在肯达里市曼东加地区洪水影响的特征和地区研究

Hasddin Hasddin, Erny Tamburaka
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引用次数: 0

摘要

摘要本研究旨在分析苏拉威西省东南部Kendari市Mandong地区的洪水特征。本研究采用定性描述设计和调查。分析的对象是洪水的分类(山洪、泛滥、潮汐泛滥)、泛滥的条件(泛滥高度)和泛滥的原因。主要数据是在野外获得的,次要数据是在2013-2018年与洪水事件相关的各种来源获得的。这项研究涉及31名被调查者。数据分析采用定量描述和空间分析(GIS,即ArcView 3.2)。研究结果表明,发生在满洞a地区的洪水被归类为淹没洪水。水坑高度在1 ~ 2米之间,平均淹没时间为1天(下雨时)。其原因是高降雨、河流和排水不良的积累导致沿溪流产生废物,以及由于建筑活动(建筑物)而失去吸水性。满洞a地区受洪水影响的面积约占总面积的37.45%。它分布在所有街道,最大的面积是拉比比亚村,约占受影响总面积(416.23公顷)的29.10%,其次是瓦翁巴拉塔村,约占23.01%,最小的是Anggilowu村
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Studi Karakteristik dan Wilayah Terdampak Banjir di Kecamatan Mandonga, Kota Kendari
Karakteristik, Luas Genangan ABSTRACT The study aims to analyze the characteristics of floods that occurred in Mandong District, Kendari City, Southeast Sulawesi Province. The study used a qualitative descriptive design and survey. The object of analysis is flood classification (flash floods, inundation, and tidal flooding), inundation conditions (inundation height), and causes of flooding. Primary data was obtained in the field, while secondary data was obtained from various sources related to flood events in 2013-2018. This study involved 31 informants. Data were analyzed by quantitative descriptive and spatial analysis (GIS, namely ArcView 3.2). The results of the study showed that the floods that occurred in Mandonga District were classified as inundation floods. The height of the puddle is between 1-2 m, and the average inundation time is 1 day (during it rains). The cause is the accumulation of high rainfall, river, and poor drainage resulting in the generation of waste along the stream, as well as loss of water absorption due to construction activities (buildings). The area affected by flooding in Mandonga District is around 37.45% of the total area. It is spread across all sub-districts, with the largest area in Labibia Village around 29.10% of the total affected area (416.23 ha), followed by Wawombalata Village at around 23.01%, while the smallest is in Anggilowu Village
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