scholarly journals Main elements of nutrition content in the soil for maize crops, depending on the predecessors and methods of soil treatment

2020 ◽  
Vol 161 ◽  
pp. 01103
Author(s):  
Alexey Kozhukhov ◽  
Alexander Gurin ◽  
Svetlana Rezvyakova
Keyword(s):  
Green Manure ◽  
Nitrate Nitrogen ◽  
Arable Land ◽  
Soil Layer ◽  
Soil Treatment ◽  
Soil Horizon ◽  
Ordinary Chernozem ◽  
Available Phosphorus ◽  
Exchangeable Potassium ◽  
Land Control

The article presents data on the study of the main nutrition elements in the soil under maize crops, depending on the predecessors and methods of soil treatment in the conditions of ordinary Chernozem. The object of research is a Krasnodarsky 194MV hybrid of maize. Variants: 1. Fallow arable land (control); 2. Lupine as green manure; 3. Peas as green manure; 4. Binary sowing of lupine and peas as green manure; 5. Soy as green manure. The experiment was repeated three times, field placement was randomized, and area of each was 120 m². Agrotechnics of maize cultivation in the experiment corresponded to the recommendations for this zone. Green manure was plowed in during its reproduction phase. In the variants with green mass plowing to a depth of 23–25 cm, the largest amount of nitrate nitrogen was in the soil layer 0–20 cm. In the specified soil horizon, before sowing maize, the content of nitrate nitrogen ranged, depending on the variant, from 24.7 mg/kg to 42.8 mg/kg. In the soil layer 20–40 cm, the amount of nitrogen was lower, just 19.4–29.5 mg/kg. Similar dependence was observed for maize during its flowering phase. Tillage methods had almost no effect on the accumulation of nitrate nitrogen in the upper soil layer (0–20 cm). As in all the variants, the differences in this indicator were within the experimental error. However, the content of nitrate nitrogen during the growing season was different. The greatest amount of it was observed during the spring period, both in versions with plowing to a depth of 25–28 cm and in versions with blade loosening to a depth of 10–12 cm. The smallest amount of available phosphorus, regardless of the method of soil preparation, in the layer 0–20 cm was on fallow arable land – 122 mg/kg during the sowing period and 104 mg/kg during the flowering period. In variants with cultivation of legumes as green manure, the content of available phosphorus in the specified horizon was significantly chigher, being 147–171 mg/kg. The highest content of exchangeable potassium was provided by lupine – 209–213 mg/kg in the 0–20 cm soil layer, and lupine sown together with peas – 196–207 mg/kg. The minimum amount of exchangeable potassium was 143–146 mg/kg in fallow arable land, depending on the method of soil treatment.

scholarly journals Phosphate regime of sod-podzolic soil in natural and agrophytocenoses

2021 ◽  
pp. 92-115
Author(s):  
M. T. Vasbieva ◽  
N. E. Zavyalova
Keyword(s):  
Podzolic Soil ◽  
Fractional Composition ◽  
Calcium Phosphates ◽  
Arable Land ◽  
Soil Layer ◽  
Total Content ◽  
Available Phosphorus ◽  
Iron Phosphates ◽  
Phosphorus Forms

The phosphate regime of sod-podzolic soil (heavy loam) of Cis-Urals under natural phytocenoses (mixed forest, cereal-grass meadow) and agrophytocenoses was studied. The influence of agricultural use of arable land on phosphate regime was evaluated in the long-term stationary experiment (year of establishment – 1978) and the eastern galega (Galega orientalis L.) (year of sowing – 1988). The total content of phosphorus in soil, quantity of its organic, mineral and plant available forms were studied, the fractional composition of mineral phosphates was considered (using Ginzburg-Lebedeva method). The total content of phosphorus in the upper soil layer in all studied objects varied from 1 030 to 1 350 mg/kg. Mineral phosphorus forms prevailed over organic ones in the soil. It was found that the fractional composition of mineral phosphates was 40–62% represented by iron phosphates and 31–48% by calcium phosphates, which is due to the characteristic features of the soil-forming rock – yellow-brown non-carbonate silt drape. Aluminum phosphates amounted to 8–12%. Long-term cultivation of crops during five cycles of the eight-field crop rotation led to a significant decrease in the content of organic phosphorus in the soil. The lower content of iron phosphates (1.6–1.8 times) and the higher content (1.3–2.0 times) of calcium phosphates, available for plants, were observed in the soil of long-term experiment when compared with natural phytocenoses. The content of plant available phosphorus in soil gradually decreased from 239 to 164 mg/kg from the moment of experiment establishment to the fifth rotation. Prolonged fertilizer application (N60P60K60) resulted in the significant increase in mineral and plant available phosphorus forms content in the soil. The residual phosphorus of fertilizers was noted in the Fe-P, Ca-PI and Ca-PII fractions. Under the eastern galega the quantitative and qualitative indicators of the phosphate regime of the soil did not differ significantly from their natural analogues.

