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  2. Shields formula - Wikipedia

    en.wikipedia.org/wiki/Shields_formula

    Original diagram of Shields, 1936. The Shields formula is a formula for the stability calculation of granular material (sand, gravel) in running water.. The stability of granular material in flow can be determined by the Shields formula or the Izbash formula.

  3. Beach nourishment - Wikipedia

    en.wikipedia.org/wiki/Beach_nourishment

    As in other projects, on-shore sand availability was limited, forcing consideration of more expensive offshore sources. [60] A second project, along Stable Road, that attempted to slow rather than halt erosion, was stopped halfway toward its goal of adding 10,000 cubic yards (7,600 m 3) of sand. The beaches had been retreating at a ...

  4. Sieve analysis - Wikipedia

    en.wikipedia.org/wiki/Sieve_analysis

    A sieve analysis (or gradation test) is a practice or procedure used in geology, civil engineering, [1] and chemical engineering [2] to assess the particle size distribution (also called gradation) of a granular material by allowing the material to pass through a series of sieves of progressively smaller mesh size and weighing the amount of material that is stopped by each sieve as a fraction ...

  5. The Sand Reckoner - Wikipedia

    en.wikipedia.org/wiki/The_Sand_Reckoner

    The Sand Reckoner (Greek: Ψαμμίτης, Psammites) is a work by Archimedes, an Ancient Greek mathematician of the 3rd century BC, in which he set out to determine an upper bound for the number of grains of sand that fit into the universe. In order to do this, Archimedes had to estimate the size of the universe according to the contemporary ...

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  7. Grain size - Wikipedia

    en.wikipedia.org/wiki/Grain_size

    Wentworth grain size chart from United States Geological Survey Open-File Report 2006-1195: Note size typos; 33.1mm is 38.1 & .545mm is .594 Beach cobbles at Nash Point, South Wales

  8. Angle of repose - Wikipedia

    en.wikipedia.org/wiki/Angle_of_repose

    Angle of repose of a heap of sand Sandpile from the Matemateca collection. The angle of repose, or critical angle of repose, [1] of a granular material is the steepest angle of descent or dip relative to the horizontal plane on which the material can be piled without slumping.

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