name
Belyuchenko Ivan Stepanovich
Scholastic degree
•
Academic rank
professor
Honorary rank
—
Organization, job position
• Kuban State Agrarian University
профессор
Research interests
Web site url
—
—
Current rating (overall rating of articles)
0
TOP5 co-authors
Articles count: 38
Сформировать список работ, опубликованных в Научном журнале КубГАУ
-
SOIL DEGRADATION AND THE ROLE OF FOREST BELTS IN LAND MELIORATION
DescriptionSoil degradation (erodere – eat away, lat.) - a process when pieces of rocks and soil are separated from their initial location. Then transferred and deposited in some new place. The factors of erosion are water, wind, landslides, rock particles and etc. Erosion is the process of destruction and demolition of the soil cover (or parent rocks) by flows of water or wind which causes depletion of fertile top soil layer. The destruction of this layer occurs quickly, and for its restoration thousand years are required. Reduction of soil fertility is one of the main problems that are associated with its pollution. Erosion is a natural process that occurs very slowly ever since the Earth was formed (about 45-50 billion years ago). Realistically, mountains, valleys, plains and deltas on the Earth's surface have been created by water and wind erosion as a result of their joint action over a long period of time. Geological erosion was acted at a slow pace for hundreds of years. When humans appeared it occurred to be an invasion of species which could transform their natural environment. An artificial type of erosion, which acts much faster than the natural erosion, was formed because of human
-
Description
The article considers the peculiarities of turf and sod, specificity of formation of kidneys for regeneration, types of shoots, vegetative mobility and specificity of growth in certain conditions, turf grasses are divided into loosely-and tightly-turf characterized, by specific features of environmental, biological characteristics; forming turf from generative rosettes, elongated and shortened vegetative, side ground shoots, differing specificity of morphological, biochemical and fitocoenotical features
-
DIAGEOTROPIC SHOOTS OF PERENNIAL GRASSES IN THE SOUTHERN REGIONS OF THE CIS
DescriptionStudying of perennial cereals of southern and boreal origin led to the allocation of plagiotropic shoots of rhizomes, stolons, that are placed in the soil or on the surface from the apical or lateral kidney of various structures with modified leaves, the beginnings of roots at nodes and developing of type kidney - lengthened shoots. Two types was allocated: type of solid finned cylinder and type of intermittent cylinder with scattered around the periphery of vascular bundles: first include cereals temperate regions and is characterized by separation from the epidermis continuous sclerenchyma ring, the second type (sorghum and millet) no continuous mechanical ring and vascular bundles relatively evenly spaced along the periphery of the shoots
-
DISPERSITY OF WASTES AND THEIR PROPERTIES
DescriptionDispersity of wastes of all productions including domestic, agricultural, industrial and violations of the natural systems which are heterogeneous and dispersed formations comprising two or more phases with the developed surface is discussed. Disperse systems of wastes are classified into true solutions, systems of finely dispersed of colloids, coarsely dispersed (mainly mineral wastes) and highly dispersed (organic waste)
-
06.00.00 Agricultural sciences
DescriptionDispersed colloidal particles pertaining to positive colloids is played important role in the process of the interaction of organic wastes (sewage sludge, defeca-tion mud, chicken manure, etc.) with various wastes of mineral raw materials (phosphogypsum, lime powder, halite, etc.)
