Khoiriyah, Tia Miftahul (2016) STUDI PARAMATERIK PENGARUH INTENSITAS CURAH HUJAN TERHADAP JARAK JANGKAUAN DAN KECEPATAN LONGSOR BERDASARKAN MODEL GESEKAN COLOUMB SEDERHANA. S1 thesis, Universitas Pendidikan Indonesia.
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Abstract
Studi paramaterik pengaruh intensitas curah hujan terhadap jarak jangkauan (run-out) dan kecepatan longsor dilakukan pada lereng potensi longsor di Kabupaten Bandung Barat yang telah dikarakterisasi menggunakan uji keteknikan tanah. Daerah-1 memiliki kemiringan 68o dan Daerah-2 memiliki kemiringan 79o. Karakteristik tanah bidang gelincir Daerah-1 termasuk jenis tanah lempung kelanauan dan Daerah-2 termasuk jenis tanah lempung dengan tingkat kepadatan lebih tinggi dibandingkan dengan tanah bahan longsor yang termasuk tanah lanau. Intensitas curah hujan menurunkan nilai faktor keamanan hingga menjadi konstan pada suatu nilai tertentu dimana nilai tersebut mengindikasikan batas kemampuan tanah mengikat air. Daerah-1 memiliki kemampuan mengikat air lebih banyak dengan kecepatan yang lebih cepat dibandingkan Daerah-2 sehingga Daerah-1 akan lebih cepat jenuh seiring dengan jumlah air yang terinfiltrasi. Batas kemampuan mengikat air pada Daerah-1 yaitu pada intensitas curah hujan 10 mm/jam dan Daerah-2 pada intensitas curah hujan 30 mm/jam. Nilai faktor keamanan Daerah-1 konstan pada nilai 0,698 dengan intensitas 10 mm/jam dan Daerah-2 konstan pada nilai 0,692 dengan intensitas 30 mm/jam. Intensitas curah hujan mempengaruhi run-out dan kecepatan longsor. Semakin tinggi intensitas curah hujan maka semakin rendah run-out hingga konstan pada nilai tertentu. Run-out longsor maksimum pada Daerah-1 yaitu 1,454 m dan run-out longsor minimum pada Daerah-1 yaitu 1,364 m. Sedangkan run-out longsor maksimum pada Daerah-2 yaitu 3,175 m dan run-out longsor minimum pada Daerah-2 yaitu 1,620 m. Begitupun dengan kecepatan longsor, semakin tinggi intensitas curah hujan maka semakin rendah kecepatan longsor tersebut hingga konstan pada nilai tertentu. Daerah-1 memiliki kecepatan longsor maksimum yaitu 2,082 m/s dan kecepatan longsor minimum 1,112 m/s pada intensitas curah hujan 10 mm/jam sedangkan Daerah-2 memiliki kecepatan longsoran maksimum yaitu 5,311 m/s dan kecepatan longsor minimum yaitu 3,983 m/s pada intensitas curah hujan 30 mm/jam. Perbedaan nilai run-out dan kecepatan longsor antara Daerah-1 dan Daerah-2 disebabkan oleh perbedaan kemiringan dan sudut geser lereng. ; A parametic study on the impact of rainfall intensity to landslide run-out and velocity has been employed on potential landslide slope in West Bandung Regional. The slope was characterized by soil technical test. The result showed that Region-1 has slope about 68o and Region to has slope about 79o. The characterictic of slip area soil Region-1 was categorized as silty-clayey while the Region-2 was considered as clayey. Both of the slip area soil has the higher density rather than soil erosian material which is include as silty. The rainfall intensity descreased safety factor value until to be constan in a certain point in which it indicated the ability of soil to bind water. The ability of binding water and its velocity of Region-1 is greater than the Region-2. Therefore, Region-1 will be more saturated easier since infiltration of water. The binding water ability of Region-1 was at 10 mm/hours rainfall intensity and Region-2 was at 30 mm/hours rainfall intensity. The safety factor value of Region-1 was constantly on 0,698 with 10 mm/hours intensity and Region-2 was constantly on 0,692 with 30/hours intensity. The rainfall intensity effected landslide run-out and velocity. It was found that in terms of rainfall intensity, the higher rainfall intensity the lower landslide run-out until reach a certain constant point. The Region-1 has maximum landslide run-out about 1,454 m and minimum landslide run-out about 1,364 m. While the Region-2 has maximum landslide run-out about 3,175 m and minimum landslide run-out about 1,620 m. While in the light of landslide velocity, The higher rainfall intensity the lower landslide velocity until constant in certain point. The Region-1 has maximum landslide velocity about 2,082 m/s and minimum landslide velocity about 1,112 m/s on 10 mm/hours rainfall intensity. While the Region-2 has maximum landslide velocity about 5,311 m/s and minimum landslide velocity about 3,983 m/s in 30 mm/hours in rainfall intensity. The difference of landslide run-out and velocity rank among Region-1 and Region-2 were caused by different of slope and friction angle slope.
| Item Type: | Thesis (S1) |
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| Additional Information: | No Panggil : S FIS KHO s-2016 ; Nama Pembimbing : I. Selly Feranie . II. Adrin Tohari . |
| Uncontrolled Keywords: | intensitas curah hujan, faktor keamanan, jarak jangkauan (run-out) longsor, kecepatan longsor ; rainfall intensity, safety factor, landslide run-out, landslide velocity |
| Subjects: | L Education > L Education (General) Q Science > Q Science (General) Q Science > QC Physics |
| Divisions: | Fakultas Pendidikan Matematika dan Ilmu Pengetahuan Alam > Jurusan Pendidikan Fisika > Program Studi Fisika (non kependidikan) |
| Depositing User: | Mr mhsinf 2017 |
| Date Deposited: | 19 Sep 2017 00:35 |
| Last Modified: | 19 Sep 2017 00:35 |
| URI: | http://repository.upi.edu/id/eprint/26093 |
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