scholarly journals The Process Of Soil Cutting With Rotor Knives Of Combined Ploughsharing-Racked Plow

Author(s):  
N. Vasylynych ◽  
V. Duganec ◽  
Y. Pantsyr

Soil tillage is the most energy-intensive and costly process. Therefore, the creation of combined machines that perform multiple operations in one workflow is a pressing issue for today, the solution of which is inextricably linked to the integration of agricultural operations into one technological process that brings economic, organizational and agrobiological benefits. Based on the peculiarities of soil preparation for planting or planting crops as an object, and the need for further scientific design of the combined technological process of soil application of fertilizers, active crumbling and cultivation of root, plant residues and fertilizers as a subject, the purpose of scientific research analysis of the interaction of the rotor with the reservoir, determination and optimization of the basic parameters of knives, radius, rotational speed with a view to providing classic soil cutting and mixing with fertilizers. At State Agrarian and Engineering University in Podiya the design of the combined plow was developed. The technological process of their work combines the operations of deep plowing, the active grinding of the formation and the earning of root and crop residues, as well as the introduction of mineral fertilizers. As a result of researches, the angles of installation of the knife with respect to the radius of the rotor α, the angle of sharpening γ, the cutting angle ψ, the occipital angle ζ, the angle of conicity of the rotor β, the angle of displacement of the blades (rays) of the attachment, the magnitude of the transformation of the angle of sharpening, the analysis of the part of the sharpening , and according to its results the required speed of rotation at which the soil passes on the surface of the knife without loading is determined and the effect of its unloading is provided

Agronomy ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 1276
Author(s):  
Vaida Steponavičienė ◽  
Aušra Marcinkevičienė ◽  
Lina Marija Butkevičienė ◽  
Lina Skinulienė ◽  
Vaclovas Bogužas

The composition of weed communities in agricultural crops is dependent on soil properties and the applied agronomic practices. The current study determined the effect of different tillage systems and crop residue on the soil weed community composition. The research programme encompassed 2013–2015 in a long-term field experiment located in the Experimental Station of Vytautas Magnus University in Lithuania. The soil type in the experimental field was qualified as Endocalcaric Stagnosol (Aric, Drainic, Ruptic, Amphisiltic). Weeds were categorised into communities according to soil pH, nitrogen and moisture indicators. The results of investigations were grouped using cluster analysis. Agricultural crops were dominated by different weed species depending on the soil pH and moisture. Weed species were relatively more frequent indicating nitrogen-rich and very nitrogen-rich soils. In the reduced tillage and no-tillage systems, an increase in the abundance of weed species indicating moderate acidity and low acidity, moderately wet and wet, nitrogen-rich and very nitrogen-rich soils was observed. The application of plant residues decreased the weed species abundance. In the reduced tillage and no-tillage systems, the quantitative distribution of weed was often uneven. By evaluating the association of weed communities with groups of different tillage systems with or without plant residues, their control can be optimised.


2020 ◽  
Vol 11 (3) ◽  
pp. 61-69
Author(s):  
S. P. Tanchyk ◽  
◽  
D.V. Litvinov ◽  
V.V. Sinchenko ◽  
◽  
...  

The article analyzes the main laws of the biological cycle of soybean plant biomass, and the parameters of recirculation of nutrients depending on the method and depth of the primary tillage and various preceding crops. It was found that the share of biomass alienated from the field with soybean harvest, depending on the various preceding crops and the primary tillage varied from 31,6 to 32,8 %, which in absolute terms ranged from 1,93 to 3,25 t/ha, and received to the soil with plant residues: from 3,97 to 6,67 t/ha or from 67,2 to 68,4 %. The largest amount of nutrients from 310,2 to 420,5 kg/ha of NPK is involved in soybean crops placed after cereals (winter wheat and spring barley) in the variant of cultivated without soil tillage by 20-22 cm (chisel-deep-tiller), and the lowest after corn for grain from 251,1 to 302,9 kg / ha NPK obtained in the variant during plowing by 20-22 cm. The largest share in the total amount of nutrients in soybean biomass belongs to nitrogen from 61,6 to 65,3 %, the share of phosphorus varies from 12,4 to 14,4 %, and potassium from 20,3 to 25,7 %. The amount of nutrients returned to the soil with plant residues, in relation to their content in the biomass ranges from 41.7 to 55.4% nitrogen, 11,1-14,7 phosphorus and 30,0-46,9 % potassium. It was found that the largest amount of nitrogen enters the soil with crop residues in the variant of soybean placement after soybean and main tillage (disc harrow) by 12-14 cm – 55,4 %. The share of phosphorus was 14,7 %, potassium – 29,8 %. When growing soybeans after cereals, corn for grain and sunflower, the intake of nitrogen in the soil with plant residues was 41,7-42,8 %, phosphorus 11,1-11,2 %, potassium 45,8-46,9 %. The lowest percentage of nitrogen removal - 69.5-69.6% was for the placement of soybeans after soybeans. Although for the removal of phosphorus (14,3%) and potassium – (16,1%) the option of placing soybeans after cereals, corn and sunflower prevailed, where these indicators were respectively (13,0-13,1 %) and (14,5- 14,7 %).


