Abstract

The drainage area of the secondary drainage system of the Gunungsari often occurs inundation or flood during rain. This is due to land use change, which was originally a water catchment area transformed into a densely populated area that resulted in disruption of soil absorption so that runoff becomes bigger. The analysis used in this thesis includes hydrological analysis, land use analysis, domestic discharge analysis, cumulative discharge analysis and hydraulics analysis. The hydrological analysis calculated the rainfall at return period of 2, 5, and 10 year with the Pearson Log distribution III, discharge calculation of the plan with the return period by means of the rational method and the method of coefficient value of land use (C) the land is then divided by the area of each sub das. The analysis of domestic waste was calculated from the total population prediction in the future and the water needs of the population. The cumulative discharge was total from domestic discharge and flood discharge of the return period of 2, 5, and 10 years. Hydraulic analysis was calculated to know the existing capacity of channel. The changing of land use were represented by average land use value ( Caverage ), which the value are 0,732; 0,725 and 0,747 for the year 2002; 2007 and 2017 respectively. Based on the results of flood discharge planning analysis, cumulative discharge in return periods of 10 years and hydraulic analysis, the flooding occurred at Darmo Indah channel (segment 5-2) by comparing capacity discharge 2,49 m3 / s and cumulative discharge 4,360 m3/s, Darmo Harapan channel (segment 4-5) by comparing capacity discharge 2,90 m3/s and cumulative discharge 4,496 m3/s. Darmo Satelit channel (segment 7-8) by comparing capacity drainage 4,08 m3/s and cumulative discharge 4,586 m3/s and Simo Gunung channel (segment 18-19) by comparing capacity drainage and cumulative discharge 1,31 m3/s and 2,648m3/s. The capacity of existing secondary channels is not able to accommodate cumulative water discharge over the next 10 years. Therefore, the solution to overcome the flooding is by substituting existing channel box culvert. On the other had, another way to prevent flooding are maintenance and cleaning of solid waste and sedimention regularly.

Highlights

  • Provinsi Jawa Timur yang menjadi pusat kegiatan pemerintahan, ekonomi, politik, sosial budaya dan kegiatan lainnya

  • This is due to land use change

  • densely populated area that resulted in disruption of soil absorption

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Summary

PENDAHULUAN

Provinsi Jawa Timur yang menjadi pusat kegiatan pemerintahan, ekonomi, politik, sosial budaya dan kegiatan lainnya. Hal ini menyebabkan peningkatan perubahan tata guna lahan dan mengurangi daerah resapan air hujan, sehingga menyebabkan banjir di beberapa daerah di Surabaya. Berdasarkan uraian permasalahan diatas, maka dapat dirumuskan permasalahan yang akan dibahas yaitu perubahan tataguna lahan di Surabaya Barat tahun 2002 sampai 2017 untuk rencana tata ruang tahun 2030, merancang debit banjir perode ulang 2, 5, 10 tahun, kapasitas eksisting saluran saat ini mampukah menampung debit banjir yang terjadi, solusi yang tepat untuk upaya penanggulangan perubahan tata guna lahan yang terjadi di kota Surabaya. Batasan masalah yang diberikan ialah daerah yang dianalisis hanya daerah limpasan drainase Kota Surabaya Barat, mengevaluasi tingkat penyalahgunaan tata guna lahan, debit banjir rencana yang digunakan hanya debit limpasan, tidak memperhitungkan rencana anggaran biaya pada saluran ini, tidak memperhitungkan sedimentasi, tidak mendesain ulang dimensi saluran pada analisis system drainase Gunungsari

METODOLOGI PENELITIAN
Gumbel
G Simo Mulyo Barat
D Darmo Satelit
KESIMPULAN DAN SARAN
Full Text
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