03.00.00 Biological sciences
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Description
There is gender differences regulatory-adaptive status of the students at the beginning and at the end of the academic year in the article. The results must be considered in the allocation of training load during the academic year
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Description
The results of genetic variation and differentiation study of adjacent populations growing on swamp and on dry land was done using examine of ISSR DNA regions. The same diversity level and comparatively high division were shown in this article
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GERBERA: MAIN DISEASES AND PESTS WHEN GROWING IN COVERED GROUND
DescriptionIn the article we discuss the disease and pest damage of different Holland selection gerbera varieties when growing in covered ground
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Description
The analysis of the variability dynamics of recombination frequency in the population of splitting F2 interspecific and intraspecific tomato hybrids has been carries out. It was discovered that recombination frequency depends on the components of cross breeding. It has been established that it is reasonable to use mutant forms of Мо 393, Мо 628 and interspecific hybrid F1 Мо 628 × L. esculentum var. racemigerum in selection process as an inductor of genotypic variability
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Description
By the methods of classical histology and modern histochemistry in differential assessment of various albuminous components, we have revealed a number of new regularities of age dynamics and distribution of some albumen in cells and tissues of musky preputial glands of muskrat males inhabiting under conditions of Baikal region ecosystem
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HISTOLOGIC STRUCTURE OF THE BIOLOGICALLY ACTIVE SKIN SPOTS OF THE THORAX OF DOGS
DescriptionIn the article, we gave the review of the results of histological research of the biologically active skin points of the thorax of dogs. The results of the morphology of the skin with the biologically active spots and without them were discussed
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SOIL DEGRADATION AND THE ROLE OF FOREST BELTS IN LAND MELIORATION
DescriptionSoil degradation (erodere – eat away, lat.) - a process in which result pieces of rocks and soil are separated from of their initial location. Is 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) flows of water or wind what causes depletion of fertile top soil layer. The destruction of this layer occurs quickly, and for its restoration required the millennium. 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 as the Earth was formed (about 45-50 billion years ago). Realistically, mountains, valleys, plains and deltas on 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. With the emergence of the human occurred of invasion species which could transform their natural environment. Artificial type of erosion, which acts much faster than the natural erosion, was formed with the appearance human
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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
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ECOSYSTEM DEGRADATION OF THE LIMESTONE MASSIFS OF WESTERN CAUCASUS AFTER DEFORESTATION
DescriptionSignificant changes in mountain ecosystems occur after deforestation on limestone massifs of the Western Caucasus. Tall-mountain-meadow vegetation with a large variety of species formed at low and medium soil disturbance 3 years after logging. Physical and biological properties of calcareous soils also vary greatly. The values of biological activity decrease at the maximum load is more than 10 times. Biological activity is increased by 20-50% or more cutting stations with low disorders. Biological properties of soils (especially the enzymatic activity) are very sensitive indicators of changes that have occurred as a result of logging. Changes in the activity of soil hydrolases different from changing oxidase activity at different times after logging
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Description
Dendroclimatic analysis of stands of radial increment of the natural forest and forest plantations of Scots pine in the Khrenovoe pine forest, growing in dry-moist site conditions is conducted. Cyclic dynamics of increment, weak expression of the low-frequency oscillation amplitude in the plantations stands is revealed. Direct correlation with precipitation has increased over the past 40 years, in complex suboron – to 0,48 – 0,50