2020 ◽  
Vol 14 (3) ◽  
pp. 53-58
Author(s):  
I. V. Liskin ◽  
A. V. Mironova

The authors presented the results of laboratory studies of artificial soil based on sand-paraffin mixtures, reflecting the physical and mechanical soil properties with the presence of plant residues. They conducted tests to determine the soil-cutting working bodies’ traction resistance during tillage with the presence of root and crop residues.(Research purpose) To substantiate the parameters of an artificial soil environment containing models of root and crop residues for laboratory studies of the wear and traction characteristics of soil-cutting working bodies operated on post-harvest, virgin and fallow farmland.(Materials and methods) An artificial soil environment was developed by introducing filamentous components 5-25 millimeters long into its composition.(Results and discussion) The authors determined the criteria of geometric similarity “model – nature” for the soil conditions of the Non-Black Earth Zone of Russia. It was found that the equality of the criteria “model – nature” for laboratory research of fallow lands occurred when the length of the  filamentous components was from 20 mm and the concentration was from 20 segments per unit cross-sectional area when passing 0.1 meter in artificial soil. It was revealed that for modeling old arable lands, the length of the filamentous components should exceed 5 millimeters, the concentration should be from 10 segments per 0.1 meter of the length of passage in artificial soil. The authors conducted field tests of arable units on fallow and old arable lands.(Conclusions) The authors found out that the equality of the geometric criteria for the similarity of the artificial soil environment and real soil conditions allowed laboratory studies of the wear and traction characteristics of the tillage working bodies’ blades. It was determined that more than 30 percent of energy costs were accounted for by breaking the root system of the vegetation cover on virgin and fallow lands.


2016 ◽  
Vol 17 (3-4) ◽  
pp. 50-63 ◽  
Author(s):  
S. G. Chornyy ◽  
A. V. Volosheniuk

