International Efforts in Lifeline Earthquake Engineering 2013
DOI: 10.1061/9780784413234.086
|View full text |Cite
|
Sign up to set email alerts
|

Limits on Coastal Scour Depths due to Tsunami

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
13
0

Year Published

2015
2015
2023
2023

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 18 publications
(13 citation statements)
references
References 2 publications
0
13
0
Order By: Relevance
“…Equation 9 provides a simple empirical prediction based on observations of local scour depths and estimated flow depths for different sediment types in the aftermath of the 2011 Tohoku tsunami (Tonkin et al, 2014). In ASCE 7-16 the extent (length) of the scour hole around corner foundations l scour (see Figure 2) is dependent on the soil type and is calculated as follows:…”
Section: Index For Structural Stability Under Scour Rri Scourmentioning
confidence: 99%
“…Equation 9 provides a simple empirical prediction based on observations of local scour depths and estimated flow depths for different sediment types in the aftermath of the 2011 Tohoku tsunami (Tonkin et al, 2014). In ASCE 7-16 the extent (length) of the scour hole around corner foundations l scour (see Figure 2) is dependent on the soil type and is calculated as follows:…”
Section: Index For Structural Stability Under Scour Rri Scourmentioning
confidence: 99%
“…(a) general erosion marking a loss of land surface over large spatial extents (Dalrymple and Kriebel 2005, Shuto and Fujima 2009, Kato et al 2012, Yeh et al 2013, Fraser et al 2013), (b) sustained flow scour near corners and sides around free-standing structures, with scour depth ranging from 0.5 -4.0 m being reported by post-tsunami field surveys (Bricker et al 2012, Tonkin et al 2013), (c) channelized scours in between gaps of larger buildings, as reported by Yeh et al (2013) in the city of Onagawa, Japan during the 2011 Tohoku Earthquake Tsunami, and (d) overtopping scour behind coastal line defenses such as sea walls, where overtopping jets plunging over the structures cause excessive soil erosion (Yeh et al 2004, Kato et al 2012, Mikami et al 2014, Jayaratne et al 2016. All forms of scouring listed above may, when the extreme flow event is persistent and exposes the soil to shear stresses larger than the critical shear stress, result in scouring that could eventually damage structures; only recently, guidelines and standards have started to address this important issue.…”
Section: General Erosion 221mentioning
confidence: 99%
“…Whereas seismic liquefaction occurs during the high frequency shaking of the ground, pore pressure softening is the result of a long period inundation loading followed by a rapid drawdown, leading to an abrupt release of hydrostatic pressure. Tonkin et al (2003), Yeh et al (2004) and Tonkin et al (2013) derived an equation to describe the depth d s of tsunami-induced liquefaction based on the one-dimensional consolidation model with an excess pore pressure field from Terzaghi (1925). These studies built upon a scour enhancement parameter, which defines the critical fraction of the buoyant weight of soil supported by pore pressure.…”
Section: Pore Pressure Softening 222mentioning
confidence: 99%
See 1 more Smart Citation
“…In the case of tsunami induced scour, the literature is more limited and eld investigations of tsunami-induced scour are the primary source of scour data. Post-tsunami investigations of scour include Wilson et al (2012) in harbours, Tonkin et al (2013) at roads and structures, and Bricker et al (2012) at coastal defences. Such retrospective investigations are few in number, geographically localised and infer only post-tsunami scour depths, extents and volumes; they are unable to provide systematic elucidation of the processes and mechanisms of scour evolution.…”
Section: Introductionmentioning
confidence: 99%