scholarly journals Chicken droppings influence on sod-podzolic soil fertility change studying experience

2021 ◽  
Vol 843 (1) ◽  
pp. 012062
Author(s):  
V V Okorkov ◽  
N N Shchukin ◽  
L A Okorkova

Abstract The aim of the research was to study the effect of fresh chicken droppings on the dynamics of the physical-chemical and agrochemical properties of sod-podzolic soil and the yield of grain crops. In the sod-podzolic light loamy soil of the Yaroslavl region in the layer of 0-0.20 m in May, fresh chicken droppings were embedded at the dose of 120 t/ha. By autumn, in the 0-0.40 m layer of pHKc1 increased from 4.53-4.99 to 5.38-7.09, the content of mobile phosphorus and exchangeable potassium increased by 2.0-2.4 times, nitrate and ammonium nitrogen - 3-5 times. The content of nitrates in the soil has exceeded the Maximum Allowable Concentration level. The grain yield of the spring wheat studied varieties, triticale and barley varied from 6.7 to 9.5 t/ha, chaffy oats - from 5.7 to 5.9, hulless oats - from 4.4 to 4.6 t/ha. At the beginning of the growing season of crops in the 0-0.40 m layer, the stocks of nitrate nitrogen were close to the stocks of the autumn observation period of 2019, and ammonium nitrogen decreased by 285 kg/ha.

2018 ◽  
Vol 21 (02) ◽  
pp. 75-77
Author(s):  
O A Vlasenko

Rapeseed and rapeseed and millet mixtures are cultivated, the supply of chernozem with nitrate nitrogen is low and medium, the supply of ammonium nitrogen is high. The availability of mobile phosphorus is reduced by the end of the growing season. The availability of exchange potassium for these crops is very high.


2020 ◽  
Vol 6 (5) ◽  
pp. 224-232
Author(s):  
R. Guliyeva

The article shows the influence of mineral and organic fertilizer norms on gray–brown soils and changes in the nutritional regime in winter wheat soils under irrigation in the Ganja–Gazakh region. It was found that the application of mineral and organic fertilizers for winter wheat in gray–brown soils significantly affected the change in the nutrient regime of the soil, significantly increasing the amount of nutrients easily absorbed by plants in the plowed and subsoil layers of the soil, as compared to the control (unfertilized) option, effective fertility increased, which in turn had a significant impact on productivity. At the end of the growing season, depending on the norm of mineral fertilizers in the soil layer 0–60 cm, ammonia nitrogen is 13.1–14.1, nitrate nitrogen is 7.2–7.4, mobile phosphorus is 7.0–8.0 and exchangeable potassium — 15.6–19.2 mg/kg, depending on the rate of organic fertilizers at the end of the growing season, ammonia nitrogen 12.6-–13.7, nitrate nitrogen 5.3–5.7, mobile phosphorus 6.2–6.6 and metabolic potassium while it increased by 20.4–21.2 mg/kg.


Author(s):  
A. V. Lednev ◽  
A. V. Lozhkin ◽  
G. A. Pozdeev

The results of many years field experiment on the remediation of agro-sod-podzolic loamy soil (albeluvisoils) contaminated with nickel are analyzed. Various doses of ameliorants and fertilizers were studied as ameliorative additives: limestone and phosphorite flour, superphosphate, sodium sulfide, peat and zeolite. Studies have shown that the introduction of all studied reclamation additives into contaminated soil significantly reduced the content of mobile forms of nickel in it. The highest efficiency during the entire observation period was shown by limestone flour at a dose of 12 t/ha; it reduced the degree of its mobility by 48-69%. Nickel pollution had a strong toxic effect on plants, which led to a sharp decrease in their productivity (by 76-87%) and increased accumulation of nickel in the grain. The introduction of the studied ameliorants and fertilizers significantly improved these indicators, but they still did not reach the control (without pollution), which indicates the presence of a very serious problem of crop production on land contaminated with nickel.


