Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah

Pabelan River is one of the rivers in the western slopes of mount Merapi located in Magelang Regency, Central Java province. Pabelan River has watersheds ± 84,70 km2 with the main river length ± 28,40 km2. The purpose of this research was to estimate the amount of sediment transport that occurred at...

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Main Authors: Risky Fauziyah, Bambang Agus Kironoto, Djoko Legono
Format: Article
Language:English
Published: Universitas Muhammadiyah Yogyakarta 2018-05-01
Series:Semesta Teknika
Subjects:
Online Access:https://journal.umy.ac.id/index.php/st/article/view/4107
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spelling doaj-bcb0c584bf5d4d36a9071c3fd4f35cc62021-09-14T05:27:46ZengUniversitas Muhammadiyah YogyakartaSemesta Teknika1411-061X2502-54812018-05-01211535910.18196/st.2112102849Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa TengahRisky Fauziyah0Bambang Agus Kironoto1Djoko Legono2Universitas Gadjah MadaUniversitas Gadjah MadaUniversitas Gadjah MadaPabelan River is one of the rivers in the western slopes of mount Merapi located in Magelang Regency, Central Java province. Pabelan River has watersheds ± 84,70 km2 with the main river length ± 28,40 km2. The purpose of this research was to estimate the amount of sediment transport that occurred at the point of view in the Pabelan River and to know estimate of sediment balance that occurred at the point of view in the Pabelan River. This research was conducted to find out the sediment balance in the Pabelan River whether going on degradation, aggradation, or experience the equilibrium transport. Calculation of sediment balances based on the volume of sediment transport entering at the location selected. Based on the results of sediment transport analysis using MPM, EINSTEIN, DU BOYS and ROTTNER formula, the largest sediment transport volume occurred in PA-C 5 = 4850,592 m3/m/flood, 305,8398 m3/m/flood,  20321,979  m3/m/flood  and 80274,221 m3/m/flood, while the result of calculation based on formula FRIJLINK largest sediment transport volume occurred at PA-C 3 = 3654,817 m3/m/flood. To obtain the result of equilibrium sediment that occurred in the river of research  is by using the five formula  with the condition of the river that occurred aggradation and  degradation with the biggest condition is the result of calculation with the formula ROTTNER for aggradation occurs in PA-C X Prumpung  amount of 47272,806 m3/m/s with increase river bed amount of 13,504 m and degradation occurred at PA-C 5   -47468,692 m3/m/s with decrease at river bed -23,698 m.https://journal.umy.ac.id/index.php/st/article/view/4107sediment transport, sediment balance, and volume of sediment
collection DOAJ
language English
format Article
sources DOAJ
author Risky Fauziyah
Bambang Agus Kironoto
Djoko Legono
spellingShingle Risky Fauziyah
Bambang Agus Kironoto
Djoko Legono
Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
Semesta Teknika
sediment transport, sediment balance, and volume of sediment
author_facet Risky Fauziyah
Bambang Agus Kironoto
Djoko Legono
author_sort Risky Fauziyah
title Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
title_short Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
title_full Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
title_fullStr Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
title_full_unstemmed Kajian Angkutan Sedimen Di Sungai Pabelan, Kabupaten Magelang, Jawa Tengah
title_sort kajian angkutan sedimen di sungai pabelan, kabupaten magelang, jawa tengah
publisher Universitas Muhammadiyah Yogyakarta
series Semesta Teknika
issn 1411-061X
2502-5481
publishDate 2018-05-01
description Pabelan River is one of the rivers in the western slopes of mount Merapi located in Magelang Regency, Central Java province. Pabelan River has watersheds ± 84,70 km2 with the main river length ± 28,40 km2. The purpose of this research was to estimate the amount of sediment transport that occurred at the point of view in the Pabelan River and to know estimate of sediment balance that occurred at the point of view in the Pabelan River. This research was conducted to find out the sediment balance in the Pabelan River whether going on degradation, aggradation, or experience the equilibrium transport. Calculation of sediment balances based on the volume of sediment transport entering at the location selected. Based on the results of sediment transport analysis using MPM, EINSTEIN, DU BOYS and ROTTNER formula, the largest sediment transport volume occurred in PA-C 5 = 4850,592 m3/m/flood, 305,8398 m3/m/flood,  20321,979  m3/m/flood  and 80274,221 m3/m/flood, while the result of calculation based on formula FRIJLINK largest sediment transport volume occurred at PA-C 3 = 3654,817 m3/m/flood. To obtain the result of equilibrium sediment that occurred in the river of research  is by using the five formula  with the condition of the river that occurred aggradation and  degradation with the biggest condition is the result of calculation with the formula ROTTNER for aggradation occurs in PA-C X Prumpung  amount of 47272,806 m3/m/s with increase river bed amount of 13,504 m and degradation occurred at PA-C 5   -47468,692 m3/m/s with decrease at river bed -23,698 m.
topic sediment transport, sediment balance, and volume of sediment
url https://journal.umy.ac.id/index.php/st/article/view/4107
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