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1Instabilities originating from suction holes used for laminar flow control (LFC)

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“Instabilities originating from suction holes used for laminar flow control (LFC)” Metadata:

  • Title: ➤  Instabilities originating from suction holes used for laminar flow control (LFC)
  • Author:
  • Language: English
  • Publisher: ➤  National Technical Information Service, distributor - National Aeronautics and Space Administration
  • Publish Date:
  • Publish Location: ➤  Springfield, Va - [Washington, DC

“Instabilities originating from suction holes used for laminar flow control (LFC)” Subjects and Themes:

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Access and General Info:

  • First Year Published: 1994
  • Is Full Text Available: No
  • Is The Book Public: No
  • Access Status: No_ebook

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    Boundary layer

    In physics and fluid mechanics, a boundary layer is the thin layer of fluid in the immediate vicinity of a bounding surface formed by the fluid flowing

    Northrop X-21

    boundary-layer air by suction through porous materials, multiple narrow surface slots, or small perforations (boundary layer suction). Two major modifications

    Proton-exchange membrane fuel cell

    sub-freezing conditions, the water produced by fuel cells can freeze in porous layers and flow channels. This freezing water can block gas and fuel transport

    Aquifer

    called an aquiclude or aquifuge. Aquitards are composed of layers of either clay or non-porous rock with low hydraulic conductivity. Groundwater can be

    Supercapacitor

    capacitance in double-layer capacitors is related to the limited moving speed of ions in the electrolyte and the resistive porous structure of the electrodes

    Wood

    customary to divide them into two large classes, ring-porous and diffuse-porous. In ring-porous species, such as ash, black locust, catalpa, chestnut

    Sintering

    materials of specific porosity. Sintered plastic porous components are used in filtration and to control fluid and gas flows. Sintered plastics are used

    Fluid mechanics

    of boundary layers is inviscid, and then matching its solution onto that for a thin laminar boundary layer. For fluid flow over a porous boundary, the

    Kambiz Vafai

    978-3036593821 Vafai, K., & Tien, C. L. (1981). Boundary and inertia effects on flow and heat transfer in porous media. International Journal of Heat and Mass

    Rayleigh number

    convection can also occur when the fluid is inside and fills a porous medium, such as porous rock saturated with water. Then the Rayleigh number, sometimes