ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ

Objective. Using biological testing, determine the environmental appropriate rates of mineralnitrogen, applied in the background of effect and aftereffect of straw and biomass of intermediatelupine green manure, in the fertilization system of potatoes and spring barley. Methods. Field experiment (gr...

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Дата:2023
Автори: Волкогон, В. В., Москаленко, А. М., Дімова, С. Б., Халеп, Ю. М., Горбань, В. П., Волкогон, К. І., Шевченко, Л. А., Штанько, Н. П., Земська, І. А.
Формат: Стаття
Мова:Англійська
Опубліковано: Institute of Agrocultural Microbiology and Agro-industrial Manufacture of NAAS of Ukraine 2023
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Agriciltural microbiology
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author Волкогон, В. В.
Москаленко, А. М.
Дімова, С. Б.
Халеп, Ю. М.
Горбань, В. П.
Волкогон, К. І.
Шевченко, Л. А.
Штанько, Н. П.
Земська, І. А.
author_facet Волкогон, В. В.
Москаленко, А. М.
Дімова, С. Б.
Халеп, Ю. М.
Горбань, В. П.
Волкогон, К. І.
Шевченко, Л. А.
Штанько, Н. П.
Земська, І. А.
author_institution_txt_mv [ { "author": "В. В. Волкогон", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "А. М. Москаленко", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "С. Б. Дімова", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "Ю. М. Халеп", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "В. П. Горбань", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "К. І. Волкогон", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "Л. А. Шевченко", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "Н. П. Штанько", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" }, { "author": "І. А. Земська", "institution": "Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН" } ]
author_sort Волкогон, В. В.
baseUrl_str https://smic.in.ua/index.php/journal/oai
collection OJS
datestamp_date 2026-07-22T10:10:51Z
description Objective. Using biological testing, determine the environmental appropriate rates of mineralnitrogen, applied in the background of effect and aftereffect of straw and biomass of intermediatelupine green manure, in the fertilization system of potatoes and spring barley. Methods. Field experiment (growing crops in crop rotation in the conditions of a long-term (since 2009) stationaryexperiment on leached chornozem); gas chromatographic (to determine the potential nitrogenfixing (nitrogenase) and potential denitrifying activities in the rhizosphere soil of plants dependingon the fertilizer); statistical. Results. With the systematic application of fresh organic matter to thesoil in the form of 5.0 t/ha of straw and 5.3 t/ha of dry biomass of intermediate lupine green manure, the excess of nitrogen mineral compounds is metabolically bound (immobilized) by microorganisms, the process of nitrogen fixation is restored, the emission of N2O decreases, and the ratesof mineral fertilizers not exceeding N80P80K80 become environmentally appropriate when growingpotatoes. At the same time, the introduction of straw does not require additional provision of mineral nitrogen to optimize the C/N ratio. The highest rate of mineral fertilizers N120P120K120 in theexperiment, even when combined with organic matter for a long time is environmentally inappropriate — only at the end of the growing season, the studied indicators demonstrate its acceptability.When growing spring barley on leached chornozem, the optimization of the processes of biologicaltransformation of nitrogen compounds is achieved if mineral fertilizers are applied on the background of aftereffect of organic matter in a rate not exceeding N60P60K60. Systemic application ofN90P90K90 suppresses the activity of nitrogen fixation and ensures significant losses of nitrous oxide.This rate of fertilizers should be applied only on the condition that it is applied against the background of the aftereffect of straw and green manure mass, which contributes to the mitigation ofenvironmental consequences. Conclusion. The use of mineral fertilizers against the backgroundof systematic application of winter wheat straw and intermediate lupine green manure biomass tothe soil contributes to the optimization of the biological state of the leached chornozem. The improvement of environmental indicators contributes to the growth of the yield of agricultural crops.
doi_str_mv 10.35868/1997-3004.38.3-15
first_indexed 2025-07-17T12:26:46Z
format Article
fulltext 3 ҐРУНТОВА МІКРОБІОЛОГІЯ Сільськогосподарська мікробіологія. 2023. Вип. 38. С. 3–15. ISSN 1997-3004 https://doi.org/10.35868/1997-3004.38.3-15 UDC 579.64:631:631.427:631.8:631.86/87:631.95 OPTIMIZATION OF NITROGEN FERTILIZATION FOR AGRICULTURAL CROPS UPON ADDITIONAL APPLICATION OF FRESH ORGANIC MATTER TO THE SOIL V. V. Volkohon, A. M. Moskalenko, S. B. Dimova, Yu. M. Khalep, V. P. Horban, K. I. Volkohon, L. A. Shevchenko, N. P. Shtanko, I. A. Zemska Institute of Agricultural Microbiology and Agroindustrial Manufacture, NAAS 97 Shevchenka Str., Chernihiv, 14030, Ukraine; e-mail: volkogon@ukr.net Objective. Using biological testing, determine the environmental appropriate rates of mineral nitrogen, applied in the background of effect and aftereffect of straw and biomass of intermediate lupine green manure, in the fertilization system of potatoes and spring barley. Methods. Field ex- periment (growing crops in crop rotation in the conditions of a long-term (since 2009) stationary experiment on leached chornozem); gas chromatographic (to determine the potential nitrogen- fixing (nitrogenase) and potential denitrifying activities in the rhizosphere soil of plants depending on the fertilizer); statistical. Results. With the systematic application of fresh organic matter to the soil in the form of 5.0 t/ha of straw and 5.3 t/ha of dry biomass of intermediate lupine green ma- nure, the excess of nitrogen mineral compounds is metabolically bound (immobilized) by microor- ganisms, the process of nitrogen fixation is restored, the emission of N2O decreases, and the rates of mineral fertilizers not exceeding N80P80K80 become environmentally appropriate when growing potatoes. At the same time, the introduction of straw does