Soil Research ◽  
1970 ◽  
Vol 8 (1) ◽  
pp. 21 ◽  
Author(s):  
AW Moore ◽  
JS Russell

A lateritic podzolic soil and a solodized solonetz soil, with histories of organic matter increase under tropical and temperate pastures respectively, were incubated over a period of a year with a weekly wetting and drying cycle. Decreases in organic matter (7 and 11%), total nitrogen (12 and 10%), and non-distillable acid-soluble nitrogen (30 and 25%) occurred, but there were no significant changes in residual nitrogen. Although there were marked increases in mineral nitrogen at the beginning of the incubation in both soils, nitrification was relatively poor in both soils. In a short-term (4 weeks) incubation of a lateritic podzolic soil and a grey clay soil the addition of labelled nitrogen followed by fractionation allowed nitrogen transformations to be examined precisely. Although differences in total nitrogen (labelled + unlabelled) with time were not statistically significant (P = 0.05) in the sandy soil (lateritic podzolic) a loss (28%) of total labelled nitrogen did occur. Parallel with this was an increasing incorporation of labelled nitrogen in all three organic fractions and a disappearance of ammonium nitrogen without the appearance of an equivalent amount of nitrate nitrogen. On the other hand, in the clay soil there was no loss of total labelled nitrogen with time and little incorporation of labelled nitrogen in the organic fractions after the first week. There was little change in the pool of labelled mineral nitrogen between the first and fourth weeks, but virtually complete and quantitative conversion from ammonium nitrogen to nitrate nitrogen. Some of the results point to varying biological lability of chemical fractions of soil nitrogen. These fractions are unlikely to be of much use as indices for sensitive measurement of nitrogen changes in the field, however, possibly because of the continuing accretion and losses which occur in the field.


Author(s):  
А. М. Grebennikov ◽  
V. А. Isaev ◽  
S. А. Yudin ◽  
S. V. Saprykin ◽  
Yu. I. Cheverdin

In the conditions of field experience, the influence of different methods of primary processing (plowing, dump, surface and zero) on the reserves of nutrients (nitrate nitrogen, mobile phosphorus and exchangeable potassium) at depths of 0…10, 10…20 and 20…30 cm and in the layer 0…30 cm was considered. The degree of heterogeneity of the arable layer was estimated by the coefficient of variation at depths of 0…10 and 10…20 cm for each plant nutrient being determined. Stocks of all nutrients both at separate depths and in the layer 0…30 cm of agrochernozems under the conditions of the experiment increased by the end of the growing season of winter wheat. It is shown that the increase in nitrate stocks most significantly occurred when using small treatments, the depth of the impact on agrochernozems which did not exceed 10 cm (surface and zero treatment). The highest reserves of mobile phosphorus in the layer 0…30 cm had the options of experience with in-depth treatment of agrochernozems. However, during the growing season, the rate of increase in the reserves of this food element in the specified layer was higher in options with small treatments due to their significant increase at the upper depths. Approximately the same picture was observed for the exchange of potassium. Clear, observed time trends of homogeneity of arable horizon on stocks of batteries depending on the considered methods of tillage, have been identified. The expected trend related to a higher degree of homogeneity of the distribution of nutrients in the arable horizon of ploughing plots compared to other variants of experience, especially with zero treatment, is not always confirmed.


2020 ◽  
pp. 115-124
Author(s):  
Zhanna A. Rupasova ◽  
Alexandr P. Yakovlev ◽  
Pavel N. Bely ◽  
Svetlana F. Zhdanets ◽  
Ol’ga S. Kozyr’ ◽  
...  

The article deals with the results of a biennial (2017–2018) comparative study of physico-chemical and agrochemical properties of the residual layer of a peat deposit under the plantation of two-year virginal plants of model Vaccinium corymbosum varieties (Northcountry, Bluecrop and Northland) on a recultivated developed lowland peat deposit under introduction of complete mineral fertilizer (‘Rastvorin’ brand ‘B’, N16P16K16), microfertilizer (Nanoplant-8, including eight trace elements: Co, Mn, Cu, Fe, Zn, Cr, Mo and Se) and organic fertilizers (Ekosil and Gidrogumat). In all variants of the experiment in both years of observations during the growing season in the root-inhabited layer, an increase relative to the initial level of the content of hydrolysable nitrogen and exchange potassium was found against the background of a decrease in the content of mobile phosphorus. In the first season, a slight increase in the level of hydrolytic acidity was registered, while the amount of absorbed bases decreased against the background of opposite changes in these indicators in the second season. In the first year of application of fertilizers by the end of the season, a significant enrichment of the substrate with mainly nitrate form of nitrogen and exchange potassium was established, with no noticeable changes in the content of mobile phosphorus. In the second year of application of fertilizers, there was a replenishment of ammonium nitrogen reserves with a predominant depletion of nitrate nitrogen, mobile phosphorus and exchange potassium (the greatest with Nanoplant and organic fertilizers treatment), which is due to the most intensive expenditure on the formation of the aboveground phytomass of experimental plants.


