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A conceptual model for dissolved P mobilization from legacy sources

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A conceptual model for dissolved P mobilization from legacy sources. / Nash, D. M.; Mc Dowell, R. W.; Kleinman, P. J. A. et al.
In: Journal of Environmental Quality, Vol. 54, No. 2, 30.04.2025, p. 303-318.

Research output: Contribution to Journal/MagazineReview articlepeer-review

Harvard

Nash, DM, Mc Dowell, RW, Kleinman, PJA, Moore, PA, Duncan, JM, Haygarth, PM, Smith, DR & Iho, A 2025, 'A conceptual model for dissolved P mobilization from legacy sources', Journal of Environmental Quality, vol. 54, no. 2, pp. 303-318. https://doi.org/10.1002/jeq2.70003

APA

Nash, D. M., Mc Dowell, R. W., Kleinman, P. J. A., Moore, P. A., Duncan, J. M., Haygarth, P. M., Smith, D. R., & Iho, A. (2025). A conceptual model for dissolved P mobilization from legacy sources. Journal of Environmental Quality, 54(2), 303-318. https://doi.org/10.1002/jeq2.70003

Vancouver

Nash DM, Mc Dowell RW, Kleinman PJA, Moore PA, Duncan JM, Haygarth PM et al. A conceptual model for dissolved P mobilization from legacy sources. Journal of Environmental Quality. 2025 Apr 30;54(2):303-318. Epub 2025 Feb 20. doi: 10.1002/jeq2.70003

Author

Nash, D. M. ; Mc Dowell, R. W. ; Kleinman, P. J. A. et al. / A conceptual model for dissolved P mobilization from legacy sources. In: Journal of Environmental Quality. 2025 ; Vol. 54, No. 2. pp. 303-318.

Bibtex

@article{6ea71c95e8e44a31af428b7f6a2c52f9,
title = "A conceptual model for dissolved P mobilization from legacy sources",
abstract = "Excessive phosphorus (P) concentrations can lead to conditions that limit the amenity of freshwater resources. This problem is particularly acute in agricultural catchments, where P fertilizer and manure amendments have been used to increase soil fertility and productivity. In these catchments, P indices are often used to help target critical source areas in order to reduce P exports. However, the overall impact of agricultural mitigation efforts on receiving waters has not always been consistent with declines in total P exports from catchments. In this paper we propose a model of dissolved P mobilization (i.e., entrainment) in surface runoff that accounts for this outcome and examine modifications to P indices that better accommodate dissolved P mobilization. We suggest that dissolved P mobilization commences near the soil surface and has two phases. When water is first applied, labile P is mostly mobilized by dissolution and advection. Subsequently, as the supply of readily accessible P is exhausted, diffusion and hydrodynamic dispersion mobilize P from other sources at a near constant rate for the remainder of the event. As most P exports occur in larger (i.e., longer) events, the second phase appears responsible for most dissolved P exports. Such a model of dissolved P mobilization is consistent with runoff monitoring data under natural and simulated rainfall, suggesting that on low (shallow) slopes where the interaction between surface soil and water may be prolonged, dissolved P concentrations are likely to be higher. Dissolved P mobilization from low‐slope areas is not well represented in P indices at present. We suggest that there needs to be a more complex, mechanistic structure to P indices that involves additional compartmentalization. Further, we suggest that this can be achieved without losing the simplicity of P indices or flexibility to integrate research data and experiential knowledge into tools that are relevant to specific regions.",
author = "Nash, {D. M.} and {Mc Dowell}, {R. W.} and Kleinman, {P. J. A.} and Moore, {P. A.} and Duncan, {J. M.} and Haygarth, {P. M.} and Smith, {D. R.} and A. Iho",
year = "2025",
month = apr,
day = "30",
doi = "10.1002/jeq2.70003",
language = "English",
volume = "54",
pages = "303--318",
journal = "Journal of Environmental Quality",
issn = "0047-2425",
publisher = "ASA/CSSA/SSSA",
number = "2",

}

RIS

TY - JOUR

T1 - A conceptual model for dissolved P mobilization from legacy sources

AU - Nash, D. M.

