侵蚀和泥石流传播的形态计量指标:以保加利亚卡尔扎利镇西北部byyukdere河流域为例

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
V. Nikolova, Dimitar Sachkov, R. Rizova
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引用次数: 0

摘要

地形表面的形态特征是侵蚀和泥石流发生的主要前提(条件因素)之一。本研究计算了比育克德尔河流域的以下形态计量参数:流域面积、流域起伏度、流域长度、起伏比、梅尔顿指数、坡度和水流功率指数。分析表明,一级和二级盆地对侵蚀和泥石流的敏感性较高(Strahler方法)。河功率指数的升高表明,比育克德尔河流域下游侵蚀强烈,这与火山-沉积岩和河谷断裂性质有关。基于12.5 m分辨率的数字高程模型,在ArcGIS Pro中进行形态计量学分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Morphometric indicators for erosion and debris flows propagation: a case study of the river Byuyukdere watershed, northwest of Kardzhali town (Bulgaria)
Morphometric features of the topographic surface are one of the main prerequisites (conditioning factors) for the occurrence of erosion and debris flows. The following morphometric parameters of the river Byuyukdere watershed were calculated in the current study: basin area, basin relief, basin length, relief ratio, Melton’s index, slope and stream power index. The analysis shows higher susceptibility to erosion and debris flows of the 1st and 2nd order basins (Strahler’s method). The elevated values of the stream power index indicate an intensive erosion in the lower part of the river Byuyukdere watershed, which is related to the volcanogenic-sedimentary rocks and the faulted nature of the river valley. The morphometric analysis was performed in ArcGIS Pro on the base of a 12.5 m resolution digital elevation model.
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