Changes in the absorptive capacity of soils of Donbass degraded agroecosystems

D. V. Syshchykov, I. V. Agurova
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Abstract

The aim of the work was to study the qualitative and quantitative composition of the soil-absorbing complex of degraded soils of agricultural land on the territory of the Donetsk People's Republic (DPR). The main tasks of the work were to study the amount of exchangeable bases, as well as the exchangeable calcium and magnesium of degraded soils. To study the soil cover of degraded agroecosystems, model plots were selected, located in the northern part of the Shakhterskiy region of the DPR, represented by gravelly chernozems unwashed and medium-washed. The site with steppe vegetation (ordinary medium-humus chernozem) was selected as the control variant. The results of studies of soil absorption capacity of agrocenoses in general indicate the development of degradation processes. The sum of the exchangeable bases of all studied soils is significantly reduced in comparison with the zonal soil, and the minimum values of the studied indicator, compared to the control, are recorded on slope areas of the fields (76.6–81.8% in relation to the control). On the fallow field, no statistically significant differences were found between the values of the sum of exchangeable bases compared to the control, which is most likely due to the lack of intensive agricultural exploitation and the application of mineral nutritive elements to the soil of this site. In the soils of almost all model sites (with the exception of the fallow field), the content of exchangeable calcium decreased by 27.4–42.7% compared to zonal soil. While studying the content of exchangeable magnesium, some regularities have been noticed, which are due to correlation with exchangeable calcium. Thus, the intensification of agricultural soil use resulted in an increased ratio of magnesium to calcium – on average to 1 : 3, while in the control it was 1 : 5. Such a transformation in the future can negatively affect the soilabsorbing complex and the soil as a whole, further loss of soil structure and a number of other negative consequences.
顿巴斯退化农业生态系统土壤吸收能力的变化
这项工作的目的是研究顿涅茨克人民共和国(DPR)境内农田退化土壤的土壤吸收复合体的定性和定量组成。这项工作的主要任务是研究退化土壤中可交换碱的含量以及可交换钙和镁的含量。为研究退化农业生态系统的土壤覆盖情况,选择了位于朝鲜民主主义人民共和国沙赫特斯基州北部的示范地块,这些地块由未清洗和中度清洗的砾质垩土构成。有草原植被(普通中度腐殖质)的地块被选为对照变体。对农田土壤吸收能力的研究结果表明,土壤退化过程正在发展。与地带性土壤相比,所有研究土壤的可交换碱基总和都明显降低,与对照相比,研究指标的最小值出现在田地的坡地上(与对照相比为 76.6-81.8%)。在休耕地上,与对照组相比,可交换碱基总和的数值在统计学上没有显著差异,这很可能是由于没有进行密集的农业开发,也没有在该地土壤中施用矿物营养元素。在几乎所有示范点的土壤中(休耕地除外),可交换钙的含量比地带性土壤减少了 27.4-42.7%。在研究可交换镁的含量时,发现了一些规律性的东西,这与可交换钙有关。因此,农业土壤的强化利用导致镁钙比增加--平均为 1:3,而对照组为 1:5。未来的这种变化会对土壤吸收复合体和整个土壤产生负面影响,进一步破坏土壤结构,并产生一系列其他负面后果。
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