AU - Mc Dowell, R. W.

AU - Kleinman, P. J. A.

AU - Moore, P. A.

AU - Duncan, J. M.

AU - Haygarth, P. M.

AU - Smith, D. R.

AU - Iho, A.

PY - 2025/4/30

Y1 - 2025/4/30

N2 - Excessive phosphorus (P) concentrations can lead to conditions that limit the amenity of freshwater resources. This problem is particularly acute in agricultural catchments, where P fertilizer and manure amendments have been used to increase soil fertility and productivity. In these catchments, P indices are often used to help target critical source areas in order to reduce P exports. However, the overall impact of agricultural mitigation efforts on receiving waters has not always been consistent with declines in total P exports from catchments. In this paper we propose a model of dissolved P mobilization (i.e., entrainment) in surface runoff that accounts for this outcome and examine modifications to P indices that better accommodate dissolved P mobilization. We suggest that dissolved P mobilization commences near the soil surface and has two phases. When water is first applied, labile P is mostly mobilized by dissolution and advection. Subsequently, as the supply of readily accessible P is exhausted, diffusion and hydrodynamic dispersion mobilize P from other sources at a near constant rate for the remainder of the event. As most P exports occur in larger (i.e., longer) events, the second phase appears responsible for most dissolved P exports. Such a model of dissolved P mobilization is consistent with runoff monitoring data under natural and simulated rainfall, suggesting that on low (shallow) slopes where the interaction between surface soil and water may be prolonged, dissolved P concentrations are likely to be higher. Dissolved P mobilization from low‐slope areas is not well represented in P indices at present. We suggest that there needs to be a more complex, mechanistic structure to P indices that involves additional compartmentalization. Further, we suggest that this can be achieved without losing the simplicity of P indices or flexibility to integrate research data and experiential knowledge into tools that are relevant to specific regions.

AB - Excessive phosphorus (P) concentrations can lead to conditions that limit the amenity of freshwater resources. This problem is particularly acute in agricultural catchments, where P fertilizer and manure amendments have been used to increase soil fertility and productivity. In these catchments, P indices are often used to help target critical source areas in order to reduce P exports. However, the overall impact of agricultural mitigation efforts on receiving waters has not always been consistent with declines in total P exports from catchments. In this paper we propose a model of dissolved P mobilization (i.e., entrainment) in surface runoff that accounts for this outcome and examine modifications to P indices that better accommodate dissolved P mobilization. We suggest that dissolved P mobilization commences near the soil surface and has two phases. When water is first applied, labile P is mostly mobilized by dissolution and advection. Subsequently, as the supply of readily accessible P is exhausted, diffusion and hydrodynamic dispersion mobilize P from other sources at a near constant rate for the remainder of the event. As most P exports occur in larger (i.e., longer) events, the second phase appears responsible for most dissolved P exports. Such a model of dissolved P mobilization is consistent with runoff monitoring data under natural and simulated rainfall, suggesting that on low (shallow) slopes where the interaction between surface soil and water may be prolonged, dissolved P concentrations are likely to be higher. Dissolved P mobilization from low‐slope areas is not well represented in P indices at present. We suggest that there needs to be a more complex, mechanistic structure to P indices that involves additional compartmentalization. Further, we suggest that this can be achieved without losing the simplicity of P indices or flexibility to integrate research data and experiential knowledge into tools that are relevant to specific regions.

U2 - 10.1002/jeq2.70003

DO - 10.1002/jeq2.70003

M3 - Review article

C2 - 39973459

VL - 54

SP - 303

EP - 318

JO - Journal of Environmental Quality

JF - Journal of Environmental Quality

SN - 0047-2425

IS - 2

ER -