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Scaling up the phosphorus signal from soil hillslopes to headwater catchments

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Scaling up the phosphorus signal from soil hillslopes to headwater catchments. / Haygarth, P. M.; Page, T. J. C.; Beven, K. J. et al.
In: Freshwater Biology, Vol. 57, No. s1, 07.2012, p. 7-25.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Haygarth, PM, Page, TJC, Beven, KJ, Freer, J, Joynes, A, Butler, P, Wood, GA & Owens, PN 2012, 'Scaling up the phosphorus signal from soil hillslopes to headwater catchments', Freshwater Biology, vol. 57, no. s1, pp. 7-25. https://doi.org/10.1111/j.1365-2427.2012.02748.x

APA

Vancouver

Haygarth PM, Page TJC, Beven KJ, Freer J, Joynes A, Butler P et al. Scaling up the phosphorus signal from soil hillslopes to headwater catchments. Freshwater Biology. 2012 Jul;57(s1):7-25. doi: 10.1111/j.1365-2427.2012.02748.x

Author

Bibtex

@article{7694398911754774bb52ac7c52bab002,
title = "Scaling up the phosphorus signal from soil hillslopes to headwater catchments",
abstract = "1. Phosphorus (P) transfer from agricultural land to freshwater systems has been studied across many scales and environmental compartments that range from understanding biogeochemical processes in soils and fields, to assessment of localised in-stream biotic and ecological impacts. 2. This study tackles the challenges of scale when moving from soil hillslope to headwater catchment scale. The focus is on process rules derived from reductionist approaches at the relatively fine scale, and exploring the signal and evidence thereof at the headwater catchment scale. 3. The methodology uses new data of P dynamics in agricultural grassland headwater catchments in south-west England. 4. We found the following: (i) it was not possible to disaggregate an influence of soil (Olsen) P concentration on P export at the larger scale; (ii) there was no clear temporally dynamic relationship between P additions of fertiliser and recycled manure and the resulting P transferred to the headwater scale; however, (iii) ploughing, digging of stream channel and leakage from farm storage all affected the temporal concentration dynamics; and (iv) overall P loss was influenced by higher long-term history of P inputs, livestock and the domination of hydrologic processes. 5. It is concluded that process rules derived at the finer soil or plot scale cannot always produce a clearly discernable signal when studied at the larger headwater catchment scale.",
keywords = "UNCERTAINTIES, continuum, PATHWAYS, catchment, Phosphorus, EVENT DYNAMICS, UK, GRAZED GRASSLAND LYSIMETERS, HEREFORDSHIRE, run-off, VARIABILITY, WATER-QUALITY, SEDIMENT CONCENTRATION, SUSPENDED SEDIMENT, uncertainty",
author = "Haygarth, {P. M.} and Page, {T. J. C.} and Beven, {K. J.} and J. Freer and A. Joynes and P. Butler and Wood, {G. A.} and Owens, {P. N.}",
year = "2012",
month = jul,
doi = "10.1111/j.1365-2427.2012.02748.x",
language = "English",
volume = "57",
pages = "7--25",
journal = "Freshwater Biology",
issn = "0046-5070",
publisher = "Blackwell Publishing Ltd",
number = "s1",

}

RIS

TY - JOUR

T1 - Scaling up the phosphorus signal from soil hillslopes to headwater catchments

AU - Haygarth, P. M.

AU - Page, T. J. C.

AU - Beven, K. J.

AU - Freer, J.

AU - Joynes, A.

AU - Butler, P.

AU - Wood, G. A.

AU - Owens, P. N.

PY - 2012/7

Y1 - 2012/7

N2 - 1. Phosphorus (P) transfer from agricultural land to freshwater systems has been studied across many scales and environmental compartments that range from understanding biogeochemical processes in soils and fields, to assessment of localised in-stream biotic and ecological impacts. 2. This study tackles the challenges of scale when moving from soil hillslope to headwater catchment scale. The focus is on process rules derived from reductionist approaches at the relatively fine scale, and exploring the signal and evidence thereof at the headwater catchment scale. 3. The methodology uses new data of P dynamics in agricultural grassland headwater catchments in south-west England. 4. We found the following: (i) it was not possible to disaggregate an influence of soil (Olsen) P concentration on P export at the larger scale; (ii) there was no clear temporally dynamic relationship between P additions of fertiliser and recycled manure and the resulting P transferred to the headwater scale; however, (iii) ploughing, digging of stream channel and leakage from farm storage all affected the temporal concentration dynamics; and (iv) overall P loss was influenced by higher long-term history of P inputs, livestock and the domination of hydrologic processes. 5. It is concluded that process rules derived at the finer soil or plot scale cannot always produce a clearly discernable signal when studied at the larger headwater catchment scale.

AB - 1. Phosphorus (P) transfer from agricultural land to freshwater systems has been studied across many scales and environmental compartments that range from understanding biogeochemical processes in soils and fields, to assessment of localised in-stream biotic and ecological impacts. 2. This study tackles the challenges of scale when moving from soil hillslope to headwater catchment scale. The focus is on process rules derived from reductionist approaches at the relatively fine scale, and exploring the signal and evidence thereof at the headwater catchment scale. 3. The methodology uses new data of P dynamics in agricultural grassland headwater catchments in south-west England. 4. We found the following: (i) it was not possible to disaggregate an influence of soil (Olsen) P concentration on P export at the larger scale; (ii) there was no clear temporally dynamic relationship between P additions of fertiliser and recycled manure and the resulting P transferred to the headwater scale; however, (iii) ploughing, digging of stream channel and leakage from farm storage all affected the temporal concentration dynamics; and (iv) overall P loss was influenced by higher long-term history of P inputs, livestock and the domination of hydrologic processes. 5. It is concluded that process rules derived at the finer soil or plot scale cannot always produce a clearly discernable signal when studied at the larger headwater catchment scale.

KW - UNCERTAINTIES

KW - continuum

KW - PATHWAYS

KW - catchment

KW - Phosphorus

KW - EVENT DYNAMICS

KW - UK

KW - GRAZED GRASSLAND LYSIMETERS

KW - HEREFORDSHIRE

KW - run-off

KW - VARIABILITY

KW - WATER-QUALITY

KW - SEDIMENT CONCENTRATION

KW - SUSPENDED SEDIMENT

KW - uncertainty

UR - http://www.scopus.com/inward/record.url?scp=84862660914&partnerID=8YFLogxK

U2 - 10.1111/j.1365-2427.2012.02748.x

DO - 10.1111/j.1365-2427.2012.02748.x

M3 - Journal article

VL - 57

SP - 7

EP - 25

JO - Freshwater Biology

JF - Freshwater Biology

SN - 0046-5070

IS - s1

ER -