Initial and residual benefits of soil amendments in reducing phosphorus release from soils with simulated snowmelt flooding
Darshani Kumaragamage, Ahmed Lasisi, Madelynn Perry, Douglas Goltz, Nora Casson, Srimathie Indraratne, Inoka Amarakoon

TL;DR
Alum reduces phosphorus loss from soils during snowmelt flooding, but its effects fade within a year.
Contribution
This study evaluates the initial and residual effectiveness of soil amendments in reducing phosphorus release during simulated snowmelt flooding.
Findings
Alum reduced porewater and floodwater phosphorus by up to 68% and 69%, respectively, in the year of application.
Alum's effectiveness decreased over time, with only a 35% porewater phosphorus reduction one year later.
Gypsum and Epsom salt showed negligible or no long-term benefits in reducing phosphorus loss.
Abstract
In the Canadian prairies, spring snowmelt occurs rapidly and causes flooding in low‐lying areas, inducing anaerobic soil conditions and exacerbating phosphorus (P) release to meltwater. Soil amendments can mitigate P loss from flooded soils soon after amendment application; however, their residual benefits are less understood. We examined the initial and residual benefits of alum (Al2(SO4)3·18H2O), gypsum (CaSO4·2H2O), and Epsom salt (MgSO4·7H2O) in a simulated snowmelt flooding experiment. Intact soil columns were taken from amended and unamended field plots in the same year and 1 year after the amendment application. The soil columns were flooded and incubated at a cold temperature. Porewater and floodwater samples were analyzed for dissolved reactive P (DRP), calcium (Ca), magnesium (Mg), iron (Fe), and manganese (Mn) concentrations, and pH. During the year of application, alum,…
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Taxonomy
TopicsSoil and Water Nutrient Dynamics · Soil Carbon and Nitrogen Dynamics · Soil erosion and sediment transport
