Particle size (grain size)

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A display of sorted grains ranging in size from silt to very coarse sand.

Particle size or grain size refers to the diameter of a grain of granular material, such as sediment or the lithified particles in clastic rock. Granular material can range from very small colloidal particles, through clay, silt, sand, and gravel, to boulders.

In contrast, crystallite size is the size of a single crystal inside the grain. A single grain can be composed of several crystals.

Contents

[edit] Wentworth

The Wentworth scale or Udden-Wentworth scale is used in the United States. It names size ranges in inches.

[edit] Krumbein φ

A modification of the Wentworth scale created by W. C. Krumbein, the Krumbein phi scale, is a logarithmic scale defined by:

D = D02 − φ

Such that:

D is the diameter of the particle
D0 is a reference diameter, equal to 1 mm
φ is the phi scale

[edit] Chart

φ scalesize rangeWentworth rangenameother names
-8 to -∞256-∞ mm10.1-∞ inboulder
-6 to -864–256 mm2.5–10.1 incobble
-5 to -632–64 mm1.26–2.5 invery coarse gravelpebble
-4 to -516–32 mm0.63–1.26 incoarse gravelpebble
-3 to -48–16 mm0.31–0.63 inmedium gravelpebble
-2 to -34–8 mm0.157–0.31 infine gravelpebble
-1 to -22–4 mm0.079–0.157 invery fine gravelgranule
0 to -11–2 mm0.039–0.079 invery coarse sand
1 to 00.5–1 mm0.020–0.039 incoarse sand
2 to 10.25–0.5 mm0.010–0.020 inmedium sand
3 to 2125–250 µm0.0049–0.010 infine sand
4 to 362.5–125 µm0.0025–0.0049 invery fine sand
8 to 43.9–62.5 µm0.00015–0.0025 insiltmud
∞ to 81/∞-3.9 µm1/∞ –0.00015 inclaymud
∞ to 101/∞-1 µm1/∞–0.000039 incolloidmud

In some schemes[which?] gravel is anything larger than sand and includes granule, pebble, cobble, and boulder in the above table. In the chart above, pebble covers the size range 4 to 64 mm.

[edit] See also

[edit] References

  • W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition (Freeman, San Francisco, 1963).
  • J A Udden, "Mechanical composition of clastic sediments", Bull. Geol. Soc. Am. 25:655–744 (1914).
  • C K Wentworth, "A scale of grade and class terms for clastic sediments", J. Geology 30:377–392 (1922).