The aim of the research was to the efficiency wind erosion control of farming system «no-till» (NT) for conditions of South Steppe of Ukraine. The research was conducted at heavy load southern chornozem in the crop rotation «pea – winter (spring) wheat – sorghum – mustard». In field experiment two options of processing of the soil (traditional and minimum) and NT were studied. Options aggregate of surface soil (0–5 cm), the weight of crop residues and projective covering the soil surface were determined. Research field was equipped by meteorological station and field’s wind erosion dust-meter. The efficiency wind erosion control by NT was evaluated in three directions: the presence of dangerous wind erosion period (February–April) a certain amount of plant residues, that protect of soil surface from extreme winds (1); presence during this period of high values of «random» surface roughness of the soil, which reduces the strength of the wind in ground layer of air (2) and values of soil wind erodibility index (3). Evaluation promises more effective in terms of opening up the soil surface crop residues reveals that NT fully meets the criterion of preserving (erosion control) technology – projective cover ground in a dangerous deflationary period is an average of three years of research on the crops of spring wheat – 37.9 % for sorghum crops – 71.1 % and on crops of mustard – 60.2 %. An important indicator of the erosion control efficiency of soil tillage is percentage of vertically oriented surface plant residues. Unbroken soil surface tillage after harvesting will have the maximum amount of such residues. Analysis of these studies show that when used NT observed maximum value of this parameter – 35–55 %, more than that in other tillage. So the version with traditional soil tillage this parameter does not exceed 5 %, and versions with minimal system soil tillage – 30 %. Estimation of effectiveness of soil protection NT via a «random» surface roughness also shows a high ability wind erosion control this technology. At the same time, it should be stated that the presence of high «random» roughness autumn plowing deep plowed fields, despite the fact that the surface of the soil in the case of poorly protected plant residues. The main index of soil wind erodibility is the fraction greater than 1 mm, the so-called «lumpiness». It is known, lumpiness indicator correlate with various other soil wind erodibility indicators, in particular, the mechanical strength of soil aggregates, containing wind erosion fraction by (<0.25 mm) and wind erodibility indicators there were obtained in portable wind tunnel. Intensive plowing of the soil leads to formation of a surface of the soil with high resistance by the strong winds in the fall (lumpiness – 70–90 %). It is connected with specific mechanisms of formation of soil structure. Plowing of solonetzic chernozems, especially after dry summer and an early autumn, leads to formation of soil structure units of the larger sizes. But during the winter of lumpiness by all options of researches gradually decreases, what is explained, first of all, by action on soil units of the procedures «melting» – «freezing» that, in turn, is function from the number of transitions of temperature of the soil through 0 °C. There is a destruction of soil aggregates and dispersion of the soil, in the conditions of an unstable temperature schedule in the winter, that is a consequence of warming of climate when in the afternoon of air temperature and the soil positive, and at night the soil freezes. At the same time, when the surface of the soil during the winter and at the beginning of spring is unploughed the soil condition, as it is observed on options with NT, the number of procedures of transition through 0 °C soil temperatures sharply decreases, so a destruction of aggregates goes not so intensively on the soil surfaces. But, according to our research, in the spring, lumpiness in variants of the NT is not diminished, was 50–70 %, the lower limit soil wind erodibility for chernozem. This phenomenon is bound to higher humidity of the soil which promotes coagulation of soil particles and existence of a large number of plant residues as source of the biological substances with capacity for bonding. These factors strengthen process of formation of aggregates, large by the size, what leads to increase soil lumpiness. Direct observations of NT wind erosion control efficiency during dust storms on 26th and 27th of January, 2014 showed that soil loss in NT was 3.5 times less them on a variant of traditional tillage and 2.9 times less them on a variant of minimum tillage.


2017 ◽  
Vol 4 (3) ◽  
pp. 43-49
Author(s):  
M. Miroshnychenko ◽  
O. Siabruk

Aim. The comparison of the effect of hydrothermal conditions and various agricultural practices on the emission of CO 2 from chernozems in the Left-Bank Forest-Steppe of Ukraine. Methods. The dynamics of the intensity of carbon dioxide emissions from chernozem calcic (typical chernozem – in Ukrainian classifi cation) was studied during the growing season of 2011–2012. The observations were based on two fi eld experiments with various methods of soil till- age (6–7 years from the beginning of the experiment) and fertilization systems (21–22 years from the beginning of the experiment). Particularly, plowing at 20–22 cm, disking at 10–12 cm, cultivation at 6–8 cm and direct seeding using Great Plains drill were studied among the soil tillage methods. Mineral system (N 45 P 50 K 45 ), organic system (manure 8 t/ha) and combined organic-mineral system (manure 8 t/ha + N 45 P 50 K 45 ) were studied among fertilization systems. The intensity of CO 2 fl ux was determined using the non-stationary respiratory chambers by the alkaline absorption method, with averaging of the results during the day and the frequency of once a month. Results. During the warm period, the emission of carbon dioxide from the soil changes dynamically depending on temperature and humidity. The maximum of emission coincides with the periods of warm summer showers in June-July, the minimum values are characteristic for the late autumn period. The total emission losses of carbon in chernozems over the vegetation period ranged from 480 to 910 kg/ha and varied depending on the methods of tillage ± (4.0–6.0) % and fertilization systems ± (3.8–7.1) %. The changes in the intensity of CO 2 emission from the soil under different methods of soil tillage are associated with hydrothermal regime and the depth of crop residues location. The biggest difference is observed im- mediately after tillage, but in the spring period the differences are only 12–25 %, and after drying of the top layer of soil become even less. Direct seeding technology provides the greatest emission of CO 2 from chernozem, which is fa- cilitated by better water regime and more complete mineralization of plant residues on the soil surface. Annual losses of carbon are the least under disking of soil at 10–12 cm. The changes in the intensity of CO 2 emission from the soil under different fertilization systems are associated with the involvement of the additional organic matter from plant residues and manure to the microbiological decomposition. The greatest emission was observed under the organic- mineral fertilization system, which increased the loss of carbon by 7–8 % in comparison with the mineral system in the unfavorable hydrothermal year and by 11–15 % in the more favorable year. These differences are observed mainly during the fi rst half of the growing season when there is a clear tendency to increase the intensity of soil respiration. Conclusions. The hydrothermal conditions of the warm period of the year are decisive in the formation of the CO 2 emission fl ow from chernozems. Due to the improvement of agricultural practices, emissions might be reduced but not more that by 15 % of natural factor contribution.


