
alfisol
Sign in to savethumb|upright=1.6|Alfisols of the world thumb|upright=1.6|One of the environments in which Alfisols can develop is the Temperate deciduous forest
Key facts
- Soil.name
- Alfisol
- Soil.image
- Alfisol profile.jpg
- Soil.image_size
- 250px
- Soil.image_caption
- An Alfisol profile
- Soil.classification_system
- USDA soil taxonomy
- Soil.climate
- various
via Wikipedia infobox
Wikidata facts
- Image
- Alfisol Italy.jpg
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- Commons category
- Alfisols
Sources (3)
via Wikidata · CC0
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Article
5 sectionsContents
- Suborders
- Fossil record of Alfisols
- See also
- References
- External links
thumb|upright=1.6|Alfisols of the world thumb|upright=1.6|One of the environments in which Alfisols can develop is the Temperate deciduous forest
Alfisols are a soil order in USDA soil taxonomy. Alfisols form in semi-arid to humid areas, typically under a hardwood forest cover. They have a clay-enriched subsoil and relatively high native fertility. "Alf" refers to aluminium (Al) and iron (Fe). Because of their productivity and abundance, Alfisols represent one of the more important soil orders for food and fiber production. They are widely used both in agriculture and forestry, and are generally easier to keep fertile than other humid-climate soils, though those in Australia and Africa are still very deficient in nitrogen and available phosphorus. Those in monsoonal tropical regions, however, have a tendency to acidify when heavily cultivated, especially when nitrogenous fertilizers are used.
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