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The potential for soil phosphorus tests to predict phosphorus losses in overland flow.

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The potential for soil phosphorus tests to predict phosphorus losses in overland flow. / Quinton, John N.; Strauss, Peter; Miller, Nicola et al.
In: Journal of Plant Nutrition and Soil Science, Vol. 166, No. 4, 08.2003, p. 432-437.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Quinton, JN, Strauss, P, Miller, N, Azazoglu, E, Yli-Halla, M & Uusitalo, R 2003, 'The potential for soil phosphorus tests to predict phosphorus losses in overland flow.', Journal of Plant Nutrition and Soil Science, vol. 166, no. 4, pp. 432-437. https://doi.org/10.1002/jpln.200321122

APA

Quinton, J. N., Strauss, P., Miller, N., Azazoglu, E., Yli-Halla, M., & Uusitalo, R. (2003). The potential for soil phosphorus tests to predict phosphorus losses in overland flow. Journal of Plant Nutrition and Soil Science, 166(4), 432-437. https://doi.org/10.1002/jpln.200321122

Vancouver

Quinton JN, Strauss P, Miller N, Azazoglu E, Yli-Halla M, Uusitalo R. The potential for soil phosphorus tests to predict phosphorus losses in overland flow. Journal of Plant Nutrition and Soil Science. 2003 Aug;166(4):432-437. doi: 10.1002/jpln.200321122

Author

Quinton, John N. ; Strauss, Peter ; Miller, Nicola et al. / The potential for soil phosphorus tests to predict phosphorus losses in overland flow. In: Journal of Plant Nutrition and Soil Science. 2003 ; Vol. 166, No. 4. pp. 432-437.

Bibtex

@article{e65acb405d944191b4b3780fd0f065b3,
title = "The potential for soil phosphorus tests to predict phosphorus losses in overland flow.",
abstract = "Soil phosphorus tests offer a potentially powerful tool for land managers trying to predict the areas which will contribute diffuse losses of phosphorus (P) to surface water bodies through the overland flow vector - but do they work? We address this question at a range of scales, from patch (< 1 m2), through plot (several m2) to small watershed (several hectares). Our hypothesis is that as we increase the scale, and therefore the complexity of the system, soil P tests will predict P concentrations and losses associated with overland flow less well, and that this is partly due to a shift from dissolved P losses to P losses associated with eroded soil material. At the patch scale soil P tests were used to predict the P concentration and load from 24 European soils exposed to simulated rainfall under controlled conditions in the laboratory. Results showed that soil P tests were generally good predictors of reactive P <0.45 m, but did less well at predicting total P > 0.45 m. By combining the soil P test with measured sediment concentrations predictions of total P concentrations improved. Outdoor rainfall simulation experiments on bare soil plots (10 m2) revealed the overwhelming influence of particle bound P losses compared with P losses in the water phase. Soil P tests, which relate primarily to the dissolved P fractions in soil, were not able to predict total P losses, but were related to reactive P < 0.45 m losses. At the watershed scale soil P tests were able to predict reactive P < 0.45 m losses, but with considerable uncertainty. We conclude that soil P tests, in combination with sediment concentration provide a useful means of assessing the mobilization of P in overland flow, but should not be expected to provide watershed scale predictions of the movement of P into overland flow.",
keywords = "phosphorus tests environment diffuse pollution",
author = "Quinton, {John N.} and Peter Strauss and Nicola Miller and Erol Azazoglu and Markku Yli-Halla and Risto Uusitalo",
note = "Times Cited: 20 718TX J PLANT NUTR SOIL SCI",
year = "2003",
month = aug,
doi = "10.1002/jpln.200321122",
language = "English",
volume = "166",
pages = "432--437",
journal = "Journal of Plant Nutrition and Soil Science",
issn = "1436-8730",
publisher = "Wiley-VCH Verlag",
number = "4",

}

RIS

TY - JOUR

T1 - The potential for soil phosphorus tests to predict phosphorus losses in overland flow.

AU - Quinton, John N.

AU - Strauss, Peter

AU - Miller, Nicola

AU - Azazoglu, Erol

AU - Yli-Halla, Markku

AU - Uusitalo, Risto

N1 - Times Cited: 20 718TX J PLANT NUTR SOIL SCI

PY - 2003/8

Y1 - 2003/8

N2 - Soil phosphorus tests offer a potentially powerful tool for land managers trying to predict the areas which will contribute diffuse losses of phosphorus (P) to surface water bodies through the overland flow vector - but do they work? We address this question at a range of scales, from patch (< 1 m2), through plot (several m2) to small watershed (several hectares). Our hypothesis is that as we increase the scale, and therefore the complexity of the system, soil P tests will predict P concentrations and losses associated with overland flow less well, and that this is partly due to a shift from dissolved P losses to P losses associated with eroded soil material. At the patch scale soil P tests were used to predict the P concentration and load from 24 European soils exposed to simulated rainfall under controlled conditions in the laboratory. Results showed that soil P tests were generally good predictors of reactive P <0.45 m, but did less well at predicting total P > 0.45 m. By combining the soil P test with measured sediment concentrations predictions of total P concentrations improved. Outdoor rainfall simulation experiments on bare soil plots (10 m2) revealed the overwhelming influence of particle bound P losses compared with P losses in the water phase. Soil P tests, which relate primarily to the dissolved P fractions in soil, were not able to predict total P losses, but were related to reactive P < 0.45 m losses. At the watershed scale soil P tests were able to predict reactive P < 0.45 m losses, but with considerable uncertainty. We conclude that soil P tests, in combination with sediment concentration provide a useful means of assessing the mobilization of P in overland flow, but should not be expected to provide watershed scale predictions of the movement of P into overland flow.

AB - Soil phosphorus tests offer a potentially powerful tool for land managers trying to predict the areas which will contribute diffuse losses of phosphorus (P) to surface water bodies through the overland flow vector - but do they work? We address this question at a range of scales, from patch (< 1 m2), through plot (several m2) to small watershed (several hectares). Our hypothesis is that as we increase the scale, and therefore the complexity of the system, soil P tests will predict P concentrations and losses associated with overland flow less well, and that this is partly due to a shift from dissolved P losses to P losses associated with eroded soil material. At the patch scale soil P tests were used to predict the P concentration and load from 24 European soils exposed to simulated rainfall under controlled conditions in the laboratory. Results showed that soil P tests were generally good predictors of reactive P <0.45 m, but did less well at predicting total P > 0.45 m. By combining the soil P test with measured sediment concentrations predictions of total P concentrations improved. Outdoor rainfall simulation experiments on bare soil plots (10 m2) revealed the overwhelming influence of particle bound P losses compared with P losses in the water phase. Soil P tests, which relate primarily to the dissolved P fractions in soil, were not able to predict total P losses, but were related to reactive P < 0.45 m losses. At the watershed scale soil P tests were able to predict reactive P < 0.45 m losses, but with considerable uncertainty. We conclude that soil P tests, in combination with sediment concentration provide a useful means of assessing the mobilization of P in overland flow, but should not be expected to provide watershed scale predictions of the movement of P into overland flow.

KW - phosphorus tests environment diffuse pollution

U2 - 10.1002/jpln.200321122

DO - 10.1002/jpln.200321122

M3 - Journal article

VL - 166

SP - 432

EP - 437

JO - Journal of Plant Nutrition and Soil Science

JF - Journal of Plant Nutrition and Soil Science

SN - 1436-8730

IS - 4

ER -