VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL

In regions of intensive precipitation, slopes tend to become viscid due to accumulated moisture. The ultimate resistance of soils susceptible to landslides is equal to zero, while shear stresses between layers are proportional to the velocity gradient. To prevent landslides, slope soil is stabilized...

Full description

Bibliographic Details
Main Authors: Buslov Anatoliy Semenovich, Kalacheva Elena Nikolaevna
Format: Article
Language:English
Published: Moscow State University of Civil Engineering (MGSU) 2012-10-01
Series:Vestnik MGSU
Subjects:
Online Access:http://vestnikmgsu.ru/files/archive/issues/2012/3/ru/3.pdf
id doaj-a64589db841d4f85903b3f1b4d753cee
record_format Article
spelling doaj-a64589db841d4f85903b3f1b4d753cee2020-11-24T23:21:33ZengMoscow State University of Civil Engineering (MGSU)Vestnik MGSU 1997-09352012-10-0131624VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALLBuslov Anatoliy Semenovich0Kalacheva Elena Nikolaevna1Moscow State University of Mechanical Engineering (UMech)Ryazanskiy Branch, Moscow State Open University named after V.S. ChernomyrdinIn regions of intensive precipitation, slopes tend to become viscid due to accumulated moisture. The ultimate resistance of soils susceptible to landslides is equal to zero, while shear stresses between layers are proportional to the velocity gradient. To prevent landslides, slope soil is stabilized by a continuous retaining wall or a row of sparsely erected piles. The effectiveness of these methods is measured by the diminishing rate of the sliding speed at the landslide-prone slope. Due to the non-linear nature of the viscid flow, the Navier - Stokes equations cannot be applied. To perform a more precise calculation, the entire flow is broken down into segments in respect of which the analysis of the viscid flow can be performed; individual results are consolidated on the basis of a common parameter. The first flow section, located at a substantial distance from the buttresses, can be considered as a steady stream of plane gravitational motion alongside the slope. In the second section, the slide is obstructed by the buttress and the parallel flow pattern is formed. There occurs a split of the flow at the critical point of entry, located on the front surface of a solid wall or a buttress. The third section, which can be compared with the flow of viscid fluid in a canal, is typical for buttresses that have a significant length in the direction of the landslide flow. The papers hows that the common parameter applicable both to solid and dispersed barriers is the controlled volume of the fluid flow at the point of entry to the pre-boundary area. As a result of application of the proposed methodology, equations were obtained that made it possible to calculate the speed of the viscid slide depending on different types of piles. The paper describes the conditions that make the viscid mass climb over the constructed barrier.http://vestnikmgsu.ru/files/archive/issues/2012/3/ru/3.pdfviscous flowretaining wallflood control volumelandslidepile row
collection DOAJ
language English
format Article
sources DOAJ
author Buslov Anatoliy Semenovich
Kalacheva Elena Nikolaevna
spellingShingle Buslov Anatoliy Semenovich
Kalacheva Elena Nikolaevna
VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
Vestnik MGSU
viscous flow
retaining wall
flood control volume
landslide
pile row
author_facet Buslov Anatoliy Semenovich
Kalacheva Elena Nikolaevna
author_sort Buslov Anatoliy Semenovich
title VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
title_short VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
title_full VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
title_fullStr VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
title_full_unstemmed VELOCITY OF VISCID FLOW LANDSLIDES IN THE EVENT OF A PILE CURTAIN AND A CONTINUOUS RETAINING WALL
title_sort velocity of viscid flow landslides in the event of a pile curtain and a continuous retaining wall
publisher Moscow State University of Civil Engineering (MGSU)
series Vestnik MGSU
issn 1997-0935
publishDate 2012-10-01
description In regions of intensive precipitation, slopes tend to become viscid due to accumulated moisture. The ultimate resistance of soils susceptible to landslides is equal to zero, while shear stresses between layers are proportional to the velocity gradient. To prevent landslides, slope soil is stabilized by a continuous retaining wall or a row of sparsely erected piles. The effectiveness of these methods is measured by the diminishing rate of the sliding speed at the landslide-prone slope. Due to the non-linear nature of the viscid flow, the Navier - Stokes equations cannot be applied. To perform a more precise calculation, the entire flow is broken down into segments in respect of which the analysis of the viscid flow can be performed; individual results are consolidated on the basis of a common parameter. The first flow section, located at a substantial distance from the buttresses, can be considered as a steady stream of plane gravitational motion alongside the slope. In the second section, the slide is obstructed by the buttress and the parallel flow pattern is formed. There occurs a split of the flow at the critical point of entry, located on the front surface of a solid wall or a buttress. The third section, which can be compared with the flow of viscid fluid in a canal, is typical for buttresses that have a significant length in the direction of the landslide flow. The papers hows that the common parameter applicable both to solid and dispersed barriers is the controlled volume of the fluid flow at the point of entry to the pre-boundary area. As a result of application of the proposed methodology, equations were obtained that made it possible to calculate the speed of the viscid slide depending on different types of piles. The paper describes the conditions that make the viscid mass climb over the constructed barrier.
topic viscous flow
retaining wall
flood control volume
landslide
pile row
url http://vestnikmgsu.ru/files/archive/issues/2012/3/ru/3.pdf
work_keys_str_mv AT buslovanatoliysemenovich velocityofviscidflowlandslidesintheeventofapilecurtainandacontinuousretainingwall
AT kalachevaelenanikolaevna velocityofviscidflowlandslidesintheeventofapilecurtainandacontinuousretainingwall
_version_ 1725571281645993984