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Minor contribution of leaf litter to N nutrition of beech (Fagus sylvatica) seedlings in a mountainous beech forest of Southern Germany

机译:叶凋落物对德国南部山区山毛榉森林中山毛榉(Fagus sylvatica)幼苗氮营养的微小贡献

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摘要

Our aims were to characterize the fate of leaf-litter-derived nitrogen in the plant-soil-microbe system of a temperate beech forest of Southern Germany and to identify its importance for N nutrition of beech seedlings. N-15-labelled leaf litter was traced in situ into abiotic and biotic N pools in mineral soil as well as into beech seedlings and mycorrhizal root tips over three growing seasons. There was a rapid transfer of N-15 into the mineral soil already 21 days after tracer application with soil microbial biomass initially representing the dominant litter-N sink. However, N-15 recovery in non-extractable soil N pools strongly increased over time and subsequently became the dominant N-15 sink. Recovery in plant biomass accounted for only 0.025 % of N-15 excess after 876 days. After three growing seasons, N-15 excess recovery was characterized by the following sequence: non-extractable soil N extractable soil N including microbial biomass plant biomass > ectomycorrhizal root tips. After quick vertical dislocation and cycling through microbial N pools, there was a rapid stabilization of leaf-litter-derived N in non-extractable N pools of the mineral soil. Very low N-15 recovery in beech seedlings suggests a high importance of other N sources such as root litter for N nutrition of beech understorey.RI Simon, Judy/C-7875-2011
机译:我们的目标是表征德国南部温带山毛榉森林的植物-土壤-微生物系统中源自叶凋落物的氮的命运,并确定其对山毛榉幼苗氮素营养的重要性。 N-15标记的叶子凋落物在三个生长季节被原位追踪到矿物土壤中的非生物和生物氮库以及山毛榉幼苗和菌根根尖。施用示踪剂后21天,N-15已迅速转移到矿质土壤中,土壤微生物生物量最初代表主要的凋落N汇。但是,不可提取的土壤氮库中的N-15回收量会随着时间的推移而显着增加,并随后成为主要的N-15汇。 876天后,植物生物量的回收仅占N-15过量的0.025%。在三个生长季节后,N-15过量恢复的特征是以下顺序:不可提取的土壤N 包括微生物生物量植物生物量>根外菌根的可提取土壤N。快速垂直脱位并通过微生物氮池循环后,矿物土壤中不可提取的氮池中源自叶凋落物的氮迅速稳定。山毛榉幼苗中N-15的回收率非常低,这表明其他氮源(例如根垫)对于山毛榉下层氮素营养非常重要.RI Simon,Judy / C-7875-2011

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