This article describes the soil types used in the description of soil profiles within the european ISO 14688 norm. In the Netherlands, this norm is used with slight adjustments and called the NEN-EN-ISO-14688.

Soil into fractions

Within the ISO14688 soil consists of several fractions. The primary fraction (which is the most prevalent soil type within the current soil layer), and possible secondary or even tertiary fractions.

Soil types

The distinction between soil types is almost entirely decided by the grain size of the individual particles in the soil for all non-organic constituents. The organic soil type depends on the level of decomposition of the soil. The ISO 14688 contains the following soil types:

Soil catergorySoil typeGrain fraction
Very coarse soilLarge boulder>630 mm
 Boulder200 - 630 mm
 Cobble 63 - 200 mm
Coarse soilGravel2 - 63 mm
 Sand0,063 - 2 mm
Fine soilSilt0,002 - 0,063 mm
 Clay<0,002
Organic soilPeatN/a
 GyttjaN/a
 TopsoilN/a

These individual soiltypes are described more in depth on their own respective pages; You can click a soiltype in the table to navigate to the correct page, which contains a short overview and image.

Gradations

Of Sand and Gravel, the gradations can be described as well, these come in three categories: Fine, medium and coarse. These gradations exist for silt as well, but this is too small to be determined by hand and must be done within a lab if described.

Example descriptions

The main fraction is given as a noun, while the secundary and tertiary fractions are given as adjectives or added after the main fraction in a 'With x' statement. Some examples include:

-Sandy gravel

-Coarse sandy fine gravel

-Medium sandy silt

-Fine gravelly silty coarse Sand

References

  • ISO 14688
Tags:
 
TerraIndex