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首页> 外文期刊>Journal of Hydrology >Change of interception process due to the succession from Japanese red pine to evergreen oak
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Change of interception process due to the succession from Japanese red pine to evergreen oak

机译:从日本红松到常绿橡木的继承,拦截过程发生了变化

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Extensive measurements of rainfall, throughfall and stemflow in a forest during succession from Japanese red pine (Pinus densiflora Sieb. et Zucc.) to a combination of red pine and lower canopy trees-evergreen oak (Quercus myrsinaefolia Blume) and evergreen theaceous tree (Eurya japonica Thunb.) allowed the effect of this succession on the interception of rainfall to be evaluated. The measurements were conducted on two occasions: 1984/1985, and 2001/2002 when the lower canopy trees had become dominant. During this period, 75% of the red pines had been removed, and there was a substantial increase in stemflow (p < 0.01), essentially no change in throughfall (p < 0.01), and a substantial decrease in interception (p < 0.01). The increase in stemflow was attributed to the increase in lower canopy trees; trees that have steeply angled branches, smooth bark surfaces and water repellent leaves; all of which enhance stemflow. The decrease in interception was due to the decrease in canopy water storage (2.6-1.1 mm/event) and an increase in evaporation during rainfall event (0.7-1.1 mm/event). The decrease in storage partly resulted from the removal of red pines, the bark of which is thick, flaky, and therefore, very absorptive. It was responsible for 88% of the actual rainfall storage at the beginning of the experiment. During the 17 year-period, the size of the lower canopy trees increased more rapidly than that of red pines. The increase in evaporation was due to the increase in canopy gaps by the removal of 75% of the red pines during the succession, and was a minor factor in affecting interception loss. (c) 2005 Elsevier B.V. All rights reserved.
机译:从日本赤松(Pinus densiflora Sieb。et Zucc。)到赤松和下冠层树-常绿橡树(Quercus myrsinaefolia Blume)和常绿豆科树(Eurya)的演替期间,森林中的降雨,穿透水和茎流的广泛测量japonica Thunb。)允许评估该演替对降雨截留的影响。在以下两种情况下进行了测量:1984/1985和2001/2002,当时较低的树冠层已占优势。在此期间,去除了75%的红色松树,茎流量显着增加(p <0.01),穿透力基本没有变化(p <0.01),截留率显着降低(p <0.01) 。茎流的增加归因于下层冠层树的增加。树枝倾斜的树皮,光滑的树皮表面和憎水的叶子;所有这些都能增强茎流。截留量的减少是由于冠层储水量的减少(2.6-1.1毫米/事件)和降雨事件期间的蒸发增加(0.7-1.1毫米/事件)。贮藏量的减少部分是由于去除了红色的松树而造成的,该树皮厚,呈片状,因此具有很强的吸收性。在实验开始时,它占实际降雨量的88%。在17年期间,下部树冠的大小增长速度快于红色松树的增长速度。蒸发的增加是由于在演替过程中去除了75%的红松而增加了树冠间隙,这是影响拦截损失的次要因素。 (c)2005 Elsevier B.V.保留所有权利。

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