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  <title>ANALISIS KESTABILAN LERENG BERDASARKAN KLASIFIKASI MASSA BATUAN RMR DAN SMR DI JALAN RAYA BANDA ACEH-LHOKSEUDU, KM 30 DAN KM 31, KECAMATAN LEUPUNG, ACEH BESAR</title>
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 <name type="Personal Name" authority="">
  <namePart>M. Fahmi</namePart>
  <role>
   <roleTerm type="text">Primary Author</roleTerm>
  </role>
 </name>
 <typeOfResource manuscript="no" collection="yes">mixed material</typeOfResource>
 <genre authority="marcgt">bibliography</genre>
 <originInfo>
  <place>
   <placeTerm type="text">Banda Aceh</placeTerm>
   <publisher>Universitas Syiah Kuala</publisher>
   <dateIssued>2019</dateIssued>
  </place>
 </originInfo>
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  <languageTerm type="code">id</languageTerm>
  <languageTerm type="text">Indonesia</languageTerm>
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 <note>ABSTRAK &#13;
Ruas jalan yang membentang pada topografi perbukitan dengan kemiringan lereng&#13;
yang curam sangat beresiko terhadap terjadinya kelongsoran. Berdasarkan studi&#13;
literatur menunjukkan bahwa lereng pada ruas jalan raya Banda Aceh- Lhokseudu&#13;
KM 30 dan KM 31, Kecamatan Leupung, Aceh Besar tersebut termasuk kedalam&#13;
jenis batuan gamping. Penelitian ini dilakukan dengan tujuan untuk mengetahui&#13;
potensi dan jenis longsoran yang  akan terjadi berdasarkan analisis kinematik serta&#13;
memberikan penilian terhadap kualitas massa batuan berdasarkan klasifikasi massa&#13;
batuan Rock Mass Rating (RMR) dan Slope Mass Rating (SMR). Penelitian ini&#13;
menggunakan metode Scanline dengan panjang total keseluruhan lereng. Hasil&#13;
analisis kinematik pada ruas jalan KM 30 yaitu terdapat 4 longsoran yang&#13;
berpotensi terjadi diantaranya longsoran baji (perpotongan joint set 1 dan joint set&#13;
3), longsoran baji (perpotongan joint set 1 dan joint set 5), longsoran bidang (joint&#13;
set 3), dan longsoran bidang (joint set 2) dengan nilai bobot RMR sebesar 66.40&#13;
dan bobot SMR untuk ke-4 jenis longsoran tersebut adalah 23.02, 49.57, 45.97 dan&#13;
66.37. Sedangkan pada KM 31 terdapat 3 longsoran jenis baji yang berpotensi yaitu&#13;
(perpotongan joint set 1 dan joint set 2), (perpotongan joint set 2 dan joint set 3),&#13;
dan (perpotongan joint set 1 dan joint set 3) dengan nilai bobot RMR 68.22 dan&#13;
nilai bobot SMR berturut-turut 17.22, 62.92 dan 60.72. Hasil kesimpulan dari&#13;
penelitian ini yaitu lereng di KM 30 diklasifikasikan ke dalam kelas IV (buruk) dan&#13;
potensi terjadinya longsor sebesar 60% sedangkan lereng di KM 31 diklasifikasikan&#13;
ke dalam kelas V (sangat buruk) dan potensi terjadinya longsor sebesar 90%.&#13;
&#13;
&#13;
Kata Kunci:  Lereng, Kestabilan Lereng, Analisis Kinematik, Rock Mass Rating &#13;
&#13;
 &#13;
(RMR) dan Slope Mass Rating (SMR). &#13;
&#13;
&#13;
ABSTRACT &#13;
Roads that stretch on hills topography with steep slopes are very risky for&#13;
landslides. Based on literature studies show that the slopes on the Banda AcehLhokseudu&#13;
&#13;
highway KM 30 and KM 31, Leupung sub-District, Aceh Besar are&#13;
included in the type of limestone. This study was conducted with the aim to&#13;
determine the potential and types of landslides that will occur based on kinematic&#13;
analysis and provide an assessment of rock mass quality based on rock mass&#13;
classification Rock Mass Rating (RMR) and Slope Mass Rating (SMR). This study&#13;
uses the Scanline method with the total length of the overall slope. The results of&#13;
kinematic analysis on KM 30 road section are 4 landslides that have the potential&#13;
to occur including wedge landslides (joint set 1 intersection and joint set 3), wedge&#13;
landslide (joint set 1 intersection and joint set 5), planar landslides (joint set 3), and&#13;
planar landslides (joint set 2) with a weight value of RMR of 66.40 and the weight&#13;
of the SMR for the 4 types of landslides are 23.02, 49.57, 45.97 and 66.37. Whereas&#13;
in KM 31 there are 3 potential wedge landslides that are (joint set 1 and joint set 2&#13;
intersections), (joint set 2 and joint set 3 intersections), and (joint set 1 and joint set&#13;
3 intersections) with a weight of RMR 68.22 and the value of the SMR weights are&#13;
17.22, 62.92 and 60.72. The conclusion of this study is that the slopes in KM 30 are&#13;
classified into class IV (bad) and the potential for landslides is 60% while the slopes&#13;
in KM 31 are classified into class V (very poor) and the potential for landslides is&#13;
90%.&#13;
&#13;
&#13;
Keywords: Slope, Slope Stability, Kinematic Analysis, Rock Mass Rating (RMR)&#13;
and Slope Mass Rating (SMR).</note>
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  <physicalLocation>ELECTRONIC THESES AND DISSERTATION Universitas Syiah Kuala</physicalLocation>
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