1Loka Riset Sumber Daya dan Kerentanan Pesisir, Kementerian Kelautan dan Perikanan, Indonesia
2Pusat Riset Kelautan, Kementerian Kelautan dan Perikanan, Indonesia
BibTex Citation Data :
@article{JKT6076, author = {Guntur Rahmawan and Ulung Wisha and Wisnu Gemilang and ilham ilham and Semeidi Husrin}, title = {Prediksi Akumulasi Sedimen Berdasarkan Survei Batimetri dan Hidrodinamika di Pesisir Teluk Mandeh, Kabupaten Pesisir Selatan, Sumatera Barat}, journal = {Jurnal Kelautan Tropis}, volume = {23}, number = {1}, year = {2020}, keywords = {Sedimentasi; batimetri; hidrodinamika; Teluk Mandeh}, abstract = { Mandeh Bay is a semi-enclosed water area that there are two main estuaries, Mandeh and Nyalo River estuary. Sedimentation issue has been gotten worse due to the massive development in coastal area. This study aims to determine the sediment accumulation within Mandeh bay and its distribution patterns. The measurement of sedimentation rate applied in the Mandeh and Nyalo Estuaries. Oceanography parameters (tides and currents) recorded for 30 days measurement. The thickness of sediment accumulation was predicted by applying single beam echosounder dual frequency. The calculation of sediment volume was done using frustum formula grid 10 x10 meters. Flow model approach was also simulated to depict the distribution pattern of sediment. The thickness of sediment accumulation categorized into five spatial categories that are 0-0,3m, 0,4-0,6m, 0,7-0,9,1-1,2m, and 1,3-1,5m. The sedimentation rate in Mandeh estuary ranged from 60,85 up to 62,16 g.m -2 .day -1 , while in Nyalo estuary is approximately 48,86 g.m -2 .day -1 . The tidal current speed that is weak ranged from 0-0,05 m/s induces the sediment accumulation which mainly occurs during the neap tidal conditions. The thickness of sediment accumulation which is more than one meter identified around Mandeh River estuary and several areas near Carocok Tarusan Port where the sediment intake takes place and due to the weak current feature, it causes the increase of sedimentation in this region. Teluk mandeh merupakan kawasan teluk semi tertutup yang mempunyai 2 muara sungai besar yaitu sungai Mandeh dan sungai Nyalo. Masalah sedimentasi menjadi semakin parah karena pengembangan wilayah pesisir yang masif. Tujuan dari penelitian ini adalah untuk mengetahui ketebalan akumulasi sedimen di dalam Teluk Mandeh dan pola distribusinya. Pengukuran laju sedimentasi dilakukan pada dua fokus area yakni muara Sungai Mandeh dan Sungai Nyalo. Pengukuran parameter oseanografi (arus dan pasang surut) dilakukan selama 30 hari pengukuran. Ketebalan akumulasi sedimen diukur menggunakan alat Single Beam Echosounder Dual Frekuensi. Perhitungan volume sedimen dihitung dengan rumus frustum grid 10x10 meter. Simulasi flow model juga dilakukan untuk mengetahui pola distribusi sedimen. Sebaran ketebalan sedimen yang dibagi dalam 5 kategori spasial yakni 0-0,3m, 0,4-0,6m, 0,7-0,9,1-1,2m, dan 1,3-1,5m. Laju sedimentasi di muara Sungai Mandeh berkisar antara 60,85 sampai 62,16 g.m -2 .hari -1 dan di muara Sungai Nyalo rata-rata 48,86 g.m -2 .hari -1 . Kecepatan arus pasang surut yang cukup lemah berkisar antara 0-0,05 m/s menyebabkan potensi akumulasi sedimen akan berlangsung terutama saat kondisi perbani. Sedimen dengan ketebalan lebih dari 1 meter teridentifikasi di sekitar Sungai Mandeh dan beberapa Kawasan Pelabuhan Carocok Tarusan dimana asupan sedimen mendominasi. Karena karakteristik arus yang lemah, sedimentasi meningkat diwilayah ini. }, issn = {2528-3111}, pages = {105--116} doi = {10.14710/jkt.v23i1.6076}, url = {https://ejournal2.undip.ac.id/index.php/jkt/article/view/6076} }
Refworks Citation Data :
Mandeh Bay is a semi-enclosed water area that there are two main estuaries, Mandeh and Nyalo River estuary. Sedimentation issue has been gotten worse due to the massive development in coastal area. This study aims to determine the sediment accumulation within Mandeh bay and its distribution patterns. The measurement of sedimentation rate applied in the Mandeh and Nyalo Estuaries. Oceanography parameters (tides and currents) recorded for 30 days measurement. The thickness of sediment accumulation was predicted by applying single beam echosounder dual frequency. The calculation of sediment volume was done using frustum formula grid 10 x10 meters. Flow model approach was also simulated to depict the distribution pattern of sediment. The thickness of sediment accumulation categorized into five spatial categories that are 0-0,3m, 0,4-0,6m, 0,7-0,9,1-1,2m, and 1,3-1,5m. The sedimentation rate in Mandeh estuary ranged from 60,85 up to 62,16 g.m-2.day-1, while in Nyalo estuary is approximately 48,86 g.m-2.day-1. The tidal current speed that is weak ranged from 0-0,05 m/s induces the sediment accumulation which mainly occurs during the neap tidal conditions. The thickness of sediment accumulation which is more than one meter identified around Mandeh River estuary and several areas near Carocok Tarusan Port where the sediment intake takes place and due to the weak current feature, it causes the increase of sedimentation in this region.
