2012
DOI: 10.1016/j.jhydrol.2012.08.050
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An analytical approach for levee underseepage analysis

Abstract: Keywords:Analytical approach Groundwater flow Levees Underseepage Pressure head Seepage quantity s u m m a r y Levee underseepage analyses are commonly performed to assess the risk of erosion and piping of levee foundation soils. They are also commonly used to estimate the quantity of seepage that is expected to pass beneath a levee over time, and to assess the risk of excessively high pore pressures at various points in the foundation. A variety of approaches have historically been utilized to perform steady-… Show more

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Cited by 17 publications
(15 citation statements)
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“…2 Semiconfined Groundwater Flow: Cartesian Coordinate System (Planar Seepage) Meehan and Benjasupattananan (2012) provide a detailed discussion for the rationale behind using a closed-form blanket theory analytical approach to model planar seepage behavior in the foundation soil beneath levees. This type of analytical approach for modeling levee underseepage has a long history of use by the USACE (USACE 1956a(USACE , b, 2000Turnbull and Mansur 1961) accepted as a reasonable levee underseepage analysis tool, given the many uncertainties that are typically present when characterizing seepage model input parameters for levee analysis.…”
Section: Introductionmentioning
confidence: 99%
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“…2 Semiconfined Groundwater Flow: Cartesian Coordinate System (Planar Seepage) Meehan and Benjasupattananan (2012) provide a detailed discussion for the rationale behind using a closed-form blanket theory analytical approach to model planar seepage behavior in the foundation soil beneath levees. This type of analytical approach for modeling levee underseepage has a long history of use by the USACE (USACE 1956a(USACE , b, 2000Turnbull and Mansur 1961) accepted as a reasonable levee underseepage analysis tool, given the many uncertainties that are typically present when characterizing seepage model input parameters for levee analysis.…”
Section: Introductionmentioning
confidence: 99%
“…When modeling seepage in a semiconfined aquifer using a Cartesian coordinate system characterized by x, y, z-coordinates [ Fig. 1(b)], existing analytical models typically assume (1) that the permeable foundation layer is of constant thickness, d, and (2) that vertical velocities in the permeable foundation layer (v z ) are small compared with the horizontal velocities (v x , v y ) (Meehan and Benjasupattananan 2012). The second assumption is important in the derivation because it indicates that the change in head along the thickness of the permeable layer (∂h/∂z) will be relatively small compared with the change in head that occurs in the other spatial directions throughout the aquifer (∂h/∂x, ∂h/∂y).…”
Section: Introductionmentioning
confidence: 99%
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