Our method helps answer the question of how likely a given soil or sediment is to release soluble phosphorous under prolonged saturation. Quantifying phosphorous release potential in variably saturated environments is important for determining tra
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Accurate quantification of phosphorus (P) desorption potential in saturated soils and sediments is important for P modeling and transport mitigation efforts. To better account for in situ soil-water redox dynamics and P mobilization under prolonged saturation, a simple approach was developed based on repeated sampling of laboratory microcosms.
