The content of heavy metals in the soil is presented in Tables 1-3.
Analysis of the results of determining the total content of heavy metals in the arable soil layer (0-20 cm) according to the variants of the experiment, which was carried out in 2017, made it possible to identify the following patterns.
In all variants of the experiment, the total content of heavy metals in the sod-podzolic light loamy soil did not exceed the approximate permissible concentrations.
The gross content of lead in the soil was higher in the control variant, as well as in the aftereffect of the mineral (N90P90K90) and organomineral fertilizer systems in three- (N90P90K90 + 9 t* ha
-1 of compost) and five-fold doses (N150P150K150 + 15 t* ha
-1 compost) (Table 1).
The content of lead in the soil of the arable layer of the control variant, which amounted to 23.9 mg kg
-1, exceeds the analogous indicators for the variants where mineral, organic and organomineral fertilization systems were used in the indicated doses.
It is necessary to clarify here that in this case there is a high probability of active removal of lead with the yield when metal ions are absorbed from the soil solution by the root system of experimental plants; we will consider this aspect when analyzing the actual accumulation of lead in oat grain.
The lowest value for the heavy metals under study was achieved in the variant with the use of a threefold dose of nitrogen (variant 2); this is probably due to the fact that ammonium nitrate, acidifying the soil solution, converts acid-soluble forms of metals into mobile salt ions, which is further accompanied by vertical and partly by planar migration in the soil profile.
The lowest value for the heavy metals under study was achieved in the variant with the use of a threefold dose of nitrogen (variant 2); this is probably due to the fact that ammonium nitrate, acidifying the soil solution, converts acid-soluble forms of metals into mobile salt ions, which is further accompanied by vertical and partly by planar migration in the soil profile. Vertical migration of such cations leads to a decrease in the content of heavy metals in the arable layer. A decrease in the accumulation of heavy metals when using mineral nitrogen fertilizer was noted for cadmium, which was 19.4% in relation to the control.
An increase in the content in the topsoil was noted for copper when compared with the control (+ 20.8%), which is probably due to the formation of strong bonds of copper with sulfates, carbonates and phosphates and against the background of a weakly acidic reaction of the soil solution, there is no additional factor that can increase mobility copper compounds in the soil absorbing complex.
Interesting data were obtained in the variant using the organic system - variant 6. According to the accumulation of copper, an increase (+ 2%) in the soil was noted in the aftereffect after prolonged application of organic fertilization.
When applying only phosphorus fertilizer (P90), as well as potassium (K90), it should be noted that double superphosphate did not contribute to an increase in the content of analyzed metals, except for cadmium. In variant 4, the increase in comparison with the control was 8.3%, undoubtedly, this is due to the supply of cadmium to the soil with fertilization in previous years.
It should also be explained why, against the background of the use of two-fold doses of mineral fertilizers and manure, the content of heavy metals exceeds the same indicators for the option with three-fold doses. This is primarily due to the removal of heavy metals with the harvest. Table 3 show the results for the yield and the actual content of heavy metals in grain.
A significant accumulation of this metal was also noted in variant 6 (N90P90K90) - with threefold doses of only mineral components and in variant 11 (N150P150K150 + 15 t* ha
-1) - with fivefold doses of all mineral fertilizers and manure. Of view of agroecology, the use of five-fold doses on sod-podzolic soil for a long time (30 years or more) can lead to a significant increase in the cadmium content in the root layer. In the future, this can cause contamination of the main products with cadmium. Probably, the application rates presented in option 10 (N120P120K120 + 12 t* ha
-1) should be considered the optimal dose of the complex application of mineral components and organic fertilizers. Analysis of the content of metals according to the variants of the experiment in the arable layer of the soil allows us to conclude that the organomineral fertilization system is most expedient from two points of view - an insignificant increasecontent of heavy metals and, at the same time, a guaranteed yield of grain with a given quality, but at lower costs for fertilizers compared option 11.
When analyzing the aftereffect of fertilizers, an increase in oat yield was noted with an increase in fertilizer doses in organomineral systems. Table 2).
The oat yield under the influence of fertilizers on average over seven years (1982, 1989, 2001, 2008, 2009) ** differed from the yield on the aftereffect on average over two years (2015, 2016). A significant difference in the aftereffect was manifested in those variants where a complex system - mineral components and organic fertilizer - was used to study the action. The yield in option 10 (N120P120K120 + 12 t* ha
-1) slightly differed (-2.2 c ha
-1) in the direction of decrease when compared with the option with five-fold doses (N150P150K150 + 15 t* ha
-1) and taking into account previously stated, it would be environmentally sound to use the doses studied in option 10.
The analysis of the accumulation of heavy metals in the grain of oats revealed the following: for all variants of the experiment, the content of permissible levels was not exceeded (Table 3).
Against the background of the use of only a threefold dose of nitrogen and potassium, as well as a threefold dose of mineral components (N90P90K90), increased indices for copper, zinc, lead and cadmium were achieved, this is probably due to the fact that the acidity in this variant at the time of determination was 4, 8; 4.8 and 5.4, respectively. An increase in acidity increases the mobility of all salt ions and, consequently, their entry into the plant and their accumulation in the final product.
In the variants with the use of mineral components and compost, the most significant differences are seen in the content of zinc, lead and cadmium and arsenic. So, at a fivefold dose (option 11), the zinc value is maximum and is 26.2 mg kg
-1 dry mass, which is probably determined by the acidity of the soil solution, which in this option is 4.6. The organic component and double superphosphate in this variant is no longer a regulating factor for stabilizing the pH in the soil against the background of high doses of nitrogen and potassium, which undoubtedly contribute to acidification.
It is also worth highlighting the ecological function of phosphorus fertilizer against the background of its use, which in the after effect, the acidity of the soil solution is already 5.2, which positively affects the stabilization of the mobility of various cations, including heavy metals. That is why the lowest content of copper and lead was noted here, which was - 2.03; and 0.042, respectively.
The most interesting results were obtained in the variant using a fourfold dose of the organomineral system (N120P120K120 + 12 t* ha
-1). With a high probability, it can be argued that such a ratio is most suitable for long-term use of the organomineral system in the conditions of the western part of the Smolensk region of the Non-chernozem zone on sod-podzolic soil.