Ped

In soil science, peds are aggregates of soil particles formed naturally as a result of pedogenic processes; this natural organization of particles forms discrete units separated by pores or voids. The term is generally used for macroscopic (visible; i.e. greater than 1 mm in size) structural units when observing soils in the field. Soil peds should be described when the soil is dry or slightly moist, as they can be difficult to distinguish when wet.^[1] An artificially formed aggregate of soil particles can be called a clod.^[2]

There are five major classes of macrostructure seen in soils: platy, prismatic, columnar, granular, and blocky. There are also structureless conditions. Some soils have simple structure, each unit being an entity without component smaller units. Others have compound structure, in which large units are composed of smaller units separated by persistent planes of weakness.

References

^ Jahn, R.; Blume, H.-P.; Asio, V.B.; Spaargaren, O.; Schad, P. (2006). Guidelines for soil description (4th ed.). Rome: FAO. pp. 44–48. ISBN 9251055211.
^ Allaby, Ailsa; Allaby, Michael (1999). A Dictionary of Earth Sciences (2nd ed.). Oxford: Oxford University Press. ISBN 0-19-280079-5.

[Jahn2006-1] Jahn, R.; Blume, H.-P.; Asio, V.B.; Spaargaren, O.; Schad, P. (2006). Guidelines for soil description (4th ed.). Rome: FAO. pp. 44–48. ISBN 9251055211.

[Allaby1999-2] Allaby, Ailsa; Allaby, Michael (1999). A Dictionary of Earth Sciences (2nd ed.). Oxford: Oxford University Press. ISBN 0-19-280079-5.

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See also

References