Deductive museumization of the phytodetritus component of forest community

Y. Chernobay
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Abstract

Detritus, in particular litter, turf and peat strata, silt along streams, as well as benthos, are systemic formations that can be differentiated into both elements and components. As an independent indicator of structural and functional indicator, litter-falling coefficient (LFC) - acts only up to the level of biogeocenosis. The suprabiogeocenotic (landscape) level is not a simple or weighted sum of biogeocenotic estimates. This should be a network integration of biogeochemical flows, where whole biogeocenoses can act as barrier systems. Therefore, the LFC indicator cannot be averaged for the landscape, but the indicators of anisotropy, dispersion, or chorology can be used, which can be reduced to a point indication (rating) of the ecosystem. The priority role of litter in the small biotic cycle is due to the fact that in natural ecotopes developed an effective mechanism of heterotrophic utilization of dead biomass. Due to this, the intensity of litter decomposition, estimated by the value of LFC, can be used to diagnose the stability of the ecotope. For the cycle of substances and the flow of energy, forest litter serves as a reserve fund, which ensures the stability of the ecosystem. From the point of view of system organization, the litter is a structural layer (detrital biogeohorizon). Therefore, litter as a bio-mineral formation can be considered from different positions - as part of the soil profile, or subsystem of the soil system, as an independent biogeocenotic body (as a system) and as a component link in the system of biogeocenoses. Detrital diagnostics allows to fairly objectively assess the risks to the continued existence of forests in an unstable buffer environment. With the help of these criteria it is possible to identify the direction of changes in sustainability indicators, which is extremely important in the early stages of decision-making on further plans to optimize and strengthen the buffer structures of forest community.
森林群落植物碎屑成分的演绎博物馆化
碎屑,特别是凋落物、草皮和泥炭层、河流沿岸的淤泥以及底栖生物,是可以分为元素和组成部分的系统地层。凋落物系数(LFC)作为结构和功能指标中的一个独立指标,仅在生物地质体水平上起作用。超生新生代(景观)水平不是一个简单的或加权的生物生新生代估计的总和。这应该是一个生物地球化学流的网络整合,整个生物地球海洋可以作为屏障系统。因此,LFC指标不能对景观进行平均,但可以使用各向异性、分散或时序指标,这些指标可以简化为生态系统的点指示(评级)。凋落物在小生物循环中的优先作用是由于在自然生态环境中形成了一种有效的异养利用死生物量的机制。因此,通过LFC值估算凋落物分解强度,可用于诊断生态环境的稳定性。对于物质循环和能量流动来说,森林凋落物是一种储备资金,保证了生态系统的稳定。从系统组织的角度看,凋落物是一个结构层(碎屑生物地层)。因此,凋落物作为一种生物矿物可以从不同的位置来考虑——作为土壤剖面的一部分,或作为土壤系统的子系统,作为一个独立的生物生地体(作为一个系统),作为生物生地体系统中的一个组成环节。碎片诊断可以相当客观地评估在不稳定的缓冲环境中森林继续存在的风险。在这些标准的帮助下,可以确定可持续性指标的变化方向,这在制定进一步优化和加强森林群落缓冲结构的计划的早期阶段是极其重要的。
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