not require additional provision of mi- neral nitrogen to optimize the C/N ratio. The highest rate of mineral fertilizers N120P120K120 in the experiment, even when combined with organic matter for a long time is environmentally inappro- priate — only at the end of the growing season, the studied indicators demonstrate its acceptability. When growing spring barley on leached chornozem, the optimization of the processes of biological transformation of nitrogen compounds is achieved if mineral fertilizers are applied on the back- ground of aftereffect of organic matter in a rate not exceeding N60P60K60. Systemic application of N90P90K90 suppresses the activity of nitrogen fixation and ensures significant losses of nitrous oxide. This rate of fertilizers should be applied only on the condition that it is applied against the back- ground of the aftereffect of straw and green manure mass, which contributes to the mitigation of environmental consequences. Conclusion. The use of mineral fertilizers against the background of systematic application of winter wheat straw and intermediate lupine green manure biomass to the soil contributes to the optimization of the biological state of the leached chornozem. The im- provement of environmental indicators contributes to the growth of the yield of agricultural crops. Key words: biological testing, nitrogen fixation, denitrification, potato, spring barley, mineral nitrogen fertilizers, straw, green. Introduction. As is known, the degree of assimilation of nitrogen from fertilizers by cul- tivated plants does not exceed 35–55 % [1; 2]. With a shortage of fresh organic matter in the soil, the unused portion of mineral nitrogen compounds is partially washed out, which leads to eutrophication [3], pollution of surface and groundwater [4], and partially enters the atmos- phere in the form of ozone-destroying gas N2O [5]. In addition, under such conditions, an ex- cess of mineral nitrogen in the soil can initi- ate the development of specific groups of soil © V. V. Volkohon, A. M. Moskalenko, S. B. Dimova, Yu. M. Khalep, V. P. Horban, K. I. Volkohon, L. A. Shevchenko, N. P. Shtanko, I. A. Zemska, 2023 4 microorganisms capable of using humus com- pounds as a source of carbon [6]. The conse- quence of this, in addition to the pollution of groundwater with nitrates and the growth of N2O emissions, is the development of biological soil dehumification. However, when available carbon in the form of fresh organic matter is systemically supplied to the soil, a significant part of the nitrogen not assimilated by plants can be temporarily immobilized by microorga- nisms. The average turnover time of nitrogen immobilized in microbial biomass is about 1.5 years [7], so its return (mineralization) for as- similation by plants will contribute to increasing the yield of the following agricultural crops in the crop rotation. Systematic observance of the principles of optimizing the content of readily available carbon in the soil (e. g., using post- harvest residues, growing intermediate green manure crops, etc.) and the use of scientifically based rates of mineral nitrogen fertilizers will be able to ensure the balance of nitrogen transfor- mation processes and the stabilization of agro- ecosystems [8]. Therefore, the portion of mine- ral nitrogen compounds not used by plants must be kept from leaching and emission through metabolic binding by microorganisms, the de- velopment of which requires an additional sup- ply of fresh organic matter with a wide C/N ratio. Evaluation of the recent studies and pa- pers. Today, there is no doubt that many eco- logical problems must be solved taking into ac- count the activity of soil microbiota, since the grouping of microorganisms and their activity in the soil is of crucial importance for maintaining the functions of terrestrial ecosystems due to their role in the circulation, retention and release of the main nutrients [9; 10]. According to numerous studies, groups of microorganisms are a sensitive indicator of stress, reflecting even small changes in the composition of their habitat [11–23]. Therefore, using the reaction of microorganisms to chan- ges, it is possible to monitor the influence of the studied factors on the direction of biological processes in the soil. This may fully apply to the determination of optimal rates of mineral nitro- gen as the biggest pollutant of the environment due to low rates of assimilation of the element from fertilizers. At the same time, it is practical- ly quite difficult to do this, especially when it is needed to synchronize the influence of mineral nitrogen and fresh organic matter on the for- mation of the yield of agricultural crops, the ne- cessity of which was discussed above. An important indicator of optimization or excess nitrogen fertilization of agricultural crops can be the reaction of nitrogen-fixing bacteria. As it is known, the binding of atmospheric ni- trogen is an extremely energy-intensive process. Therefore, nature has evolved effective regula- tory mechanisms that ensure the expression of nitrogen fixation genes and the functioning of the necessary enzymes only under the condition of nitrogen deficiency in the environment and opportunities for N2 binding. If there is mineral nitrogen in the environment in the quantities necessary to ensure metabolism, mechanisms are included to block unjustified energy ex- penditure for nitrogen fixation. In the presence of nitrate, cells begin to synthesize the enzyme nitrate reductase (molybdenum-dependent pro- tein), which competes with nitrogenase (the key enzyme of the nitrogen fixation process, and al- so molybdenum-dependent), thereby inhibiting its synthesis (ammonium also prevents the syn- thesis of nitrogenase, but in this case other me- chanisms are involved) [24]. Therefore, a uni- que property of most diazotrophic bacteria is their ability to perform several stages of the ni- trogen cycle, in particular, nitrogen fixation and denitrification. In other words, nature is ex- tremely rational in carrying out the nitrogen cy- cle and regulates the processes of its transfor- mation at the enzyme level. Taking into account the fact that rhizosphere nitrogen-fixing bacteria practically