The studies revealed that the average indicators of the content of lead, cadmium, zinc, copper in the soil are higher than Clarke, but did not exceed the MPC. Determination of mobile forms of HMs showed their variability in the upper soil layers. Natural HM levels in soils were subject to fluctuations and depended on their geochemical background, topography, climate and anthropogenic input of industrial emissions to the earth’s surface. A number of principles, such as nickel, chromium, arsenic, cadmium, lead, mercury, having no definite functional significance for plants and animals, have a toxic effect on the ecosystem as a whole.
The solution to the problem of obtaining environmentally friendly products in contaminated areas is impossible without considering the migration and accumulation of elements. The soil serves as a natural barrier for HMs, which somewhat hinders their entry into plants and migration to adjacent environments.
It is known that as long as HMs are firmly bound to the constituent parts of the soil, they are difficult for plants to access and their negative effect on the soil and plants will be insignificant
(Vinogradov et al., 2019; Lupova et al., 2020; Khabarova et al., 2018; Zubkova et al., 2021). However, if changing soil conditions allow the transfer of HMs into the soil solution, there is a direct danger of their use by plants (
Vinogradov and Zubkova, 2021;
Mustafayev and Mazhaysky, 2018;
Shchur and Valckho, 2016). Plants most actively assimilate actual reserves (extractant NH
4Ac) HMs and potential ones (1-n HCl) are used as they enter the soil solution. Table 1 and 2 show the results of the content of HMs in 1-n HCl and NH
4Ac buffer.
The lead content has exceeded Clarke (10 mg/kg) in almost all soil samples, that indicated its accumulation. Lead can reduce the mobility of molybdenum, iron, chromium, phosphorus, sulfates, carbonates in the soil. The maximum content of mobile forms of lead has been noted in the 0-20 cm layer of gray forest soils of the experimental site, which is about 40% of the total reserves. At the same time, the pollution with this element is characterized as “moderately hazardous” and “average”, respectively.
Significant fluctuations in HMs was observed in the studied soils. The excess of Clarke and MPC was observed in 41% of samples of gray forest soils of the experimental site. Therefore, according to the scale of environmental regulation, on average, gray forest soils can be classified as heavily polluted.
Copper, like mercury, inhibits enzymes, causes rupture in plant cell membranes and an increase of copper in soils causes an increase of fulvic acids in humus. These fluctuations range from 8 to 99 mg/kg in the 40-60 cm layer, which is almost 1.2 times higher than Clarke and MPC. These soils are classified as highly contaminated on the scale. The actual reserves of mobile forms of copper are insignificant, but the mobility of copper is 2 times higher in layers 0-20 and 20-40 cm than in the lower ones.
The content of total chromium in soils is below Clarke. Chromium, soluble in 1-n HCl, is along the profile of gray forest soil in the range from 1.5 to 2.0 mg/kg, that is, according to the scale of TMs ecological standardization “moderately hazardous”.
The conducted studies of the samples taken from the experimental site show that there is a relatively unfavourable ecological situation in terms of soil contamination with HMs. The soil is highly contaminated with some HMs.
Annual fluctuations in the yield of rapeseed and mustard on differently fertilized backgrounds are strongly associated with changes in weather conditions and soil fertility. An accurate and objective indicator of moisture conditions is the HTI, especially during the period of “rosette of leaves” - “flowering”
(Vinogradov et al., 2019; Vinogradov et al., 2020). With insufficient moisture and arid conditions of the marked segment of the growing season of crops, the use of increased doses of fertilizers is ineffective. The increased amount of precipitation throughout the entire period of development of rapeseed and mustard, as well as heat, allowed the maximum use of the applied mineral fertilizers, especially nitrogen fertilizers. While fertilizing for cultivation, signs of nitrogen deficiency were observed in the early stages of development and later disappeared. Nitrogen fertilizers, due to dry conditions, did not move in the soil, so it took a little longer for the roots to gain access to nitrogen.
Regardless of the nutritional background, the dynamics of linear growth of spring rapeseed and mustard plants had the same course: a uniform increase in plant height during the growing season of crops with reaching maximum values before harvesting. The studied types and combinations of mineral fertilizers had an unequal effect on the growth and development of plants.
Thus, the unilateral application of phosphorus-potassium fertilizers did not have a significant effect on the plant height of both rapeseed and mustard and was at the control level: rapeseed - 80 cm, white mustard - 62 cm, gray mustard - 77 cm. Introduction of nitrogen (N60) and full (N
60-120P
60K
60) doses of fertilizers significantly increased the considered indicator in the first half of the growing season. In the rosette phase, fertilized plants exceeded the plant height in the control by 18-36%, which indicated the predominant role of nitrogen in the processes of vegetative growth.
The interphase period - rosette-budding - was characterized by intensive growth of aboveground plant organs. The advantage of the options with the action of fertilizers remained, but the difference between fertilized plants and control was leveled in linear growth. Nevertheless, the introduction of various nitrogen-containing backgrounds increased the height of plants in comparison with the natural agrochemical background in the budding phase by 10-18%, in the flowering phase by 5-15% and in the full ripeness phase by 3-17%.
The use of higher doses of nitrogen fertilizers N
90-120 under spring rape did not have any significant effect on the onset and duration of the development phases and the growing season. However, they increased the amount of dry matter accumulation and consumption of nutrients in rapeseed. The processes of dry matter biosynthesis by rapeseed and mustard proceeded most intensively during the interfacial period “rosette of leaves - flowering”, when more than half of the final harvest was formed and more than 70% of nitrogen and potassium, as well as about 60% of phosphorus were consumed. Studies of spring rapeseed, white mustard and gray mustard plants on a higher background of mineral nutrition showed the increase of yield structure elements and, as a consequence, the yield (Fig 1).
Against the background of N
120P
60K
60, the number of rapeseed siliquae per plant was 9.6 higher than in the control. The indicator of the mass of 1,000 seeds during the study period in rape plants was within 2.7-3.5 g, it was 2.1-2.6 g in gray mustard and 3.4-3.9 g in white mustard, which corresponded to the average values for these crops. A higher level of mineral nutrition contributed to an increase in the mass of 1,000 seeds for rapeseed and gray mustard and had practically no effect on an increase in the mass of seeds for white mustard. The number of seeds in the pod of white mustard practically did not depend on the level of mineral nutrition, possibly due to the short growing season of the crop.
The highest yields, both for spring rapeseed (19.3 dt ha
-1) and for gray mustard (13.7 dt ha
-1) and white mustard (12.2 dt ha
-1), were observed in the variants with the action of N
90-120P
60K
60. The oil content in spring rape was 42-45% and 36.5% in gray mustard. Low oil content was observed in white mustard (about 30%). The yield of rapeseed and mustard seeds per hectare under the action of increased norms of mineral fertilizers increased, in comparison with the control, by 15-33.5%, which clearly proved the high responsiveness of these crops to additional nutrition.
Nitrogen had a significant effect on rapeseed and mustard, where it became stronger as the application rate increased. At the same time, cabbage crops showed that they were crops for which the early damage of lack of fertilization was overcome by compensating growth. End-season harvest has not dropped as much as might have been expected given the damage at the start of the season.
Accumulating in stems and roots of plants, heavy metals practically do not get into the seeds, therefore, rapeseed, mustard and other cabbage crops from the contaminated zone can be used for oil production and further processing.