COMPUTATIONAL MODELING OF SEDIMENTATION ON THE KALIMANTAN COAST AS A MANGROVE HABITAT
Abstract
The coastline of East Kalimantan, extending approximately 1,185–3,500 km, serves as an important habitat for extensive mangrove forests and directly faces the Makassar Strait and the Java Sea. Coastal dynamics in this region are strongly influenced by hydrodynamic factors such as currents, waves, and tides, which significantly affect sediment transport and shoreline morphology. This study aims to model sediment transport patterns and deposition rates along the East Kalimantan coast using a computational approach. Field data on wave height, current velocity, tides, and sediment transport were collected from three representative coastal locations in East Kalimantan, namely Berau Regency, Bontang City, and North Penajam Paser Regency. The numerical model integrated hydrodynamic parameters with Stokes' Law and the Ferguson–Church equation to simulate sediment transport under different tidal conditions. The results showed that average current velocities ranged from 0.5 to 0.8 cm/s, while average wave heights varied between 0.3 and 1.0 m. Sediment transport modeling was conducted by integrating wave equations with the Stokes settling law and the Ferguson–Church equation through the ECOMSED application. The results showed that sediment deposition velocities ranged from 0.5 to 4.5 × 10⁻⁴ g/L/s, indicating moderate sediment accumulation across several coastal segments. The dominant sediment transport direction was toward the southern coastline and concentrated near river mouths, where deposition processes were more intensive. These findings highlight the importance of understanding coastal sediment dynamics for shoreline management, mangrove conservation, and mitigation of coastal degradation in East Kalimantan. Computational modeling provides an effective tool for predicting future sedimentation patterns and supporting sustainable coastal ecosystem management.
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References
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