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Effects of Volcanic Ash on the Runoff Process in Sakurajima Volcano

机译:火山灰对撒库岛火山径流过程的影响

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We investigated the effects of volcanic ash covering on the runoff process and the areas contributing to the occurrence of Hortonian overland flow on a bare land slope by spreading Sakurajima volcanic ash over the experimental catchment. Results of analyses by a runoff model and field investigation showed that the ash-covering caused a decrease of rainfall loss and Manning's coefficient of roughness and an increase of the area contributing to the occurrence of Hortonian overland flow, surface runoff, and sediment discharge. However, the rainfall loss and Manning's coefficient of roughness increased over time through the armoring of the surface volcanic ash layer, and as a result, the area contributing to the occurrence of Hortonian overland flow, surface runoff, and sediment discharge also decreased.
机译:我们调查了火山灰覆盖对径流过程的影响以及通过在实验集水区传播Sakurajima火山灰在裸陆坡上产生霍顿陆陆流动的领域。径流模型和现场调查分析结果表明,灰烬覆盖率导致降雨量减少和曼宁的粗糙系数,增加了对霍顿陆型流动,表面径流和沉积物排放的贡献。然而,通过表面火山灰层的装甲随着时间的推移,降雨量损失和曼宁的粗糙系数随着时间的推移而增加,因此有助于霍顿陆孔流动,表面径流和沉积物排放的面积也降低。

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