Geo-Risk 2017 2017
DOI: 10.1061/9780784480724.012
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Assessing the Implications of Sand Boils for Backward Erosion Piping Risk

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Cited by 6 publications
(6 citation statements)
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“…Similar conditions have been reported in laboratory experiments by Van Beek et al., 37 where equilibrium was observed in pipe formation and the head was required to be increased to study further pipe progression. Similarly, Schaefer et al 15 . report piping in multiple embankments along the river Mississippi where pipe initiation had not progressed to failure.…”
Section: Laboratory Investigation Of 2d Seepage Flow In a Domain Consisting A Predefined Piping Zonementioning
confidence: 98%
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“…Similar conditions have been reported in laboratory experiments by Van Beek et al., 37 where equilibrium was observed in pipe formation and the head was required to be increased to study further pipe progression. Similarly, Schaefer et al 15 . report piping in multiple embankments along the river Mississippi where pipe initiation had not progressed to failure.…”
Section: Laboratory Investigation Of 2d Seepage Flow In a Domain Consisting A Predefined Piping Zonementioning
confidence: 98%
“…Contrary to initial belief that once BEP initiates at the downstream face, it progresses rapidly upstream and causes failure, 13 recent laboratory studies 14 suggest that this is not always the case and the rate of BEP progression is dependent on grain size. Furthermore, field observations 15 of sand boils on the Mississippi river provide evidence that not all BEP initiations progress to failure. These findings motivate the need and possibility of designing a method for the detection of the extent of BEP.…”
Section: Introductionmentioning
confidence: 99%
“…The Sellmeijer model was validated to perform good predictions for all laboratory scales with 2D configurations, but overpredicts the critical gradient in a 3D configuration [23] even after being recently adapted based on the results of additional experiments [24]. The Hoffmans model is used to calculate the critical hydraulic gradient under the condition that backward erosion leads to dike failure, but only a small percentage of BEP initiation cases can progress to failure conditions through field evidence [25,26]. For these reasons, assessing the hydraulic conditions related to the stages of BEP is of interest.…”
Section: Literature Reviewmentioning
confidence: 99%
“…Among them, sand boils, also known as sand volcanoes, are one of the most common and dangerous hazards, especially during floods, which occur when the velocity of water flowing from the flood side to the protected side is sufficiently large to erode the soil and allow sand and water to seep through the soil surface. These formations provide evidence for the presence of weak points in a levee [2], [3], indicating the potential for dangerous soil erosion. Hence, it is crucial to detect them precisely to identify new sand boils and monitor their growth for flood-fighting and levee-monitoring purposes during floods.…”
Section: Introductionmentioning
confidence: 99%