Abstract

As a result of the studies carried out by the Department of Chemistry, Agrochemistry and Agroecology to improve the physicochemical parameters of sod-podzolic soils in the conditions of the Pskov region, positive results were obtained. It was noted that on the sod-podzolic sandy loam soil in the period from 2016 to 2019, in the control option, there was a gradual increase in soil acidity over the years. For 5 years, the exchange acidity increased by 0.1 units, and the hydrolytic acidity of the soil by 0.07 meq/100 g of soil. Against the background with mineral fertilizers, as well as in the control, during the study period there was no decrease in the value of exchangeable acidity, and the increase in hydrolytic acidity was not significant by 0.02 meq/100 g of soil, respectively, in relation to 2016. Application of manure in the amount of 30 and 40 t/ha contributed to a significant improvement in the acid-base state of the soil. During the years under study, exchangeable acidity decreased by 0.7-1.1 units (from 5.8 to 6.1 units), and the hydrolytic acidity of the soil decreased by 0.08 meq/100 g of soil due to the influx of stubble-root residues. Application of manure reduced the negative indicators of the Ca and Mg balance by 564 kg/ha or by 83 %, and in the organomineral and mineral options only by 64 and 39 %, respectively. The results of studies on sandy loamy sod-podzolic soil also showed a high efficiency of the influence of fertilization systems on the productivity of crops in the crop rotation link. The best performance indicators were obtained from the organomineral fertilization system.

Highlights

  • Sod-podzolic soils form the basis of the arable fund of the Non-Chernozem zone of Russia

  • Our study on soddy-podzolic sandy loam soil showed that in the control option there was a tendency towards an increase in exchangeable acidity, over the years of study it was 0.10.2 units

  • There was a gradual increase in soil acidity over the years

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Summary

Introduction

Sod-podzolic soils form the basis of the arable fund of the Non-Chernozem zone of Russia. The main way to regulate the acidity of sod-podzolic soils is the introduction of various lime materials, one of which is limestone flour. Organic fertilizers can act as regulators of the acid-base properties of soils [6, 8, 17]. Due to the reduction in use of mineral fertilizers acidifying the soil, the general rate of acidification of Russian lands may slow down, but this stagnation is temporary. The positive effect of manure is due to the fact that it has an almost neutral reaction, and is a source of calcium and magnesium, which help to neutralize soil acidity and improve its structural state [8]

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