Alisol | FAO Soil Group - Encyclopedia Britannica

Ask the Chatbot Games & Quizzes History & Society Science & Tech Biographies Animals & Nature Geography & Travel Arts & Culture ProCon Money Videos Alisol Introduction References & Edit History Related Topics Images Alisol soil profile from China, showing a dense subsurface horizon rich in clay and aluminum. climate and soil Britannica AI Icon Contents Science Earth Science, Geologic Time & Fossils Earth Sciences CITE verifiedCite While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions. Select Citation Style MLA APA Chicago Manual of Style Copy Citation Share Share Share to social media Facebook X URL https://www.britannica.com/science/Alisol Feedback External Websites Feedback Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login). Feedback Type Select a type (Required) Factual Correction Spelling/Grammar Correction Link Correction Additional Information Other Your Feedback Submit Feedback Thank you for your feedback

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  • International Society of Soil Sciences - World Soil Information - Alisol
Alisol soil profile from China, showing a dense subsurface horizon rich in clay and aluminum.
Alisol soil profile from China, showing a dense subsurface horizon rich in clay and aluminum. (more)
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Alisol, one of the 30 soil groups in the classification system of the Food and Agriculture Organization (FAO). Alisols are highly acidic, poorly drained soils prone to aluminum toxicity and water erosion. Liming and fertilization are essential to their agricultural use—primarily for growing oil palm, corn (maize), and cotton. Their extent has not been established definitively, but they are believed to occupy less than 1 percent of the total land area on Earth, predominately in the southeastern United States (in soil zones currently classified as Acrisols) and Malaysia.

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Alisols are characterized by the presence of a dense subsurface layer of accumulated clay of mixed mineralogy (mostly kaolinitic) containing a significant amount of readily soluble aluminum ions bound to soil particles and by the lack of an extensively leached layer below the surface horizon (uppermost layer). They occur under the same topographic conditions as Acrisols but in climates with greater precipitation and higher temperatures. Alisols are also related to the Lixisol and Nitisol groups in the FAO classification system and to the Ultisol order of the U.S. Soil Taxonomy.

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