“土壤生物物理肥力:理论与应用支持”概念

G. Jigau, Boris Turchin, T. Ciolacu, Nina Placinta, Angela Stadnic
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引用次数: 0

摘要

:在基本成土过程理论中,成土过程代表了构成土壤基本物质的非生物物质和生物物质整合过程的总和,代表了土壤中特定于土壤的物质整合的第一级。它的进一步发展是由"活的有机物↔死的有机物"这一系统所产生的腐殖质的单向作用所决定的。土壤生态系统结构-功能组织的连续过程背后的驱动力是腐殖质形成过程和结构团聚体中有机碳的积累-封存和稳定过程,这些过程负责土壤生态系统的功能,体现在生态系统功能中,包括土壤肥力。所有的过程都是在物质相对平衡的生物地球化学回路中进行的。相对稳定的主要诊断特征。在物质闭环中单向实现土壤肥力扩大再生产的微观、中观和宏观过程。
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The concept “soil biophysical fertility: theoretical and applied support”
: In terms of the theory of elementary pedogenetic processes, the pedogenetic process represents the totality of the integration processes of abiotic and biotic matter in the composition of the basic soil matter, which represents the first level of integration of matter in the soil, specific to it. Its further evolution is determined by the unidirectional action of humic substances resulting from the operation of the system "living organic matter ↔ dead organic matter". The driving force behind the continuous processes of structural-functional organization of the soil ecosystem are the processes of humus formation and those of accumulation-sequestration and stabilization of organic carbon in the structural aggregates responsible for the functioning of the soil ecosystem materialized in ecosistemic functions, including soil fertility. maintained All processes are performed in relatively balanced biogeochemical circuits of substances. Relative stability of the main diagnostic features. One-way realization of micro-, meso- and macroprocesses of expanded reproduction of soil fertility in closed circuits of substances.
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