1995•Journal of Hydraulic EngineeringRequires access

Head Requirement for Incipient Fluidization of Fine Sands in Unbounded Domains

Gerard P. Lennon, Richard N. Weisman

Open publisher page 7 citations

Abstract

Fluidization systems in the coastal environment can be used to maintain channels and aid in sand bypassing. Induced flow from small holes in a buried source pipe will fluidize the overlying sand for a sufficiently high flow rate. One important design parameter is the required hydraulic head at the incipient fluidization condition to overcome the porous media head loss. The three-dimensional governing equation for head was solved with the finite-difference method using the theoretical critical hydraulic gradient at the incipient fluidization condition. After comparison to two-dimensional solutions and experimental results, the incipient-condition head-loss requirement was simulated for field geometries. The results indicate that 3-D effects are dissipated within 3 cm from the holes, where about 80% of the head loss occurs. The head requirement is higher for the 3-D simulations compared to 2-D due to the rapid decrease of head near a hole.

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What this paper is about

Fluidization systems in the coastal environment can be used to maintain channels and aid in sand bypassing. Induced flow from small holes in a buried source pipe will fluidize the overlying sand for a sufficiently high flow rate. One important design parameter is the required hydraulic head at the incipient fluidization condition to overcome the porous media head loss. The three-dimensional governing equation for head was solved with the finite-difference method using the theoretical critical hydraulic gradient at the incipient fluidization condition. After comparison to two-dimensional solutions and experimental results, the incipient-condition head-loss requirement was simulated for field geometries. The results indicate that 3-D effects are dissipated within 3 cm from the holes, where about 80% of the head loss occurs. The head requirement is higher for the 3-D simulations compared to 2-D due to the rapid decrease of head near a hole.

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Available abstract

Fluidization systems in the coastal environment can be used to maintain channels and aid in sand bypassing. Induced flow from small holes in a buried source pipe will fluidize the overlying sand for a sufficiently high flow rate. One important design parameter is the required hydraulic head at the incipient fluidization condition to overcome the porous media head loss. The three-dimensional governing equation for head was solved with the finite-difference method using the theoretical critical hydraulic gradient at the incipient fluidization condition. After comparison to two-dimensional solutions and experimental results, the incipient-condition head-loss requirement was simulated for field geometries. The results indicate that 3-D effects are dissipated within 3 cm from the holes, where about 80% of the head loss occurs. The head requirement is higher for the 3-D simulations compared to 2-D due to the rapid decrease of head near a hole.

Key concepts: Hydraulic head, Fluidization, Head (geology), Geotechnical engineering, Mechanics, Flow (mathematics), Geology, Porous medium

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