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Mobility, solubility and lability of fluid and granular forms of P fertiliser in calcareous and non-calcareous soils under laboratory conditions

Despite a long history of application of phosphorus fertilisers, P deficiency is still a major limitation to crop production on calcareous soils. Recent field research conducted in highly calcareous soils in southern Australia has demonstrated that both grain yield and P uptake of wheat (Triticum ae... Full description

Journal Title: Plant and soil 2005-02-01, Vol.269 (1/2), p.25-34
Main Author: LOMBI, E
Other Authors: MCLAUGHLIN, M. J , JOHNSTON, C , ARMSTRONG, R. D , HOLLOWAY, R. E
Format: Electronic Article Electronic Article
Language: English
Subjects:
Publisher: Dordrecht: Springer
ID: ISSN: 0032-079X
Link: http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16864303
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title: Mobility, solubility and lability of fluid and granular forms of P fertiliser in calcareous and non-calcareous soils under laboratory conditions
format: Article
creator:
  • LOMBI, E
  • MCLAUGHLIN, M. J
  • JOHNSTON, C
  • ARMSTRONG, R. D
  • HOLLOWAY, R. E
subjects:
  • 2nd International Symposium on Phosphorus Dynamics in the Soil-Plant Continuum
  • Acid soils
  • Agricultural site preparation
  • Agricultural soils
  • Agrology
  • Agronomy. Soil science and plant productions
  • Alkaline soils
  • Biological and medical sciences
  • Calcareous soils
  • Fertilizers
  • Fundamental and applied biological sciences. Psychology
  • General agronomy. Plant production
  • Nitrogen, phosphorus, potassium fertilizations
  • Phosphates
  • Phosphorus fertilization
  • Soil chemistry
  • Soil samples
  • Soil-plant relationships. Soil fertility. Fertilization. Amendments
  • Soils
  • Triticum aestivum
ispartof: Plant and soil, 2005-02-01, Vol.269 (1/2), p.25-34
description: Despite a long history of application of phosphorus fertilisers, P deficiency is still a major limitation to crop production on calcareous soils. Recent field research conducted in highly calcareous soils in southern Australia has demonstrated that both grain yield and P uptake of wheat (Triticum aestivum L.) is greater when fluid forms of P are used compared to granular forms. To improve our understanding of the mechanisms underlying this response to P in the field, we compared the lability, solubility and mobility of P applied as either a fluid (3 products) or granular (3 products) form to two calcareous and one alkaline non-calcareous soils in the laboratory. Over a five-week period, between 9.5 and 18% of the P initially present in the fertiliser granules did not diffuse into the surrounding soil. The degree of granule dissolution was independent of the soil type. In contrast, P solubility, lability and diffusion were significantly greater when fluid products were applied to the calcareous soils, but not to the alkaline non-calcareous soil. These findings are discussed in relation to field trials results where fluid products outperformed granular fertilisers.
language: eng
source:
identifier: ISSN: 0032-079X
fulltext: no_fulltext
issn:
  • 0032-079X
  • 1573-5036
url: Link


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descriptionDespite a long history of application of phosphorus fertilisers, P deficiency is still a major limitation to crop production on calcareous soils. Recent field research conducted in highly calcareous soils in southern Australia has demonstrated that both grain yield and P uptake of wheat (Triticum aestivum L.) is greater when fluid forms of P are used compared to granular forms. To improve our understanding of the mechanisms underlying this response to P in the field, we compared the lability, solubility and mobility of P applied as either a fluid (3 products) or granular (3 products) form to two calcareous and one alkaline non-calcareous soils in the laboratory. Over a five-week period, between 9.5 and 18% of the P initially present in the fertiliser granules did not diffuse into the surrounding soil. The degree of granule dissolution was independent of the soil type. In contrast, P solubility, lability and diffusion were significantly greater when fluid products were applied to the calcareous soils, but not to the alkaline non-calcareous soil. These findings are discussed in relation to field trials results where fluid products outperformed granular fertilisers.
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subject2nd International Symposium on Phosphorus Dynamics in the Soil-Plant Continuum ; Acid soils ; Agricultural site preparation ; Agricultural soils ; Agrology ; Agronomy. Soil science and plant productions ; Alkaline soils ; Biological and medical sciences ; Calcareous soils ; Fertilizers ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Nitrogen, phosphorus, potassium fertilizations ; Phosphates ; Phosphorus fertilization ; Soil chemistry ; Soil samples ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Soils ; Triticum aestivum
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02nd International Symposium on Phosphorus Dynamics in the Soil-Plant Continuum
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02nd International Symposium on Phosphorus Dynamics in the Soil-Plant Continuum
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jtitlePlant and soil
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abstractDespite a long history of application of phosphorus fertilisers, P deficiency is still a major limitation to crop production on calcareous soils. Recent field research conducted in highly calcareous soils in southern Australia has demonstrated that both grain yield and P uptake of wheat (Triticum aestivum L.) is greater when fluid forms of P are used compared to granular forms. To improve our understanding of the mechanisms underlying this response to P in the field, we compared the lability, solubility and mobility of P applied as either a fluid (3 products) or granular (3 products) form to two calcareous and one alkaline non-calcareous soils in the laboratory. Over a five-week period, between 9.5 and 18% of the P initially present in the fertiliser granules did not diffuse into the surrounding soil. The degree of granule dissolution was independent of the soil type. In contrast, P solubility, lability and diffusion were significantly greater when fluid products were applied to the calcareous soils, but not to the alkaline non-calcareous soil. These findings are discussed in relation to field trials results where fluid products outperformed granular fertilisers.
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