


编号 7 (2025)
APPLICATION OF FERTILIZERS AND PRECISION FARMING: THE CONCEPT OF “INDUSTRY 4.0”
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Soil Fertility
CHANGES IN THE STRUCTURAL STATE OF ACIDIC SOD-PODZOLIC LIGHT LOAMY SOIL DURING LIMING WITH DOLOMITE PARTICLES OF DIFFERENT SIZES
摘要
In a 10-variant field experiment lasting 13 experimental years, laid on acidic sod-podzolic soil, the effect of dolomite particles with a size of <0.25 (0.25–1, 1–3 and 3–5 mm), introduced in an amount corresponding to the full dose of hydrolytic acidity (1 Ha) in pure form and their combinations (2, 3 and 6 Ha each), on the dynamics of the pH value of KCl. It has been established that the effect of liming with fine fractions of dolomite measuring 0.25–1, 1–3 mm with limestone (LF) and dolomite (DF) flour on soil acidity can be traced for at least 9 experimental years. With an increase in the dose of dolomite particles in various combinations, the duration of liming action increased and continued throughout the entire period of the experiment. The higher the dose of application, the higher the pH value of the soil. 13 experimental years after land reclamation and completion of the experiment, the effect of liming on the structural condition of the soil was evaluated. It is shown that the effect of liming on the amount of agronomically valuable (AV) and water-resistant (WR) aggregates in the soil persisted after 13 experimental years. The relationship between the content of water-resistant aggregates in the soil and the dose of application of dolomite particles has been revealed.



EFFECT OF MAGNESIUM FERTILIZERS BASED ON NATURAL BRUCITE ON THE ACID-BASE PROPERTIES OF SOILS IN GROWING POTATOES
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EFFECT OF SIDERAL BINARY MIXTURES INVOLVING SOYBEANS ON THE QUALITY AND FERTILITY OF TYPICAL CHERNOZEMS
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VARIABILITY OF AGROCHEMICAL INDICATORS OF ARABLE SOILS ACCORDING TO THE DATA OF SASS “KURGANSKAYA”
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Fertilizers
EFFECT OF MINERAL FERTILIZERS AND VEGETATIVE BIOMASS ON THE AVAILABILITY OF POTASSIUM IN GRAIN CROPS
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EFFECT OF MINERAL FERTILIZERING DEPENDS ON AGROCHEMICAL AND TECHNOLOGICAL CONDITIONS OF THEIR USE
摘要
The effects of mineral fertilizers have been shown to depend on different conditions of their use – agrochemical and technological. When choosing the type of fertilizer, it is necessary to base it on the properties of the soil, the predecessor and the previous fertilizer application system in each individual field. Based on the results of long-term stationary experiments at the Kurgan Research Institute of Agriculture, approximate doses of nitrogen and phosphorus have been established depending on the content of N-NO3 and mobile P2O5 in the soil. The content of exchangeable potassium in most of the chernozems of the Kurgan region is sufficient. The choice of fertilizer form, dose, method, and time of application changes their effectiveness both agrotechnically and economically. In one experiment, when comparing the effects of ammonium nitrate, urea, and ammonium sulfate on the yield and quality of spring wheat, urea lost slightly, while ammonium sulfate had a slight advantage. In another experiment, ammonium nitrate and urea were equivalent in the pre-sowing period for wheat, and early fertilization showed a slight loss of urea, but it benefited from a combination of early and late fertilization. The most profitable of the methods of applying simple and complex fertilizers turned out to be local, both before sowing and during sowing. Liquid fertilizers tested in corn sowing were slightly more effective than solid fertilizers. It is convenient to evaluate the effect of different doses of nutrients in crops in experiments with a sufficient set of doses. It is necessary to take into account not only the overall increase in yield, but also the marginal increase from each step of increasing the dose. In an experiment at the Makushinsky experimental field testing doses of phosphorus P15–30–45 on soil where superphosphate was highly effective, the marginal yield increases were compared. The marginal increase in grain yield and the marginal payback from the first P15 were the highest. The two subsequent P15s, as they were added to the first portion, were characterized by a decrease in yield growth and a 2.3–2.6 times decrease in the active ingredient of fertilizers.



