https://journals.itb.ac.id/index.php/jts/issue/feed Jurnal Teknik Sipil 2023-09-05T08:35:51+07:00 Prof. Dr. Bambang Sugeng S., DEA. jts@si.itb.ac.id Open Journal Systems <div style="text-align: justify;"><a href="https://journals.itb.ac.id/index.php/jts" target="_blank" rel="noopener"><strong>Jurnal Teknik Sipil</strong> is a scientific journal published periodically every three months on <strong>April, August</strong> and <strong>December.</strong></a></div> <div> </div> <div style="text-align: justify;">Jurnal Teknik Sipil was published for the first time in 1990 with a mission as a pioneer in the scientific research publication of Civil Engineering in Indonesia.</div> <div> </div> <div style="text-align: justify;">As a national media, Jurnal Teknik Sipil is expected to accommodate the need for a media to disseminate information and latest publication for researchers and practitioners of Civil Engineering in Indonesia. In its development, Jurnal Teknik Sipil has been accredited based on the decision <a href="https://lppm.itb.ac.id/wp-content/uploads/sites/55/2021/12/Surat-pemberitahuan-hasil-akreditasi-elektronik-periode-I-tahun-2017.pdf">letter of Directorate General of Research and Development Strengthening, Ministry of Research, Technology and Higher Education of the Republic of Indonesia, no. : 32a/E/KPT/2017</a>, dated 26 April 2017 as a national scientific journal since 1996 and is currently has been re-accredited on April 2017.</div> <div> </div> <div style="text-align: justify;">With this achievement, Jurnal Teknik Sipil has been established as a media with high quality. Until now the Jurnal Teknik Sipil still an process to maintain its quality scientific publishing only the latest research results in the domain of Civil Engineering.</div> <div> </div> <div><strong><a href="https://get.google.com/albumarchive/107091118610478581121/album/AF1QipN2Jn_OA8Or2Y6sbVxIx4GnuI0V4nRlxqaTq1R0?authKey=CJLBweWC8JnEBA">SK Accreditation</a></strong></div> <div><a href="https://get.google.com/albumarchive/107091118610478581121/album/AF1QipN2Jn_OA8Or2Y6sbVxIx4GnuI0V4nRlxqaTq1R0/AF1QipMpjtWXq4hMFMZ7UdatlHqdRLBEF6BvnBz224o3?authKey=CJLBweWC8JnEBA"><img src="http://167.205.57.68/public/site/images/admin_jts/Sertifikat_JTS001.jpg_btl_.jpg" alt="" /></a><strong>ISSN</strong> 0853-2982 since 29/05/2007</div> <div><strong>E-ISSN</strong> 2549-2659 since 26/10/2016</div> <div> </div> <div><strong><span style="text-decoration: underline;">Publication History</span></strong></div> <div>Last edition journal : <a href="https://ftsl.itb.ac.id/jurnal-teknik-sipil/">https://ftsl.itb.ac.id/jurnal-teknik-sipil/</a></div> <div> </div> <div><strong>Indexing</strong> : <a href="https://scholar.google.co.id/citations?user=7y8sI58AAAAJ&amp;hl=id">Google Scholar</a> | <a href="https://doaj.org/toc/2549-2659?source=%7B%22query%22%3A%7B%22filtered%22%3A%7B%22filter%22%3A%7B%22bool%22%3A%7B%22must%22%3A%5B%7B%22term%22%3A%7B%22index.issn.exact%22%3A%222549-2659%22%7D%7D%2C%7B%22term%22%3A%7B%22_type%22%3A%22article%22%7D%7D%5D%7D%7D%2C%22query%22%3A%7B%22match_all%22%3A%7B%7D%7D%7D%7D%2C%22from%22%3A0%2C%22size%22%3A100%7D">Directory of Open Access Journals (DOAJ)</a> | <a href="https://garuda.kemdikbud.go.id/journal/view/9165">Indonesian Publication Index (IPI)/Portal Garuda</a> | <a href="https://www.doi.org/index.html">Digital Object Identifier (DOI)</a> | <a href="https://search.crossref.org/?q=jurnal+teknik+sipil">Crossref</a> |<a href="https://sinta.kemdikbud.go.id/journals/detail?id=945">Science and Technology Index (SINTA) </a>| Indonesian Scientific Journal Database (ISJD)</div> <div> </div> <div><strong><a href="https://statcounter.com/p11256474/summary/?guest=1">View My Stats</a></strong></div> <div><a href="https://scholar.google.co.id/citations?user=7y8sI58AAAAJ&amp;hl=id"><strong><img src="http://167.205.57.68/public/site/images/admin_jts/google_scholar.jpg" alt="" /></strong></a> <a title="hit counter" href="https://statcounter.com/p11256474/summary/?guest=1" target="_blank" rel="noopener"><img src="http://c.statcounter.com/11256474/0/04439389/0/" alt="hit counter" /></a></div> <div> </div> <div><a