研究海岸建筑实验室修复南苏拉威西苏拉威西的海啸病例

Yolla Jessika, I. Dharma, I. G. N. Dirgayusa, Adi Prasetyo
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引用次数: 0

摘要

印尼位居第二,是受海啸袭击最频繁的国家,大大小小的地震经常发生在印尼。2018年发生在南苏拉威西省巴鲁东加拉的7.4级地震引发了高达3-5米的海啸,震中位于海湾北部,导致死亡人数和基础设施被毁。为了最大限度地减少损失和人员伤亡,以红树林和植被作为自然保护,海堤作为海岸加固物的沿海建筑形式的结构减灾可能是预测巴鲁湾地区脆弱性的正确步骤。本研究旨在分析沿海结构的衰减水平,并确定海啸减灾规划的最佳替代方案。该试验在Balai Pantai实验室使用物理模型(波浪水槽)进行,共进行了48次试验,三个波浪产生目标(0.07 m、0.09 m和0.11 m)、深度(0.40 m、0.414).m和0.428 m)和植被宽度(0.40米、0.70 m和1 m)的变化分为24个场景。物理模型试验结果表明,海岸结构的存在对传输波的特性和速度有显著影响。红树林和植被的存在成功地将波浪传播减少了20-100%,在相对水位(平均水位)下也能够显著降低高达100%的波浪速度,在平均海拔(海平面)下可降低高达87%,在最高潮汐状态(高水位)下可降低高达22%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Studi Laboratorium Bangunan Pantai Untuk Mereduksi Gelombang Tsunami Kasus Palu, Sulawesi Selatan
Indonesia ranked second as the country most frequently hit by tsunamis, earthquakes large and small often occur in Indonesia. The earthquake in Palu-Donggala, South Sulawesi in 2018 with a magnitude of 7.4 had generated a tsunami as high as 3-5 m, and the epicenter was in the north of the bay which resulted in the death toll and the destruction of infrastructure. In minimizing losses and casualties, structural disaster mitigation in the form of coastal buildings consisting of mangroves and vegetation as natural protection and sea walls as coastal reinforcement can be the right step to anticipate the vulnerability of the Palu Bay area. This study aimed to analyzed the level of attenuation in coastal structures and determine the best alternative for tsunami disaster mitigation planning. The test was carried out with a physical model using (wave flume) at the Balai Pantai Laboratory with a total of 48 times of testing with variations of three wave generation targets (0.07 m, 0.09 m, and 0.11 m), depth (0.40 m, 0.414). m, and 0.428 m) and the width of the vegetation (0.40 m, 0.70 m, and 1 m) which are divided into 24 scenarios. The results of the physical model test showed that the presence of coastal structures has a significant effect on the characteristics of the transmission waves, and the speed. The existence of mangrove forests and vegetation has succeeded in reducing wave transmission by 20-100%, also being able to reduce wave speed up to 100% significantly in the relative water level (Mean Water Level), reducing up to 87% at average elevation (Sea Water Level) ), and reduce up to 22% at the highest tide state (High Water Level).
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