reflect the reaction of plants to the concentration of nitrogen compounds, since they are in close spatial and functional interac- tion with it [25], we conclude that the reaction of diazotrophs in the root zone makes it possible to monitor the reaction of plants to the nitrogen content in soil [26]. In addition to determining the activity of ni- trogen fixation by a test to find out the expedi- ency of using certain doses of nitrogen fertili- zers in the technologies of growing crops, a stu- dy of the activity of denitrification in the root zone of plants can be applied. At the same time, excessive amounts of nitrogen fertilizers will ensure the greatest losses of gaseous nitrogen compounds [27]. In connection with the above, the objective of our study was to find out the ecological feasibi- lity of using different rates of mineral nitrogen, ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 5 applied both with and without the addition of fresh organic matter to the soil. Materials and methods. The study was conducted in 2023 in the field stationary expe- riment of the Institute of Agricultural Micro- biology and Agroindustrial Manufacture of the National Academy of Agrarian Sciences on lea- ched chornozem under conditions of short crop rotation (potatoes → spring barley → peas → winter wheat). The study was initiated in 2009. It included three crop rotations. The agroche- mical characteristic of the soil is as follows: рНsalt — 5.3; humus content — 3.03 %; easily hydrolyzable nitrogen — 95 mg/kg of soil; mo- bile phosphorus compounds (Р2О5) — 150 mg/ /kg of soil (according to Kirsanov); content of exchangeable potassium (K2O) (according to Kirsanov) — 108 mg/kg of soil. The rhizosphere soil of potatoes of the Be- laroza variety and spring barley of the Hosia va- riety was analysed when crops were cultivated on different agrarian backgrounds. The scheme of the experiment (potato and barley fertiliza- tion systems) is given in Table 1. Table 1. Crop fertilization systems Crop fertilization potato spring barley without fertilizers without fertilizers Straw, 5 t/ha + green manure (narrow-leaved lupine, ≈ 5.2 t/ha of dry aboveground mass and dry roots) a N40P40K40 N30P30K30 N40P40K40 + straw + green manure N30P30K30 + a N80P80K80 N60P60K60 N80P80K80 + straw + green manure N60P60K60 + a N120P120K120 N90P90K90 N120P120K120 + straw + green manure N90P90K90 + a a) aftereffect of organic fertilizers. Fresh organic matter was applied under po- tatoes. Shredded straw in the amount of 5.0 t/ha was worked into the soil immediately after har- vesting winter wheat by disking, after which narrow-leaved lupine was sown on the interme- diate green manure. The green manure mass of lupine (≈ 2.6 t/ha of dry aboveground mass + ≈ 2.7 t/ha of dry roots) was worked into the soil by disking followed by shallow plowing (15 cm) in late autumn. The area of the experimental plot is 43.2 m2 (3.6 × 12.0 m), the experiment was repeated four times. Placement of plots is randomized. In the previous study of the features of the transformation of nitrogen compounds in the soil, we concluded that more objective indica- tors of the influence of certain factors on the studied processes can be obtained by determi- ning not the actual (field) activity of nitrogen fixation and denitrification, but the potential [26; 27]. By determining the potential activity, it is possible to level the influence of climatic factors (since low moisture content in the soil or a decrease in its temperature can stop the activi- ty of soil microorganisms). The analysis of the potential activity of both nitrogen fixation and denitrification involves optimizing the moisture content of soil samples and their exposure at the optimal temperature. Under these conditions, the influence of the studied factor is clearly dis- tinguished (in our case, the effect of different concentrations of mineral nitrogen in the soil). Extrapolation of the results of determining the potential activity of processes is carried out ac- cording to the principle of detecting doses of mineral nitrogen, which provide changes in ac- tivity for a longer time compared to the control. In connection with the above, potential ni- trogen-fixing and denitrifying activities were studied. The potential activity of nitrogen fixation (potential nitrogenase activity) in the rhizo- sphere soil of potato and barley plants was de- termined by the acetylene method [28] in a mo- dification [29]. For this purpose, fresh rhizo- sphere soil was freed from plant remains and a median sample was prepared. Soil samples weighing 10.0 g were placed in 40 cm3 glass vessels. At the same time, samples were taken to determine soil moisture. 1 cm3 of D-glucose solution with a mass fraction of 20 % was added to the soil samples and the humidity was adjust- ed to 60 % of the full moisture content with sterile water. It was thoroughly mixed to ho- mogenisation. The vessels were closed with cot- ton plugs and kept for 72 hours in a thermostat at 26 ± 2 °С. After the end of the incubation, cotton plugs were replaced with rubber ones in ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 6 the vessels, and acetylene was introduced in the amount of 10 % of the volume of the gas phase (3 cm3). After exposure of the samples to acety- lene for 1 hour, gas samples were taken with a syringe and analysed on a gas chromatograph Chrom-5 (Czech Republic) with a flame ioniza- tion detector (a 3 mm steel, filled with Porapak Q 60–80 mesh sorbent (Waters Corporation, USA); thermostat temperature 40 °C; gas con- sumption: hydrogen — 15 cm3/min, nitrogen — 100 cm3/min, air — 500 cm3/min). The potential nitrogenase activity in the rhi- zosphere soil in nmol of С2Н4 per 1 g of soil per hour was calculated according to formula 1. PNA = E · V1 · K / (V2 · m), (1) where E — the amount of ethylene in the gas sample introduced into the chromato- graph, nmol; V1 — the volume of the gas phase in the vessel, cm3; K — the soil moisture coefficient; V2 — the volume of the sample intro- duced into the chromatograph, cm3; m — the weight of the soil sample, g. The potential denitrification activity in the rhizosphere soil of plants was determined by the acetylene method [30]. For this purpose, mea- surements of rhizosphere soil weighing 10.0 g were prepared and placed in 40 cm3 vessels. 