Grain size (or particle size) is the diameter of individual grains of sediment, or the lithified particles in clastic rocks. The term may also be applied to other granular materials. This is different from the crystallite size, which refers to the size of a single crystal inside a particle or grain. A single grain can be composed of several crystals. Granular material can range from very small colloidal particles, through clay, silt, sand, gravel, and cobbles, to boulders.

This article includes a list of general references, but it lacks sufficient corresponding inline citations. (July 2011)

Quick Facts Granulometry, Basic concepts ...

Granulometry
Basic concepts
Particle size, Grain size, Size distribution, Morphology
Methods and techniques
Mesh scale, Optical granulometry, Sieve analysis, Soil gradation
Related concepts
Granulation, Granular material, Mineral dust, Pattern recognition, Dynamic light scattering
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Size ranges define limits of classes that are given names in the Wentworth scale (or Udden–Wentworth scale) used in the United States. The Krumbein phi (φ) scale, a modification of the Wentworth scale created by W. C. Krumbein^[1] in 1934, is a logarithmic scale computed by the equation

${\displaystyle \varphi =-\log _{2}{\frac {D}{D_{0}}},}$

where

${\displaystyle \varphi }$ is the Krumbein phi scale,

${\displaystyle D}$ is the diameter of the particle or grain in millimeters (Krumbein and Monk's equation)^[2] and

${\displaystyle D_{0}}$ is a reference diameter, equal to 1 mm (to make the equation dimensionally consistent).

This equation can be rearranged to find diameter using φ:

${\displaystyle D=D_{0}\cdot 2^{-\varphi }\,}$

In some schemes, gravel is anything larger than sand (comprising granule, pebble, cobble, and boulder in the table above).

ISO 14688-1:2017, establishes the basic principles for the identification and classification of soils on the basis of those material and mass characteristics most commonly used for soils for engineering purposes. ISO 14688-1 is applicable to natural soils in situ, similar man-made materials in situ and soils redeposited by people.^[3]

An accumulation of sediment can also be characterized by the grain size distribution. A sediment deposit can undergo sorting when a particle size range is removed by an agency such as a river or the wind. The sorting can be quantified using the Inclusive Graphic Standard Deviation:^[4]

${\displaystyle \sigma _{I}={\frac {\phi 84-\phi 16}{4}}+{\frac {\phi 95-\phi 5}{6.6}}}$

where

${\displaystyle \sigma _{I}}$ is the Inclusive Graphic Standard Deviation in phi units

${\displaystyle \phi 84}$ is the 84th percentile of the grain size distribution in phi units, etc.

The result of this can be described using the following terms:

More information , 0.35 < ...

Diameter (phi units)	Description
${\displaystyle \sigma _{I}}$ < 0.35	very well sorted
0.35 < ${\displaystyle \sigma _{I}}$ < 0.50	well sorted
0.50 < ${\displaystyle \sigma _{I}}$ < 1.00	moderately sorted
1.00 < ${\displaystyle \sigma _{I}}$ < 2.00	poorly sorted
2.00 < ${\displaystyle \sigma _{I}}$ < 4.00	very poorly sorted
4.00 < ${\displaystyle \sigma _{I}}$	extremely poorly sorted

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• Deposition (geology)
• Feret diameter
• Martin diameter
• Orders of magnitude (volume)
• Soil texture
• Substrate (biology)
• Unified Soil Classification System (USCS)