scholarly journals Influence of Fertilization on Gray-Brown Soils on Change of Food Mode in Soil Under Winter Wheat

2020 ◽  
Vol 6 (5) ◽  
pp. 224-232
Author(s):  
R. Guliyeva
Keyword(s):  
Winter Wheat ◽  
Nitrate Nitrogen ◽  
Organic Fertilizer ◽  
Soil Layer ◽  
Growing Season ◽  
Ammonia Nitrogen ◽  
Organic Fertilizers ◽  
Mineral Fertilizers ◽  
Exchangeable Potassium ◽  
Mobile Phosphorus

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.

Effect of Non-flooded Plastic Film Mulching Cultivation for Rice in Southeast China

Weed Science ◽  
2017 ◽  
Vol 66 (1) ◽  
pp. 134-141 ◽  
Author(s):  
Xin Yang ◽  
Wenhai Mi ◽  
Xiaoli Tan ◽  
Lianghuan Wu ◽  
Vladimir G. Onipchenko
Keyword(s):  
Rice Yield ◽  
Soil Layer ◽  
Abundant Species ◽  
Available Phosphorus ◽  
Plastic Film ◽  
Exchangeable Potassium ◽  
Weed Species ◽  
Plastic Film Mulching ◽  
Weed Diversity ◽  
Film Mulching

The effects of non-flooded plastic film mulching cultivation (PM) and polymer-coated urea (PCU) on rice yield, soil properties, and weed diversity were investigated in experimental plots of rice monoculture in Lanxi, China. The combination of PM and PCU increased rice yield. Compared with traditional flooded cultivation, under PM, soil pH remained higher, but decreased soil organic matter, total nitrogen, available phosphorus, and exchangeable potassium in the 0- to 10-cm soil layer. Soil fertility influenced winter weed communities, with hairy bittercress, Asian mazus, and shortawn foxtail being the most abundant species. Multivariate analysis indicated that changes in the winter weed species diversity were primarily due to exchangeable potassium. PCU had no significant influence on weed diversity, while plots without nitrogen fertilizer had higher spring-germinating weed density.

scholarly journals The content of exchangeable potassium in the soil depending on the method of tillage and meteorological factors

2021 ◽  
pp. 41-48
Author(s):  
Ya. A. Pogromska ◽  
Keyword(s):  
Meteorological Factors ◽  
Regional Climate ◽  
Soil Layer ◽  
Mineral Fertilizer ◽  
Regional Climate Change ◽  
Ordinary Chernozem ◽  
General Tendency ◽  
Exchangeable Potassium ◽  
Hydrothermal Coefficient ◽  
Fertilizer System

The article is a continuation of a series of publications on the results of the study of nutrient elements in the soil-plant system against the background of global and regional climate change, given the possibility of minimizing tillage. In the conditions of stationary field experiment on ordinary chernozem (Calcic Chernozem) in the Donetsk region for five years (1994-1998) it was monitored the content of exchangeable potassium in the arable layer of the soil under the row crop corn within the grain-growing crop rotation on the options of plowing and subsurface non-turning tillage under the same mineral fertilizer system. At the same time, the dynamics of precipitation and air and soil temperature were recorded. According to the results of research, it is a steady effect of meteorological factors on the level of potassium nutrition of plants and a general tendency to decrease the average level of exchangeable potassium contents in the soil under vegetative plants of maize within the arable layer, mainly due to layers of 10-20 cm and 20-30 cm. It is shown that for plowing the optimum of humidity of the previous year is characterized by hydrothermal coefficient of Selianinov (HTC) 1.0, and for subsurface non-turning tillage - 1.25. With a very dry (HTC 1.5), subsurface non-turning tillage may be more favorable for potassium mobility. But within the HTC 0.5-1.5 is more acceptable plowing. It is determined that the refusal to plowing leads to a decrease in the dependence of potassium mobility in the soil layer 0-30 cm on temperature, protecting from temperature fixation of potassium, and enhances the influence of the humidification regime in May. But dry and cool autumn is a likely cause of reduced potassium mobility without plowing. All conclusions are confirmed by the results of correlation, regression and variance (ANOVA) analysis.