1 cm3 of D-glucose solution with a mass frac- tion of 20 % and 1 cm3 of KNO3 solution with a mass fraction of 2 % were added to the sam- ples. The humidity was adjusted to 60 % of the full moisture content with sterile water. The vessels were closed with rubber stoppers, and helium was passed under pressure to displace air and create anaerobic conditions (anaerobic con- ditions in the vessels ensure the measurement of only the activity of denitrification, and exclude the formation of N2O in the process of nitrifica- tion, which requires aerobic conditions). For this purpose, the rubber plug was pierced with two injection needles, one of which was con- nected to the helium cylinder, and the other was used to release gases and equalize the pressure in the vessels. Helium was passed for 30 se- conds, after which the needles were simultane- ously removed. 3 cm3 of acetylene was injected into each vessel with a syringe. Previously, 3 cm3 of the gas mixture was taken from each vessel (to maintain the normal partial pressure of gases in the vessels). Soil samples prepared in this way were kept in a thermostat at 26 ± ± 2 °C for 24 hours. After the end of the expo- sure period, gas samples were taken with an in- jection syringe and analysed using Tsvet-500 M gas chromatograph (Russia) with an electron capture detector. 3 m sorption columns were filled with Porapak Q 60–80 mesh sorbent (Wa- ter Corporation, USA). The temperature of the columns is 40 °С, the temperature of the evapo- rator is 120 °С, the temperature of the detector is 330 °С. Consumption of carrier gas (argon with methane 95/5) — 35 cm3/min. The calculation of potential denitrification activity was carried out according to formula 2: N2OD = Е · V1 · K / (V2 · m), (2) where N2OD — the potential activity of denitri- fication in the rhizosphere soil, nmol N2O/g of soil per day; E — the amount of N2O in the analysed sample, nmol; V1 — the volume of the gas phase in the vessel, cm3; K — the soil moisture coefficient; V2 — the volume of the gas sample in- troduced into the chromatograph, cm3; m — the mass of wet weight of soil, g. Since the concentration of nitrogen mineral compounds in the soil during the growing sea- son changes, the nature of the dependence of the studied processes on the types and rates of ferti- lizers may also change accordingly. In this re- gard, the analyses were performed in dynamics. Crop yield was determined by weighing products from each plot. The obtained results were subjected to the analysis of variance using the Student’s coeffi- cient (with a probability of 5 %). Statistica 6.0 program (StatSoft Inc., USA) was used for cal- culations. Results and discussion. Study of the bio- logical activity of the rhizosphere soil of potato plants and the yield of the crop under different fertilization systems. Determination of the dy- namics of potential nitrogenase activity in the rhizosphere soil of potato plants indicates opti- mization of the process after the combined use of straw and green manure (Table 2). Mineral fertilizers in a small amount stimu- late the activity of the studied process, in the medium — reduce the indicators in the first pe- riod and stimulate in the flowering phase and beginning of the top necrosis. The use of high ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 7 Table 2. Dynamics of potential nitrogenase activity of rhizosphere soil of potato plants under different fertilization systems Variants of experiment Nitrogenase activity, nmol С2Н4/g of soil per day seedling phase flowering phase top necrosis phase Without fertilizers, control 118.5 148.0 250.9 Straw + green manure 198.0 252.3 425.0 N40P40K40 149.2 200.5 270.5 N40P40K40 + straw + green manure 190.5 273.8 360.2 N80P80K80 100.2 190.0 300.5 N80P80K80 + straw + green manure 160.8 238.2 395.4 N120P120K120 49.0 125.5 210.9 N120P120K120 + straw + green manure 70.4 150.0 320.0 НІР05 13.9 16.0 22.5 rates of mineral fertilizers leads to suppression of nitrogen fixation during the growing season. Significant changes in the activity of nitro- gen fixation are reported for the combination of fertilizers with fresh organic matter. Low and medium doses of mineral nitrogen, applied on a background of straw and green manure, con- tribute to increasing the activity of nitrogen fixation throughout the growing season of pota- to plants. With the introduction of a dose of fer- tilizers at the rate of 120 kg/ha of the active sub- stance against the background of fresh mort- mass, we registered the restoration of the pro- cess of nitrogen fixation to the level of control indicators in the flowering phase and stimula- tion of activity at the end of the growing season. Considering that the process of nitrogen fixation is inherently rational and cannot be manifested in the presence of an excess amount of bound forms of nitrogen, the presented data are a reliable test of the ecological feasibility of certain fertilizer rates, primarily nitrogen. In this regard, the following conclusions are valid: the use of mineral fertilizers in the rate of N80P80K80 and N120P120K120 inhibits the process of nitrogen fixation for a long time, but providing the soil with fresh organic matter eliminates this nega- tive effect: in the variant with N80P80K80 — al- ready in the first period of experiment, and for N120P120K120 — starting from the flowering phase. Therefore, under the condition of applying mineral fertilizers against the background of or- ganic matter in the form of 5.0 t/ha of winter wheat straw and biomass of intermediate lupine green manure, the part of fertilizers not used by plants is metabolically assimilated by soil mi- croorganisms, which in this case have to pro- vide both nitrogen and carbon. This influences the restoration of the functioning of nitrogen- fixing bacteria, since the excessive concentra- tion of mineral nitrogen compounds in the soil under these conditions decreased due to their transformation into organic compounds. In the dynamic experiment, this was clearly manifes- ted first in the variant with the lowest rate of mineral fertilizers in the experiment, later — with the medium, and at the end