強淋溶土
维基百科，自由的百科全书
| 強淋溶土 Acrisol |
|
|---|---|
| 強淋溶土Acrisol Image | |
| A gleyic acrisol profile from Malaysia | |
| Used in: | WRB |
| WRB code: | AC |
| Profile: | AEBtC |
| Parent material: | various |
| 氣候： | 熱帶、亞熱帶濕潤 |
強淋溶土（通用名稱Acrisols）是一種由聯合國糧食及農業組織劃分的土壤 。它是一種含豐富黏土的土壤，與濕潤的熱帶氣候相關，例如在巴西 ，而且往往支撐森林地區[1]。它是世界土壤參考基準30個主要群體的之一[2]。Acrisols correspond to the aquult, humults, udults and ustults sub-orders of ultisols in the USDA soil taxonomy and also to oxisols with a candic horizons and some alfisols.[3] The acrisols low fertility and toxic amounts of aluminium pose limitations to its agricultural use, favouring in many places its use for silviculture, low intensity pasture and protected areas. Crops that can be successfully cultivated, if climate allows, include tea, rubber tree, oil palm, coffee and sugar cane.[3]
強淋溶土的類別是：
- ACf Ferric Acrisols
- ACg Gleyic Acrisols
- ACh Haplic Acrisols
- ACp Plinthic Acrisols
- ACu Humic Acrisols
參見 [编辑]
參考文獻 [编辑]
- ^ T. R. Yu. Chemistry of Variable Charge Soils. Oxford University Press. 1997. 36. ISBN 0-19-509745-9.
- ^ World reference base for soil resources
- ^ 3.0 3.1 CHESWORTH, WARD. Encyclopedia of Soil Science. 2001. pp. 22-24
外部連結 [编辑]
- （英文）強淋溶土
- 本条目的部分内容翻译自英語維基百科条目Acrisols（版本276966945）並以知识共享-署名-相同方式共享3.0协议授权使用。原文作者列表請參閱其页面历史。
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