2002
DOI: 10.2112/1551-5036-36.sp1.249
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Life expectancy of shingle beaches: measuring in situ abrasion

Abstract: BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses.

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Cited by 24 publications
(13 citation statements)
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“…Furthermore, Allan (2006) and Dickson et al (2011) have reported that the distance an individual sediment particle travel can influence abrasion percentage losses. Dornbusch et al (2002Dornbusch et al ( , 2003 have investigated the influence of wave conditions on abrasion, finding that abrasion rates are linked to mean wave height. Bertoni et al (2011Bertoni et al ( , 2012 explained the difference in abrasion rates of pebbles released on the lower swash zone (4.2%) and those pebbles on the upper swash zone (1.6%) as a function of differences in wave exposure.…”
Section: Discussionmentioning
confidence: 99%
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“…Furthermore, Allan (2006) and Dickson et al (2011) have reported that the distance an individual sediment particle travel can influence abrasion percentage losses. Dornbusch et al (2002Dornbusch et al ( , 2003 have investigated the influence of wave conditions on abrasion, finding that abrasion rates are linked to mean wave height. Bertoni et al (2011Bertoni et al ( , 2012 explained the difference in abrasion rates of pebbles released on the lower swash zone (4.2%) and those pebbles on the upper swash zone (1.6%) as a function of differences in wave exposure.…”
Section: Discussionmentioning
confidence: 99%
“…However, this is not sufficient to explain the variations in abrasion rates as it is only based on the change in offshore wave heights similar to Dornbusch et al (2002Dornbusch et al ( , 2003. Due to the complicated process by which waves transfer from the sea to the beach, more detailed consideration is required, especially for the process of wave transfer from the breakpoint to the termination of the upwash on the beach.…”
Section: Spatial Pattern Of Abrasionmentioning
confidence: 99%
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“…The abrasion rate of beach sediments depends on pebble characteristics (especially hardness), hydrodynamics (especially wave energy), and exposure (especially the amount of time exposed to transport) (Dornbusch et al 2002;Cammelli et al forthcoming). The iron-rich sediments that remain on the active foreshore surface at Cavo are more rounded and better sorted than sediments at depth (Figures 3 and 4), revealing that some sorting and reshaping by waves has occurred in only three and one-half years.…”
Section: Discussionmentioning
confidence: 99%
“…On the other hand, during stages of reduced eruptive activity (as, for instance, in the interval 1938-55 or 1987-2001), a diffused reduction in beach volume has been documented, possibly induced by washing out and loss of sediment to deeper waters under storm conditions and/or by in situ abrasion (see also DORNBUSCH et al, 2002).…”
Section: Historical Shoreline Evolutionmentioning
confidence: 99%