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Tree Age Effects on Fine Root Biomass and Morphology over Chronosequences of Fagus sylvatica Quercus robur and Alnus glutinosa Stands

机译:树龄对青冈栎刺槐林分时序的细根生物量和形态的影响

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摘要

There are few data on fine root biomass and morphology change in relation to stand age. Based on chronosequences for beech (9–140 years old), oak (11–140 years) and alder (4–76 years old) we aimed to examine how stand age affects fine root biomass and morphology. Soil cores from depths of 0–15 cm and 16–30 cm were used for the study. In contrast to previously published studies that suggested that maximum fine root biomass is reached at the canopy closure stage of stand development, we found almost linear increases of fine root biomass over stand age within the chronosequences. We did not observe any fine root biomass peak in the canopy closure stage. However, we found statistically significant increases of mean fine root biomass for the average individual tree in each chronosequence. Mean fine root biomass (0–30 cm) differed significantly among tree species chronosequences studied and was 4.32 Mg ha-1, 3.71 Mg ha-1 and 1.53 Mg ha-1, for beech, oak and alder stands, respectively. The highest fine root length, surface area, volume and number of fine root tips (0–30 cm soil depth), expressed on a stand area basis, occurred in beech stands, with medium values for oak stands and the lowest for alder stands. In the alder chronosequence all these values increased with stand age, in the beech chronosequence they decreased and in the oak chronosequence they increased until ca. 50 year old stands and then reached steady-state. Our study has proved statistically significant negative relationships between stand age and specific root length (SRL) in 0–30 cm soil depth for beech and oak chronosequences. Mean SRLs for each chronosequence were not significantly different among species for either soil depth studied. The results of this study indicate high fine root plasticity. Although only limited datasets are currently available, these data have provided valuable insight into fine root biomass and morphology of beech, oak and alder stands.
机译:细根生物量和形态变化与林分年龄有关的数据很少。基于山毛榉(9–140岁),橡树(11–140岁)和al木(4–76岁)的时间序列,我们旨在研究林分年龄如何影响细根生物量和形态。研究中使用了0-15 cm和16-30 cm深度的土壤核心。与以前发表的研究表明,在林分发育的冠层闭合阶段达到最大的细根生物量相反,我们发现在时间序列内,随着年龄的增长,细根生物量几乎呈线性增加。我们在冠层封闭阶段未观察到任何细根生物量峰值。但是,我们发现每个时间序列中平均单个树木的平均细根生物量在统计上有显着增加。在研究的树种时序中,平均细根生物量(0–30 cm)存在显着差异,分别为4.32 Mg ha -1 ,3.71 Mg ha -1 和1.53 Mg ha -1 ,分别用于山毛榉,橡树和al木林。最高的细根长度,表面积,体积和细根尖的数量(0–30厘米土壤深度)以林分面积表示,发生在山毛榉林中,橡木林分中等,al木林最低。在al木的时序中,所有这些值都随着树龄的增加而增加,在山毛榉的时序中,它们减小,而在橡木的时序中,这些值一直增大直到大约。 50岁的老人站立,然后达到稳态。我们的研究证明,山毛榉和橡树的时序序列在0–30 cm土壤深度下,树龄和特定根长(SRL)之间在统计学上具有显着的负相关关系。对于每种土壤深度,物种之间每个时间序列的平均SRL均无显着差异。这项研究的结果表明较高的细根可塑性。尽管目前只有有限的数据集,但这些数据为深入研究山毛榉,橡树和al木的细根生物量和形态提供了宝贵的见识。

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