Modeling of individual debris flows based on DEMNAS using Flow-R: A case study in Sigi, Central Sulawesi

IF 0.1 Q4 GEOSCIENCES, MULTIDISCIPLINARY Riset Geologi dan Pertambangan Pub Date : 2022-06-30 DOI:10.14203/risetgeotam2022.v32.1215
Moch Hilmi Zaenal Putra, Indra Andra Dinata, I. Sadisun, D. Sarah, A. Aulia, S. Sukristiyanti
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Abstract

On 2018 September 28, 18:03 a local time (10:03 am UTC), the Mw 7.5 earthquake with a focal depth of about 20 km devastated the Palu region in Central Sulawesi, Indonesia resulting in a catastrophic disaster and many casualties. The Palu earthquakes triggered widespread landslides upstream, contributing to the sizeable material volume accumulated in rivers and mountain slopes. After the Palu earthquake, from September 28, 2018, until December 2021, at least 24 events of debris floods have occurred, which have spread to 15 villages. As of late, the empirical debris flow model Flow-R, software for susceptibility mapping of debris flows at a regional scale, was published. While Flow-R's applicability on a regional scale has been confirmed in several studies, the calibrated case using back-analysis of individual debris flow events in Indonesia based on DEMNAS with a spatial resolution of 8.3 m has never been conducted. Local debris flows modeling using Flow-R was evaluated with three well-documented debris flow events on the break slopes on the west and east sides of the Palu Valley. Quantitative analysis was carried out in this study to assess the accuracy, positive predictive value, and negative predictive value of models. First, the result shows the individual back-analysis model of debris flows found good agreement between debris-flow paths predicted and documented debris flow path extent. However, the parameters for rheological properties and erosion rate required in the software are limited. Second, the quantitative analysis shows accuracy, positive, and negative predictive value, which varies considerably. Based on the study, Flow-R is not suitable for comprehensive hazard mapping but provides a direct information about possible run-outdebris flow paths. Furthermore, lateral spreading and friction of Flow-R model results can be used to calibrate the process with rheological properties and erosion rate in other numerical modeling software, either for forward or back analysis.
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基于Flow-R的基于DEMNAS的单个泥石流建模:以苏拉威西岛中部锡吉岛为例
当地时间2018年9月28日18时03分(世界标准时间10时03分),印尼苏拉威西岛中部帕卢地区发生震源深度约20公里的里氏7.5级地震,造成巨大灾害和人员伤亡。帕卢地震引发了广泛的上游滑坡,导致大量物质堆积在河流和山坡上。帕卢地震后,从2018年9月28日到2021年12月,至少发生了24次泥石流事件,并蔓延到15个村庄。最近,在区域尺度上发布了泥石流敏感性制图软件flow - r的经验泥石流模型。虽然flow - r在区域尺度上的适用性已经在几项研究中得到证实,但从未进行过基于空间分辨率为8.3 m的DEMNAS对印度尼西亚个别泥石流事件进行反分析的校准案例。利用flow - r进行局部泥石流建模,并对帕卢河谷西侧和东侧断裂坡上的三个有充分记录的泥石流事件进行了评估。本研究对模型的准确性、正预测值和负预测值进行了定量分析。结果表明,泥石流个体反分析模型在预测的泥石流路径范围与文献记录的泥石流路径范围之间具有较好的一致性。然而,软件中要求的流变性能和侵蚀速率参数是有限的。第二,定量分析显示准确性、正预测值和负预测值差异较大。研究表明,flow - r不适合用于综合灾害制图,但它提供了可能的溢出泥石流路径的直接信息。此外,Flow-R模型的横向扩展和摩擦结果可用于其他数值模拟软件中校准具有流变特性和侵蚀速率的过程,用于正向或反向分析。
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Riset Geologi dan Pertambangan
Riset Geologi dan Pertambangan GEOSCIENCES, MULTIDISCIPLINARY-
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