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Reduction in soil water availability and tree transpiration in a forest with pedestrian trampling.

机译:践踏行人的森林中土壤水的供应量和树木的蒸腾作用减少。

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摘要

Many studies have reported tree growth reduction in forests with pedestrian trampling, implying a reduction of tree transpiration in such forests. We undertook observations of tree transpiration based on the heat-pulse method in a forest (Lithocarpus edulis) with pedestrian trampling. We prepared trampled and control plots in the forest. Tree transpiration in the trampled plot was reduced compared to that in the control plot after precipitation with a small-precipitation period preceding this. No difference was observed between plots in the small-precipitation period itself; during which tree transpiration was limited in both plots. After the period, tree transpiration recovery was not as complete in the trampled plot as in the control plot. This was caused by incomplete soil matric potential recovery at 20 cm and deeper in the trampled plot due to a lower infiltration rate. We believe this study is the first to report reduction of tree transpiration in a forest with pedestrian trampling.
机译:许多研究报告说,践踏行人会减少森林中树木的生长,这意味着这类森林中树木的蒸腾作用会减少。我们在行人践踏的森林中(Lithocarpus edulis)基于热脉冲法对树木的蒸腾作用进行了观察。我们在森林中准备了践踏和控制的土地。与降雨后的控制区相比,践踏区的树蒸腾量有所减少,而在此之前的降水量较小。小降水期本身之间没有发现差异。在这两个地块中,树木的蒸腾作用受到限制。在这段时期之后,被践踏的地块的蒸腾作用恢复不如对照地块。这是由于在20 cm处土壤基质电位恢复不完全所致,并且由于渗透率较低,在被践踏的土壤中更深。我们相信这项研究是第一个报告行人践踏森林中树木蒸腾作用减少的研究。

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