尼科波尔锰矿盆地技术蚀变土壤脲酶活性分布的生态特征

V. Chorna, I. Wagner
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引用次数: 0

摘要

由于人类活动造成的自然生态系统退化的挑战被国际社会认为是人类面临的最严重的问题。由于矿物开采,人造景观和环境破坏地区取代了自然栖息地和农业生态系统;这类景观的典型特征是一系列人为过程,导致这些地区物种丰富度和生物多样性的减少。在煤炭开采过程中形成的退化土地往往通过修复措施得到部分恢复。在修复技术阶段的实施过程中,使用具有不同环境特性和质量的不同潜在肥力的基质。建立了Nikopol锰矿盆地人工土壤、灰绿色和红棕色粘土和类黄土壤土上的草质岩质土壤的分布总量、有效氮浓度和脲酶酶活性水平的具体特征。通过尿素酶易水解酶活性的浓度对技术土壤状况进行一般性评价,该酶在有机质矿化过程中为土壤提供了丰富的矿质氮。土壤中脲酶的活性水平决定了影响土壤肥力的生化过程方向的强度。人工土壤(r = 0.81)、灰绿色土壤(r = 0.98)、红棕色土壤(r = 0.72)和类黄土壤土(r = 0.85)上不同层间的可溶性氮浓度与脲酶活性值呈高度相关。在所有类型的人工土壤中,水解酶活性随深度的增加而降低。已经确定的是,超越水解酶脲酶活性水平的技术过程的生化诊断,可以估计人工土壤层的变化方向,在灰绿色和红棕色粘土和黄土样壤土上的草质岩质土壤。复耕土壤在下层土壤肥力较低,土壤含盐量较高,但具有一定的生态功能,既可用于经济用途,又可用于生态功能。
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Ecological features of urease activity distribution in technogenically altered soils of the Nikopol manganese ore basin
The challenge of degradation of natural ecosystems because of human activity is considered by the world community to the most serious problems facing mankind. As a result of mineral extraction, man-made landscapes and environmentally ruined areas replace natural habitats and agroecosystems; a whole spectrum of man-made processes are typical for such landscapes, which leads to a decrease in species richness and biological diversity within such areas. Degraded territories formed in the process of coal mining are often partially restored through remediation measures. During the implementation of the technical stage of remediation, substrates with different potential fertility having different environmental properties and quality are used. Specific features of distribution total, available nitrogen concentrations and levels of urease enzymatic activity at the layers of artificial soil, sod-lithogenic soils onto gray-green and red-brown clays and on loess-like loams in the Nikopol manganese ore basin are established. It is presented general assessment of technosol status by concentration of general easily hydrolysed nitrogen enzyme activity of urease and this enzyme enriches the soil with mineral nitrogen in the process of mineralization of organic substances.  The level of activity of urease,  investigated soils, determines the intensity of the direction of biochemical processes that affect soil fertility.High correlation between concentrations of soluble nitrogen and urease activity values by layers of artificial soil (r = 0.81), sod-lithogenic soils onto gray-green (r = 0.98), red-brown clays (r = 0.72) and onto loess-like loam (r = 0.85) were found. Tendency of decreasing hydrolytic enzyme activity, urease, with depth in all types of artificial soil studied was established. It has been established that biochemical diagnostics of technozem processes beyond the level of activity of the hydrolytic enzyme urease makes it possible to estimate the direction of changes at the layers of artificial soil, sod-lithogenic soils onto gray-green and red-brown clays and on loess-like loams. The recultivated soil has some what lower fertility and greater salimity at the lower horizons, but is capable of performing ecological functions and can not only be used for economic purposes, but also perform ecological functions.
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