scholarly journals Nutrient regime of irrigated meadow-chernozem soils under long-term intensive use

2021 ◽  
Vol 51 (2) ◽  
pp. 5-12
Author(s):  
I. F. Khramtsov ◽  
V. S. Boyko
Keyword(s):  
Mineral Nutrition ◽  
Arable Land ◽  
Irrigated Agriculture ◽  
Available Phosphorus ◽  
Forest Steppe ◽  
Exchangeable Potassium ◽  
Agricultural Technologies ◽  
Mobile Phosphorus ◽  
Intensive Use

The patterns of phosphorus and potassium status of soils were studied given the improvement of agricultural technologies of irrigated agriculture. Long-term studies were carried out in an experimental grain-grass crop rotation on irrigated meadow-chernozem soil. The experimental plot is located in the southern forest-steppe of Omsk region. Intensive use of irrigated arable land with a rational combination of moisture and mineral nutrition regimes contributes to obtaining maximum yields of forage and grain crops. The creation of various conditions for mineral nutrition due to an increased and high supply of mobile phosphorus and with the application of different options of agricultural technologies made it possible to simulate possible agro-ecological conditions that form contrasting indices of crop productivity. A comparative assessment of the effectiveness of various agricultural approaches to growing crops under irrigation conditions indicates that soil cultivation techniques and forecrops did not significantly affect the content of available phosphorus in the soil. The equilibrium content of mobile phosphorus given a long-term negative balance changed insignificantly. The systematic application of phosphorus-containing fertilizers significantly increased the phosphate status of the soil. However, an adequate assessment of the phosphate status of arable soils is possible using several diagnostic indices (methods). Long-term intensive use of irrigated arable land has reduced the reserves of easily exchangeable potassium from 4 to 1–2 mg/100 g of soil in the arable layer. The content of exchangeable potassium has also decreased by almost 2 times, but the soil remains in a high and very high class of its availability. However, a number of indicators show its increasing depletion in the most mobile fractions of soil potassium. The reserves of non-exchangeable potassium are more stable, which have decreased by about 19% over 40 years, and the soil has passed into the category with an unstable supply.

scholarly journals CONCENTRATION OF NITRATE NITROGEN IN THE SOIL AND PRODUCTIVITY OF CROPS WHEN LONG-TERM MINIMIZING OF TILLAGE ACCORDING TO VARIOUS FORECROPS

2019 ◽  
pp. 59-66
Author(s):  
V. E. Sineshchekov ◽  
G. I. Tkachenko
Keyword(s):  
Nitrogen Content ◽  
Crop Rotation ◽  
Nitrate Nitrogen ◽  
Soil Layer ◽  
Soil Treatment ◽  
Nitrate Content ◽  
Forest Steppe ◽  
Grain Crops ◽  
River Region

In a multifactor stationary field experiment on the area of the Elitnoye Holding in the Novosibirsk region (central forest-steppe subzone) in 2002-2018 the seasonal dynamics of nitrate nitrogen in the fields of four full grain-steam crop rotation by steam and grain predecessors against an extensive background (without chemical means) in four versions of the main mechanical treatment of leached black soil was investigated. Along with this, the productivity of grain crops was studied with long-term minimization of the main tillage on extensive and intensive backgrounds. The authors found out that in the central forest-steppe of the Ob river region before sowing grain crops according to the various methods of steam preparation most of all in the meter layer of nitrate soil was found in black steam with plowing (150 kg / ha) and less in variants with soil-protective treatments (132-141 kg / ha ). The lowest level of this element in the soil (124 kg / ha) in spring was noted by the early minimum steam. Before sowing the second wheat after steam, the nitrate nitrogen content in the meter soil layer for plowing (79 kg / ha) was slightly higher than in the options with soil treatment (61-64 kg / ha). In the final field of crop rotation, regardless of the studied soil cultivation systems, the minimum initial amount of nitrogen (56-57 kg / ha) was noted. By the end of the growing season of crops, the nitrate content in the soil was sharply reduced. Before harvesting wheat by steam, the nitrogen content in the upper meter profile was 41-55 kg / ha, for grain precursors even less - 27-33 kg / ha. The steam yield of grain crops on extensive and intensive backgrounds was 3.09-3.21 and 3.96-4.02 t / ha, respectively, and practically did not depend on the methods of its preparation. On repeated sowing the wheat yield in comparison with an extensive background in plowing (1.26-1.79 t / ha) was significantly higher than in the studied options for minimizing the main tillage (1.02-1.55 t / ha). When optimizing the mineral nutrition of plants and the phytosanitary situation of crops, wheat productivity by grain predecessors in crop rotation fields increased 2.0-2.9 times without significant differences in soil treatment options.

