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Soil fauna and soil function in the fabric of the food web

机译:食物网结构中的土壤动物区系和土壤功能

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Over the last four decades, spanning David Coleman's career, and in no small measure thanks to him, soil ecologists have made tremendous progress in describing and understanding the overwhelming complexity of biological, biophysical and biochemical, interactions in soil. These interactions shape the soil as a habitat for the soil food web and the vegetation and, thereby, regulate the two main life-supporting processes on Planet Earth: production and decomposition. Changes in decomposition and production processes are governed by (human-induced) changes in vegetation composition/cover, the amounts and quality of organic residues and (in)organic fertilizers entering the soil. Such modifications alter the physical environment and the soil. biota. Hence, decomposition and production processes cannot be understood and/or manipulated without explicitly addressing the composition and activity of the soil food web. Using a conceptual. model, we argue that quantitative understanding of biophysical interactions, in particular those between soil fauna and soil structure, are paramount to understanding biological, and biochemical. processes in soil and the availability of water and nutrients to plants. The need to increase the efficiency of crop production worldwide, to reverse soil degradation and to increase soil resilience wilt set the agenda for soil ecologists in the near future. (c) 2006 Elsevier GmbH. All rights reserved.
机译:在过去的四十年中,在大卫·科尔曼(David Coleman)的整个职业生涯中,土壤生态学家在描述和理解土壤中生物,生物物理和生化相互作用的极其复杂性方面取得了巨大进步,这在很大程度上要归功于他。这些相互作用使土壤成为土壤食物网和植被的栖息地,从而调节了地球上两个主要的生命维持过程:生产和分解。分解和生产过程的变化受以下因素的影响:植被组成/覆盖物的(人为原因)变化,进入土壤的有机残留物和(有机)有机肥料的数量和质量。此类修改会改变物理环境和土壤。生物群系。因此,如果不明确解决土壤食物网的组成和活性,就无法理解和/或控制分解过程和生产过程。使用概念。在模型中,我们认为对生物物理相互作用(尤其是土壤动物和土壤结构之间的相互作用)的定量理解对于理解生物学和生物化学至关重要。土壤中的过程以及植物中水和养分的可用性。提高全球农作物生产效率,扭转土壤退化和提高土壤复原力的需求在不久的将来为土壤生态学家设定了议程。 (c)2006 Elsevier GmbH。版权所有。

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