Author(s):  
T. Prilipko ◽  
R. Yakubash

The results of the study of the basic physical, chemical, microbiological and hydrochemical characteristics of water ponds for growing freshwater fish. Data analysis hydrochemical regime studied ponds throughout the observation period showed that it was relatively stable fluctuated within small and do not exceed the maximum allowable substances in water. PH of water management ponds research ranged 6.1 – 7.5. Nitrites and nitrates were also in small concentrations that do not exceed regulatory and amounted to 0.1 mg N/l and 1.1 mg N/l. Established in the summer studied water samples contained more E.coli, than in the spring and autumn months and had a circle–titer less than 0.1 in 18.3% of cases. Indicator KMAFAnM water was almost 13 times higher in summer compared to spring and autumn. KilkistE.coli fall in surface water was on average within 1 – 3 CFU / cm3, and in the summer 6– 9. In the bottom water kilkistE.coli autumn was on average within 0 – 1 CFU / cm3, and in the summer 5 – 9 cfu / cm3. Indicator Value KMAFAnM in the mud was higher than the value in the bottom water fall nearly 210 times in the summer – in 417 times.


2021 ◽  
pp. 116-121
Author(s):  
N. N. Dubenok ◽  
A. V. Gemonov ◽  
A. V. Lebedev ◽  
O. E. Efimov ◽  
A. A. Prokhorov

Relevance. The use of irrigation is one of the directions of intensification of fruit growing. Drip irrigation is considered one of the promising methods of irrigation, which provides the creation of the most favorable conditions for the growth and development of plants, makes it possible to supply irrigation water directly to their roots and allows the use of automation tools in the irrigation process. The results of ongoing scientific research show that changes in the water-physical and agrochemical properties of soils can be observed on irrigated lands. For the Central Region of the Non-Chernozem Zone of Russia, studies on the influence of drip irrigation on soil properties are fragmentary.Methods. Field studies were conducted on the territory of the educational experimental farm of the Michurinsky Garden fruit growing laboratory of the Russian State Agrarian University - Moscow Timiryazev Agricultural Academy. A two-factor experience in the study of different ranges of moisture for the formation of varietal plum seedlings grafted on plum tree stock was laid in the spring of 2018. Before setting up the experiment, organic fertilizers were introduced in the form of horse manure with sawdust in the amount of 100 t/ha. Soil moisture was controlled using tensiometers, calibrated based on the data of the thermostat-weight method. Irrigation rates were set in such a way as to increase the moisture content by 20% of the lowest moisture capacity. The identification of the main agrochemical and water-physical properties of the soil in the experimental plot was carried out according to generally accepted methods and techniques.Results. The data obtained on the characteristics of the water-physical and agrochemical properties of sod-podzolic soil make it possible to reasonably design the irrigation regime, reclamation and agrotechnical measures. The results of the study show that the local irrigation of soils with sparing irrigation rates with the application has led to certain changes in some soil parameters. However, the obtained research results suggest that in quantitative terms, these changes are not yet significant.


