A series of 19 flume tests was conducted, in which flow was routed through a riprap layer, and the average interstitial or through-flow, velocity was measured and recorded. Flow measurements varied plus/minus 40% about the average velocity. A predictive relationship was developed in which the average interstitial velocity was determined to be a function of the embankment slope and rock size. The predictive relationship provides the designer with a method for estimating through flow based upon a representative stone size, gradation, and embankment slope.

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  • Accession Number: 00609214
  • Record Type: Publication
  • Files: TRIS
  • Created Date: May 31 1991 12:00AM