture reserves in the humus-accumulative horizon were satisfactory. But in the illuvial horizon, the moisture reserves were estimated to be good, which did not require irrigation.