浅层平移滑坡地形易发性分类的水文地质条件:地质水文生态学方法

Roberta Silva, Ana Netto, Willy Lacerda
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摘要

这项工作是按照地质水文生态学方法对浅层平移滑坡的地形易发性进行分析和分类的方法程序审查的一部分。试点地区位于新弗里堡(RJ),特别是在达安塔斯溪流域(53 平方公里)。在这一阶段的工作中,对地貌参数和指数进行了评估,包括坡角、曲率、排水效率指数(DEI)和地形位置指数(TPI),这些参数和指数被认为与调节土壤的水文和机械行为有关。获得的结果与 2011 年 1 月里约热内卢州高原地区(Região Serrana)发生的极端降雨事件中的滑坡疤痕(n = 382)清单进行了交叉分析。通过这一交叉点,可以评估这些参数与斜坡断裂之间的关系。根据 AHP 方法,每个等级的滑坡面积集中度有助于为所采用的每个等级确定权重。建议重新调整斜坡角度等级,并将标准曲率纳入水文地质条件图的绘制中。结果令人欣喜,88.74%(0.85 平方公里)的滑坡区域集中在高侵蚀潜力等级。
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Hydro-geomorphological conditions for the classification of terrain susceptibility to shallow translational landslides: a geo-hydro ecological approach
This work is part of the review of methodological procedures for the analysis and classification of terrain susceptibility to shallow translational landslides, following the geohydro ecological approach. The pilot area is located in Nova Friburgo (RJ), specifically in the D’Antas Creek basin (53 km2). At this stage of the work, geomorphological parameters and indices were evaluated, including slope angle, curvature, drainage efficiency index (DEI) and topography position index (TPI), seen as relevant in regulating the hydrological and mechanical behavior of soils. The results obtained were intersected with an inventory of landslide scars (n = 382) referring to the extreme rainfall event in January 2011, which occurred in the highland region, called Região Serrana, of the state of Rio de Janeiro. This intersection allowed an evaluation between these parameters and the slopes rupture. The concentration of landslide area per class subsidized the establishment of weights for each of the adopted classes, based on the AHP method. A readjustment of the slope angle classes was proposed, as well as the inclusion of the standard curvature in the construction of the Hydro-Geomorphological Conditions Map. The results were promising, with a concentration of 88.74% (0.85 km2) of the landslide areas in the class of high erosive potential.
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