The Role of Free Iron Oxides in the Retention of Phosphorus in Some Highly Weathered Soils of the Tropics PDF Download
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Author: Kingston W. Nyamapfene
Publisher:
ISBN:
Category : Iron oxides
Languages : en
Pages : 326
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Book Description
Author: Kingston W. Nyamapfene
Publisher:
ISBN:
Category : Iron oxides
Languages : en
Pages : 326
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Book Description
Author: Mehruinsa Memon
Publisher:
ISBN: 9783866442412
Category :
Languages : en
Pages : 144
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Book Description
Author: Daud Bin Chinta
Publisher:
ISBN:
Category : Phosphorus
Languages : en
Pages : 276
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Book Description
Author: Peter Adams
Publisher:
ISBN:
Category : Soils
Languages : en
Pages : 260
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Book Description
Author: Amir Hass
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Book Description
Forest soil phosphorus (P) chemical behavior was evaluated in some mid-rotation fertilized loblolly pine (Pinus taeda L.) plantations in East Texas, that differed in their site drainage characteristics. Forest floor mass and carbon content in the forest floor were determined. Total P (PT) in the forest floor, and total and Mehlich-1 P and citrate dithionite (CD) and acid ammonium-oxalate (AAO) extractable P, Al, Fe, and Mn within the mineral soil upper 100 cm were determined. Colorimetric determination of AAO and CD-extractable P by the molybdenum blue ascorbic acid method, without the use of pre-digestion, was assessed by an automated continuous flow injection system. Phosphorus distribution between different operationally defined solid phases and its relationships with CD and AAO extractable Mn, Al, Fe among depth, site, drainage class and treatment were evaluated. Soil P forms were highly correlated with iron oxides across sites, drainage classes, treatments, and depth intervals with significant differences in P content and distribution in the soil profile and solid phases among drainage classes. Soil P distribution patterns differed among drainage classes, yet it followed the distribution of the iron oxides. Iron oxide's role as a sink for soil P was higher in the well-drained compared to the poorly drained sites. Amorphous phases of iron oxides were higher in the poorly drained sites and dominated the role of iron oxides as a sink for P under the poor drainage conditions. Fertilization resulted in significantly higher forest floor mass, P content in the forest floor, and total P (PT) and CD-extractable P (Pd) in the soils' upper 10 cm. The treatment effect on P in the forest floor, and on PT and Pd in the upper 10 cm of the mineral soil was equivalent to 6, 19, and 11% of the applied P, respectively. AAO-extractable P was highly correlated with Mehlich-1 P in the fertilized plots. Treatment and site drainage class effects on P accumulation in the different solid phases in the mineral soil and in the forest floor and the potential contribution of these pools to P availability in subsequent rotations, following clearcutting, are discussed.
Author: Handi Wang
Publisher:
ISBN:
Category : Liming of soils
Languages : en
Pages : 226
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Book Description
Author:
Publisher:
ISBN:
Category : Agriculture
Languages : en
Pages : 712
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Book Description
Sept.-Oct. issue includes list of theses and dissertations for U.S. and Canadian graduate degrees granted in crop science, soil science, and agronomic science during the previous academic year.
Author: Pedro A. Sanchez
Publisher: Cambridge University Press
ISBN: 1107176050
Category : Business & Economics
Languages : en
Pages : 685
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Book Description
Long-awaited second edition of classic textbook, brought completely up to date, for courses on tropical soils, and reference for scientists and professionals.
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 396
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Book Description
Author: Sarah Elizabeth Johnson
Publisher:
ISBN:
Category :
Languages : en
Pages : 270
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Book Description
Phosphate deficiency is fiequently a limiting factor in crop production on acid soils due to the tendency of iron oxides to strongly bind phosphate through inner-sphere ligand adsorption. Two of the reported responses of some plants to P-deficiency stress are organic-acid exudation from the roots and increased phosphatase activity. Organic-acid-induced P release from iron-oxide surfaces was studied using synthetic iron oxides. The amounts of P released and Fe dissolved fiom ferrihydrite and goethite at pH 4.0, 5.5, and 7.0 by citric, malic, malonic, oxalic, succinic, and tartaric acids were measured. At low initial P-adsorption levels, ligand-induced dissolution of the oxide surface as the primary mechanism of P release from oxides was supported by the strong positive relationship between Fe dissolved and P released. At higher initial P-adsorption levels, ligand exchange played a greater role in P release. Ten cultivars of sorghum exhibiting a range of P efficiencies were obtained from EMBRAPA in Brazil and tested for organic-acid exudation and phosphatase activity under P-deficiency stress in hydroponic culture. HPLC analysis of root exudates revealed increases in oxalate and succinate under P-deficient conditions, with significant differences between cultivars. There was no evidence of citrate in the root exudates at either P leveI. Western blots using arabidopsis purple acid-phosphatase antibodies revealed varying increases in phosphatase activity under P deficiency among the different cultivars. It was concluded that organic-acid exudation might not be expected to significantly improve P uptake by plants grown on weathered soils dominated by well crystalline iron oxide under low P-fertility conditions. Under higher initial P-fertility conditions, organic-acid exudation might play a greater role in plant P acquisition.