scholarly journals Nutritional Regime of the Soil and Growth Activity of the Apple Tree Root System in Orchards with Legume-Cereal Grass Intercropping

2021 ◽  
Vol 247 ◽  
pp. 01029
Author(s):  
Aleksandr Gurin ◽  
Svetlana Rezvyakova ◽  
Nikolay Revin
Keyword(s):  
Apple Tree ◽  
Nitrate Nitrogen ◽  
Soil Layer ◽  
Red Clover ◽  
Exchangeable Potassium ◽  
Tree Roots ◽  
Timothy Grass ◽  
Control Option ◽  
Mobile Phosphorus ◽  
Growth Activity

This work aims to study the influence of legume-cereal grasses in the inter-row spacings of the garden on the content of nutrients in the soil and the growth of apple tree roots. The amount of nitrate nitrogen was in direct proportion to the ratio of the legume component in the phytocenosis. The nitrogen content in the control option was the smallest: 19.7 mg/kg in the soil layer of 0-30 cm and 13.4 mg/kg in the layer of 30-60 cm. In the case of natural grassing-down between rows, cereal forbs prevailed. The largest amount of nitrate nitrogen was achieved when sowing the red clover and timothy grass in a ratio of 7:3. The accumulation of nitrate nitrogen is due to the activity of nodule bacteria on the roots of red clover. The accumulation of mobile phosphorus and exchangeable potassium depends on the amount of mowed mass in the inter-row spacings of the garden. The lowest content of mobile phosphorus was detected for natural grassing. In the control option, its amount was 118 mg/kg. In the 0-30 cm soil layer, the content of mobile phosphorus was 127.4-142.6 mg/kg depending on the ratio of legume-cereal grasses, and it amounted to 95.1-103.2 mg/kg in the 30-60 cm layer. For the ratio of red clover and timothy grass 3:7, the highest phosphorus content was detected. The intercropping of the garden with a legume-cereal herbal mixture also contributed to a greater accumulation of exchangeable potassium in the soil relative to natural grassing-down - 122.3-134.9 mg/kg. The optimal ratio of legume-cereal component was 3:7. A higher growth activity of the roots of the apple tree was noted in the option with sodding with a mixture of red clover and timothy grass in a ratio of 7:3.

scholarly journals The effect of different rates and forms of sulphur applied on changes of soil agrochemical properties

2008 ◽  
Vol 54 (No. 4) ◽  
pp. 171-177 ◽  
Author(s):  
M. Skwierawska ◽  
L. Zawartka ◽  
B. Zawadzki
Keyword(s):  
Soil Layer ◽  
Soil Horizon ◽  
Soil Reaction ◽  
Available Phosphorus ◽  
First Year ◽  
Soil Layers ◽  
Fertilization Rates ◽  
North East ◽  
Agrochemical Properties ◽  
Soil Agrochemical Properties

A three-year field experiment was conducted from 2000 to 2002 in North-East Poland. Each year three sulphur fertilization rates in the form of sulphate (S-SO<sup>2–</sup><sub>4</sub>) and pure (S-S<sup>0</sup>) sulphur were applied: 40, 80 and 120 kg/ha. In the soil horizon at the depth of 0–40 cm the triple rate of S- and S-S<sup>0</sup>) depressed soil reaction. Acidification of soil caused by S-SO<sup>2–</sup><sub>4</sub> became evident already in the first year of the study while that resulting from S-S<sup>0</sup>) application appeared as late as in the third year. The effect of sulphur on soil in the 40–80 cm horizon was irregular. As the sulphur rates increased and the duration of the experiment progressed, sulphates accumulated in soil. In the 0–40 cm soil layer, the increasing rates of sulphur tended to increase the content of N-NH<sup>+</sup><sub>4</sub>. In most objects, the NPK + S fertilization, and especially the single S-SO<sup>2–</sup><sub>4</sub> treatment, caused an increase in N-NO<sup>–</sup><sub>3</sub> in both soil layers compared with the NPK fertilized object. The dose of 120 kg/ha S-SO<sup>2–</sup><sub>4</sub> caused a significant increase in the concentration of available phosphorus in soil in the 0–40 and 40–80 cm layers.

