施用藻类生物肥料条件下典型黑钙土结构聚集过程的评价

Sergiu Dobrojan, Boris Turchin, Nina Placinta, T. Ciolacu, Galina Dobrojan
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引用次数: 0

摘要

聚集-结构过程的管理意味着在其生物群的直接和间接作用下,土壤质模拟过程的强化。在本研究中,我们从考虑藻类微生物群作为细菌-藻类共生的核心负责分解各种有机物(基因组代谢网络)开始。随着土壤有机无机生物质结构功能组织聚集水平的发展,它们对有机废物进行连续串联分解,保证了物质和能量的闭环。研究表明,在典型的中度腐殖层重度过度耕黑钙土中,通过藻类生物修复使其藻化,导致腐殖化过程的再生和土壤结构团聚体状况的改善。这一过程的机制是由藻类生物量作为腐殖化过程的生物氮源的参与决定的。在藻化条件下,聚集过程主要是5-1和3-0.5 mm的聚集体的形成,并由新形成的腐殖质参与的聚集过程决定。不同种类的蓝藻,其聚集-结构过程的强度不同,从递减的意义上可以用以下顺序来描述:Nostoc gelatinosum > Combined lot > Cilindrospermum licheniformme > Calothrix gracilis > Nostoc linickia。蓝藻参与土壤生物质直接聚集过程较少。同时,实践的技术要求轮作能够有助于提高总体稳定性的程度。在土壤功能方面,黑钙土的藻化过程为维持土壤微生物组的组成和多样性提供了先决条件。
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Evaluation of structural aggregation processes of typical chernozem under conditions of algal biofertilizers application
: The management of the aggregation-structuring processes implies the intensification of the soil pedoplasm modeling processes under the direct and indirect action of the its biota. In the present research we started from the consideration of algal microflora as the nucleus of bacterial-algal cenosis responsible for the decomposition of various groups of organic substances (geno-metabolic networks). They decompose organic waste in consecutive series ensuring a closed circuit of substances and energy with development of the aggregate level of structural-functional organization of the soil organo-mineral biopedoplasm. It has been established that algalization of the typical moderately humiferous strongly overplowed chernozem through administration of algal biopreparations leads to the regeneration of the humification process and the improvement of the structural-aggregate condition of the soil. The mechanisms of this process are determined by the participation of algal biomass as a source of biological nitrogen for the humification process. Under algalization conditions, the aggregation processes proceed with the formation, mainly, of 5-1 and 3-0.5 mm aggregates and are determined by the agglutination processes with the participation of newly formed humic substances. The intensity of the aggregation-structuring processes differs depending on the species of administered cyanophyte algae and can be described with the following sequence in the sense of decreasing it: Nostoc gelatinosum > Combined lot > Cilindrospermum licheniforme > Calothrix gracilis > Nostoc linckia . The cyanophyte algae participate less in the direct aggregation processes of soil biopedoplasm. At the same time, the practiced technologies require crop rotations capable of contributing to increasing the degree of aggregate stability. In the pedofunctional aspect, the process of algalization of chernozems presupposes perspectives for sustaining the composition and diversity of the soil microbiome.
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