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首页> 外文期刊>Plant Species Biology >Comparisons of soil-water content between a Moso bamboo (Phyllostachys pubescens) forest and an evergreen broadleaved forest in western Japan
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Comparisons of soil-water content between a Moso bamboo (Phyllostachys pubescens) forest and an evergreen broadleaved forest in western Japan

机译:日本西部毛竹林与常绿阔叶林土壤水分含量的比较

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In Japan, forests of Moso bamboo (Phyllostachys pubescens, an exotic invasive giant bamboo) have naturalized and expanded rapidly, replacing surrounding broadleaved and coniferous forests. To evaluate impacts caused by these forest-type replacements on the hydrological cycle, soil-water content and its spatial variability in a Moso bamboo forest were compared with those in an adjacent evergreen broadleaved forest, in a case study of a stand in western Japan (northern Kyushu). The volumetric soil-water content averaged over depths between 0 and 60cm was consistently higher in the bamboo stand than that in the broadleaved stand. These results contrast with previous studies comparing the soil-water content in Moso bamboo forests with that in other forest types. The sum of canopy transpiration and soil evaporation (E) in the bamboo stand tended to be larger than that in the broadleaved stand. Small canopy interception loss was reported in the bamboo forest. Therefore, the large amount of E would counterbalance the small canopy interception loss in the bamboo forest. Differences in soil characteristics between the two stands may be the main factor causing differences in soil-water content. Spatial variation in soil-water content in the bamboo stand was larger than that in the broadleaved stand, confirming findings in a previous series of our study. This could happen because the well-developed root-system in the bamboo forest enhances preferential flow in the soil. To evaluate the effects of aggressive invasion of alien giant bamboo on the ecosystem functions, we recommend further studies measuring various hydrological components in various Moso bamboo forests.
机译:在日本,毛竹林(Phyllostachys pubescens,一种外来入侵性巨型竹林)已经自然化并迅速扩张,取代了周围的阔叶和针叶林。为了评估这些森林类型的替换对水文循环的影响,在日本西部一个林分的案例研究中,比较了毛竹林中的土壤水含量及其空间变异性与相邻的常绿阔叶林中的土壤水含量及其空间变异性(九州北部)。竹林地的平均土壤水含量在0至60cm的深度上始终高于阔叶林。这些结果与以前的研究比较,后者比较了毛竹林和其他森林类型中的土壤水分。毛竹林冠层蒸腾和土壤蒸发的总和往往比阔叶林更大。据报道,在竹林中小冠层截留损失。因此,大量的E将抵消竹林中小的冠层截留损失。两个林分之间土壤特性的差异可能是导致土壤含水量差异的主要因素。竹林地的土壤水分含量空间变化大于阔叶林,这证实了我们先前研究的结果。这可能是由于竹林中发达的根系增强了土壤中的优先流动。为了评估侵略性外来巨型竹子对生态系统功能的影响,我们建议进行进一步的研究以测量各种毛竹林中的各种水文成分。

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