2017
DOI: 10.1080/03650340.2017.1346372
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Organic amendments as a source of phosphorus: agronomic and environmental impact of different animal manures applied to an acid soil

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Cited by 30 publications
(15 citation statements)
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“…The organic fertilizer, C VER , was applied at a dose of 80 Mg/ha. According to Saha et al [49] and Horta et al [54], the application of C VER leads to the increased content and availability of basic nutrients in the soil through the mineralization of SOM. The double dose of C VER had a significant positive effect on plant available phosphorus content in the soil (Table 7).…”
Section: Soil Enzyme Activitiesmentioning
confidence: 99%
“…The organic fertilizer, C VER , was applied at a dose of 80 Mg/ha. According to Saha et al [49] and Horta et al [54], the application of C VER leads to the increased content and availability of basic nutrients in the soil through the mineralization of SOM. The double dose of C VER had a significant positive effect on plant available phosphorus content in the soil (Table 7).…”
Section: Soil Enzyme Activitiesmentioning
confidence: 99%
“…Thus, fertilizer application is one of the important factors dictating the abundance of different P fractions and pools of P. Without P addition, P pool is mainly considered as non-labile but may become increasingly available to plants at variable amounts depending on soil type and other environmental conditions 17 , 18 . Long-term application of animal manures and other organic amendments have shown to increase soil total, available, and soluble P concentrations and at soil depths 19 21 . Whalen and Chang 22 have reported that total and available P pools increased greatly in soils amended with manure annually for 16 years and were 1.2–3.8 and 0.8–1.9 Mg P ha −1 greater than in the soils that did not receive any manure.…”
Section: Introductionmentioning
confidence: 99%
“…The main processes to explain this conclusion include: 1) Competitive sorption between humic and fluvic acids [10] [11] [12] or low molecular weight aliphatic acids (LOA) and P for soil sorption sites resulting in increased P concentration in the soil solution [13] [14] [15]; 2) Metal complexation with OM compounds (LOA) or dissolution reactions affecting mainly Fe an Al oxides decreasing P sorption sites [14] [16] and 3) Sorption of OM compounds that could increase the negative charge on the soil surface, or decrease the point of zero charge (PCZ) increasing the resistance to P sorption. Unlike these effects, OM added to soil could increase the formation of metal bridges leading to increased P sorption sites [17] or in turn the P content of the added OM could also be a source of available P to soil solution [18] [19]. To assess P phytoavailability, some soil tests P (STP), like the Olsen (Olsen-P, [20]) and the Ammonium Lactate (AL-P, [21]) are commonly used.…”
Section: Introductionmentioning
confidence: 99%