INFLUENCE OF DIFFERENT FERTILIZER SYSTEMS ON THE CONSUMPTION OF NUTRIENTS BY THE STANDARD HARVEST OF TABLE CARROTS AND THE ECONOMIC BALANCE OF THESE SUBSTANCES
摘要
The removal of nutrients by table carrots was compared with their amount in the composition of fertilizers applied and the economic balance of these substances was calculated for different carrot fertilizer systems. The study was conducted in 2015–2017 in the Ramenskoye district of the Moscow region (the central floodplain of the Moskva River). The soil of the site is alluvial meadow, medium loamy. The tested crop is carrots of the Losinoostrovskaya 13 variety, fertilizer systems are mineral, organic, and organomineral. Sowing was carried out in the 3rd decade of May, in ridges with a height of 15 cm, with a seeding rate of 900 thousand units/ha, in oneline. During the growing season, 2 row-to-row cultivator treatments and 3–4 manual weeding were carried out. The harvest was recorded in the 3rd decade of September, with the division of products into standard and non-standard fractions. The experimental scheme included the following options: control (without fertilizers) – potential fertility of arable land, N45P30K90 – half the recommended dose, N45P30K90 – half the recommended dose + root dressing in the phase of the beginning of root crop formation (bunch ripeness) based on the results of leaf petiole analysis (on average N20K10), N45P30K90 – half the recommended dose + root dressing in the phase of the beginning of root crop formation (bunch ripeness) based on the results of soil analysis (on average N10K40), N90P60K180 – full recommended dose, biocompost 3 t/ha, N90P60K180 full recommended dose + biocompost 3 t/ha. In an average of 3 years, carrots of the Losinoostrovskaya 13 variety against the background of potential soil fertility produced a standard yield of 46.1 t/ha. The effectiveness of fertilizer systems was as follows: half of the calculated dose of ½ NPK yielded 7.0 t/ha of additional products, ½ NPK + top dressing – 9.8, NPK (full calculated dose) – 6.2, biocompost – 8.7, NPK + biocompost – 12.0 t/ha. A fertilizer dose equal to half of the calculated one was effective enough to obtain an additional crop of standard root crops on this type of soil, and a further increase in the fertilizer dose in the main application could be ineffective. The increase in the yield of standard root crops was achieved mainly due to an increase in the mass of root crops and partly due to an increase in the number of plants with standard root crops. On average, in the experiment, the consumption of basic nutrients for the formation of a standard crop unit was: nitrogen – 15.9, phosphorus – 9.8, potassium – 30.0, calcium – 11.8, magnesium – 4.3 kg/10 t. As the doses of fertilizers increased, the consumption of nutrients per crop unit increased. The complete mineral system (NPK variant) and the organomineral system (NPK + biocompost variant) fully covered the removal of nitrogen, phosphorus and potassium with a standard yield, determining their positive balance, while the organomineral system also fully covered the removal of calcium and, to a large extent – magnesium. With other variations of mineral fertilizer systems, a negative balance of all these nutrients was revealed. In addition, there was a negative balance of calcium and magnesium, which is important to take into account when using the soil for a long time. When using an organic system, with a positive balance of nitrogen, phosphorus and calcium, the potassium balance was negative. Calculation of the coefficients of nutrient utilization (СNU) from mineral and organic fertilizers using the difference method showed that with an increase in the dose of the introduced element, its utilization coefficient, as a rule, decreased. In general, the variations were as follows: СNU N – 18–37, СNU P2O5 – 12–29, СNU K2O – 33–69, СNU CaO – 17–30, СNU MgO – 33–56%.



Пестициды
USE OF INSECTICIDES IN THE RUSSIAN FEDERATION AND THEIR DANGERS FROM ORAL, DERMAL AND INHALATION INTAKE
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Agroecology
CONTRIBUTION OF SOIL MICROBIOTA AND SOIL CARBONATES TO CO2 EMISSION FROM STEPPE AND DRY-STEPPE SOILS OF WESTERN TRANSBAIKALIA
摘要
Carbon reservoirs were identified, and the quantitative contribution of soil carbonates and microbial biomass carbon to CO2 emissions from soils was revealed. The objects of the study were dispersed carbonate chernozems (Haplic Chernozems Hypocalcic) and chestnut soils (Haplic Kastanazems) of Western Transbaikalia. The data from the assessment of carbon reservoirs, as well as the contribution of carbonates and carbon from microbial biomass to the transformational carbon dioxide emission stream, will be used to calculate the carbon balance of terrestrial ecosystems and model its response to climatic and anthropogenic environmental changes. The total carbon reserves in chernozems and chestnut soils were compared. It has been revealed that there are different ratios of organic and inorganic forms within carbon pools. In chestnut soils, carbon is mostly accumulated in the form of carbonates (61–67%), while the organic component dominates in chernozems (52–78%). The contribution of carbonates to C-CO2 emissions has been determined, the indicator is significant and amounts to 1–3% of the total in chernozems and 3% in chestnut soils, which should be taken into account in balance calculations. The contribution of Ctotal to carbon dioxide emissions is significant and amounted to 1.1–2.5 in virgin soils, 0.8–3.1% in agrogenic soils. The participation of microbial biomass carbon in the total organic carbon reserve was insignificant and amounted to 1.4–2.5% of chernozems and 1.8–3.3% of Corg of chestnut soils. It was revealed that microbial respiration of soils decreased in the series: dispersed-carbonate chernozem → chestnut soil.



EFFECT OF CHANGES IN THE AGRO-CLIMATIC RESOURCES OF THE STEPPE VOLGA REGION ON THE EFFECTIVENESS OF LONG-TERM USE OF MINERAL FERTILIZERS IN MILLET CROPS
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History of science
DEDICATED TO THE 125TH ANNIVERSARY OF PROFESSOR A.G. SHESTAKOV, A FOLLOWER OF ACADEMICIAN D.N. PRYANISHNIKOV
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