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Soil fungal diversity and biological activity as indicators of fertilization strategies in a forest ecosystem after spruce disintegration in the Karpaty Mountains

机译:土壤真菌多样性和生物活性作为森林生态系统中云杉崩解后森林生态系统的施肥策略指标

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Forest soils are being exposed to nutrient deficiency and acidification at increasing rates as a result of intensive management. Mineral fertilization, however, provides a way to improve soil nutrient balance. The aim of this study is to present the effects of mineral fertilization on the properties of forest soil 11 years after fertilization. Our research investigated the effects of dolomite, magnesite and serpentinite fertilization on the physicochemical properties of the soil, soil biological activity, and fungal diversity. We also determined the condition of a new generation of fir trees after mineral fertilization. In autumn, 2008, fertilizers (dolomite, magnesite and serpentinite, specifically) in the amount of 4000 kgha~(-1) were added to plots in the Wista Forest District in Poland; one area was left unfertilized to act as the control area for this research. Our results reveal that all fertilization improved the selected soil's physicochemical properties (pH, Ca and Mg content) and accordingly, its biochemical activity; in particular, we found that dolomite (4000 kgha~(-1)) contributed heavily to soil improvement. The findings also showed that soil pH and calcium content were strongly dependent on enzymatic activity, while dolomite fertilization resulted in a significant increase in biomass size in the fir trees included in this study. In addition to being associated with the highest plant biomass and amounts of enzymatic activity, dolomite-fertilized soil also had the highest number of fungal operational taxonomic units (OTUs): 403, compared to 322 OTUs in the control soil. Finally, the fungal communities in the control soil varied significantly from the fungal communities in soils fertilized with dolomite and serpentinite. The results of this research support mineral fertilization, and in particular, fertilization using dolomite in amounts of 4000 kgha~(-1), to improve soil nutrient supply and to shape the biological activity expressed by the enzymatic activity of forest soils.
机译:由于密集管理,森林土壤正在暴露于营养缺乏和酸化,以较高的速度。然而,矿物施肥提供了改善土壤养分平衡的方法。本研究的目的是培养矿物施肥对施肥后11年林土的性质。我们的研究研究了白云石,菱镁矿和蛇形抗施肥对土壤,土壤生物活性和真菌多样性的物理化学性质的影响。我们还确定了矿物施肥后新一代杉木树的状况。 2008年秋季,在波兰维斯塔森林区的地块中加入了4000 kgha〜(-1)的肥料(白云石,菱镁矿和蛇形素);一个区域被绝不为妥,以充当该研究的控制区域。我们的研究结果表明,所有施肥都改善了所选土壤的物理化学性质(pH,CA和Mg含量),因此,其生化活性;特别是,我们发现白云石(4000 kgha〜(-1))促进了土壤改善。结果还表明,土壤pH和钙含量强烈依赖于酶活性,而白云石施肥导致本研究中包括的杉木树中的生物质尺寸大幅增加。除了与最高植物生物质和酶活性的量相关的外,白云石施肥土壤还具有最多的真菌运作分类单位(OTU):403,与322 oTus在对照土壤中相比。最后,对照土壤中的真菌社区从用白云石和蛇形矿石受精的土壤中的真菌社区具有显着变化。该研究的结果支持矿物精,特别是使用白云石的施肥量为4000 kGHA〜(-1),以改善土壤养分供应和塑造森林土壤酶活性表达的生物活性。

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