Teluk mandeh merupakan kawasan teluk semi tertutup yang mempunyai 2 muara sungai besar yaitu sungai Mandeh dan sungai Nyalo. Masalah sedimentasi menjadi semakin parah karena pengembangan wilayah pesisir yang masif. Tujuan dari penelitian ini adalah untuk mengetahui ketebalan akumulasi sedimen di dalam Teluk Mandeh dan pola distribusinya. Pengukuran laju sedimentasi dilakukan pada dua fokus area yakni muara Sungai Mandeh dan Sungai Nyalo. Pengukuran parameter oseanografi (arus dan pasang surut) dilakukan selama 30 hari pengukuran. Ketebalan akumulasi sedimen diukur menggunakan alat Single Beam Echosounder Dual Frekuensi. Perhitungan volume sedimen dihitung dengan rumus frustum grid 10x10 meter. Simulasi flow model juga dilakukan untuk mengetahui pola distribusi sedimen. Sebaran ketebalan sedimen yang dibagi dalam 5 kategori spasial yakni 0-0,3m, 0,4-0,6m, 0,7-0,9,1-1,2m, dan 1,3-1,5m. Laju sedimentasi di muara Sungai Mandeh berkisar antara 60,85 sampai 62,16 g.m-2.hari-1 dan di muara Sungai Nyalo rata-rata 48,86 g.m-2.hari-1. Kecepatan arus pasang surut yang cukup lemah berkisar antara 0-0,05 m/s menyebabkan potensi akumulasi sedimen akan berlangsung terutama saat kondisi perbani. Sedimen dengan ketebalan lebih dari 1 meter teridentifikasi di sekitar Sungai Mandeh dan beberapa Kawasan Pelabuhan Carocok Tarusan dimana asupan sedimen mendominasi. Karena karakteristik arus yang lemah, sedimentasi meningkat diwilayah ini.
Article Metrics:
Last update:
Upon acceptance for publication, authors agree to transfer the copyright of their article to Jurnal Kelautan Tropis, while retaining the right to reuse their work under the terms of the open license applied.
From the date of publication, the copyright for each article is held by Jurnal Kelautan Tropis. This transfer allows the journal to manage, disseminate, and preserve scholarly content in accordance with international standards and open access best practices.
Although copyright is held by the journal, all published articles are made available under the Creative Commons Attribution-ShareAlike 4.0 International License (CC BY-SA 4.0). Under this license, anyone may:
Copy and redistribute the material in any medium or format
Remix, transform, and build upon the material for any purpose, even commercially
provided that:
Appropriate credit is given to the original author(s) and the source
Indications are made of any changes that were made
Derivative works are distributed under the same license (CC BY-SA 4.0)
While copyright is held by the journal, authors retain important reuse rights. Authors may:
Reuse the published version of their article in future works, including books, compilations, and lectures
Deposit the published version in institutional or subject repositories
Share the article freely, including on personal websites or academic networks
as long as the original publication in Jurnal Kelautan Tropis is cited and the CC BY-SA 4.0 license terms are respected.
Authors must ensure that any third-party content included in the article (e.g., figures, images, datasets) is either original, in the public domain, or licensed for reuse under compatible terms. If specific permissions are required, authors must obtain them prior to submission.
For questions regarding copyright or licensing, please contact the editorial office at: j.kelautantropis@gmail.com
View My Stats
Jurnal Kelautan Tropis is published by Departement of Marine Science, Faculty of Fisheries and Marine Science, Universitas Diponegoro under a Creative Commons Attribution-ShareAlike 4.0 International License.
