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  2. Phi - Wikipedia

    en.wikipedia.org/wiki/Phi

    Internal or effective angle of friction. In cartography and navigation, ɸ denotes latitude; likewise, in geodesy it denotes geodetic latitude. In aircraft flight mechanics as the symbol for bank angle (sometimes represented with the letter theta, which is also used for pitch angle). The work function of a surface, in solid-state physics.

  3. Shear strength (soil) - Wikipedia

    en.wikipedia.org/wiki/Shear_strength_(soil)

    φ' = the effective stress friction angle, or the 'angle of internal friction' after Coulomb friction. The coefficient of friction is equal to tan(φ'). Different values of friction angle can be defined, including the peak friction angle, φ' p, the critical state friction angle, φ' cv, or residual friction angle, φ' r.

  4. Friction - Wikipedia

    en.wikipedia.org/wiki/Friction

    Lubricated friction is a case of fluid friction where a lubricant fluid separates two solid surfaces. [9] [10] [11] Skin friction is a component of drag, the force resisting the motion of a fluid across the surface of a body. Internal friction is the force resisting motion between the elements making up a solid material while it undergoes ...

  5. Mohr–Coulomb theory - Wikipedia

    en.wikipedia.org/wiki/Mohr–Coulomb_theory

    Angle of internal friction for some materials Material Friction angle in degrees Rock: 30 ° Sand: 30 ° to 45 ° Gravel: 35 ° Silt: 26 ° to 35 ° Clay: 20 ° Loose sand 30 ° to 35 ° Medium sand 40 ° Dense sand 35 ° to 45 ° Sandy gravel > 34 ° to 48 °

  6. Angle of repose - Wikipedia

    en.wikipedia.org/wiki/Angle_of_repose

    The internal angle between the surface of the pile and the horizontal surface is known as the angle of repose and is related to the density, surface area and shapes of the particles, and the coefficient of friction of the material. Material with a low angle of repose forms flatter piles than material with a high angle of repose.

  7. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    The angle of internal friction is thus closely related to the maximum stable slope angle, often called the angle of repose. But in addition to friction, soil derives significant shear resistance from interlocking of grains. If the grains are densely packed, the grains tend to spread apart from each other as they are subject to shear strain.

  8. Bearing capacity - Wikipedia

    en.wikipedia.org/wiki/Bearing_capacity

    φ′ is the effective internal angle of friction. K pγ is obtained graphically. Simplifications have been made to eliminate the need for K pγ. One such was done by Coduto, given below, and it is accurate to within 10%. [2] = (+) ⁡ ′ + ⁡ ′

  9. Rankine theory - Wikipedia

    en.wikipedia.org/wiki/Rankine_theory

    φ = angle of internal friction of soil. The expression for passive pressure is: = where: = ⁡ + (⁡ ⁡) / ⁡ (⁡ ⁡) / ⁡ Or in the case of β=0, then the two ...