Open Access
BIO Web Conf.
Volume 17, 2020
International Scientific-Practical Conference “Agriculture and Food Security: Technology, Innovation, Markets, Human Resources” (FIES 2019)
Article Number 00128
Number of page(s) 4
Published online 28 February 2020

© The Authors, published by EDP Sciences, 2020

Licence Creative CommonsThis is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

1 Introduction

Agriculture has now reached such a level that its further development is inevitably connected with forecasting and management of the current soil properties. The analysis of factors influencing soil fertility and agricultural productivity is relevant and in-demand at present for all regions.

Soil fertility determines the yield of crops and stimulates biological, chemical and physical, as well as other processes of soil formation. This is a systemic concept, as the soil is formed in a certain ecological state and is always influenced by the anthropogenic factor.

Currently, there is a new level of research conducted in the field of soil science — a systematic analysis of soil fertility. The various processes occurring in the soil have complex and numerous relationships and therefore this method can be considered as one of the most important and modern of soil research methods. This method is called soil fertility modelling. The main objective of modelling processes related to soil fertility is to identify the most significant factors covering the main features of the research process [1, 2].

At present, a large number of practical and theoretical materials allowing application of the methods and principles of system analysis in soil science have been accumulated. By this reasoning, the soil is evaluated as a dynamic quantitative system. In many regions of Europe, studies of the application effect of organic and mineral fertilizers on the fertility of different genesis soils are carried out. New experiments have been initiated in Sweden and Finland in order to study the impact of organic fertilizer on soil fertility [3, 4].

In Eastern Europe and the Baltic countries, studies are carried out on model changes in soil complex and organic matter after the introduction of different farming systems and fertilizers [59]. The reforms carried out in the 1990-s led to radical changes in the economy of Russia, including market relations formed in agriculture. Insufficient fertilizer application has caused degradation of soil fertility and decreased crop productivity [10].

Agricultural production has become unprofitable and many agricultural enterprises have reduced the area of agricultural land or have completely ceased their production. As a result, large areas of land have been removed from agricultural circulation. For example, only in the North-Western region of Russia, these areas amount to 2.5 million hectares [10].

Podzolic soils in their natural state are of low fertility and degrade relatively rapidly when being removed from agricultural circulation. Therefore, the return of these soils to agricultural use requires a complex of soil improvement measures. At present, agricultural enterprises with the support of regional authorities partially return the land to agricultural circulation, implement farmland reclamation programs.

At the same time, large areas of land in agricultural circulation also have poor fertility parameters from the point of view of the agricultural producer and need to be reclaimed. Soil improvement programs need to be developed on a regulatory basis that characterizes soil fertility, including optimal soil properties, soil fertility rates, costs of chemization means in order to achieve them, as well as indicators of soil fertility for different crop yield levels [1120].

2 Methods and materials

The objects of research are the experimental fields of the Leningrad Research Institute of Agriculture Belogorka and the production seeding of the North-Western region of the Russian Federation.

To solve the problem, the method of simultaneous accounting of yield and soil sampling was developed. It is necessary to have at least 50 units of observations in order to obtain reliable mathematical and statistical estimates on the studied parameters. The essence of the method is that soil and crop samples are selected in the areas of cultivated soil bodies during the period of the plant ripening.

The area of the plot is sized from 1 to 4 m2, depending on the crop and objectives of the study.

Optimal values of soil properties were determined by the diagram showing the relationship between the crop yield and the tested physico-chemical index.

The assessment of the relationship between generally accepted soil fertility indicators and crop yields is associated with methodological difficulties. In the course of a field experiment, it is difficult to provide significant fluctuations in soil properties in natural conditions. Therefore, the schemes of experiments were developed, when the necessary levels of mobile forms of phosphorus, potassium, humus, and acidity were formed due to high doses of technogenic fertilizers.

Sampling and determination of the soil agrochemical condition were determined according to common methods used in soil complex researches.

The determination of mobile phosphorus and exchange potassium was carried out in a single extract by using the A.T. Kirsanov method. The humus content was determined by the Tyurin method in Nikitin modification. The sum of the exchange bases is determined by the Kappen-Gilkowitz method in Godlin modification, and hydrolytic acidity was determined ionometrically.

The determination of the granulometric composition is carried out with the use of N.A. Kachinsky pipette. In the course of the field multifactor experiment, in order to achieve the planned levels of sod-podzolic light loamy soil reclamation, the following norms of fertilizers were introduced in the experiment variants in different combinations (per 1 ha): phosphorus fertilizers — 250, 750, 2400 kg ha−1; potash fertilizers — 300, 900, 1950, 3900 kg ha−1; lowland peat — 240, 420, 840 t ha−1; lime- 7.0; 14.5 t ha−1.

Nitrogen fertilizers for crops were introduced as a common background at a rate of N60. The initial level of soil fertility was characterized by the following indicators; humus — 1.6 -1.7%; salt pH 4.2-4.3; mobile forms of phosphorus and potassium — 8–10 mg/per 100g of soil.

3 Results and discussion

The soil environment parameters are crucial for the effective implementation of agricultural technologies [1, 21, 22]. Among a large number of indicators evaluating certain parameters of soil fertility from the point of view of fertility reproduction, the most important are the relatively stable characteristics that determine the agronomic value of soils [9, 10, 13]. Long-term research carried out in field experiments, as well as taking into account crop yields and soil properties in production seeding, allowed establishing the most favorable values of soil properties for obtaining high yields (Table 1).

