Evolution of the Porong River Estuary, Indonesia: Morphological Changes of Lusi Island through Sediment Modeling and Time-Series Interpretation of MNDWI

IF 2.5 Q4 ENVIRONMENTAL SCIENCES
Agus Sufyan, Rudhy Akhwady, Dini Purbani, Aprizon Putra, Ulung Jantama Wisha, Kintan Nurani Ekawati, Safar Dody, Sari Nova, Dendy Mahabror,  Sujantoko, Widya Prarikeslan, Andik Dwi Muttaqin, Moch Shofwan
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Abstract

A sedimentation issue in the estuary of Porong induced by Lapindo hot mud discharge had caused a significant morphological alteration. This study aims to determine the geomorphological evolution in the Porong Estuary and the geochronological formation of Lusi Island. This study employed a numerical modeling approach, consisting of flow and sediment transport modeling modules (Delft3D-FLOW and Delft3D-SED), with a curvilinear grid resolution of 25–50 m over a 5 × 6 km domain. A satellite imagery processing was also performed using multitemporal Landsat data (2000–2024) analyzed using the Modified Normalized Difference Water Index (MNDWI), followed by binary classification and vector digitization. The results show that sediment accumulation of ± 0.06 m in 15 days, increasing to over 1 m after four years (MORFAC 96), with land expansion confirmed by satellite data from 6.29 hectares in 2000 to 147.86 hectares in 2024. Of particular concern, the increasing sediment thickness from 0.0026 m to 0.38 m over a 14-year equivalent simulation suggests a sustained process of geomorphological development. The findings of this study emphasize significant sedimentation trends and the dynamics of the estuarine environment in the Porong Estuary. It is, therefore, crucial to implement coastal hazard mitigation strategies, effective land use planning, and environmental monitoring to minimize further environmental degradation resulting from excessive sedimentation.

印尼柏龙河河口演化:基于沉积物模拟和MNDWI时间序列解释的Lusi岛形态变化
拉平多热泥排放引起的柏龙河口沉积问题造成了明显的地貌改变。本研究旨在确定坡龙口的地貌演化和芦泗岛的年代形成。本研究采用数值模拟方法,包括流动和泥沙输运建模模块(Delft3D-FLOW和Delft3D-SED),在5 × 6 km的区域内,曲线网格分辨率为25-50 m。利用修正归一化差水指数(MNDWI)对2000-2024年多时段Landsat数据进行卫星图像处理,然后进行二值分类和矢量数字化。结果表明:15 d泥沙累积量为±0.06 m, 4 d后增加到1 m以上(MORFAC 96),卫星资料证实土地面积从2000年的6.29公顷增加到2024年的147.86公顷。特别值得关注的是,在14年的等效模拟中,沉积物厚度从0.0026 m增加到0.38 m,表明地貌发育是一个持续的过程。本研究的结果强调了柏龙河口显著的沉积趋势和河口环境的动力学。因此,必须执行沿海减灾战略、有效的土地利用规划和环境监测,以尽量减少过度沉积造成的进一步环境退化。
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CiteScore
3.80
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