PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG

Creep or soil movement as the interesting part of landslide, already happened since 1980's at south side of Talang Bawong Kalibawang Irrigation Channel km 15.9. Various researches have been conducted by using elasto-plastic model which can not accommodate the time dependent behaviour. The objec...

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Main Authors: , Didik Junaidi, , Dr. Ir. ahmad Rifa'i, M.T.
Format: Theses and Dissertations NonPeerReviewed
Published: [Yogyakarta] : Universitas Gadjah Mada 2011
Subjects:
ETD
Online Access:https://repository.ugm.ac.id/90276/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=52718
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spelling id-ugm-repo.902762014-08-20T02:51:04Z https://repository.ugm.ac.id/90276/ PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG , Didik Junaidi , Dr. Ir. ahmad Rifa'i, M.T. ETD Creep or soil movement as the interesting part of landslide, already happened since 1980's at south side of Talang Bawong Kalibawang Irrigation Channel km 15.9. Various researches have been conducted by using elasto-plastic model which can not accommodate the time dependent behaviour. The objective of this research is to study the creep behaviour using numerical model.Soil constitutive model that used are Mohr-Coulomb and soft soil creep that already available in Plaxis. Some engineering judgements are used to give good correspond to field strain data recorded. The behaviour of creeping slope is studied by concerning groundwater level, static loads, seismic and collapse condition of slope.The study result showed that creep depends on groundwater level and its fluctuation which the ground movement can reach about 0.192 mm/year at side of street. Due to the load increment, maximum creep at inspection road reach 0.08 mm/year. For one second period seismic force the slope able to creep until 37.28 mm/year although reduction form 0.395 mm/year up to 0.547 mm/year in three years after. In assumption failure will be happened after 1.05 m up to 1.56 m displacement, the slope failure can occurred about 6 month untill 12 month later. Towards failure in progress the creep increased up to 564.6 mm/year up to 2549.8 mm/year. [Yogyakarta] : Universitas Gadjah Mada 2011 Thesis NonPeerReviewed , Didik Junaidi and , Dr. Ir. ahmad Rifa'i, M.T. (2011) PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=52718
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
topic ETD
spellingShingle ETD
, Didik Junaidi
, Dr. Ir. ahmad Rifa'i, M.T.
PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
description Creep or soil movement as the interesting part of landslide, already happened since 1980's at south side of Talang Bawong Kalibawang Irrigation Channel km 15.9. Various researches have been conducted by using elasto-plastic model which can not accommodate the time dependent behaviour. The objective of this research is to study the creep behaviour using numerical model.Soil constitutive model that used are Mohr-Coulomb and soft soil creep that already available in Plaxis. Some engineering judgements are used to give good correspond to field strain data recorded. The behaviour of creeping slope is studied by concerning groundwater level, static loads, seismic and collapse condition of slope.The study result showed that creep depends on groundwater level and its fluctuation which the ground movement can reach about 0.192 mm/year at side of street. Due to the load increment, maximum creep at inspection road reach 0.08 mm/year. For one second period seismic force the slope able to creep until 37.28 mm/year although reduction form 0.395 mm/year up to 0.547 mm/year in three years after. In assumption failure will be happened after 1.05 m up to 1.56 m displacement, the slope failure can occurred about 6 month untill 12 month later. Towards failure in progress the creep increased up to 564.6 mm/year up to 2549.8 mm/year.
format Theses and Dissertations
NonPeerReviewed
author , Didik Junaidi
, Dr. Ir. ahmad Rifa'i, M.T.
author_facet , Didik Junaidi
, Dr. Ir. ahmad Rifa'i, M.T.
author_sort , Didik Junaidi
title PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
title_short PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
title_full PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
title_fullStr PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
title_full_unstemmed PEMODELAN PERILAKU RAYAPAN TANAH (CREEP) STUDI KASUS LERENG KALIBAWANG
title_sort pemodelan perilaku rayapan tanah (creep) studi kasus lereng kalibawang
publisher [Yogyakarta] : Universitas Gadjah Mada
publishDate 2011
url https://repository.ugm.ac.id/90276/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=52718
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