In most cases, agricultural land users can not allow using of large quantities of organic, mineral fertilizers and lime to accelerate the soil improvement according to the economic criteria. The main thing that is dictated by economic conditions is getting the maximum profit from fertilizers and lime, with the obligatory observance of environmental requirements, i.e. good or at least satisfactory product quality, taking into account the minimization of soil and groundwater contamination by residues of fertilizers.

The problem of bringing soil properties to optimal parameters or at least the problem of preservation of fertility level [1214] remains relevant. The basis of fertility is the processes of accumulation and transformation of substances, energy occurring in soils. Organic matter of soil and fertilizers actively participates in these processes, affects their orientation and intensity [1516]. In theory, based on the humification coefficient, the application of 100 tonnes of manure per 1 hectare should increase the humus content in the soil by 0.2%. However, according to long-term experiments of the Leningrad Research Institute Belogorka, systematic application of manure in field crop rotation at a dose of 10 t ha−1 per year for 26 years only slightly increased the content of humus in the soil (0.15% according to 400 observations).

The annual introduction of 20 t ha−1 of manure for 17 years (336 observations) increased the humus content only by 0.27%. The fact is that along with the accumulation of humus, the processes of its decomposition are simultaneously strengthened and an unstable balance between these processes is established. According to the results of the field multi-factor experiment after applying the specified rates of fertilizers to the soil, there was certain regularity in the change of soil and agrochemical properties. The average data on the experiment variants are characterized by the long-term dynamics of individual soil properties in the arable layer (tables 24).

Long-term observations indicate a low variability of its content in the soil over time in the experiment variants, where different rates of phosphorus fertilizers were introduced. Unlike phosphorus, mobile potassium is subject to a significant change in the experiment variants after the fertilizer application. First, there is a significant accumulation of it in the arable soil layer, and then a sharp decrease. The criterion for assessing the agronomic optimum for the potassium exchange is the level of potassium nutrition, providing a high yield of agricultural crops.

It seems that the ecological balance of potassium content in the arable layer of sod-podzolic soil of light mechanical composition, according to the data we have received, occurs at its content of up to 6–10 mg /100 g of soil. There is no clear pattern in the change of mobile potassium, as well as phosphorus, depending on other soil properties.

The increase in the content of mobile forms of potassium and phosphorus in the arable soil layer per 1 mg/100 g of soil required an average introduction of 5070 kg of potassium and 120–140 kg of phosphorus fertilizers respectively.

Planned levels of high humus content in the soil were mainly achieved due to the introduction of high doses of lowland peat. Long-term observations show that the decrease in organic matter is greater than the initial level created.

In the control case, organic matter was stable throughout the observation period in case when no peat was used.

The specific reclaiming efficiency is determined by the dynamics of peat mineralization in the soil. Thus, the increase in organic matter content from 100 t ha−1 of peat for the second year after its introduction amounted to 0.33-0.36% of different peat rates, and in the future, these values decreased in the process of dynamics (see Table 3).

When applying lowland peat (pHKCl 6,8-7,0), the reaction of the soil environment changed. The shift amount of the soil reaction depends on the initial state of the soil. Thus, at the initial pH KCI — 4.2 the change from 100 t ha−1 of peat is 0.29-0.33 (peat rate 240, 420 t ha−1), and at pH — 5.7 the shift from the same rates amounted to 0.05-0.13 units of pHKCl. In the future, the reaction of the soil changed in accordance with the noted dynamics.

Specific cultivating efficiency of lime (pH shift from 1 t ha−1) depends on the applied rate. When using 7.0 t ha−1 of lime, the soil reaction varied from the initial pH 4.2 in the arable layer during the year at the rate of 1 t ha−1 to 0.19 pH units KCl, and at the lime rate of 14.5 t, to 0.14 respectively. The obtained results are consistent with the literature data. In the future, the specific efficiency of lime per 1 t ha−1 decreased significantly.

Table 1.

Favorable intervals of agrochemical properties of sod-podzolic light-loamy and sandy soils.

Table 2.

Influence of fertilizer rates on changes in the content of mobile forms of phosphorus and potassium

Table 3.

Influence of low peat application on change of organic matter content

Table 4.

Influence of lime application on soil acidity change

4 Conclusion

Modeling of soil cultivation in the conditions of the field experiment with the use of high fertilizer rates allows determining the nature of changes in soil properties over a long period of time, their long-term dynamics, as well as to establish rates for fertilizer costs in the development of programs for cultivation, reproduction of soil fertility.

It is obvious that agricultural producers can make decisions on the practical implementation of soil cultivation programs after analyzing the cost efficiency of these measures.

The practical essence of establishing optimal values of soil properties consists, first of all, in the fact that they are the theoretical basis for specialization and concentration on cultivating particular crop species, the choice of the most rational crop rotation scheme for specific field and farming conditions.

The development of criteria for optimal soil properties, expressed in specific quantitative indicators, is of great importance for scientific forecasting and development of a harvest formation program in specific soil-climatic conditions.

The established criteria of soil properties, optimal parameters serve as target functions in the development of the land reclamation program.


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All Tables

Table 1.

Favorable intervals of agrochemical properties of sod-podzolic light-loamy and sandy soils.

Table 2.

Influence of fertilizer rates on changes in the content of mobile forms of phosphorus and potassium

Table 3.

Influence of low peat application on change of organic matter content

Table 4.

Influence of lime application on soil acidity change

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