href="https://creativecommons.org/licenses/by-nd/4.0/" rel="license"><img src="https://i.creativecommons.org/l/by-nd/4.0/88x31.png" alt="Lisensi Creative Commons" /></a></div> <div>This work is licensed under a <a href="https://creativecommons.org/licenses/by-nd/4.0/">Creative Commons Attribution-NoDerivatives 4.0 International License</a></div> <div> </div> https://journals.itb.ac.id/index.php/jts/article/view/21768 The Effect of Coastal Dike and Retention Pond Performance on Flood and Tidal Control in Pekalongan 2023-08-25T10:50:43+07:00 Adhitya Gilang Irawanto gilangadhit.irawan@gmail.com Joko Nugroho joko@si.itb.ac.id Adi Prasetyo adi.prasetyo@pu.go.id <p>Abstract.<br>Pekalongan is one of the areas located in the north of Java Island. The main problem in Pekalongan is tidal<br>flooding. This tidal flood worsens when there is a high discharge in the river. For this reason, the government built<br>a Coastal Dike and a Retention Pond to overcome these problems. The concept of this system is to create a coastal<br>dike that crosses the river to eliminate tidal effects. The retention pond is located along the coastal dike to<br>accommodate the discharge from the river, then the water will be pumped downstream of the river. This study aims<br>to obtain pump operating time for each pump built in this system to reduce the flood elevation of Q25 to – 0.5 m in<br>the retention pond. One dimensional flow modeling was used in the approach with the Hydrologic Engineering<br>Center-River Analysis System (HEC-RAS) 6.0 model. This research shows that the pump operating time for the<br>Silempeng and Sengkarang pumps is 150 hours. The addition of Mrican pumps and flap gates can reduce pump<br>operating time to support the success of Coastal Dike and Retention Ponds in controlling floods and tidal in<br>Pekalongan.<br>Keywords: Tidal flood, coastal dike, retention pond, pump.</p> <p><br>Abstrak.<br>Pekalongan merupakan salah satu daerah yang terletak di utara Pulau Jawa. Masalah utama di Pekalongan<br>adalah banjir rob. Banjir rob ini semakin parah ketika terjadi debit yang tinggi di aliran sungai. Untuk itu<br>pemerintah membangun tanggul rob dan kolam retensi untuk mengatasi permasalahan tersebut. Konsep sistem ini<br>adalah membuat tanggul rob yang melintang sungai, menghalangi backwater dari laut untuk menghilangkan efek<br>pasang surut. Kolam retensi terletak di sepanjang tanggul rob untuk menampung debit dari sungai, kemudian air<br>akan dipompa ke arah hilir sungai. Tujuan dari penelitian ini adalah mendapatkan waktu operasional pompa untuk<br>masing-masing pompa yang terbangun di sistem ini dalam menurunkan elevasi banjir Q25 sampai dengan elevasi –<br>0,5 m di kolam retensi. Di dalam penelitian ini juga dilihat waktu operasional pompa setelah penambahan pompa<br>mrican dan pintu klep di Mrican. Pemodelan satu aliran dimensi dilakukan dengan model HEC-RAS 6.0. Hasil dari<br>penelitian ini adalah waktu operasional pompa untuk pompa silempeng dan sengkarang adalah 150 jam.<br>Penambahan pompa Mrican dan pintu klep dapat mengurangi waktu operasi pompa untuk mendukung<br>keberhasilan Tanggul Pesisir dan Kolam Retensi dalam pengendalian banjir dan pasang surut di Pekalongan.</p> <p><br>Kata-kata Kunci: Banjir rob, tanggul rob, kolam retensi, pompa.</p> 2023-08-25T00:00:00+07:00 Copyright (c) 2023 Jurnal Teknik Sipil https://journals.itb.ac.id/index.php/jts/article/view/21769 Study of Flood Risk Assessment on Banyumas and Cilacap District in Downstream Serayu River Basin, Indonesia 2023-08-25T15:07:47+07:00 Pratita Hana Kirana kiranahanap@gmail.com Mohammad Farid mfarid_si99@yahoo.com Mohammad Bagus Adityawan bagus.adityawan@ftsl.itb.ac.id Arno Adi Kuntoro arnoak@ftsl.itb.ac.id Widyaningtyas Widyaningtyas widya@ftsl.itb.ac.id <p>Abstract.</p> <p>Floods due to the Downstream Serayu River overflow inundate agricultural land and houses in parts of Banyumas<br>and Cilacap district every year. Based on the classification of flood hazard level referring to Chief of BNPB<br>Regulation Number 2 the Year 2012 on General Guidelines for Assessment of Disaster Risk, some location points<br>experienced a high level of flood hazard (&gt;1.5 m). The objective of this study is to develop a flood risk map by using<br>GIS. Flood hazard assessment uses the HEC-RAS 5.0.6 two-dimensional model, verified with field observation data.