2013
DOI: 10.1016/b978-0-12-417187-9.00002-4
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Assessment and Modeling of Soil Available Phosphorus in Sustainable Cropping Systems

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Cited by 73 publications
(48 citation statements)
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“…Liming enhances plant- ions from the soil adsorption sites resulting in increase in soil pH. Therefore, the increase in soil available P could be due to the reduction in phosphorus fixation by Al and Fe oxides effected of lime (Kisinyo et al, 2012;Ziadi et al, 2013). Data presented in Table 4 indicate that the amounts of plant-available P taken up by the plants in acid soil were quite small -186 mg kg -1 P 2 O 5 , or 20.8% of total P (Table 4).…”
Section: Resultsmentioning
confidence: 99%
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“…Liming enhances plant- ions from the soil adsorption sites resulting in increase in soil pH. Therefore, the increase in soil available P could be due to the reduction in phosphorus fixation by Al and Fe oxides effected of lime (Kisinyo et al, 2012;Ziadi et al, 2013). Data presented in Table 4 indicate that the amounts of plant-available P taken up by the plants in acid soil were quite small -186 mg kg -1 P 2 O 5 , or 20.8% of total P (Table 4).…”
Section: Resultsmentioning
confidence: 99%
“…Plant-available P is the fraction of total P in soil that is readily available for absorption by plant roots. The major constraint in achieving adequate phosphorus nutrition in crops arises from the fact that plant available P diffuses slowly through the soil solution toward roots, complicated by the fact that migrating P ions are susceptible to chemical fixation in most agricultural soils (Ziadi et al, 2013). Phosphorus extracted from the soil and determined using A-L method was regarded in our research as a constituent of the plant-available phosphate group.…”
Section: Resultsmentioning
confidence: 99%
“…The lower Olsen-P in ADM-than CM-and SS-amended soils and similar Olsen-P between CM-and SS-amended soils largely reflected the amount of P applied during the experimental period due to the greater N/P ratio in ADM (7.0) than CM (3.5) and SS (3.8). Limiting Olsen-P (soil test P) accumulation is important because this P is susceptible to hydrologic loss pathways, primarily via runoff and leaching (Pote et al, 1996;Sims et al, 2000;Olson et al, 2010a;Kumaragamage et al, 2011;Ziadi et al, 2013). Because the N/P ratio of ADM (7.0) was relatively close to that of the barley forage (8.8), the ADM-amended soil had a significantly lower risk of P accumulation than soils receiving CM or SS.…”
Section: Olsen-phosphorusmentioning
confidence: 99%
“…Digestate had the lowest soil-test P risk, while cattle manure and pellets were similar, but separated solids had a 29% greater risk of soil-test P accumulation per unit of N applied than cattle manure, indicating that this amendment requires careful management to minimize soil-test P accumulation when applied at N-based rates. This is important because soil-test P is an indicator for loss via runoff and leaching pathways (Pote et al, 1996;Sims et al, 2000;Olson et al, 2010;Kumaragamage et al, 2011;Ziadi et al, 2013;Li et al, 2016). It also provides evidence that P-based rates may be more suitable for the higher risk amendments such as cattle manure and separated solids.…”
Section: Residual Nitrate-nitrogen and Soiltest Phosphorus Risk Factorsmentioning
confidence: 99%