The University of Southampton
University of Southampton Institutional Repository

Impulse product parameter in landslide generated impulse waves

Impulse product parameter in landslide generated impulse waves
Impulse product parameter in landslide generated impulse waves
Subaerial landslide generated impulse waves were investigated in a prismatic wave channel based on Froude similitude and granular slide material. The tests included the seven governing parameters still water depth, slide impact velocity, slide thickness, bulk slide volume, bulk slide density, slide impact angle, and grain diameter. All governing parameters, except for the grain diameter with a negligible effect, are included in the impulse product parameter P allowing for a simple application. Empirical equations based on 211 experiments for all relevant wave features in practice including the maximum wave height, the maximum wave amplitude with its location and period in the slide impact zone and both the wave height and amplitude decay and the period increase in the wave propagation zone are a simple function of P. The presented equations were validated with 223 runs of Fritz (2002) and Zweifel (2004) resulting in improved goodness of fit. The limitations of the herein derived empirical equations are also highlighted. The wave height and amplitude equations based on a wave channel (2D) agree well with the 1958 Lituya Bay case.
landslides, reservoirs, sliding, tsunamis, water waves, wave generation
0733-950X
Heller, Valentin
f99b2e6a-4f77-45bc-b742-20cd0de26b4f
Hager, Willi H.
bbcfbbe5-8584-4756-8898-7dbabd6fed66
Heller, Valentin
f99b2e6a-4f77-45bc-b742-20cd0de26b4f
Hager, Willi H.
bbcfbbe5-8584-4756-8898-7dbabd6fed66

Heller, Valentin and Hager, Willi H. (2009) Impulse product parameter in landslide generated impulse waves. Journal of Waterway, Port, Coastal, and Ocean Engineering, 135 (5). (doi:10.1061/(ASCE)WW.1943-5460.0000037).

Record type: Article

Abstract

Subaerial landslide generated impulse waves were investigated in a prismatic wave channel based on Froude similitude and granular slide material. The tests included the seven governing parameters still water depth, slide impact velocity, slide thickness, bulk slide volume, bulk slide density, slide impact angle, and grain diameter. All governing parameters, except for the grain diameter with a negligible effect, are included in the impulse product parameter P allowing for a simple application. Empirical equations based on 211 experiments for all relevant wave features in practice including the maximum wave height, the maximum wave amplitude with its location and period in the slide impact zone and both the wave height and amplitude decay and the period increase in the wave propagation zone are a simple function of P. The presented equations were validated with 223 runs of Fritz (2002) and Zweifel (2004) resulting in improved goodness of fit. The limitations of the herein derived empirical equations are also highlighted. The wave height and amplitude equations based on a wave channel (2D) agree well with the 1958 Lituya Bay case.

This record has no associated files available for download.

More information

e-pub ahead of print date: 2 October 2009
Keywords: landslides, reservoirs, sliding, tsunamis, water waves, wave generation

Identifiers

Local EPrints ID: 74322
URI: http://eprints.soton.ac.uk/id/eprint/74322
ISSN: 0733-950X
PURE UUID: 7d117e5c-93c8-43af-99a2-6dc6a5f2b134

Catalogue record

Date deposited: 11 Mar 2010
Last modified: 13 Mar 2024 22:30

Export record

Altmetrics

Contributors

Author: Valentin Heller
Author: Willi H. Hager

Download statistics

Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.

View more statistics

Atom RSS 1.0 RSS 2.0

Contact ePrints Soton: eprints@soton.ac.uk

ePrints Soton supports OAI 2.0 with a base URL of http://eprints.soton.ac.uk/cgi/oai2

This repository has been built using EPrints software, developed at the University of Southampton, but available to everyone to use.

We use cookies to ensure that we give you the best experience on our website. If you continue without changing your settings, we will assume that you are happy to receive cookies on the University of Southampton website.

×