Please use this identifier to cite or link to this item: https://repositori.uma.ac.id/handle/123456789/11186
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dc.contributor.advisorHermanto, Edy-
dc.contributor.advisorLubis, Kamaluddin-
dc.contributor.authorMalau, Sandi-
dc.date.accessioned2019-11-27T04:31:55Z-
dc.date.available2019-11-27T04:31:55Z-
dc.date.issued2019-
dc.identifier.urihttps://repositori.uma.ac.id/handle/123456789/11186-
dc.descriptionSeringkali cuaca merupakan banjir di kabupaten asahan dan kota tanjung balai karena luapan dataran sungai, sangat menarik untuk digunakan solusi penanggulangan penelitian mengenai masalah banjir sungai Asahan di Kabupaten Asahan, dimulai dengan data primer dan sekunder yang berkaitan dengan lokasi dan inventarisasi data curah hujan dan data kondisi sungai yang ada. Selanjutnya, analisis frekuensi rencana metode perhitungan curah hujan dan debit banjir, Rata-rata Banjir Tahunan, melchior dan haspers. Dari analisis debit banjir, untuk merencanakan banjir yang tangguh digunakan debit banjir periode 25 tahun dengan metode Mean Annual Flood Q25 = 335.792 m3 / detik, metode kombinasi metode Melchior-Log Pearson III Q25 = 450.197 m3 / detik dan konsep metode Melchior-Haspers Q25 = 519.971 m3 / detik, metode pencarian Haspers-Log Pearson III Q25 = 1.280.405 m3 / detik dan kombinasi Haspers Haspers Q25 = 1.478.847m3 / detik. Hasil menggunakan metode langkah standar menunjukkan tambahan ketinggian banjir tidak lagi dapat ditampung oleh sungai Asahan. Berdasarkan analisis masalah di atas, tanggul tambahan diperlukan untuk mengakomodasi debit banjir maksimum dari sungai Asahan.en_US
dc.description.abstractOften the weather is a flood in kabupaten asahan and kota tanjung balai due to the overflow of the river plain, very attractive for use solutions countermeasures research on the problem of flooding rivers Asahan in Kabupaten Asahan, starting with the primary and secondary data relating to location and inventory of rainfall data and the data of existing conditions of the river Furthermore, the frequency analysis of rainfall and flood discharge calculation method plan Mean Annual Flood, melchior and haspers. From the analysis of flood discharge, to plan formidable floods are used debit flood return period of 25 years with the method of Mean Annual Flood Q25 = 335.792 m3 / sec, the method of combination of methods Melchior-Log Pearson III Q25 = 450.197 m3 / sec and methods concept Melchior-Haspers Q25 = 519.971 m3 / sec, the search method Haspers-Log Pearson III Q25 = 1,280,405 m3 sec and a combination Haspers Haspers Q25 = 1,478,847m3/sec. The result using a standard step method shows the additional flood level elevation was no longer able to be accommodated by the river Asahan. Based on the analysis of the above problems, additional embankments are required to accommodate the maximum flood discharge of the Asahan river.en_US
dc.language.isoiden_US
dc.publisherUniversitas Medan Areaen_US
dc.relation.ispartofseriesNPM;128110055-
dc.subjectsungai asahanen_US
dc.subjectmetode langkah standaren_US
dc.subjecttanggul banjiren_US
dc.subjectasahan riveren_US
dc.subjectstandard step methoden_US
dc.subjectflood embankmenten_US
dc.titleSistem Penanganan Dan Pengendalian Banjir Sungai Asahanen_US
dc.typeThesisen_US
Appears in Collections:SP - Civil Engineering

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