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The Potential of Liming to Improve Drought Tolerance of Norway Spruce Picea abies (L.) Karst.

机译:石灰改良提高挪威云杉抗旱性的潜力Picea abies(L.)Karst。

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摘要

In response to a wide-spread decline in forest vitality associated with acid rain in the 1980s, liming of soils has been implemented in many federal states in Germany to buffer further acid deposition and improve availability of nutrients such as calcium and magnesium. As a consequence, it may also increase vitality and depth of fine-root systems and hence improve the drought tolerance of species such as Norway spruce [Picea abies (L.) Karst.], which occurs mostly on acidic forest soils. However, the influence of repeated liming on drought tolerance of trees has never been studied. Here we compared the resistance, recovery and resilience of radial growth in P. abies in relation to drought in limed and control stands and assessed how the dosage and interval between lime application and drought year influences the radial growth response of P. abies. We analyzed radial growth in 198 P. abies trees of six experimental sites in south–west Germany. An analysis of the radial increment over the last 30 years allowed the analysis of drought events shortly after the first liming (short-term effect) as well as posterior drought events (mid- to long-term effects). Generalized linear models were developed to assess the influence of drought intensity, site and period since first liming on the drought tolerance of Norway spruce. Regardless of drought intensity, there was no general increase in drought resistance of Norway spruce in response to liming. However, drought resistance of radial growth improved on a loamy site that was additionally treated with wood ash 30 years after the first lime application. Furthermore, recovery and resilience of radial growth after severe drought events were generally better in spruce trees of limed treatments. This indicates a shorter stress period in spruce trees growing on limed soil, which may reduce their susceptibility to secondary, drought-related pests and pathogens.
机译:为了应对1980年代与酸雨有关的森林生命力普遍下降的情况,德国许多联邦州已开始对土壤施石灰,以缓冲进一步的酸沉降并提高钙和镁等营养素的利用率。结果,它还可以增加细根系统的活力和深度,从而提高诸如挪威云杉[Picea abies(L.)Karst。]等物种的耐旱性,这些物种主要发生在酸性森林土壤上。然而,从未研究过多次加石灰对树木的耐旱性的影响。在这里,我们比较了石灰和对照林分中相对于干旱的小白菜径向生长的抵抗力,恢复力和恢复力,并评估了石灰施用量和干旱年之间的剂量和间隔如何影响小白菜的径向生长响应。我们分析了德国西南部六个实验点的198棵冷杉树的径向生长。通过对过去30年的径向增量进行分析,可以分析在第一次加石灰后不久的干旱事件(短期影响)以及后干旱事件(中长期影响)。建立了广义线性模型以评估自第一次施石灰以来干旱强度,地点和时期对挪威云杉耐旱性的影响。不论干旱强度如何,施胶对挪威云杉的抗旱性都没有普遍提高。但是,在壤土上的径向生长的抗旱性得到了改善,在第一次施用石灰30年后,又用木灰对其进行了处理。此外,在严重干旱事件后的云杉树木中,石灰处理后径向生长的恢复和复原力通常更好。这表明在石灰土壤上生长的云杉树木的胁迫期较短,这可能会降低其对与干旱相关的次生病虫害和病原体的敏感性。

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