首页> 外文期刊>Folia Forestalia Polonica: Series A - Forestry >Hydrological properties of bark of selected forest tree species. Part 2: Interspecific variability of bark water storage capacity
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Hydrological properties of bark of selected forest tree species. Part 2: Interspecific variability of bark water storage capacity

机译:所选林木树皮的水文特性。第2部分:树皮贮水量的种间变异性

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The subject of the present research is the water storage capacity of bark of seven forest tree species: Pinus sylvestris L., Larix decidua Mill., Abies alba Mill., Pinus sylvestris L., Quercus robur L., Betula pendula Ehrh. and Fagus sylvatica L. The aim of the research is to demonstrate differences in the formation of bark water storage capacity between species and to identify factors influencing the hydrological properties of bark. The maximum water storage capacity of bark was determined under laboratory conditions by performing a series of experiments simulating rainfall and by immersing bark samples in containers filled with water. After each single experiment, the bark samples were subjected to gravity filtration in a desiccator partially filled with water. The experiments lasted from 1084 to 1389 hours, depending on the bark sample. In all the studied species, bark sampled from the thinnest trees is characterized by the highest water storage capacity expressed in mm H2O · cm-3, while bark sampled from the thickest trees - by the lowest capacity. On the other hand, bark sampled from the thickest trees is characterized by the highest water storage capacity expressed in H2O · cm-2 whereas bark from the thinnest trees - by the lowest capacity. In most species tested, as the tree thickness and thus the bark thickness and the coefficient of development of the interception surface of bark increase, the sorption properties of the bark decrease with bark depth, and the main role in water retention is played by the outer bark surface. The bark of European beech is an exception because of the smallest degree of surface development and because the dominant process is the absorption of water. When examining the hydrological properties of bark and calculating its parameters, one needs to take into account the actual surface of the bark of trees. Disregarding the actual bark surface may lead to significant errors in the interpretation of research results.
机译:本研究的主题是七种林木树皮的贮水量:樟子松,落叶松落叶松,冷杉冷杉,樟子松,栎栎,白桦。该研究的目的是证明物种之间树皮贮水能力形成的差异,并确定影响树皮水文特性的因素。树皮的最大储水量是在实验室条件下通过进行一系列模拟降雨的实验并将树皮样品浸入装有水的容器中确定的。在每个单独的实验之后,将树皮样品在部分充满水的干燥器中进行重力过滤。实验持续了1084到1389小时,具体取决于树皮样品。在所有研究物种中,从最薄的树上取样的树皮的特征在于最大的储水量,以mm H 2 O·cm -3 表示,而从最厚的树木-容量最低。另一方面,从最厚的树上取样的树皮的特征在于最高的储水量,表示为H 2 O·cm -2 ,而最薄的树皮上的树皮-最低的容量。在大多数被测物种中,随着树的厚度,进而树皮的厚度以及树皮的截留面的发展系数的增加,树皮的吸附性能随树皮深度的增加而降低,而保水的主要作用是由外部树皮表面。欧洲山毛榉的树皮是一个例外,因为其表面发育程度最小,并且主要的过程是吸水。在检查树皮的水文特性并计算其参数时,需要考虑到树皮的实际表面。忽略实际的树皮表面可能会导致研究结果解释中的重大错误。

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