of the growing season — with the highest. The conclusions reached are largely con- firmed by the results of determining the poten- tial denitrifying activity. As it is known, the process of denitrification does not always end with the formation of N2. Under natural condi- tions, it can stop at the stage of incomplete re- duction of nitrates — to nitrite (NO2-), nitrogen oxide (NO), or nitrous oxide (N2O) [31]. Com- plete denitrification with the formation of N2 is reported only in a limited number of microor- ganisms, i.e. true denitrifiers. Therefore, we be- lieve that the N2OD study method used by us in the presence of acetylene, which is a specific inhibitor of nitric oxide reductase and blocks the reduction of N2O to N2, ensures the determina- tion of the activity of all denitrifying microor- ganisms in the rhizosphere of potato plants — both that reduce nitrogen compounds to N2O, and that carry out complete denitrification — to N2. At the same time, it should be emphasized that the determination of the potential activity of denitrification in the rhizosphere soil does not characterize the total loss of N2O from a certain ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 8 area, but only reflects the reaction of rhizo- sphere microorganisms to a certain amount of mineral nitrogen compounds, and thereby demonstrates the reaction of the plant itself to a deficiency or excessive amount of mineral nitrogen. Mineral fertilizers stimulated the potential emission of N2O in proportion to the applied rates. At the same time, the use of mineral ferti- lizers against the background of straw and green manure contributed to a significant reduction of nitrous oxide losses (Table 3). And even the combination of the highest rate of fertilizers in the experiment with fresh organic matter can significantly reduce the intensity of biological denitrification. Therefore, upon the systematic application of fresh organic matter to the soil in the form of straw and biomass of intermediate lupine green manure, the excess of nitrogen mineral com- pounds is metabolically bound (immobilized) by microorganisms, the process of nitrogen fixation is restored, the emission of N2O decreases, and the rates of mineral fertilizers that do not exceed N80P80K80 become ecologically acceptable. At the same time, the introduction of straw does not require additional provision of mineral ni- trogen to optimize the C/N ratio. The highest rate of N120P120K120 mineral fertilizers in the experiment, even when com- bined with organic matter, is not ecologically appropriate for a long time — only at the end of the growing season, the studied indicators demonstrate its acceptability. We can see how effective the combination of mineral and organic factors of potato fertili- zation can be from the results given in Table 4. As suggested by the results, the systematic ap- plication of organic matter to the soil in the form of straw and biomass of intermediate green Table 3. Potential denitrification activity in rhizosphere soil of potato plants depending on the crop fertilization, nmol N2O/г of soil per day Variants of experiment Seedling phase Flowering phase Top necrosis phase Without fertilizers, control 19.3 7.6 5.8 Straw + green manure 21.2 8.1 6.9 N40P40K40 22.0 13.2 8.0 N40P40K40 + straw + green manure 18.9 8.9 6.0 N80P80K80 35.0 15.5 9.6 N80P80K80 + straw + green manure 27.9 10.1 6.2 N120P120K120 41.8 18.1 12.1 N120P120K120 + straw + green manure 37.8 11.9 9.9 НІР05 3.0 2.7 2.5 Table 4. Potato yield with different fertilization systems Variants of experiment (fertilization systems) Yield, t/ha Yield increase t/ha % Without fertilizers, control 15.07 – – Straw + green manure 18.27 3.20 21.2 N40P40K40 22.94 7.87 52.2 N40P40K40 + straw + green manure 25.27 10.20 67.7 N80P80K80 26.03 10.96 72.7 N80P80K80 + straw + green manure 30.69 15.62 103.6 N120P120K120 31.95 16.88 112.0 N120P120K120 + straw + green manure 34.78 19.71 130.8 НІР05 1.51 ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 9 manure culture contributes to a significant in- crease in indicators compared to the values in the variants using mineral fertilizers in their pure form. The increase in yield is from 2.33 t/ha in the variant with N40P40K40 against the background of straw and green manure to 4.66 t/ha in the variant “N40P40K40 + straw + green manure” and up to 2.83 t/ha in the variant “N120P120K120 + straw + green manure”. The greatest increase in the yield was re- ported when using the medium rate of mineral fertilizers in the experiment in combination with organic fertilizer, which can indicate, first of all, the formation of optimal indicators of the course of biological activity in the soil. It should also be noted the optimization of nitrogen nutrition of plants, taking into account the systemic im- mobilization of mineral nitrogen unused by plants and its subsequent release as a result of mineralization processes. A similar direction in the formation of the nitrogen regime of soils is mentioned in the literature [7]. Since the expe- riment has been carried out since 2009, it can be expected that the above-mentioned processes have stabilized, and the plants, due to the com- bination of mineral fertilizers with straw and biomass of green manure culture, constantly re- ceive an additional amount of nitrogen, as com- pared to the case when only mineral fertilizers are applied. Features of the course of biological trans- formation of nitrogen compounds in the rhizo- sphere soil of spring barley plants and crop yield under different fertilization systems. Measuring of potential nitrogenase activity in the rhizosphere soil of spring barley plants indi- cates an increase in indicators in the first year of aftereffect of straw and lupine green manure (Table 5). A low rate of mineral fertilizers (N30P30K30) in the experiment stimulates the activity of ni- trogen fixation, a medium rate reduces the indi- cators in the first studied phase, but promotes their growth in the following phases of organo- genesis of the crop. A high rate of nitrogen ferti- lizers leads to a decrease in the activity of the studied process practically throughout the gro- wing season of the crop. Only at the end of the growing season of barley, we