Infiltration effects on cross-shore sedimnet transport

Theory is reviewed which relates infiltration into a permeable beach with the net onshore or offshore transport of sediment by wave action. This theory is tested experimentally by using sands of different permeability and by using underdrains in the beach and a pump to increase the infiltration c...

Full description

Bibliographic Details
Main Author: Elliott, Trevor Ross
Format: Others
Language:English
Published: 2009
Online Access:http://hdl.handle.net/2429/4044
id ndltd-UBC-oai-circle.library.ubc.ca-2429-4044
record_format oai_dc
spelling ndltd-UBC-oai-circle.library.ubc.ca-2429-40442018-01-05T17:31:47Z Infiltration effects on cross-shore sedimnet transport Elliott, Trevor Ross Theory is reviewed which relates infiltration into a permeable beach with the net onshore or offshore transport of sediment by wave action. This theory is tested experimentally by using sands of different permeability and by using underdrains in the beach and a pump to increase the infiltration capacity. Previous studies are reviewed, although these earlier studies have had different purposes. Some prior investigations have studied wave propagation over a permeable slope or have determined wave damping and energy dissipation due to percolation into a porous bed. Other studies have investigated wave interactions with permeable structures such as rubblemound breakwaters and have shown that the exchange of fluid between the external and internal flow regions markedly affects wave uprush, backrush and set-up in the surf zone. A limited number of previous studies have considered the flow of fluid into a permeable beach and its role in beach stabilization and erosion control. The present tests were performed in the wave flume of the Hydraulics Laboratory of the Department of Civil Engineering at the University of British Columbia. Intermediate and equilibrium beach profiles are presented and compared. The findings of this study indicate substantial differences between impermeable and porous material. Experimental results show more permeable beaches form steeper profiles, while less permeable beaches form shallower profiles. Moreover, increasing infiltration by pumping initiates immediate onshore sediment motion and considerable steepening of the cross-sectional profile. To a large extent this steepening process was reversible when pumping was stopped. The results of this study confirm the predictions of the theory that infiltration contributes directly to a net onshore stress and onshore sediment transport. Applied Science, Faculty of Civil Engineering, Department of Graduate 2009-01-31 2009-01-31 1995 1995-11 Text Thesis/Dissertation http://hdl.handle.net/2429/4044 eng For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use. 4385754 bytes application/pdf
collection NDLTD
language English
format Others
sources NDLTD
description Theory is reviewed which relates infiltration into a permeable beach with the net onshore or offshore transport of sediment by wave action. This theory is tested experimentally by using sands of different permeability and by using underdrains in the beach and a pump to increase the infiltration capacity. Previous studies are reviewed, although these earlier studies have had different purposes. Some prior investigations have studied wave propagation over a permeable slope or have determined wave damping and energy dissipation due to percolation into a porous bed. Other studies have investigated wave interactions with permeable structures such as rubblemound breakwaters and have shown that the exchange of fluid between the external and internal flow regions markedly affects wave uprush, backrush and set-up in the surf zone. A limited number of previous studies have considered the flow of fluid into a permeable beach and its role in beach stabilization and erosion control. The present tests were performed in the wave flume of the Hydraulics Laboratory of the Department of Civil Engineering at the University of British Columbia. Intermediate and equilibrium beach profiles are presented and compared. The findings of this study indicate substantial differences between impermeable and porous material. Experimental results show more permeable beaches form steeper profiles, while less permeable beaches form shallower profiles. Moreover, increasing infiltration by pumping initiates immediate onshore sediment motion and considerable steepening of the cross-sectional profile. To a large extent this steepening process was reversible when pumping was stopped. The results of this study confirm the predictions of the theory that infiltration contributes directly to a net onshore stress and onshore sediment transport. === Applied Science, Faculty of === Civil Engineering, Department of === Graduate
author Elliott, Trevor Ross
spellingShingle Elliott, Trevor Ross
Infiltration effects on cross-shore sedimnet transport
author_facet Elliott, Trevor Ross
author_sort Elliott, Trevor Ross
title Infiltration effects on cross-shore sedimnet transport
title_short Infiltration effects on cross-shore sedimnet transport
title_full Infiltration effects on cross-shore sedimnet transport
title_fullStr Infiltration effects on cross-shore sedimnet transport
title_full_unstemmed Infiltration effects on cross-shore sedimnet transport
title_sort infiltration effects on cross-shore sedimnet transport
publishDate 2009
url http://hdl.handle.net/2429/4044
work_keys_str_mv AT elliotttrevorross infiltrationeffectsoncrossshoresedimnettransport
_version_ 1718586676936179712