-
FORMS OF PERENNIAL GRASSES WITH RHIZOMES
DescriptionConsidering the nature of the development of sod, gemmation resumption for a period of unfavorable conditions, types of shoots, their vegetative mobility and placement in terms of ecological niches rhizomatous grasses are divided into rhizomatous, rhizome-loosely-turf and sod-rhizomatous biomorphological types, that stand out the specifics of environmental and biological characteristics forming generative, elongated, lateral shoots and roots, differing features of morphology, anatomy, biochemistry and phytocoenology forming continuous grass stand
-
THE STEPPE RIVERS OF KUBAN, STATE OF THEIR BIOTA AND PROSPECTS OF DEVELOPMENT
DescriptionThe steppe rivers of Kuban, which form their landscapes in the space between the basins of the rivers Don and Kuban, are divided into two subtypes: the rivers of internal flow which flow into the small ponds (Panura, Kirpili et al.), and the rivers of external flow which flow into the Sea of Azov (Eja, Beysug, Chelbas); direction of flow of these rivers is defined slightly downward from the high right bank of the Kuban (up to 50m) and the eastern slopes (altitude up to 50-170m) of Stavropol Upland; shores of rivers are heavily deforested, subjected to strong anthropogenic pressure and water systems contaminated of organic substances. Plowing of catchment areas to foreshore and plowing dry beams, as well as cutting of forests caused huge harm of river systems. The qualitative composition of microorganisms is not very varied. Polluted rivers and bottom sediments are dominated by saprotrophic microorganisms, spore-bearing and other rod-shaped bacteria. In the samples of sludge we marked high titer thiobacteria and sulfate-reducing bacteria. Complex of actinomycetes was investigated. The species composition of vascular plants includes 135 species from 48 families, most numerous asteraceae, cereals and legumes. The dominant plant of many floodplains steppe rivers is common reed, which contributes to the process of silting soil particles from the fields and the destruction of the sod with overgrazing. Among phytocenoses there is a domination of reed grass-forb deposits on moist soils, mesophilic couch grass-forb and grass-forb xerophytic. In soil biota of floodplains it is dominated by oligochaetes, bottom fauna molluscs and oligochaetes, water - rotifers and cladocerans
-
MICROORGANISMS OF PEDOSPHERE AND PECULIARITIES OF THE SOIL COVER OF AGRICULTURAL LANDSCAPES
DescriptionThe soil by it physical and chemical properties is a poly-dispersed heterogeneous multicomponent unique environment for development of most microorganisms. The soil is the richest natural substrate according to microbial gene fund. Presence of plants and animals in soil maintains it heterogeneous as environment of soil microorganisms, which are main regulators of natural gas composition of atmosphere of Earth, including its macro- and micro-components (including the main "greenhouse" gases - methane, carbon dioxide, nitrous oxide). Recently, the elucidation of these singularities of vital activity of soil organisms has resulted in general conclusion - due to them soil cover serves as a global bio-geo-chemical membrane, through which the exchange of matter and energy between pedosphere, lithosphere, atmosphere, hydrosphere and main living inhabitants of Earth does its work
-
MORPHOLOGICAL AND CYTO-BIOCHEMICAL BASIS OF SHOOT FORMATION OF CEREALS
DescriptionProcess of shoot formation of cereals is associated with the formation of zone shortened internodes, establishes buds certain capacity and completes transition by growth and formation of crop aboveground mass of each individual. Process of shoot formation is divided into three phases - preparatory, hidden and visible tillering, each of which is different peculiar morphological and cytobiochemical development
-
Description
Studying the situation and the impact on mountain landscapes of Caucasus allows by means of measurements to establish the most important sources of pollution, to identify the main forms of pressure (emissions, solid wastes, etc.) on the natural landscapes and agricultural systems, to develop a monitoring program with allocation the main objectives and most important tasks of its implementation. The main purpose of monitoring – is to collection of basic information, which will be aimed at addressing specific environmental problems for improvement soil cover on northern slopes of Caucasus and protect it from water erosion. The monitoring program allows getting information, which is due specific problem and conditions of certain area. The main tasks of monitoring the soil cover of northern slopes include concrete achievements in solving problems. At the beginning of monitoring follows determine the range of issues under study. More than often limited resources strictly dictate the need to reduce of measurement program, but always save quality of received material. For solving this problem we have to define the polygons of monitoring and select the objects that are affected by anthropogenic and natural factors. Considering defined technique, it is possible to evaluate the direction of development of particular ecosystem under the influence of a specific mode of action