register the resto- ration of nitrogenase activity in the rhizosphere soil to the indicators of the control variant. When mineral fertilizers have been intro- duced against the background of the first year of aftereffect of straw and intermediate green ma- nure, we register a significant increase in nitro- genase activity both in relation to the control and in relation to the indicators of the corres- ponding variants, where the fertilizers were used in their pure form. This indirectly indicates a de- crease in the concentration of mineral nitrogen in the rhizosphere soil of plants due to its im- mobilization by microorganisms. At the same time, even the highest rate of mineral fertilizers in the experiment in the flowering phase does not reduce the nitrogenase activity of the rhizo- sphere soil versus the control indicators. Table 5. Dynamics of potential nitrogenase activity in rhizosphere soil of spring barley plants depending on the crop fertilization Variants of experiment Nitrogen fixation (nitrogenase) activity, nmol С2Н4/g of soil per day seedling phase booting phase milk-wax phase Without fertilizers, control 78.6 56.1 127.3 Strawа + green manureа 122.0 108.8 165.5 N30P30K30 80.5 94.1 138.0 N30P30K30 + strawа + green manureа 145.4 113.0 167.2 N60P60K60 55.8 106.5 156.5 N60P60K60 + strawа + green manureа 93.0 135.2 188.6 N90P90K90 36.3 48.7 123.1 N90P90K90 + strawа + green manureа 52.9 77.4 153.5 НІР05 14.1 21.0 23.5 Note: From this point onward in Tables 6 and 7 “strawа + green manureа” — the first year aftereffect of organic fertilizers. ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 10 The intensity of potential denitrification in addition to indicators of nitrogen fixation activi- ty can indicate optimal or excess amounts of nitrogen compounds in the soil. The results of the conducted research show that the greatest potential losses of nitrogen compounds are characteristic of variants using mineral fertilizers (Table 6), which is quite na- tural given the fact that under these conditions, denitrifying microorganisms receive the neces- sary substrate for their vital activity in the form of nitrates. Nitrogen fertilizers contributed to the increase of the potential activity of the emission of nitrous oxide as their rate increased. Howe- ver, their use against the background of addi- tional sources of carbon (straw and green ma- nure) contributed to the reduction of the loss of gaseous nitrogen. As it can be seen, nitrogen losses in the va- riants of low and medium mineral fertilizer rates in the experiment against the background of the aftereffect of straw and green manure biomass are insignificant and in some periods of the analysis even lower than the indicators of the control variant, which undoubtedly indicates the immobilization of nitrogenous compounds and, the avoidance of their losses under these condi- tions, accordingly. And only the application of N90P90K90 against the background of the aftereffect of straw and green manure does not allow to re- duce the specific losses of nitrogen above the control ones. At the same time, during the vege- tation period, specific nitrogen losses in this variant significantly decrease and at the end of the barley vegetation period, they practically approach the control level. Therefore, both the determination of the po- tential activity of nitrogen fixation, which is a kind of biological marker of the ecological feasibility of nitrogen fertilization of agricultu- ral crops (since it can only occur with a defi- ciency of mineral nitrogen compounds in the environment), and the indicators of potential denitrification activity, testify to the feasibility of using mineral fertilizers for barley, when growing on leached chornozem at the rates not exceeding N60P60K60. At the same time, the op- timization of the processes of biological trans- formation of nitrogen compounds is achieved faster with the introduction of mineral fertilizers against the background of the aftereffect of or- ganic matter. Fertilizers in the rates of N90P90K90 should be applied on the condition that they are introduced against the background of the after- effect of straw and green manure mass. Improving nutrition of spring barley plants due to the combination of mineral and organic (after-effect) fertilization factors had a positive effect on crop yield (Table 7). For instance, the yield increase from the application of N30P30K30 against the background of the aftereffect of straw and green manure amounted to 0.36 t/ha compared to the indicator of the variant with the introduction of only mi- neral fertilizers at the same rate. At the same time, the yield level of barley practically did not differ from the indicator of the yield of the crop after the introduction of N60P60K60 (3.93 and 4.03 t/ha, respectively). A similar nature of yield formation was also reported for the use of medium and high rates of fertilizers, respec- tively, against the background of the aftereffect of straw and green manure and without the Table 6. Potential denitrification activity in rhizosphere soil of spring barley plans depending on the crop fertilization, nmol N2O/g of soil per day Variants of experiment seedling phase booting phase milk-wax phase Without fertilizers, control 19.1 22.0 20.2 Strawа + green manureа 21.5 23.8 22.8 N30P30K30 25.9 24.5 24.5 N30P30K30 + strawа + green manureа 14.5 20.6 19.8 N60P60K60 33.5 30.8 25.9 N60P60K60 + strawа + green manureа 29.1 20.6 20.4 N90P90K90 47.5 37.5 30.3 N90P90K90 + strawа + green manureа 40.6 29.3 24.5 НІР05 4.3 5.1 3.8 ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 11 Table 7. Yield of spring barley under different fertilization systems Variants of experiment (fertilization systems) Yield, t/ha Yield increase t/ha % Without fertilizers, control 2.39 – – Strawа + green manureа 2.71 0.32 13.4 N30P30K30 3.57 1.18 49.4 N30P30K30 + strawа + green manureа 3.93 1.54 64.4 N60P60K60 4.03 1.64 68.6 N60P60K60 + strawа + green manureа 4.26 1.87 78.2 N90P90K90 4.44 2.05 85.8 N90P90K90 + strawа + green manureа 4.75 2.36 98.7 НІР05 0.20 organic factor — 4.26 t/ha versus 4.03 t/ha and 4.75 t/ha versus 4.44 t/ha (Table 7). Therefore, it is possible to solve the urgent task of increasing the