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Impact of Forest Harvesting on Slope Stability in Managed Forest Catchment, Nara Prefecture, Japan

机译:日本奈良县管理森林集水区坡稳定性的影响

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Forest harvesting that induces the root decay of logged trees and the root recovery of replanted trees affects stability of slopes over time; these factors influence the occurrence of shallow landslides. Landslides cause loss of life and property; thus, the occurrence of landslides is considered to be one of the most detrimental effects of forest harvesting. Although many studies have been carried out to evaluate the effect of forest harvesting on the occurrence of landslides, the impact of harvesting differs in each study due to dissimilar site conditions (i.e., geology, physiography, and climate). Thus, field data that can neglect the influence of these complex conditions is necessary for testing simulation model predictions of the effects of forest harvesting on landslide occurrences. Using aerial photograph investigations and field surveys, we examined the occurrence of landslides with regard to forest harvesting in the Sanko catchment (Nara prefecture, central Japan), where rotational management yields a mosaic of different forest ages over the years. In the Sanko catchment, geology and slope gradient are rather uniformly distributed, allowing the evaluation of the forest harvesting effect by ignoring other factors. The trends in the landslide frequency in the managed forests correspond to changes in slope stability; this is explained by root strength decay and recovery. The impact of landslide occurrence can be summarized to be strongest for 1-10 yr after forest harvesting and smaller impacts continue up to 25 yr after harvesting. In the Sanko catchment, the influence of forest harvesting on landslide occurrence is more evident in steep slopes as compared to gentler slopes. Only smaller landslides (< 100 m~3) whose slide surface might be shallower than root depth are accelerated by forest harvesting, while the effect of forest harvesting is not obvious for larger landslides (> 100 m~3). These characteristics of landslide frequency relevant to forest harvesting can be demonstrated by landslide models based on infinite slope stability.
机译:森林收获诱导登陆树的根衰减和被复制树木的根系回收率影响斜坡的稳定性;这些因素会影响浅层滑坡的发生。山体滑坡导致生命和财产丧失;因此,山体滑坡的发生被认为是森林收获的最不利影响之一。虽然已经进行了许多研究来评估森林收获对山体滑坡发生的影响,但由于不同的位点状况(即地质,地质,气候),收获的影响与每种研究的影响不同。因此,可以忽视这些复杂条件影响的现场数据是测试森林收割对滑坡发生效果的模拟模型预测所必需的。使用空中照片调查和现场调查,我们研究了Sanko集水区(日本中部奈良县)的森林收获的山体滑坡的发生,旋转管理在多年来几年内产生了不同森林年龄的马赛克。在Sanko集水区内,地质和坡度梯度相当均匀分布,允许通过忽略其他因素来评估森林采伐效果​​。管理林中滑坡频率的趋势对应于坡度稳定性的变化;这是根本强度衰减和恢复解释的。在森林收获后1-10岁的情况下,山体滑坡发生的影响最强,并且在收获后较小的影响越长达25次。在SANKO集水区内,与温和斜坡相比,森林收获对山坡发生的影响在陡坡中更明显。只有森林收割的较大的山体滑坡(<100 m〜3)的滑块(<100 m〜3)较浅的山水深度加速,而森林收获的效果对于较大的滑坡(> 100m〜3)而言并不明显。与森林收获相关的滑坡频率的这些特征可以通过基于无限坡度稳定性的滑坡模型来证明。

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