Modeling soil and plant phosphorus dynamics in calcareous and highly weathered soils
Material type: ArticleLanguage: En Publication details: 1989ISSN:- 0361-5995
- America
- Chemical soil types
- Climatic soil types
- Ecology
- Ecosystems
- Elements
- Environment
- Fertilizers AGROVOC
- Fertilizing
- Inorganic compounds
- Lithological soil types
- Mathematics
- Methods
- Nonmetals
- North America
- Organic compounds
- Phosphates
- Salts
- Site factors
- Soil types
- Soils
- Soil fertility AGROVOC
- Soil fertility AGROVOC
- 89-146835
Item type | Current library | Collection | Call number | Copy number | Status | Date due | Barcode | Item holds | |
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Article | CIMMYT Knowledge Center: John Woolston Library | AGRIS Collection | 89-146835 (Browse shelf(Opens below)) | 1 | Available | 89-146835 |
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Peer-review: Yes - Open Access: Yes|http://science.thomsonreuters.com/cgi-bin/jrnlst/jlresults.cgi?PC=MASTER&ISSN=0361-5995
Labile and organic phosphorus (P) and sorbed P are required as the minimum data set to run a soil-plant P cycling model recently developed for continental U.S. soils. Labile and organic P and P sorption index were related to physical and chemical properties of 23 calcareous (greater than 50 g kg-1 CaCO3 content) and 32 highly weathered soils (greater than 30% Al saturation), to allow estimation of these P forms from readily available soil data. The P sorption or fertilizer AV index was estimated as the fraction of fertilizer P remaining as labile (resin extractable) P following incubation of soil and fertilizer. Labile P was linearly related (R2
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