Enzyme diagnostics for evaluation of effect of nitrogen fertilizers on mineralization and humification processes in sod-podzolic soils

N. Mikhailouskaya, S. A. Kasyanchyk, A. G. Mezentseva, T. V. Pagirnitskaya
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Abstract

Ecological management of soil resources is an urgent task involving periodic assessment of effect of fertilizers and other anthropogenic factors on the rate and direction of organic matter transformation. Mineralization and humification of organic residues are the most important functions of the soil, which determine its fertility and are closely related to the biochemical activity of microbial communities. When using intensive agricultural technologies, it is required to timely identify potential risks of reducing soil fertility. Taking into account the biochemical nature of the processes of mineralization and humification of organic substances, it is advisable to use indicators of enzymatic activity for this purpose. Enzymes are the most important metabolites of microorganisms. When choosing enzymatic indicators for a reliable assessment of influence of natural and anthropogenic factors on the activity of mineralization and humification, we took into account large-scale and universal processes in the cycles of the main biogenic elements – carbon and nitrogen. Soil enzyme diagnostics was shown to be likely useful instrument for evaluation of natural and anthropogenic factors effect on mineralization and humification processes in sod-podzolic soils. The most informative enzymatic tests for characterization of soil biochemical status in C and N cycles were determined. Biochemical coefficient was proposed as a resulting criteria for interpretation of enzymes activity data, allowing to compare humification and mineralization activities, reveal their disbalance and control of anthropogenic impact on soils. Experimental data on the effect of nitrogen fertilizers on the activity and ratio of humification and mineralization, obtained in long-term field experiments on soddy-podzolic soils of different granulometric composition and level of fertility are presented.
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酶诊断评价氮肥对灰化土矿化和腐殖质化过程的影响
土壤资源生态管理是一项紧迫的任务,需要定期评估肥料和其他人为因素对有机质转化速度和方向的影响。有机残留物的矿化和腐殖化是土壤最重要的功能,它决定着土壤的肥力,并与微生物群落的生化活性密切相关。在使用集约化农业技术时,需要及时识别降低土壤肥力的潜在风险。考虑到有机物质的矿化和腐殖质化过程的生化性质,建议为此目的使用酶活性指标。酶是微生物最重要的代谢产物。在选择酶促指标以可靠地评估自然和人为因素对矿化和腐殖化活动的影响时,我们考虑了主要生物源元素-碳和氮循环中的大规模和普遍过程。土壤酶诊断是评价自然和人为因素对草灰化土壤矿化和腐殖质化过程影响的有效工具。确定了在C和N循环中表征土壤生化状态的最具信息性的酶促试验。生物化学系数被提出作为解释酶活性数据的结果标准,允许比较腐殖化和矿化活动,揭示它们的不平衡和人为影响对土壤的控制。本文介绍了在不同颗粒组成和肥力水平的钠灰化土长期田间试验中,氮肥对土壤腐殖质化和矿化活性及比例影响的试验数据。
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