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Updated: Dec 6, 2025

Measuring Phosphorus Release in Laboratory Microcosms for Water Quality Assessment
Published on: July 22, 2019
Development of phosphorus sorption capacity-based environmental indices for tile-drained systems
Pauline Welikhe1, Sylvie M Brouder1, Jeffrey J Volenec1
1Dep. of Agronomy, Purdue Univ., 915 W State St., West Lafayette, IN, 47907, USA.
Estimating phosphorus sorption capacity (PSC) using pedotransfer functions (pedoTFs) is feasible for routine soil management. These PSC-based indices can predict phosphorus loss to surface waters, aligning with agronomic thresholds.
Area of Science:
- Soil Science
- Environmental Chemistry
- Water Quality Management
Background:
- Phosphorus (P) loss to surface waters is an environmental concern, necessitating routine soil management strategies.
- Quantifying P sorption capacity (PSC) via laborious isotherms is impractical for regular decision-making.
- Pedotransfer functions (pedoTFs) offer a viable alternative for estimating PSC from standard soil properties.
Purpose of the Study:
- To develop and validate a pedoTF for estimating PSC.
- To evaluate PSC-based indices, specifically P saturation ratio (PSR) and soil P storage capacity (SPSC), for predicting P loss.
- To assess the relationship between these indices and soluble P concentrations in tile drain effluent.
Main Methods:
- Development of a pedoTF using soil aluminum and organic matter to predict PSC.
- Analysis of segmented-line relationships between PSR and soluble P in desorption assays and drainflows.
- Investigation of SPSC relationships with soluble P concentrations in both laboratory and field conditions.
Main Results:
- A pedoTF accurately predicted PSC (R² = .60) using soil aluminum and organic matter.
- Apparent PSR thresholds of 0.21 (desorption) and 0.24 (drainflow) were identified.
- SPSC showed linear relationships with soluble P, with negative values indicating potential P loss and positive values indicating low P concentrations.
Conclusions:
- PedoTF-derived PSC indices can effectively estimate subsurface soluble P loss potential.
- Identified index thresholds align with critical soil-test P levels for agronomic sufficiency.
- Agronomic P sufficiency thresholds may also serve as environmental P thresholds for water quality protection.
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