Plinthosol
| Plinthosols | |
|---|---|
| Groundwater Laterite, Plinthaquox (USDA) | |
 | |
| Used in | WRB |
| WRB code | PT |
| Key process | Accumulation of Fe under hydromorphic conditions |
| Parent material | basic rock, Fe |
| Climate | wet tropics |
Plinthosols are iron-rich soils characterized by the presence of plinthite, petroplinthite or pisoliths.
Distribution
Softer plinthosols are common in the wet tropics, including in the eastern Amazon basin, the central Congo basin and parts of Southeast Asia. Dryer areas, including the Sudano-Sahelian zone, Southern African savannah, the Indian subcontinent, and parts of Southeast Asia and northern Australia feature mostly harder pisoliths and petroplinthite.
See also
- Laterite – Product of rock weathering in wet tropical climates rich in iron and aluminium
References
- IUSS Working Group WRB: World Reference Base for Soil Resources 2014, Update 2015. World Soil Resources Reports 106, FAO, Rome 2015. ISBN 978-92-5-108369-7 (PDF 2,3 MB).
External links
- profile photos (with classification) WRB homepage
- profile photos (with classification) IUSS World of Soils
 | This soil science–related article is a stub. You can help Wikipedia by expanding it. |