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Storm and snow damage in a Norway spruce thinning experiment in southern Sweden

机译:瑞典南部挪威云杉间伐试验中的暴风雪灾害

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To assess uncertainties regarding the effects of thinning on risks of storm and snow damage, three thinning treatments (control, normal and heavy: 0,30 and 61 per cent basal area removal, respectively) with four replications were applied in a 33-year-old Norway spruce plantation on a fertile site in south-west Sweden. A major storm event occurred three growing seasons after thinning followed by snow damage 2 months later and another storm 2 years later. There was a near-linear relationship between thinning intensity and damage caused by the first storm (adj R2 = 0.94): 7, 42 and 74 per cent of the standing basal area was damaged in the control, normally and heavily thinned plots, respectively. Corresponding percentages after both the storm and snowdamage were also approximately linearly correlated with thinning intensity: 8, 53 and 89 per cent, respectively (adj R2 = 0.91). Damage caused by the second storm was related to both previous damage levels and standing basal area in the control and normally thinned plots. Stem taper between breast height and 6 m stem height was negatively correlated with risk for storm and snow damage in the normally thinned plots. Of the trees categorized as damaged (up-rooted, broken or heavily leaning), the frequencyof stem breakage after the first storm was almost negligible in the normally thinned plots, (<5 per cent), while 24 - 50 per cent of the damaged stems were broken (mean, 36 per cent) in the heavily thinned plots. The relative diameter growth of the remaining trees in the control plots, for the first and second growing seasons following the storm and snow damage, were significantly decreased compared with the three preceding years. The results confirm previous findings that increasing thinning intensity increases risks of windfall and highlight the need for new Norway spruce management programmes if climate change results in more frequent storm events.
机译:为了评估间伐对风暴和雪灾风险的不确定性,在33年的时间里,采用了三种间伐处理(分别为对照,正常和重度:分别除去0.30和61%的基面积)和四次重复处理。老挪威云杉人工林在瑞典西南部肥沃的土地上。在稀疏后的三个生长季节中发生了一次重大风暴事件,随后两个月后发生了雪灾,两年后又发生了一次风暴。稀疏强度与第一次暴风雨造成的损害之间存在近乎线性的关系(adj R2 = 0.94):在对照,正常稀疏和严重稀疏的土地上,分别有7%,42%和74%的站立基础面积受到损害。暴风雪和降雪后的相应百分比也与稀疏强度呈线性关系:分别为8%,53%和89%(adj R2 = 0.91)。第二次暴风雨造成的破坏与控制区和通常为稀疏地块中的先前破坏程度以及站立的基础面积有关。在通常变薄的地块中,胸高与6 m茎高之间的茎锥度与暴风雪灾害的风险呈负相关。在被分类为损坏的树木(连根拔起,折断或严重倾斜)中,在通常稀疏的地块中,第一次暴风雨后茎断裂的频率几乎可以忽略不计(<5%),而受损的树木则占24%至50%在极度稀疏的地块中,茎被折断(平均占36%)。与前三年相比,在风暴和雪灾之后的第一个和第二个生长季节,对照地块中其余树木的相对直径增长显着下降。结果证实了以前的发现,即稀疏强度的增加会增加意外收获的风险,并强调如果气候变化导致更频繁的风暴事件,则需要新的挪威云杉管理计划。

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