Particle Size (Grain Size) Chart
Particle size, also called grain size, refers to 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 is the size of a single crystal inside the particles or grains. A single grain can be composed of several crystals. Granular material can range from very small colloidal particles, through clay, silt, sand, and gravel, to boulders.
Size ranges define limits of classes that are given names in the Wentworth scale (or Udden-Wentworth) used in the United States. The Krumbein phi (φ) scale, a modification of the Wentworth scale created by W. C. Krumbein, (Krumbein & Sloss 1963) is a logarithmic scale computed by the equation
Where
φ is the Krumbein phi scale,
D is the diameter of the particle,
D0 is a reference diameter, equal to 1 mm to make the equation dimensionally consistent.
This equation can be rearranged to find diameter using φ:
| φ scale |
Size range |
Size range |
Aggregate
class |
Other names |
| (metric) |
(inches) |
(Wentworth) |
| < -8 |
> 256 mm |
> 10.1 in |
Boulder |
|
| -6 to -8 |
64–256 mm |
2.5–10.1 in |
Cobble |
|
| -5 to -6 |
32–64 mm |
1.26–2.5 in |
Very coarse
gravel |
Pebble |
| -4 to -5 |
16–32 mm |
0.63–1.26 in |
Coarse gravel |
Pebble |
| -3 to -4 |
8–16 mm |
0.31–0.63 in |
Medium gravel |
Pebble |
| -2 to -3 |
4–8 mm |
0.157–0.31 in |
Fine gravel |
Pebble |
| -1 to -2 |
2–4 mm |
0.079–0.157 in |
Very fine gravel |
Granule |
| 0 to -1 |
1–2 mm |
0.039–0.079 in |
Very coarse sand |
|
| 1 to 0 |
0.5–1 mm |
0.020–0.039 in |
Coarse sand |
|
| 2 to 1 |
0.25–0.5 mm |
0.010–0.020 in |
Medium sand |
|
| 3 to 2 |
125–250 µm |
0.0049–0.010 in |
Fine sand |
|
| 4 to 3 |
62.5–125 µm |
0.0025–0.0049 in |
Very fine sand |
|
| 8 to 4 |
3.9–62.5 µm |
0.00015–0.0025 in |
Silt |
Mud |
| > 8 |
< 3.9 µm |
< 0.00015 in |
Clay |
Mud |
| >10 |
< 1 µm |
< 0.000039 in |
Colloid |
Mud |
|
|
|
|
|
Source: Wikipedia
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