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Ecosystem changes following the 2016 Kumamoto earthquakes in Japan: Future perspectives

机译:2016年日本熊本地震后的生态系统变化:未来展望

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摘要

Major earthquakes cause widespread environmental and socioeconomic disruptions that persist for decades. Extensive ground disturbances that occurred during the shallow-focus Kumamoto earthquakes will affect future sustainability of ecosystem services west of Aso volcano. Numbers of earthquake-initiated landslides per unit area were higher in grasslands than forests, likely owing to greater root reinforcement of trees, and mostly initiated on ridgelines and/or convex/planar hillslopes. Most landslides traveled short distances and did not initially evolve into debris flows; resultant sediments and wood accumulating in headwater channels can be mobilized into debris flows during future storms. Fissures along ridgelines may promote water ingress and induce future landslides and debris flows that affect residents downstream. Native grasses are at risk because of habitat fragmentation caused by ground disturbances, extensive damage to rural roads, and abandonment of traditional pasture management practices. Sustainable management of affected areas needs to consider future risk of cascading hazards and long-term socioeconomic impacts.
机译:大地震造成了广泛的环境和社会经济破坏,并持续了数十年。在熊本浅焦点地震中发生的广泛地面干扰将影响阿苏火山以西的生态系统服务的未来可持续性。草原上单位面积的地震引发的滑坡数量高于森林,这可能是由于树木的根系增强所致,并且多数是在山脊线和/或凸面/平面山坡上引发的。大多数滑坡行进的距离很短,最初并没有演变成泥石流。由此产生的沉积物和堆积在源头水道中的木材可以在未来的暴风雨中动员为泥石流。沿山脊的裂缝可能会促进水的进入,并引发未来的滑坡和泥石流,从而影响下游居民。由于地面干扰,对农村道路的广泛破坏以及放弃传统的牧场管理做法而造成的栖息地破碎,原生草面临着危险。对受灾地区的可持续管理需要考虑到级联危害和长期社会经济影响的未来风险。

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