2006
DOI: 10.1007/s11104-005-5929-6
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Phosphorus Transformations under Reduction in Long-term Manured Soils

Abstract: The widespread recycling of animal wastes as fertilizers can severely affect the phosphorus cycle, especially in soils that undergo periodical flooding and anaerobiosis. The aim of this study was to investigate the effect that reducing conditions have on the release and forms of P in soils that have received different doses (0, 60 and 120 Mg/ha) of liquid hog manure for 15 years. Samples of the topsoil (0-20 cm) and of subsoil (20-40 cm) were placed under static reducing condition. At the onset of the reductio… Show more

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Cited by 44 publications
(31 citation statements)
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“…Under prolonged flooded conditions, decrease in redox potential (Eh) and associated pH changes may play a direct or indirect role in controlling P sorption and release. Anaerobic conditions can increase P availability in soils and accelerate P loss to water bodies (Ajmone‐Marsan et al, 2006; Hoffman et al, 2009; Kröger et al, 2012; Scalenghe et al, 2012).…”
mentioning
confidence: 99%
“…Under prolonged flooded conditions, decrease in redox potential (Eh) and associated pH changes may play a direct or indirect role in controlling P sorption and release. Anaerobic conditions can increase P availability in soils and accelerate P loss to water bodies (Ajmone‐Marsan et al, 2006; Hoffman et al, 2009; Kröger et al, 2012; Scalenghe et al, 2012).…”
mentioning
confidence: 99%
“…A recent publication with Re´gis as a posthumous coauthor confirmed the nature of his observations and concerns, showing a three to twenty fold increase in water soluble P in manured soils from Quebec after 2 weeks of submergence (Ajmone-Marsan et al 2006). Sequential extraction analyses showed that the increase in soluble P came from all P fractions in soil, including those fractions usually regarded as recalcitrant under aerobic conditions.…”
Section: Grant Et Al * a Tribute To Regis Simard 139mentioning
confidence: 70%
“…In contrast, organically bound P increases with the lowering of redox potential and accounts for a greater fraction of total P; accumulation of organic P relatively to inorganic P helps to limit overall P loss (e.g., Reddy and Rao, 1983;Martin et al, 1997;Ruiz et al, 1997;Sallade and Sims, 1997;Vadas and Sims, 1998;Turner and Haygarth, 2001;Shenker et al, 2005;Castillo and Wright, 2008). The loss of inorganic P sorption surfaces starts in soils with moderate reduction (Miller et al, 2001) and later the soil solutions contain enough Fe to effectively retain the released P by means of coprecipitation or adsorption onto newly formed Fe hydroxides as the solution encounters oxidized conditions (Shenker et al, 2005;Ajmone Marsan et al, 2006). As redox reactions influence indirectly the soil P chemistry through effects on the solubility of Fe and Mn minerals and the associated changes in pH affect the Ca phosphate solubility, the change in P concentration during a redox cycle depends on a combination of the shifts of redox potential and pH (Scalenghe et al, 2002).…”
Section: Phophorus-release Potential and Environmental Changes: Redoxmentioning
confidence: 99%