efficiency of nitrogen use by agricultural crops, taking into account the peculiarities of the course of microbiological transformation of nitrogen compounds and the influence of organic matter — straw in com- bination with intermediate green manure bio- mass — on these processes. Under these condi- tions, immobilized nitrogen compounds after mineralization are directed to the metabolic needs of plants. Conclusion. Systemic application of mine- ral fertilizers in the background of effect and aftereffect of 5.0 t/ha of straw and 5.3 t/ha of dry biomass of lupine green manure optimizes the biological condition of the leached chorno- zem versus using mineral fertilizers without ad- ditional application of organic matter to the soil. The improvement of environmental indicators contributes to the growth of the yield of pota- toes and spring barley. REFERENCES 1. Vitousek, P. M., Aber, J. D., Howarth, R. W., Likens, G. E., Matson, P. A., Schindler D. W. … Tilman, D. G. (1997). Human alteration of the glo- bal nitrogen cycle: sources and consequences. Ecol. Applications, 7(3), 737–750. 2. Tilman, D. (1999). Global environmental im- pacts of agricultural expansion: the need for sustai- nable and efficient practices. P Natl Acad Sci USA, 96, 5995–6000. 3. 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Soil Microorganisms as Controllers of Atmospheric Trace Gases (H2, CO, CH4, OCS, N2O and NO). Microbiol. Reviews, 60(4), 609–640. Received 04.10.2023 ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 13 https://doi.org/10.35868/1997-3004.38.3-15 УДК 579.64:631:631.427:631.8:631.86/87:631.95 ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ В. В. Волкогон, А. М. Москаленко, С. Б. Дімова, Ю. М. Халеп, В. П. Горбань, К. І. Волкогон, Л. А. Шевченко, Н. П. Штанько, І. А. Земська Інститут сільськогосподарської мікробіології та агропромислового виробництва НААН, м. Чернігів e-mail: volkogon@ukr.net Мета. За біологічного тестування визначити екологічно доцільні норми мінерального Нітрогену, застосованого по фону дії і післядії соломи та біомаси проміжного люпинового сидерату, в системі удобрення картоплі і ячменю ярого. Методи. Польового досліду (виро- щування сільськогосподарських культур у сівозміні в умовах тривалого (з 2009 р.) стаціонар- ного досліду на чорноземі вилугуваному); газохроматографічні (для визначення потенційної азотфіксувальної (нітрогеназної) та потенційної денітрифікувальної активностей у ризо- сферному ґрунті рослин залежно від удобрення); статистичні. Результати. За системного внесення до ґрунту свіжої органічної речовини у вигляді 5,0 т/га соломи і 5,3 т/га сухої біо- маси проміжного люпинового сидерату надлишок мінеральних сполук азоту метаболічно зв’язується (іммобілізується) мікроорганізмами, відновлюється процес азотфіксації, змен- шується емісія N2O і норми мінеральних добрив, що не перевищують N80P80K80, стають еко- логічно доцільними за вирощування картоплі. До того ж внесення соломи не потребує дода- ткового забезпечення мінерального азоту для оптимізації співвідношення C/N. Найбільша в досліді норма туків N120P120K120 навіть за поєднання з органічною речовиною тривалий час є екологічно недоцільною — лише наприкінці вегетаційного періоду досліджувані показники демонструють її прийнятність. За вирощування ячменю ярого на чорноземі вилугуваному оптимізація процесів біологічної трансформації сполук Нітрогену досягається за внесення по фону післядії органічної речовини туків у нормі, що не перевищує N60P60K60. Системне за- стосування N90P90K90 пригнічує активність азотфіксації і забезпечує значні втрати закису Нітрогену. Цю норму добрив варто застосовувати лише за умови її внесення по фону після- дії соломи і сидеральної маси, що сприяє пом’якшенню екологічних наслідків. Висновки. За- стосування мінеральних добрив по фону системного внесення до ґрунту соломи пшениці озимої та біомаси проміжного люпинового сидерату сприяє оптимізації біологічного стану чорнозему вилугуваного. Покращення екологічних показників сприяє зростанню урожайності сільськогосподарських культур. Ключові слова: біологічне тестування, азотфіксація, денітрифікація, картопля, ячмінь ярий, мінеральні азотні добрива, солома, сидерати. ЦИТОВАНА ЛІТЕРАТУРА 1. Vitousek P. M., Aber J. D., Howarth R. W., Likens G. E., Matson P. A., Schindler D. W. … Tilman D. G. Human alteration of the global nitro- gen cycle: sources and consequences. Ecol. Applica- tions. 1997. № 7(3). P. 737–750. 2. Tilman D. Global environmental impacts of agricultural expansion: the need for sustainable and efficient practices. P Natl Acad Sci USA. 1999. № 96. P. 5995–6000. 3. Stoate C., B’aldi A., Beja P., Boatman N. D., Herzon I., van Doorn A. … Ramwell C. Ecological impacts of early 21st century agricultural change in Europe — a review. J Environ Manage. 2009. № 91. P. 22–46. https://doi.org/10.1016/j.jenvman.2009.07. 005 4. Spalding R. F., Exner M. E. Occurrence of nitrate in groundwater — a review. 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Методологічні аспекти визначення екологічно доцільних доз мінераль- ного азоту в землеробстві. Агрохімія і ґрунто- знавство. 2006. Спецвипуск. С. 17−19. 27. Волкогон В. В., Бердніков О. М., Лопу- шняк В. І. Екологічні аспекти систем удобрення сільськогосподарських культур. К. : Аграрна на- ука, 2019. 264 с. ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38. 15 28. Hardy R. W. F., Burns R. C., Holsten R. D. Application of the acetylene-ethylene assay for measurement of nitrogen fixation. Soil. Biol. Bio- chem. 1973. № 5(1). P. 41−83. https://doi.org/ 10.1016/0038-0717(73)90093-X 29. Умаров М. М. Ацетиленовый метод изу- чения азотфиксации в почвенно-микробиологи- ческих исследованиях. Почвоведение. 1976. № 11. С. 119−123. 30. Smith M. S., Firestone M. K., Tiedje J. M. The Acetylene Inhibition Method for Short-term Measurement of Soil Denitrification and its Evalua- tion Using Nitrogen-13. Soil Sci. Soc. America J. 1978. № 42(4). P. 611−615. https://doi.org/10.2136/ sssaj1978.03615995004200040015x 31. Conrad R. Soil Microorganisms as Control- lers of Atmospheric Trace Gases (H2, CO, CH4, OCS, N2O and NO). Microbiol. Reviews. 1996. № 60(4). Р. 609–640. Отримано 04.10.2023 ISSN 1997-3004 Сільськогосподарська мікробіологія. 2023. Вип. 38.
