Lessons from the Case History of a Massive Landslide Dam

A massive landslide created a natural dam on two tributaries of Jhelum River near the town of Hattian Bala in Kashmir in October 2005. The landslide was triggered by a 7.6 Mw earthquake. The resulting unconsolidated dam and water impoundment upstream carried hazard potential of downstream damage to...

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Main Authors: Fawad S. Niazi, Aranzazu Pinan-Llamas, Kamran Akhtar
Format: Article
Language:English
Published: Hindawi-Wiley 2020-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2020/8840629
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spelling doaj-fa30c0e268474637a593f6ddb758f98e2020-12-14T09:46:34ZengHindawi-WileyGeofluids1468-81151468-81232020-01-01202010.1155/2020/88406298840629Lessons from the Case History of a Massive Landslide DamFawad S. Niazi0Aranzazu Pinan-Llamas1Kamran Akhtar2Department of Civil & Mechanical Engineering, Purdue University Fort Wayne, Indiana 46805, USASchool of Polytechnic, Purdue University Fort Wayne, Indiana 46805, USANational University of Sciences and Technology, Balochistan Campus, Quetta, PakistanA massive landslide created a natural dam on two tributaries of Jhelum River near the town of Hattian Bala in Kashmir in October 2005. The landslide was triggered by a 7.6 Mw earthquake. The resulting unconsolidated dam and water impoundment upstream carried hazard potential of downstream damage to both infrastructure and population due to potential flooding caused by its breach. Comprehensive investigations and monitoring were implemented to analyse dam stability. Fresh topographic profiles were generated. Samples of the matrix materials were utilized in the laboratory investigations including grain-size analysis, laboratory electrical resistivity and permeability tests at varying densities and degrees of saturation, and sediment concentration assessment in the seepage discharge. A noninvasive geophysical method was employed together with new topographic information to develop transient subsurface pictures and to assess the advancement of seepage fronts within the dam body. Internal erosion/filtering potential of the matrix material was assessed by comparing grain size distributions with those of the earlier failed dams. Upstream inflows, downstream discharges, daily precipitation, and lake levels monitored during the study period were utilized in hydrological data analysis in an attempt to assess the potential seepage volume. A combination of empirical, analytical, and numerical methods and simulations, together with laboratory and field investigations, led to the interpretations regarding short- and long-term stability of the dam. This paper highlights alternative methods of investigation employed differently from those used by other national and international agencies in analysing the failure potential of this natural dam. It offers lessons learned from a case history that can be beneficial in future evaluation of seepage-induced failure of similar natural features.http://dx.doi.org/10.1155/2020/8840629
collection DOAJ
language English
format Article
sources DOAJ
author Fawad S. Niazi
Aranzazu Pinan-Llamas
Kamran Akhtar
spellingShingle Fawad S. Niazi
Aranzazu Pinan-Llamas
Kamran Akhtar
Lessons from the Case History of a Massive Landslide Dam
Geofluids
author_facet Fawad S. Niazi
Aranzazu Pinan-Llamas
Kamran Akhtar
author_sort Fawad S. Niazi
title Lessons from the Case History of a Massive Landslide Dam
title_short Lessons from the Case History of a Massive Landslide Dam
title_full Lessons from the Case History of a Massive Landslide Dam
title_fullStr Lessons from the Case History of a Massive Landslide Dam
title_full_unstemmed Lessons from the Case History of a Massive Landslide Dam
title_sort lessons from the case history of a massive landslide dam
publisher Hindawi-Wiley
series Geofluids
issn 1468-8115
1468-8123
publishDate 2020-01-01
description A massive landslide created a natural dam on two tributaries of Jhelum River near the town of Hattian Bala in Kashmir in October 2005. The landslide was triggered by a 7.6 Mw earthquake. The resulting unconsolidated dam and water impoundment upstream carried hazard potential of downstream damage to both infrastructure and population due to potential flooding caused by its breach. Comprehensive investigations and monitoring were implemented to analyse dam stability. Fresh topographic profiles were generated. Samples of the matrix materials were utilized in the laboratory investigations including grain-size analysis, laboratory electrical resistivity and permeability tests at varying densities and degrees of saturation, and sediment concentration assessment in the seepage discharge. A noninvasive geophysical method was employed together with new topographic information to develop transient subsurface pictures and to assess the advancement of seepage fronts within the dam body. Internal erosion/filtering potential of the matrix material was assessed by comparing grain size distributions with those of the earlier failed dams. Upstream inflows, downstream discharges, daily precipitation, and lake levels monitored during the study period were utilized in hydrological data analysis in an attempt to assess the potential seepage volume. A combination of empirical, analytical, and numerical methods and simulations, together with laboratory and field investigations, led to the interpretations regarding short- and long-term stability of the dam. This paper highlights alternative methods of investigation employed differently from those used by other national and international agencies in analysing the failure potential of this natural dam. It offers lessons learned from a case history that can be beneficial in future evaluation of seepage-induced failure of similar natural features.
url http://dx.doi.org/10.1155/2020/8840629
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