Modeling of the sliding process in condition of disturbed soil stability
Main goal of this investigation is to present a mechanism, terrain shaping of a certain slope during the sliding process, in time history, up to its final form. It means that except slope material movement what is the slope composed, in time of slope occurrence is emphasized becoming of a new terrai...
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Serbian Geographical Society
2010-01-01
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Series: | Glasnik Srpskog Geografskog Društva |
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Online Access: | http://www.doiserbia.nb.rs/img/doi/0350-3593/2010/0350-35931001035S.pdf |
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doaj-b6bd062bb6104ab787bde6ef1a6ecb2d2020-11-25T00:13:49ZengSerbian Geographical SocietyGlasnik Srpskog Geografskog Društva0350-35932010-01-01901354910.2298/GSGD1001035SModeling of the sliding process in condition of disturbed soil stabilityStojnić NedeljkoMain goal of this investigation is to present a mechanism, terrain shaping of a certain slope during the sliding process, in time history, up to its final form. It means that except slope material movement what is the slope composed, in time of slope occurrence is emphasized becoming of a new terrain form as a result of the process itself, too. This way of investigation definitively opens a new approach in a terrain relief form prediction depends on terrain characteristics and expecting weather occurrence. Here is analyzed a process of land crumbing and sliding on a Neogene slope at Ubilci place (part of urban area of Smederevo city), which was triggered by humane activities (undercutting of slope) and weather influence (rainy period). To present continuity flow of the slope material movement, it is used extended distinct element method. Profile line of the terrain surface which is obtained by numerical analyzes is in very good agreement with the finale profile line of the slope where a real case of crumbing and soil sliding has occurred. . http://www.doiserbia.nb.rs/img/doi/0350-3593/2010/0350-35931001035S.pdfnumerical analysismaterial movementfinale profile shape |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Stojnić Nedeljko |
spellingShingle |
Stojnić Nedeljko Modeling of the sliding process in condition of disturbed soil stability Glasnik Srpskog Geografskog Društva numerical analysis material movement finale profile shape |
author_facet |
Stojnić Nedeljko |
author_sort |
Stojnić Nedeljko |
title |
Modeling of the sliding process in condition of disturbed soil stability |
title_short |
Modeling of the sliding process in condition of disturbed soil stability |
title_full |
Modeling of the sliding process in condition of disturbed soil stability |
title_fullStr |
Modeling of the sliding process in condition of disturbed soil stability |
title_full_unstemmed |
Modeling of the sliding process in condition of disturbed soil stability |
title_sort |
modeling of the sliding process in condition of disturbed soil stability |
publisher |
Serbian Geographical Society |
series |
Glasnik Srpskog Geografskog Društva |
issn |
0350-3593 |
publishDate |
2010-01-01 |
description |
Main goal of this investigation is to present a mechanism, terrain shaping of a certain slope during the sliding process, in time history, up to its final form. It means that except slope material movement what is the slope composed, in time of slope occurrence is emphasized becoming of a new terrain form as a result of the process itself, too. This way of investigation definitively opens a new approach in a terrain relief form prediction depends on terrain characteristics and expecting weather occurrence. Here is analyzed a process of land crumbing and sliding on a Neogene slope at Ubilci place (part of urban area of Smederevo city), which was triggered by humane activities (undercutting of slope) and weather influence (rainy period). To present continuity flow of the slope material movement, it is used extended distinct element method. Profile line of the terrain surface which is obtained by numerical analyzes is in very good agreement with the finale profile line of the slope where a real case of crumbing and soil sliding has occurred. . |
topic |
numerical analysis material movement finale profile shape |
url |
http://www.doiserbia.nb.rs/img/doi/0350-3593/2010/0350-35931001035S.pdf |
work_keys_str_mv |
AT stojnicnedeljko modelingoftheslidingprocessinconditionofdisturbedsoilstability |
_version_ |
1725393010720505856 |