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首页> 外文期刊>Soil Science >Long-term Effects of Canopy Opening and Liming on Soil Nutrient Dynamics in a European Beech (Fagus sylvatica L.) Forest
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Long-term Effects of Canopy Opening and Liming on Soil Nutrient Dynamics in a European Beech (Fagus sylvatica L.) Forest

机译:林冠开放和覆盖对欧洲山毛榉(Fagus sylvatica L.)森林土壤养分动态的长期影响

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摘要

Forest management has a considerable influence on the soil nutrient dynamics of forest ecosystems. This study was designed to examine the long-term effects of lime application and canopy removal on soil nutrient budgets in a mature European beech (Fagus sylvatica L.) forest. In 1989, trees were felled to create four 30-m wide circular gaps in this beech forest, and two of these gaps and the surrounding area were limed with 3 t ha(-1) of fine dolomite, whereas the remaining two gaps and most parts of the stand were not limed. Main nutrient concentrations in the forest floor and in the mineral soil were determined in 1989, 1997, and 2011. In addition, we examined the influence of liming and gaps on the forest floor organic matter. The significant effects of liming and gap creation on the forest floor dry mass in 1997 were no longer obvious in 2011, unlike their influence on the C and N pools, which was still significant in 2011. In the long-term, the forest floor C and N pools increased less in the limed and opened plots compared with the untreated stand, and the N pool only decreased in the mineral soil of the limed gaps. Soil acidity was reduced significantly 8 years after liming at any depth in the limed plots (limed stand, limed gaps) and in the deeper layers (5-40 cm) of the unlimed plots, indicating a general soil recovery from acid depositions in earlier decades. After 22 years, the pH values were still higher at 5 to 10 cm mineral soil depth in the limed plots, which partly reflected the higher base saturation in the mineral soil of the limed gaps. However, the pH values were surprisingly dropping from 1997 to 2011 in the upper soil layers of all plots. Overall, some effects of canopy opening and liming on soil nutrients lasted for more than two decades in this European beech forest.
机译:森林管理对森林生态系统的土壤养分动态具有相当大的影响。这项研究旨在检查石灰的应用和去除冠层对欧洲成熟山毛榉(Fagus sylvatica L.)森林土壤养分收支的长期影响。 1989年,砍伐树木以在此山毛榉森林中形成四个30米宽的圆形空隙,其中两个空隙和周围地区被3 t ha(-1)细白云石粉化,而其余两个空隙和大部分展台的各个部分没有上灰。在1989年,1997年和2011年确定了林底和矿质土壤中的主要养分浓度。此外,我们研究了石灰和缝隙对林底有机质的影响。在1997年,石灰和缝隙的形成对森林地表干重的显着影响在2011年不再明显,与对碳和氮库的影响不同,后者在2011年仍然很明显。与未处理的林分相比,在石灰和开阔地块中N和N的增加较少,而在石灰间隙的矿质土壤中N和仅减少。在石灰田(石灰林,石灰间隙)和未石灰田的更深层(5-40厘米)中的任何深度施石灰后,土壤酸度均显着降低了8年,这表明几十年来从酸沉降中土壤的总体恢复。 22年后,在石灰土地上5至10 cm的矿质土壤中,pH值仍然更高,部分反映了石灰空隙中矿质土壤中较高的碱饱和度。但是,从1997年到2011年,所有土地上层土壤的pH值都出乎意料地下降。总体而言,在这个欧洲山毛榉森林中,树冠开放和结实对土壤养分的某些影响持续了超过二十年。

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