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Internal erosion information


Internal erosion is the formation of voids within a soil caused by the removal of material by seepage.[1] It is the second most common cause of failure in levees and one of the leading causes of failures in earth dams,[2] responsible for about half of embankment dam failures.[3]

Internal erosion occurs when the hydraulic forces exerted by water seeping through the pores and cracks of the material in the dam and/or foundation are sufficient to detach particles and transport them out of the dam structure. Internal erosion is especially dangerous because there may be no external evidence, or only subtle evidence, that it is taking place. Usually a sand boil can be found, but the boil might be hidden under water. A dam may breach within a few hours after evidence of internal erosion becomes obvious.

Piping is a related phenomenon and is defined as the progressive development of internal erosion by seepage, appearing downstream as a hole discharging water.[4] Piping is induced by regressive erosion of particles from downstream and along the upstream line towards an outside environment until a continuous pipe is formed.[5][6]

  1. ^ Reclamation Glossary, U.S. Department of Interior, Bureau of Reclamation
  2. ^ Progress in assessing Internal Erosion, at britishdams.org
  3. ^ Fell, R.; MacGregor, P.; Stapledon, D.; Bell, G.; Foster, M. (2014). "Chapter 8: Internal erosion and piping of embankment dams and in dam foundations". Geotechnical Engineering of Dams (2nd ed.). CRC Press/Balkema. p. 375. ISBN 978-1-13800008-7.
  4. ^ ICOLD GIGB, ICOLD Dictionary
  5. ^ Development of piping erosion conditions in the Benson area, Arizona, U.S.A.
  6. ^ The scaling law of piping erosion

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