<br>The river discharge is obtained from hydrological calculations, while the tidal component is obtained using<br>MATLAB-LP Tides BIG. River geometry uses river cross-section from field measurement data for hydraulic<br>modeling combined with MERIT DEM as its banks. The capacity level also refers to the BNPB Number 2 the Year<br>2012. In this study, BNPB and PUPR parameters are used. The vulnerability component refers to a 2014 study from<br>the Ministry of Public Work and Housing (PUPR) Indonesia. The 50-year flood return period shows that the total<br>area of risk flooded areas in the Downstream Serayu River Basin is 6.22 km2, while high-risk flooded areas are 2.2 km2.</p> <p><br>Keywords: Flood risk, HEC-RAS 2D, GIS, MATLAB–LP Tides BIG, MERIT DEM</p> <p><br>Abstrak.</p> <p>Banjir akibat luapan Sungai Serayu Hilir setiap tahun menggenangi lahan pertanian dan perumahan di sebagian<br>wilayah Kabupaten Banyumas dan Cilacap. Berdasarkan klasifikasi tingkat bahaya banjir mengacu pada<br>Peraturan Kepala BNPB Nomor 2 Tahun 2012 tentang Pedoman Umum Pengkajian Risiko Bencana, beberapa titik<br>lokasi mengalami tingkat bahaya banjir tinggi (&gt;1,5 m). Tujuan dari penelitian ini yaitu mengembangkan peta<br>risiko banjir dengan menggunakan SIG. Pemodelan banjir menggunakan model dua dimensi HECRAS 5.0.6, yang<br>diverifikasi dengan data observasi lapangan. Debit sungai diperoleh dari perhitungan hidrologi, sedangkan<br>komponen pasang surut diperoleh dari perhitungan menggunakan MATLAB-LP Tides BIG. Geometri sungai<br>menggunakan penampang sungai dari data pengukuran lapangan untuk pemodelan hidrolik yang dikombinasikan<br>dengan MERIT DEM sebagai bantarannya. Tingkat kapasitas juga mengacu pada Peraturan Kepala BNPB Nomor<br>2 Tahun 2012. Dalam penelitian ini digunakan parameter BNPB dan PUPR. Komponen kerentanan mengacu pada<br>studi tahun 2014 dari Kementerian Pekerjaan Umum dan Perumahan Rakyat (PUPR) Indonesia. Periode ulang<br>banjir 50 tahun menunjukkan bahwa total luas area yang berisiko banjir di DAS Serayu Hilir sebesar 6,22 km2,<br>sedangkan area dengan tingkat risiko banjir tinggi sebesar 2,2 km2.</p> <p><br>Kata-kata Kunci: Risiko banjir, HEC-RAS 2D, SIG, MATLAB–LP Tides BIG, MERIT DEM</p> 2023-08-25T00:00:00+07:00 Copyright (c) 2023 Jurnal Teknik Sipil https://journals.itb.ac.id/index.php/jts/article/view/21771 Study of Sedimentation Control on Bangga River, Palu Watershed, Central Sulawesi 2023-08-25T16:15:34+07:00 Fanny Aliza Savitri fannyaliza@pu.go.id Mohammad Bagus Adityawan bagus.adityawan@ftsl.itb.ac.id Widyaningtias Widyaningtias widya@ftsl.itb.ac.id <p>Abstract.</p> <p><br>Bangga River is located in a mountainous area in the Palu River Basin with an area of 74.82 km2 and a river length<br>of 16.97 km. Flood with the approximated water depth of 3 m occur in Bangga’s Village. The cliffs upstream of the<br>Bangga River areunstable and can easily collapse due to the disaster. Ministry of Public Works and Housing<br>control through Sabo dam’s structure. This study aims to analyze the performance of sabo dam’s structure in<br>reducing sediments and the floods. Analysis and modeling using two scenarios, before and after the sabo dam<br>structure’s control was built, using HEC-RAS Software with purposeful 1D modeling to simulate flow patterns, total<br>sediment. The HEC-RAS simulation shows that the water surface is stood at 2.1 m depth in the existing condition.<br>Sabo dam structure can reduce of sediment transport, which was computed according to Engelund (81%<br>reduction), Mayer Peter Muller (MPM) with 92% reduction, and Yang (91% sediment yields reduction). So, the<br>sabo dam's structure is not merely utilized to retain the sediment, but it can reduce potential flooding in the future.<br>Keywords: Sedimentation, sediment control building, HEC-RAS, sabo dam, flood.</p> <p><br>Abstrak.