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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Effects of forest harvesting on the occurrence of landslides and debris flows in steep terrain of central Japan
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Effects of forest harvesting on the occurrence of landslides and debris flows in steep terrain of central Japan

机译:森林砍伐对日本中部陡峭地形滑坡和泥石流发生的影响

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摘要

Landslides and debris flows associated with forest harvesting can cause much destruction and the influence of the timing of harvesting on these mass wasting processes therefore needs to be assessed in order to protect aquatic ecosystems and develop improved strategies for disaster prevention. We examined the effects of forest harvesting on the frequency of landslides and debris flows in the Sanko catchment (central Japan) using nine aerial photo periods covering 1964 to 2003. These photographs showed a mosaic of different forest ages attributable to the rotational management in this area since 1912. Geology and slope gradient are rather uniformly distributed in the Sanko catchment, facilitating assessment of forest harvesting effects on mass wasting without complication of other factors. Trends of new landslides and debris flows correspond to changes in slope stability explained by root strength decay and recovery; the direct impact of clearcutting on landslide occurrence was greatest in forest stands that were clearcut 1 to 10 yr earlier with progressively lesser impacts continuing up to 25 yr after harvesting. Sediment supply rate from landslides in forests clearcut 1 to 10 yr earlier was about 10-fold higher than in control sites. Total landslide volume in forest stands clearcut 0 to 25 yr earlier was 5.8 x 10(3) m(3) km(-2) compared with 1.3 x 10(3) m(3) km(-2) in clearcuts >25 yr, indicating a fourfold increase compared with control sites during the period when harvesting affected slope stability. Because landslide scars continue to produce sediment after initial failure, sediment supply from landslides continues for 45 yr in the Sanko catchment. To estimate the effect of forest harvesting and subsequent regeneration on the occurrence of mass wasting in other regions, changes in root strength caused by decay and recovery of roots should be investigated for various species and environmental conditions. Copyright (C) 2007 John Wiley & Sons, Ltd.
机译:与森林采伐有关的滑坡和泥石流可能造成很大破坏,因此,必须评估采伐时间对这些大规模浪费过程的影响,以便保护水生生态系统并制定改进的防灾战略。我们使用覆盖1964年至2003年的9个航拍图来研究森林采伐对山口流域(日本中部)滑坡和泥石流频率的影响。这些照片显示了该地区的轮作管理可归因于不同林龄的镶嵌自1912年以来,地质和坡度在三甲流域的分布相当均匀,有助于评估森林采伐对大量浪费的影响,而不会导致其他因素的复杂化。新的滑坡和泥石流的趋势与边坡稳定性的变化相对应,其根源强度衰减和恢复可以解释。砍伐对滑坡发生的直接影响最大的是在早于1至10年砍伐的林分,伐木后持续到25年的影响逐渐减小。在1至10年的时间里,森林砍伐产生的滑坡沉积物供应速率比对照地区高约10倍。 0到25年之前的林地的滑坡总量为5.8 x 10(3)m(3)km(-2),而25年以上的林地的滑坡总量为1.3 x 10(3)m(3)km(-2) ,表明在收割期间,受影响地区的边坡稳定性是对照地区的四倍。由于滑坡疤痕在初始破坏后仍继续产生沉积物,因此在山古流域,滑坡的沉积物供应持续了45年。为了估计森林采伐和随后的更新对其他地区大规模浪费发生的影响,应针对各种物种和环境条件调查因根的腐烂和恢复而引起的根强度变化。版权所有(C)2007 John Wiley&Sons,Ltd.

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