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首页> 外文期刊>European Journal of Soil Science >Soil phosphorus status and turnover in central-European beech forest ecosystems with differing tree species diversity
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Soil phosphorus status and turnover in central-European beech forest ecosystems with differing tree species diversity

机译:不同树种多样性的中欧山毛榉森林生态系统中的土壤磷状况和周转

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Problems in phosphorus (P) nutrition of forest trees raise questions concerning the soil P concentrations, pools and turnover in forests. In addition, it is not clear if, and to what extent, tree species diversity has an influence on the soil P status and turnover. The aim of this study was to investigate the P status and turnover in beech (Fagus sylvatica L.) -dominated forest ecosystems on loess over limestone and to elucidate what role heterogeneities in tree species diversity would play. The soils of mixed species stands contained more organically bound P (710-772 kg hap#) than those of pure beech stands (378 kg hap#), whereas the inorganic P content differed little between the stand types. A large proportion (44-55%) of the total soil P was organically bound. This fraction was mainly dependent on the clay content of the soils and not on the tree diversity. The P input with leaf litter (1.4-2.1 kg hap# yearp#) showed a tendency to increase with increasing diversity. The apparent P turnover times in the organic surface layers differed, with shorter turnover times in mixed species stands (2-3 years) than in pure beech stands (10 years). Possible explanations for the different turnover times were differences in the litter quality, interactions in mixed species litters and the soil pH and base saturation. Hence, the tree species mainly influence the apparent P turnover time in the organic surface layer, whereas the P concentrations and pools in the mineral soil are determined by the soil properties, particularly the clay content.
机译:林木中磷(P)营养的问题引起了有关土壤中P含量,库和森林周转的问题。此外,尚不清楚树种多样性是否以及在多大程度上影响土壤磷状况和周转率。这项研究的目的是调查石灰岩上黄土上以山毛榉(Fagus sylvatica L.)为主的森林生态系统中磷的状况和更新,并阐明异质性在树木物种多样性中将发挥什么作用。与纯山毛榉林(378 kg hap#)相比,混合物种林分土壤含有更多的有机结合磷(710-772 kg hap#),而不同林分类型之间的无机磷含量差异不大。整个土壤P中有很大一部分(44-55%)是有机结合的。该分数主要取决于土壤的粘土含量,而不取决于树木的多样性。随着凋落物(1.4-2.1 kg hap#年p#)的磷输入量显示出随着多样性增加而增加的趋势。有机表层的表观磷周转时间不同,混合树种(2-3年)的周转时间比纯山毛榉林(10年)的周转时间短。对于不同周转时间的可能解释是凋落物质量的差异,混合物种凋落物的相互作用以及土壤的pH和碱饱和度。因此,树种主要影响有机表层中磷的表观转换时间,而矿质土壤中的磷浓度和库则由土壤性质,特别是粘土含量决定。

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