</p> <p><br>Sungai Bangga terletak di daerah pegunungan di DAS Palu dengan luas 74,82 km2 dan memiliki panjang sungai<br>16,97 km. Banjir dengan kedalaman air + 3 m terjadi di Desa Bangga. Tebing-tebing di hulu Sungai Bangga tidak<br>stabil dan mudah runtuh akibat bencana. Kementerian Pekerjaan Umum dan Perumahan Rakyat mengontrol<br>melalui bangunan Sabo dam. Penelitian ini bertujuan untuk menganalisis kinerja bangunan Sabo dam dalam<br>mereduksi sedimen dan banjir. Analisis dan pemodelan dilakukan dengan dua skenario yaitu sebelum dan sesudah<br>bangunan sabo dam terbangun, menggunakan Software HEC-RAS dengan pemodelan 1D yang bertujuan untuk<br>mensimulasikan pola aliran dan total sedimen. Simulasi HEC-RAS menunjukkan bahwa kedalaman air berada<br>pada 2,1 m pada kondisi eksisting. Bangunan sabo dam dapat mereduksi transpor sedimen, yang dihitung menurut<br>beberap rumus yaitu Engelund (reduksi 81%), Mayer Peter Muller (MPM) dengan reduksi 92%, dan Yang (reduksi<br>91%). Jadi, bangunan sabo dam tidak hanya dimanfaatkan untuk menahan sedimen, tetapi dapat mengurangi<br>potensi banjir di masa depan.</p> <p><br>Kata-kata kunci: Sedimentasi, bangunan pengontrol sedimen, HEC-RAS, sabo dam, banjir.</p> 2023-08-25T00:00:00+07:00 Copyright (c) 2023 Jurnal Teknik Sipil https://journals.itb.ac.id/index.php/jts/article/view/21842 The Influence of Sedimentation to The Morfology Change of Serang River Estuary at The National Strategic Area Yogyakarta International Airport (Ksn Yia) 2023-09-05T08:35:51+07:00 Dibo Separnu diboseparnu@gmail.com M Syahril Badri Kusuma msbadrik2014@gmail.com Dantje K Natakusumah dkn.mpsda.01@gmail.com <p>Abstrak.</p> <p>Bandara Internasional Yogyakarta terletak di Kawasan Strategis Nasional, Kabupaten Kulon Progo. Daerah ini secara geologis merupakan daerah dataran rendah yang diapit oleh Sungai Bogowonto dan Sungai Serang yang menyebabkan banjir tahunan pada musim hujan. Sistem pengendalian banjir dikembangkan untuk menjaga kinerja bandara. Penetapan Kawasan Strategis Nasional juga menyebabkan perubahan tata guna lahan di sekitarnya yang dapat mempengaruhi perubahan morfologi sungai. Perubahan morfologi di kedua sungai tersebut telah diidentifikasi berdasarkan pengamatan di lapangan. Berdasarkan pengamatan tersebut dapat diketahui bahwa peningkatan laju sedimentasi merupakan parameter terpenting yang dapat mengubah morfologi kedua sungai tersebut. Pengaruh perubahan morfologi di muara sungai Serang telah dipelajari dengan menggunakan software DELFT3D, sedimentasi di muara sungai Serang telah disimulasikan dengan beberapa skenario antara lain pada saat monsun barat dan monsun timur. Hasil pemodelan menunjukkan bahwa tebal sedimentasi di muara Serang pada kondisi eksisting adalah 3,5 m pada musim barat dengan luas 0,063 ha dan 4,0 m pada musim timur dengan luas 0,437 ha.</p> <p>Kata-kata Kunci: <em>Morfologi, muara, Delft3D</em></p> <p>Abstract.</p> <p>The Yogyakarta International Airport has located in the National Strategic Area, Kulon Progo regency. This area is geologically a low-lying area flanked by the Bogowonto River and the Serang River which causes annual flooding in the rainy season. A flood control system was developed to maintain airport performance. The determination of the National Strategic Area has also led to changes in the surrounding land use which can affect changes in the morphology of the rivers. The morphological changes in the two rivers have been identified based on field observations. Based on this observation, it can be seen that the increase in sedimentation rate is the most important parameter that can change the morphology of the two rivers. The effect of morphological changes in the Serang river estuary has been studied using DELFT3D software, the sedimentation in the Serang river estuary has been simulated with several scenarios, including during the west monsoon and east monsoon. The modeling results show that the sedimentation thickness in the Serang estuary under existing conditions is 3.5 m in the west season with an area of ​​0.063 ha and 4.0 m in the east monsoon with an area of ​​0.437 ha.</p> <p>Keywords: <em>Morphology, estuary, Delft3D</em></p> 2023-09-05T00:00:00+07:00 Copyright (c) 2023 Jurnal Teknik Sipil