Assessment of the Potentiality to the Debris-Flow Occurrence from Physiographic and Morphometrics Parameters: a Case Study in Santo Antônio Basin (Caraguatatuba, São Paulo State, Brazil)
C. Corrêa, Fábio Augusto Gomes Vieira Reis, L. C. Giordano, V. Cabral, M. Gramani, B. M. Gabelini, Beatriz Guzzo Duz, V. Veloso
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引用次数: 4
Abstract
This work aims to evaluate the potential for the debris-flow triggering from Santo Antônio hydrographic basin, located in the Serra do Mar region on North Coast of the State of São Paulo, Brazil, based on physiographic attributes, rainfall data, and morphometric parameters. For this purpose, hydrographic basin techniques were applied, assessing the vulnerability to the debris flow from geomorphological, geological, climatic, and anthropic aspects, and morphometric parameters relevant to the triggering of these processes in watersheds were calculated. Seven physiographic units were identified, which supported the understanding of geological and geomorphological aspects of the basin: coastal plains; river plains; colluvium and talus ramps; escarpments of Serra do Mar; upland of Paraitinga; mountainous relief and hillocks domain. The sub-basins located in steep sections of the relief, with high slopes, valleys, and channels docked, high drainage densities present higher values in the morphometric parameters, indicating a greater potential for triggering and occurrence of debris-flow processes. The joint analysis of physiographic compartmentalization with the identification of relief features, slope, amplitude, valley, slope shapes and morphometric parameters, is extremely relevant to recognize hydrographic basins susceptible to debris flows, as it integrates, and correlates aspects of the physical environment considered to trigger in the occurrence of these processes.
这项工作旨在根据自然地理属性、降雨数据和形态测量参数,评估位于巴西圣保罗州北海岸Serra do Mar地区的Santo Antônio水文盆地引发泥石流的可能性。为此,应用了水文流域技术,从地貌、地质、气候和人文方面评估了泥石流的脆弱性,并计算了与触发流域这些过程相关的形态参数。确定了七个地貌单元,有助于了解盆地的地质和地貌方面:沿海平原;河流平原;崩积层和堆积斜坡;Serra do Mar的悬崖;Paraitinga高地;山地起伏和丘陵地带。子盆地位于地形的陡峭部分,具有高斜坡、山谷和对接的通道,高排水密度在形态参数中表现出更高的值,表明触发和发生泥石流过程的可能性更大。通过识别地形特征、坡度、幅度、山谷、斜坡形状和形态参数,对地貌分区进行联合分析,对于识别易受泥石流影响的水文盆地极为重要,因为它整合并关联了被认为会引发这些过程的物理环境的各个方面。
期刊介绍:
The Anuário do Instituto de Geociências (Anuário IGEO) is an official publication of the Universidade Federal do Rio de Janeiro (UFRJ – CCMN) with the objective to publish original scientific papers of broad interest in the field of Geology, Paleontology, Geography and Meteorology.