Geo-Risk 2017 2017
DOI: 10.1061/9780784480700.053
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Stochastic Analysis of Levee Stability Subject to Variable Seepage Conditions

Abstract: Levee stability is highly influenced by seepage. Specifically, hydraulic conductivity distribution within a levee influences pore pressure distribution and controls the drained strength of the soil. In this study the influence of hydraulic conductivity and blanket layer thickness on failure probability is evaluated within the context of reliability analyses that also include soil strength and unit weight as random variables. First-Order Reliability Method (FORM) is used to evaluate reliability, rank random var… Show more

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Cited by 4 publications
(10 citation statements)
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“… Recommendations based on Lanzafame et al (2017), Löfman and Korkiala‐Tanttu (2019) and Uzielli et al (2006). …”
Section: Resultsmentioning
confidence: 99%
“… Recommendations based on Lanzafame et al (2017), Löfman and Korkiala‐Tanttu (2019) and Uzielli et al (2006). …”
Section: Resultsmentioning
confidence: 99%
“…Despite their importance for dike stability and the valid assumption that they are heterogeneous, these two subsurface parameters are often partly unknown. As such, extending this research with variable material properties [11] may provide an even more extensive analysis of groundwaterrelated dike stability. In this way, the uncertainty of the material properties can be assessed too, which is important in real-world cases.…”
Section: Suggestions For Further Researchmentioning
confidence: 99%
“…Research on a single case [8] was often also focused on the effect of artificial reinforcements [9,10]. Attempts including a local sensitivity analysis investigated the influence of material properties [11] or geometry [12] on the stability of embankments. In sum, none of these previous studies conducted a full analysis that considers both variations in hydrological parameters as factors influencing the stability of a dike.…”
Section: Introductionmentioning
confidence: 99%
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“…Hydraulic conductivity ratio is defined as K r = K a,h /K b,v ; thus, for a particular value of K r infinite combinations of K a,h and K b,v are available and only one set must be selected as parameters to specify in the finite-element method (FEM) seepage model. However, the seepage solution is insensitive for K r less than about 50 for the model levee considered herein (Lanzafame et al, 2017), and for a given K r , the value of K b,v is chosen such that K a,h = 8 × 10 −5 m/s. K is anisotropic (K h = 4 K v ) for the blanket layer and isotropic for the embankment and aquifer soils.…”
Section: Random Variables and Probability Distributionsmentioning
confidence: 99%