scholarly journals LOESS LIKE LOAMS AS A SOIL FORMATION FACTOR FOR LIGHT-GRAY FOREST SOILS IN THE CHEBOKSARY REGION OF THE CHUVASH REPUBLIC

2021 ◽  
Vol 2 (344) ◽  
pp. 36-44
Author(s):  
O.A. Vasiliev ◽  
V.G. Semenov ◽  
Zh. Tuleubayev ◽  
A.O. Vasiliev ◽  
A. Sarsembayeva
2021 ◽  
Vol 7 (3(84)) ◽  
pp. 41-43
Author(s):  
A. Ilinskiy

The specificity of the soil formation conditions of the gray forest soils of the Ryazan region predetermined the low content of some microelements (for example, cobalt and molybdenum) in them, which take an active part in metabolism and enzymatic reactions. Their shortage leads not only to a decrease in the yield, but also to a sharp deterioration in its quality. In case of their deficiency in the basic components of complex ameliorants, it is recommended to provide for their additional introduction into the fertilizer in the form of chelate complexes.


2020 ◽  
pp. 37-45
Author(s):  
Vadim A. Kozlov ◽  
Leonid N. Voronov ◽  
Sergey P. Sapozhnikov ◽  
Nadezhda V. Smirnova ◽  
Liliya Y. Agafoshkina ◽  
...  

The analysis of ascariasis prevalence in the Chuvash Republic for the period 1997-2017 was carried out depending on natural and anthropogenic environmental factors. As a result of multiple regression analysis including 61 factors integrated into the matrix for regression analysis, 19 factors were selected which were statistically significantly associated with the incidence of ascariasis depending on the administrative-territorial structure of the Republic. The chosen factors are divided into six groups: group 1 – factors reflecting the characteristics of water balance and the distribution of water masses in the area: (a) average annual flow (coefficient = 0.761), determining the amount of water flowing along river beds per year; b) the number of drilled wells (coefficient = 0.5133); c) the average snow cover height (coefficient = 0.2940); d) 4) the average amount of precipitation for the winter period (coefficient = 0.0073); e) the average number of sources whoch do not conform to sanitary standards and regulations (coefficient = -0.3309); f) drainage network density in km per km2 (coefficient = –0.0152), i.e. water balance and distribution of water masses in the territory of the region determine the direct impact on the incidence of ascariasis; group 2 – factors created by agricultural human activities related to soil: (a) the average annual number of poultry per 100 hectares of crops (coefficient = 0.2265); b) the specific weight of agricultural livestock areas in the entire area of agricultural land,% (coefficient = 0.2537); c) sheep stock per 100 hectares of agricultural land (coefficient = 0.1838), as it is known, livestock objects maintain viable helminth eggs for a long time; group 3 – ecological-climatic factors: a) fluctuations within the limits of baseline radiation background (coefficient = -0.2537); b) average year-round temperature (coefficient = –0,1103); c) depth of soil freezing (coefficient = –0.0412) – this group of factors is a deterrent in the spread of ascariasis because it directly affects to slow down the maturation of eggs and contributes to the early loss of vitality. As a result of cartography, a high incidence of ascariasis is noted in areas with prevalence of typical gray forest soils in combination with light gray and dark gray forest soils, in areas with gray cespitose- cryptopodzol soils. It is Krasnochetaisky region – 171,17±108,36 cases per 100 thousand population, Alikovsky region – 118,5±74.4 and Shumerlinsky region – 70,5±47,8. The minimum morbidity is in Yalchiksky region – 12,10±9,14. Conclusions: 1) the incidence of ascariasis in the territory of the Chuvash Republic is of a mosaic character. The incidence of ascariasis prevails in administrative-territorial regions located in the western part of the Chuvash Republic; 2) it is statistically proved that such a hydro-geological feature of the territory as annual runoff, including spring flooding, has a significant negative impact on morbidity; 3) such environmental and climatic factors as annual average temperature and the depth of soil freezing, have a deterrent effect on the incidence of ascariasis.


THE BULLETIN ◽  
2020 ◽  
Vol 6 (388) ◽  
pp. 38-45
Author(s):  
Vasiliev Oleg Alexandrovich ◽  
◽  
Semenov Vladimir Grigoryevich ◽  
Tuleubayev Zhaxybay ◽  
Vasiliev Alexander Olegovich ◽  
...  

Covering loess-like loams are widespread in the Chuvash Republic and serve as parent rocks. They are heterogeneous both in the course and in the depth of occurrence. A distinctive feature of loess like loams from other overlying quaternary deposits is a sharp predominance in the granulometric composition of coarse dust fractions ranging in size from 0.05 to 0.01 mm, the content of which is 40% or more. Their granulometric composition varies from light loamy to clayey. Loess like loams, due to the peculiarities of their granulometric composition, have relatively good water permeability and moisture capacity and are superior to original loamy and clay parent rocks of the Permian and Jurassic systems in terms of these parameters. The content of moving forms of phosphorus and potassium (according to Kirsanov) in loess like loams is from 15 to 75 mg/kg, of exchange potassium - from 20 to 105 mg/kg. The soils formed based on them have a well-defined profile, the genetic horizons of which are easily diagnosed in the soil section. Because soils formed on loess like loams have well-developed genetic horizons, clearly manifested features of soil formation peculiar to each soil type, they occupy a central subtype and are diagnosed as typical. However, soils formed on loess-like loams and clays have low erosion resistance and marked as erosion threatening on soil maps.


The results of long-term research on the influence of main indicators on their agro-resource potential are summarized on gray forest soils of the upper Volga region. For the conditions of the Vladimir Opolie, the probable yield of biomass and the main products of field crops were calculated at different coefficients ofphotosynthetic active radiation (FAR) use. Calculations of the main product yields are made taking into account the distribution of biomass to by-products and crop-root residues. For field crops of the studied crop rotations, the coefficients of precipitation utilization are estimated. They varied from 44 to 71%, depending on the crop rotation culture. On the slope of the southern exposure when cultivating winter cereals and perennial grasses, the main moisture losses were observed in the spring during snowmelt, when growing spring crops and potatoes, they were close in the autumn and spring periods. The sizes of moisture use by crops depending on the fertilizer systems for the creation of 1 C of grain units (g.u.) and from sub-arable layers are determined. In comparison with the liming background, the use of organic fertilizers reduced the water consumption coefficient from 9.6 to 8.5 mm/C g.u., their combination with a single dose of NPK - up to 7.3, and with a double dose - up to 6.8 mm / C g.u. Based on the amount of moisture used by crops, their possible yields are calculated. In spring crops, the amount of precipitation consumed (326-356 mm) corresponds to the use of 2.7-3% of the FAR and provides 54-60 C/ha of grain, in winter rye and wheat - about 4% of the FAR (yield 71-80 C/ha). In perennial grasses for 2 mowing, the moisture consumed is enough to use about 3% of the FAR., in potatoes -1.5%.


2011 ◽  
Vol 44 (3) ◽  
pp. 326-331 ◽  
Author(s):  
A. D. Temraleeva ◽  
D. L. Pinskii ◽  
E. N. Patova ◽  
E. V. Spirina

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