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Assessment of snow accumulation and justification of parameters of stubble coulisses in the arid steppe of Northern Kazakhstan

The main limiting factor for increasing yields in the conditions of the arid steppe of Northern Kazakhstan is moisture. The accumulation of moisture during winter precipitation for plants in arid conditions in the initial stage of the growing season was a serious production problem. | Assessment of snow accumulation and justification of parameters of stubble coulisses in the arid steppe of Northern Kazakhstan International Journal of Mechanical Engineering and Technology IJMET Volume 10 Issue 03 March 2019 pp. 1392 1405 Article ID IJMET_10_03_140 Available online at http www.iaeme.com ijmet issues.asp JType IJMET amp VType 10 amp IType 3 ISSN Print 0976-6340 and ISSN Online 0976-6359 IAEME Publication Scopus Indexed ASSESSMENT OF SNOW ACCUMULATION AND JUSTIFICATION OF PARAMETERS OF STUBBLE COULISSES IN THE ARID STEPPE OF NORTHERN KAZAKHSTAN Vladimir Leonidovich Astafyev Pavel Grigoryevich Ivanchenko and Vladimir Viktorovich Kirkilevskiy Kostanay branch of LLC Scientific Production Center of Agricultural Engineering Kazakhstan 110011 Kostanay Abai Avenue 34 ABSTRACT The main limiting factor for increasing yields in the conditions of the arid steppe of Northern Kazakhstan is moisture. The accumulation of moisture during winter precipitation for plants in arid conditions in the initial stage of the growing season was a serious production problem. For four years the accumulation of snow and the amount of water in the snow were compared over the backgrounds of ordinary stubble tall stubble left after stripper header continuous combing and stubble coulisses. Research methods included field observations and mathematical modeling. It has been established that the water reserves in the snow depend on the height of stubble coulisses as well as the density of snow in the coulisses and in between the spaces. Studies of snow accumulation on stubble coulisses continuous combing and ordinary stubble showed that the density of snow between the coulisses is 9-29 higher than the density in the coulisses and the density of snow between the coulisses is 25-63 higher than the density in the stubble or continuous combing. The explanation of this phenomenon was the hypothesis that the dispersal of snow blizzards occurred between the coulisses due to this snow .