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首页> 外文期刊>Turkish Journal of Agriculture & Forestry >Partitioning rainfall into throughfall, stemflow, and interception loss in an oriental beech (Fagus orientalis Lipsky) forest during the growing season
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Partitioning rainfall into throughfall, stemflow, and interception loss in an oriental beech (Fagus orientalis Lipsky) forest during the growing season

机译:在生长季节中,将降雨分为东方山毛榉(Fagus Orientalis Lipsky)森林中的降雨,穿透流,截流损失

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Partitioning gross rainfall (GR) into throughfall (TF), stemflow (SF), and interception loss (I), which has a very significant effect on water balance and the nutrient cycle in forest ecosystems, was studied in a natural oriental beech (Fagus orientalis Lipsky) forest situated in the Caspian Forest of northern Iran. Measurements were made inside a plot with an area of 0.5625 ha located in the Kheyrud Forest Research Station of Tehran University during the 2008 growing season. GR was measured based onan average of the records of 3 rain gauges located in an open area approximately 160 m from the study plot. Thirty-six TF manual gauges were randomly placed beneath the beech canopies and SF was collected from 6 selected beech trees using spiral-type SFcollection collars. Measurements were made on a rainfall event basis. The cumulative GR depth of 23 events was 309.9 mm; TF: 209.9 mm; SF: 7.8 mm; I: 92.2 mm. On the event scale average ratios of TF:GR, SF:GR, and I:GR were 65.9%, 2.0%, and 32.1%, respectively. A strong positive correlation was observed between SF:GR and GR (r~2 = 0.963), while very weak correlations were observed between I:GR and GR (r = 0.230), and between TF:GR and GR (r = 0.173). As the size of rainfall events increased, intercepted GR by the oriental beech forest canopies, and loss through evaporation decreased. Interception loss contributes a notable amount of rainfall and its measurement is an essential element in assessing water balance on the catchment scale.
机译:在天然山毛榉中研究了将总降雨量(GR)分为通流(TF),茎流(SF)和截留损耗(I),这对森林生态系统中的水平衡和养分循环具有非常显着的影响(Fagus Orientalis Lipsky)森林位于伊朗北部的里海森林中。在2008年生长季节期间,在德黑兰大学Kheyrud森林研究站内的0.5625公顷土地上进行了测量。 GR是根据位于距研究区约160 m的空旷地区的3个雨量计的记录平均值进行测量的。将36个TF手动量规随机放置在山毛榉冠层下,并使用螺旋型SF收集项圈从6个选定的山毛榉树中收集SF。根据降雨事件进行测量。 23个事件的累积GR深度为309.9 mm; TF:209.9毫米; SF:7.8毫米; I:92.2毫米。在事件规模上,TF:GR,SF:GR和I:GR的平均比率分别为65.9%,2.0%和32.1%。 SF:GR与GR之间有很强的正相关(r〜2 = 0.963),而I:GR与GR之间(r = 0.230)以及TF:GR与GR之间有很弱的正相关(r = 0.173) 。随着降雨事件的增加,东方山毛榉林冠层截留了GR,并且蒸发损失减少了。截流损失造成了可观的降雨,其测量是评估流域尺度上水平衡的基本要素。

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