scholarly journals Chemical properties and fertility analysis of dredger-fill silt during soil formation: The tianjin dredge–fill project

2017 ◽  
Author(s):  
Huijun Gu ◽  
Xin Sui ◽  
Guogang Zhang ◽  
Meiqing Jia
Keyword(s):  
Nitrate Nitrogen ◽  
Chemical Properties ◽  
Soil Formation ◽  
Principal Component ◽  
Available Phosphorus ◽  
Forming Process ◽  
Factors Affecting ◽  
Ecological Problems ◽  
Dredger Fill ◽  
Fertility Analysis

Dredger-fill silt has been used in the port of Tianjin, China to reclaim land; however, the dredger-fill silt has no soil ecological function. Translating the silt into soil rapidly and accelerating the soil-forming process are key to solving the ecological problems of the Dredge–Fill project. This study measured 15 chemical properties of the dredger-fill silt for 8 years of the soil forming process to explore fertility changes and the critical factors affecting soil formation. The results showed that: (1) the salinity of silt changed from severe to mild with a reduction in Na+ and Cl- concentration. Other ion concentrations changed slightly. (2) Effective nutrients significantly decreased during soil formation. Soil organic matter (SOM)，the nitrate-nitrogen, available phosphorus (A-P) and available potassium (A-K) decreased by 26.22%, 86.23%, 45.92%, 33.61% respectively, indicating severe nutrients loss. (3) Principal component analysis showed that silt fertility decreased significantly and the total soil fertility loss was severe. This study has significance for the artificial improvement of silt.

scholarly journals Sourse degradation - global environmental problem

2017 ◽  
pp. 63-70 ◽  
Author(s):  
Myroslav Voloshchuk
Keyword(s):  
Soil Degradation ◽  
Agricultural Land ◽  
Arable Land ◽  
Soil Layer ◽  
Organic Fertilizers ◽  
Economic Losses ◽  
Complex Situation ◽  
Erosion Processes ◽  
Fertile Soil ◽  
Catchment Areas

Based on generalization of literary sources, normative legal, stock materials and experimental data, the complex situation of soil degradation is highlighted. Different types and intensity of the manifestation of soil degradation, their distribution and characteristics are described. The threatening situation of manifestation of degradation processes in some regions of Ukraine is shown, among which soil erosion occupies the leading place. More than 4.5 million hectares are occupied by medium and strongly ground soils, including 68 thousand hectares completely lost their humus horizon. Particularly large areas of eroded soils are distributed on arable land in the Vinnytsia, Luhansk, Donetsk, Odesa, Chernivtsi and Ternopil regions, where the average annual ground wash is 24.5–27.8 t/ha with a tolerance of 2.5–3.7 t/ha. As a result of erosion processes from the total area of agricultural land, about 500 million tons of fertile soil layer is washed out on average annually, which contains about 24 million tons of humus, 0.96 million tons of nitrogen, 0.68 million tons of phosphorus and 9.4 million tons of potassium equivalent to 320–333 million tons of organic fertilizers, and ecological and economic losses due to erosion exceed 9 billion UAH. Flat soil was associated with linear erosion. The main indicators characterizing the degree of damage to land by linear erosion are the density of ravines, the distance and area between them, the slope, the properties of soils and rocks, the morphometric parameters of the ravines and their catchment areas. According to various estimates, the area of land affected by linear erosion in the country increases by 5–10 thousand ha annually. The effect of the ravines on the complete destruction of the land, deformation of the soil cover is highlighted. Information on various types of soil pollution by poison chemicals, industrial waste is given. According to the prediction of scientists in such a situation, 120–150 years on the planet can destroy the fertile soil layer. Key words: erosion, dehumidification, pollution, waterlogging, acidity, degraded land.

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