Author(s):  
А. М. Grebennikov ◽  
А. S. Frid ◽  
V. P. Belobrov ◽  
V. А. Isaev ◽  
V. М. Garmashоv ◽  
...  

The article assesses the relationships between the morphological properties of agrochernozems and yield of peas on the plots, experience with different methods of basic treatment (moldboard plowing at the depth of 20 - 22, 25 - 27 and 14 - 16 cm, moldboard plowing to a depth of 14 - 16 cm, combined midwater moldboard, mid-water subsurface, surface to a depth of 6 - 8 cm and zero tillage) is inherent in V.V. Dokuchaev Research Institute of Agriculture of the Central Black Earth strip, in the fall of 2014. The research was conducted in 2015 - 2016, with the application of mineral fertilizers (N60Р60К60) and unfertilized background. The highest pea yields in the fertilized as the background, and without the use of fertilizers was observed in dumping plowing and especially in the variant with deep moldboard plowing, which creates in comparison with other ways of handling the best conditions for the growth and development of peas. The lowest yield of pea was obtained with zero processing. Apparently legalistic migrational-mizelial agrochernozems the Central Chernozem zone of minimum tillage in the cultivation of peas are not effective, what is evident already in the first year after the laying of experience with different basic treatments. As shown by the results of applying multifactor analysis of variance studied the mapping properties of the soil can have the same significant impact on the yield of agricultural crops, as options for the field experiments aimed at assessing the impact of various treatments on yield.


2018 ◽  
Vol 2 (95) ◽  
pp. 26-29
Author(s):  
O.S. Gavrishko ◽  
Yu.M. Olifir ◽  
T.V. Partyka

The results of studies of the change in redox potential in the profile of light gray forest surface-gleyed soil on variants with long-term agricultural use without applying fertilizers and mineral fertilizer system solely compared with the soil under the forest are presented. On the basis of the conducted analyzes it was established, that soil tillage without fertilizer application and with mineral fertilizer solely has a different effect on ROP in the profile. In the soil without fertilization (control) as compared to the forest a moderate oxidizing (514 mV) and slightly oxidizing (437 mV) processes are happening. Prolonged application of mineral fertilizers to the soil (N65R68K68) significantly reduced the redox potential of all genetic horizons compared with forest and control without fertilizers. For the given fertilizer system the highest values of ROP were obtained in arable HEgl and underarable HEgl layers: 426 mV and 416 mV respectively. Redox potential sharply decreases with the depth to 398-311 mV, which characterizes processes occurring in the soil profile, as weakly reducing and close to moderately reducing.


2009 ◽  
Vol 33 (2) ◽  
pp. 325-334 ◽  
Author(s):  
Luis Fernando Chavez ◽  
Telmo Jorge Carneiro Amado ◽  
Cimélio Bayer ◽  
Newton Junior La Scala ◽  
Luisa Fernanda Escobar ◽  
...  