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spelling oai:ojs2.smic.in.ua:article-5122026-07-22T10:10:51Z OPTIMIZATION OF NITROGEN FERTILIZATION FOR AGRICULTURAL CROPS UPON ADDITIONAL APPLICATION OF FRESH ORGANIC MATTER TO THE SOIL ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ Волкогон, В. В. Москаленко, А. М. Дімова, С. Б. Халеп, Ю. М. Горбань, В. П. Волкогон, К. І. Шевченко, Л. А. Штанько, Н. П. Земська, І. А. biological testing, nitrogen fixation, denitrification, potato, spring barley, mineral nitrogen fertilizers, straw, green біологічне тестування, азотфіксація, денітрифікація, картопля, ячмінь ярий, мінеральні азотні добрива, солома, сидерати Objective. Using biological testing, determine the environmental appropriate rates of mineralnitrogen, applied in the background of effect and aftereffect of straw and biomass of intermediatelupine green manure, in the fertilization system of potatoes and spring barley. Methods. Field experiment (growing crops in crop rotation in the conditions of a long-term (since 2009) stationaryexperiment on leached chornozem); gas chromatographic (to determine the potential nitrogenfixing (nitrogenase) and potential denitrifying activities in the rhizosphere soil of plants dependingon the fertilizer); statistical. Results. With the systematic application of fresh organic matter to thesoil in the form of 5.0 t/ha of straw and 5.3 t/ha of dry biomass of intermediate lupine green manure, the excess of nitrogen mineral compounds is metabolically bound (immobilized) by microorganisms, the process of nitrogen fixation is restored, the emission of N2O decreases, and the ratesof mineral fertilizers not exceeding N80P80K80 become environmentally appropriate when growingpotatoes. At the same time, the introduction of straw does not require additional provision of mineral nitrogen to optimize the C/N ratio. The highest rate of mineral fertilizers N120P120K120 in theexperiment, even when combined with organic matter for a long time is environmentally inappropriate — only at the end of the growing season, the studied indicators demonstrate its acceptability.When growing spring barley on leached chornozem, the optimization of the processes of biologicaltransformation of nitrogen compounds is achieved if mineral fertilizers are applied on the background of aftereffect of organic matter in a rate not exceeding N60P60K60. Systemic application ofN90P90K90 suppresses the activity of nitrogen fixation and ensures significant losses of nitrous oxide.This rate of fertilizers should be applied only on the condition that it is applied against the background of the aftereffect of straw and green manure mass, which contributes to the mitigation ofenvironmental consequences. Conclusion. The use of mineral fertilizers against the backgroundof systematic application of winter wheat straw and intermediate lupine green manure biomass tothe soil contributes to the optimization of the biological state of the leached chornozem. The improvement of environmental indicators contributes to the growth of the yield of agricultural crops. Мета. За біологічного тестування визначити екологічно доцільні норми мінерального Нітрогену, застосованого по фону дії і післядії соломи та біомаси проміжного люпинового сидерату, в системі удобрення картоплі і ячменю ярого. Методи. Польового досліду (вирощування сільськогосподарських культур у сівозміні в умовах тривалого (з 2009 р.) стаціонарного досліду на чорноземі вилугуваному); газохроматографічні (для визначення потенційної азотфіксувальної (нітрогеназної) та потенційної денітрифікувальної активностей у ризосферному ґрунті рослин залежно від удобрення); статистичні. Результати. За системного внесення до ґрунту свіжої органічної речовини у вигляді 5,0 т/га соломи і 5,3 т/га сухої біомаси проміжного люпинового сидерату надлишок мінеральних сполук азоту метаболічно зв’язується (іммобілізується) мікроорганізмами, відновлюється процес азотфіксації, зменшується емісія N2O і норми мінеральних добрив, що не перевищують N80P80K80, стають екологічно доцільними за вирощування картоплі. До того ж внесення соломи не потребує додаткового забезпечення мінерального азоту для оптимізації співвідношення C/N. Найбільша в досліді норма туків N120P120K120 навіть за поєднання з органічною речовиною тривалий час є екологічно недоцільною — лише наприкінці вегетаційного періоду досліджувані показники демонструють її прийнятність. За вирощування ячменю ярого на чорноземі вилугуваному оптимізація процесів біологічної трансформації сполук Нітрогену досягається за внесення по фону післядії органічної речовини туків у нормі, що не перевищує N60P60K60. Системне застосування N90P90K90 пригнічує активність азотфіксації і забезпечує значні втрати закису Нітрогену. Цю норму добрив варто застосовувати лише за умови її внесення по фону післядії соломи і сидеральної маси, що сприяє пом’якшенню екологічних наслідків. Висновки. Застосування мінеральних добрив по фону системного внесення до ґрунту соломи пшениці озимої та біомаси проміжного люпинового сидерату сприяє оптимізації біологічного стану чорнозему вилугуваного. Покращення екологічних показників сприяє зростанню урожайності сільськогосподарських культур. Institute of Agrocultural Microbiology and Agro-industrial Manufacture of NAAS of Ukraine 2023-12-14 Article Article Рецензована Стаття application/pdf https://smic.in.ua/index.php/journal/article/view/512 10.35868/1997-3004.38.3-15 Agricultural microbiology; Vol. 38 (2023): Agriciltural microbiology; 3-15 Сільськогосподарська мікробіологія; Том 38 (2023): Сільськогосподарська мікробіологія; 3-15 1997-3004 10.35868/1997-3004.38 en https://smic.in.ua/index.php/journal/article/view/512/584 Авторське право (c) 2023 V. V. Volkohon, A. M. Moskalenko, S. B. Dimova, Yu. M. Khalep, V. P. Horban, K. I. Volkohon, L. A. Shevchenko, N. P. Shtanko, I. A. Zemska https://creativecommons.org/licenses/by/4.0
spellingShingle біологічне тестування
азотфіксація
денітрифікація
картопля
ячмінь ярий
мінеральні азотні добрива
солома
сидерати
Волкогон, В. В.
Москаленко, А. М.
Дімова, С. Б.
Халеп, Ю. М.
Горбань, В. П.
Волкогон, К. І.
Шевченко, Л. А.
Штанько, Н. П.
Земська, І. А.
ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title_alt OPTIMIZATION OF NITROGEN FERTILIZATION FOR AGRICULTURAL CROPS UPON ADDITIONAL APPLICATION OF FRESH ORGANIC MATTER TO THE SOIL
title_full ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title_fullStr ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title_full_unstemmed ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title_short ОПТИМІЗАЦІЯ АЗОТНОГО УДОБРЕННЯ СІЛЬСЬКОГОСПОДАРСЬКИХ КУЛЬТУР ЗА ДОДАТКОВОГО НАДХОДЖЕННЯ ДО ҐРУНТУ СВІЖОЇ ОРГАНІЧНОЇ РЕЧОВИНИ
title_sort оптимізація азотного удобрення сільськогосподарських культур за додаткового надходження до ґрунту свіжої органічної речовини
topic біологічне тестування
азотфіксація
денітрифікація
картопля
ячмінь ярий
мінеральні азотні добрива
солома
сидерати
topic_facet biological testing
nitrogen fixation
denitrification
potato
spring barley
mineral nitrogen fertilizers
straw
green
біологічне тестування
азотфіксація
денітрифікація
картопля
ячмінь ярий
мінеральні азотні добрива
солома
сидерати
url https://smic.in.ua/index.php/journal/article/view/512
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