Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels
The rock mass erosion of dam spillways, a phenomenon involving the interaction between the hydraulic load of water and the capability of the rock mass to resist its destruction, remains a critical safety issue. The erosion resistance of a rock mass can be estimated through several erodibility indice...
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2021
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oai:doaj.org-article:d3c769baea33436e89f8650771226c422021-11-11T19:52:28ZIdentification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels10.3390/w132129502073-4441https://doaj.org/article/d3c769baea33436e89f8650771226c422021-10-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/2950https://doaj.org/toc/2073-4441The rock mass erosion of dam spillways, a phenomenon involving the interaction between the hydraulic load of water and the capability of the rock mass to resist its destruction, remains a critical safety issue. The erosion resistance of a rock mass can be estimated through several erodibility indices, including those of Kirsten, Pells or Bollaert. Several indices have been developed to link rock resistance to the hydraulic parameters of water, i.e., the hydraulic load applied on a rock mass. The developed indices use the average flow velocity, the average shear stress on the bottom of the flow channel, the stress applied to the internal joints of fractured rock mass, the dynamic impulse force, and the power dissipation of water to represent the erosive force of water. From these indices, several methods of assessing hydraulic erosion have been developed, and all use the threshold line concept. Nonetheless, several uncertainties are associated with these methods. This paper presents and discusses the various means of calculating the erosive force of water as a hazard parameter for predicting potential rock erosion. The representativeness of these approaches is also discussed, and we clarify nuances associated with each method. We then provide guidelines for future research aimed at improving estimates of the erosive force of the water within spillway flow channels.Aboubacar Sidiki KoulibalyAli SaeidiAlain RouleauMarco QuirionMDPI AGarticlehydraulic erodibilityhydraulic jumphydraulic loadplunging flowpower dissipationrock massHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 2950, p 2950 (2021) |
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hydraulic erodibility hydraulic jump hydraulic load plunging flow power dissipation rock mass Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
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hydraulic erodibility hydraulic jump hydraulic load plunging flow power dissipation rock mass Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 Aboubacar Sidiki Koulibaly Ali Saeidi Alain Rouleau Marco Quirion Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
description |
The rock mass erosion of dam spillways, a phenomenon involving the interaction between the hydraulic load of water and the capability of the rock mass to resist its destruction, remains a critical safety issue. The erosion resistance of a rock mass can be estimated through several erodibility indices, including those of Kirsten, Pells or Bollaert. Several indices have been developed to link rock resistance to the hydraulic parameters of water, i.e., the hydraulic load applied on a rock mass. The developed indices use the average flow velocity, the average shear stress on the bottom of the flow channel, the stress applied to the internal joints of fractured rock mass, the dynamic impulse force, and the power dissipation of water to represent the erosive force of water. From these indices, several methods of assessing hydraulic erosion have been developed, and all use the threshold line concept. Nonetheless, several uncertainties are associated with these methods. This paper presents and discusses the various means of calculating the erosive force of water as a hazard parameter for predicting potential rock erosion. The representativeness of these approaches is also discussed, and we clarify nuances associated with each method. We then provide guidelines for future research aimed at improving estimates of the erosive force of the water within spillway flow channels. |
format |
article |
author |
Aboubacar Sidiki Koulibaly Ali Saeidi Alain Rouleau Marco Quirion |
author_facet |
Aboubacar Sidiki Koulibaly Ali Saeidi Alain Rouleau Marco Quirion |
author_sort |
Aboubacar Sidiki Koulibaly |
title |
Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
title_short |
Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
title_full |
Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
title_fullStr |
Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
title_full_unstemmed |
Identification of Hydraulic Parameters Influencing the Hydraulic Erodibility of Spillway Flow Channels |
title_sort |
identification of hydraulic parameters influencing the hydraulic erodibility of spillway flow channels |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doaj.org/article/d3c769baea33436e89f8650771226c42 |
work_keys_str_mv |
AT aboubacarsidikikoulibaly identificationofhydraulicparametersinfluencingthehydraulicerodibilityofspillwayflowchannels AT alisaeidi identificationofhydraulicparametersinfluencingthehydraulicerodibilityofspillwayflowchannels AT alainrouleau identificationofhydraulicparametersinfluencingthehydraulicerodibilityofspillwayflowchannels AT marcoquirion identificationofhydraulicparametersinfluencingthehydraulicerodibilityofspillwayflowchannels |
_version_ |
1718431438574977024 |