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Scale effects in subaerial landslide generated impulse waves

Scale effects in subaerial landslide generated impulse waves
Scale effects in subaerial landslide generated impulse waves
Hydraulic scale modelling involves scale effects. The limiting criteria for scale models of subaerial landslide generated impulse waves including solid, air, and water are discussed both based on a literature review and based on detailed two-dimensional experimentation. Seven scale series based on the Froude similitude were conducted involving the intermediate-water wave spectrum. Scale effects were primarily attributed to the impact crater formation, the air entrainment and detrainment, and the turbulent boundary layer as a function of surface tension and fluid viscosity. These effects reduce the relative wave amplitude and the wave attenuation as compared with reference experiments. Wave amplitude attenuation was found to be more than 70 times larger than predicted with the standard wave theory. Limitations for plane impulse wave generation on the basis of the present research are given by which scale effects can be avoided.
0723-4864
691-703
Heller, Valentin
f99b2e6a-4f77-45bc-b742-20cd0de26b4f
Hager, Willi H.
bbcfbbe5-8584-4756-8898-7dbabd6fed66
Minor, Hans-Erwin
e009bd6d-1caa-4e6c-85d0-06dc9bfc1bd8
Heller, Valentin
f99b2e6a-4f77-45bc-b742-20cd0de26b4f
Hager, Willi H.
bbcfbbe5-8584-4756-8898-7dbabd6fed66
Minor, Hans-Erwin
e009bd6d-1caa-4e6c-85d0-06dc9bfc1bd8

Heller, Valentin, Hager, Willi H. and Minor, Hans-Erwin (2008) Scale effects in subaerial landslide generated impulse waves. Experiments in Fluids, 44 (5), 691-703. (doi:10.1007/s00348-007-0427-7).

Record type: Article

Abstract

Hydraulic scale modelling involves scale effects. The limiting criteria for scale models of subaerial landslide generated impulse waves including solid, air, and water are discussed both based on a literature review and based on detailed two-dimensional experimentation. Seven scale series based on the Froude similitude were conducted involving the intermediate-water wave spectrum. Scale effects were primarily attributed to the impact crater formation, the air entrainment and detrainment, and the turbulent boundary layer as a function of surface tension and fluid viscosity. These effects reduce the relative wave amplitude and the wave attenuation as compared with reference experiments. Wave amplitude attenuation was found to be more than 70 times larger than predicted with the standard wave theory. Limitations for plane impulse wave generation on the basis of the present research are given by which scale effects can be avoided.

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Published date: May 2008

Identifiers

Local EPrints ID: 74271
URI: http://eprints.soton.ac.uk/id/eprint/74271
ISSN: 0723-4864
PURE UUID: 2ac0a868-693b-4666-8ecd-fdbc07bd63af

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Date deposited: 12 Mar 2010
Last modified: 13 Mar 2024 22:30

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Contributors

Author: Valentin Heller
Author: Willi H. Hager
Author: Hans-Erwin Minor

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