Author(s):  
П.А. Котяк

Представлены результаты исследования уровня общей токсичности и микробного токсикоза дерново-подзолистой глееватой почвы при антропогенной нагрузке. Изучение токсичности почвы особенно актуально в агроценозах, где человек в значительной мере регулирует условия произрастания растений. Использование показателей токсичности при оценке агротехнических приёмов позволяет усовершенствовать существующие технологии, чтобы избежать нежелательных сопутствующих эффектов при агрогенном воздействии на агроэкосистемы. Сравнительный анализ полученных результатов показал, что почва опытного участка в начале вегетации имела класс средней и низкой токсичности (индекс токсичности фактора (ИТФ) от 0,63 до 0,82), а в конце вегетации – класс высокой и средней токсичности (ИТФ от 0,35 до 0,55). Оценка микробиологической токсичности почвы исследуемых вариантов опыта по всхожести семян тест-культуры показала в основном средний уровень микробного токсикоза: 69,75% – на индуцированных образцах, 60,97% – на контрольных образцах. Урожайность зелёной массы ярового рапса находилась на невысоком уровне, что могло быть связано с неблагоприятными погодными условиями вегетационного периода и варьировала в пределах от 76 до 218 ц/га. Проведённые исследования по установлению влияния антропогенной нагрузки на токсический статус дерново-подзолистой почвы в условиях Ярославской области показали, что лучшими характеристиками обладают варианты: система отвальной обработки почвы, фон «Органо-минеральный субстрат + NPK» как с внесением гербицида, так и без его применения при возделывании ярового рапса. В этих условиях снижается общая токсичность почвы, статус микробного токсикоза не меняется, что позволяет сохранять почвенное плодородие, иметь оптимальное фитосанитарное состояние и получать качественный урожай выращиваемых культур. The results of the research of general toxicity level and microbial toxicosis of soddy podzolic gleyic soil at man-caused load are presented. The study of soil toxicity is especially important in agrocenoses, where a person largely regulates the conditions of plant growth. The use of toxicity indicators in assessing agricultural practices allows improving existing technologies in order to avoid undesirable concomitant effects during agrogenic effects on agroecosystems. A comparative analysis of the obtained results showed that the soil of the test area at the beginning of the growing season had a medium and low toxicity class (factor toxicity index (FTI) from 0.63 to 0.82) and at the end of the growing season it had a high and medium toxicity class (FTI from 0.35 to 0.55). Assessment of the microbiological toxicity of the soil of test variants under investigation by seed germination of the test-crop showed mainly the average level of microbial toxicosis: 69.75% on the induced samples, 60.97% on the control samples. The yield of green mass of spring rape was at a low level, which could be associated with unfavorable weather conditions of the growing season and varied from 76 to 218 hkg / ha. Researches conducted to establish influence of man's activities on the toxic status of soddy podzolic soil in the conditions of the Yaroslavl region showed that the best characteristics are options: a system of moldboard tillage, background "Organic-mineral substrate + NPK" both with the herbicide application and without its use in the cultivation of spring rape. Under these conditions the general toxicity of the soil decreases, the status of microbial toxicosis does not change which allows maintaining soil fertility, having an optimal phytosanitary condition and obtaining a quality yield of crops grown.


1959 ◽  
Vol 31 (1) ◽  
pp. 268-281
Author(s):  
Jaakko Kivekäs ◽  
Erkki Kivinen

60 peat samples from northern Finland representing different types of peat were incubated in a laboratory at a temperature of 17—18° C. The ammonium nitrogen, the nitrate nitrogen and the pH in the samples were determined after one month of incubation as well as after three months of incubation. The results were compared to results from determinations made before incubation. An attempt was made to elucidate the factors that influence the mobilization of nitrogen. On the basis of the above results it is evident that the differences between the various peat types as mobilizers of nitrogen are under these circumstances not very distinct, nor do these differences seem to be dependent on the types of peat. The following facts can, however, be established: In the amounts of ammonium nitrogen an increase takes place in most groups of samples during the first month. This increase is fairly big in the Sphagnum-dominated peats. The increase in ammonium nitrogen continues in the unlimed samples in most peat groups during all three months of incubation. After three months of incubation the amount of ammonium nitrogen in the limed samples is smaller than in the unlimed samples, although it is usually bigger than in the original samples. After the first month of incubation the amounts of nitrate nitrogen in all types of peat have decreased compared to the amounts in the original samples. In the limed samples the decrease is not as great as in the unlimed ones. After three months of incubation the amount of nitrate nitrogen has considerably increased as compared to the amount after one month of incubation. In the limed samples it might to some extent exceed the original amount of nitrate nitrogen, however, this is seldom the case in the unlimed samples. If the results are calculated on the basis of weight unit, it can be stated that the ability to mobilize nitrogen is greater in the Sphagnum peats than in the other peat groups. Working out the results in kg per ha it will be noted that somewhat more nitrogen is mobilized in the Carex-dominated than in the Sphagnum-dominated peats. The results obtained by experiments in the laboratory are not directly applicable to conditions in the field.


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