Agricultural soils can act as a source or sink of atmospheric C, according to the soil management. This long-term experiment (22 years) was evaluated during 30 days in autumn, to quantify the effect of tillage systems (conventional tillage-CT and no-till-NT) on the soil CO2-C flux in a Rhodic Hapludox in Rio Grande do Sul State, Southern Brazil. A closed-dynamic system (Flux Chamber 6400-09, Licor) and a static system (alkali absorption) were used to measure soil CO2-C flux immediately after soybean harvest. Soil temperature and soil moisture were measured simultaneously with CO2-C flux, by Licor-6400 soil temperature probe and manual TDR, respectively. During the entire month, a CO2-C emission of less than 30 % of the C input through soybean crop residues was estimated. In the mean of a 30 day period, the CO2-C flux in NT soil was similar to CT, independent of the chamber type used for measurements. Differences in tillage systems with dynamic chamber were verified only in short term (daily evaluation), where NT had higher CO2-C flux than CT at the beginning of the evaluation period and lower flux at the end. The dynamic chamber was more efficient than the static chamber in capturing variations in CO2-C flux as a function of abiotic factors. In this chamber, the soil temperature and the water-filled pore space (WFPS), in the NT soil, explained 83 and 62 % of CO2-C flux, respectively. The Q10 factor, which evaluates CO2-C flux dependence on soil temperature, was estimated as 3.93, suggesting a high sensitivity of the biological activity to changes in soil temperature during fall season. The CO2-C flux measured in a closed dynamic chamber was correlated with the static alkali adsorption chamber only in the NT system, although the values were underestimated in comparison to the other, particularly in the case of high flux values. At low soil temperature and WFPS conditions, soil tillage caused a limited increase in soil CO2-C flux.


2020 ◽  
Vol 6 (9) ◽  
pp. 103-113
Author(s):  
I. Rusakova

Post-harvest plant residues, mainly straw of cereals and legumes, are the most important readily available biological resource for the reproduction of soil fertility. However, the data on their effectiveness and influence on the biological properties of the soil in the scientific literature are not unambiguous and contradictory. The results of long-term experiments on the study of the effectiveness of post-harvest residues of various crops are very few. The role of lupine as a green manure for increasing the productivity of potatoes is well studied, however, there are practically no data on the effect of lupine straw grown for grain on potato productivity. Studies in a long-term field experiment have established that the incorporation of lupine straw into the soil (against the background of the previous long-term introduction of straw of grain and leguminous crops of grain-tilled crop rotation), both in combination with mineral fertilizers and in pure form, contributed to an increase in the number of ecological-trophic groups of microorganisms, microbial biomass, nitrification activity of soddy-podzolic soil. The activation of microbial activity, increasing the supply of plants with available nutrients, promoted an increase in potato productivity, as well as an increase in the content of vitamin C and starchiness of tubers. A close correlation was noted between potato yield and determined microbiological parameters (r = 0.62–0.87), which indicates that the general level of biogenicity of soddy-podzolic soil, regulated by the introduction of straw of grain and leguminous crops, largely determines the level of its effective fertility and crop productivity.


2019 ◽  
Vol 12 (1) ◽  
pp. 108
Author(s):  
Paul Anguria ◽  
George N. Chemining’wa ◽  
Richard N. Onwonga ◽  
Michael A. Ugen

Sesame (Sesamum indicum. L) is one of the main sources of livelihoods in northern Uganda. However, its production is constrained by low soil fertility and moisture levels. A study was conducted at Serere, Uganda in 2013 and 2014 to investigate the effect of organo-mineral fertilizers on growth, seed yield and nutritional quality of sesame. The design of the experiment was a randomized complete block design with three replications. The treatments comprised: control (no soil amendment), mixtures of 4 crop residues each at (3 and 6 t/ha) and two rates of N, P and K. Finger millet husks (3 t/ha) plus lower fertilizer rate (30 kg N-25 kg P-40 Kg K/ha) had significantly higher seed yield of sesame; while finger millet husks (6 t/ha) plus higher fertilizer rate (60 kg N-50 kg P-80 Kg K/ha) significantly increased vegetative growth of sesame. Finger millet husks (6 t/ha) plus lower fertilizer rate had significantly higher seed crude protein content of sesame; while cowpea husks (3 t/ha) plus higher fertilizer rate and groundnut shells (3 t/ha) plus lower fertilizer rate produced significantly higher seed total ash and seed oil content of sesame, respectively. This study has demonstrated that application of a mixture of crop residues and inorganic fertilizers is the best treatment in enhancing growth, seed yield and nutritional seed quality of sesame.


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