Flow paths and phosphorus transfer pathways in two agricultural streams with contrasting flow controls

P.-E. Mellander, P. Jordan, M. Shore, A.R. Melland, G. Shortle

Research output: Contribution to journalArticle

32 Citations (Scopus)

Abstract

In this paper we analyze four years of data from simultaneous high-frequency monitoring of streamflow and phosphorus (P) concentration. This was to investigate hydrolological flow paths and P transfer pathways from diffuse sources in two intensively farmed river catchments (ca. 10km2) with contrasting flow controls and dominating flow paths. Catchment scale P loss was viewed on an annual and event flow basis and related to hydrological flow paths. A grassland catchment with mostly poorly drained soils, and a higher Q10:Q90 ratio (60 compared to 24), had three times higher annual P loss than an arable catchment with mostly well-drained soils (1.04kg TP ha-1 compared to 0.34 kg TP ha-1) despite the arable catchment having larger areas with high soil P status and more discharge. Neither of the catchments indicated supply limitations. The magnitude of the P losses from the two catchments were not defined by land use, source pressure or discharge volume, but rather by more basic rainfall-to-runoff partitioning influences that determine proportions of quickflow and slowflow. There were larger differences between the years than between the catchments and the P loss of the arable catchment appeared more sensitive to climate. The results confirmed the need to manage the quickflow components of runoff to moderate P transfers. In order to further reduce diffuse pollution it may, therefore, be necessary to account for the contrast in hydrological function before or in addition to any of the other factors known to influence P losses from catchments (such as soil P and land use). Schemes designed to attenuate diffuse P after mobilization from soil surfaces can then be targeted (and resourced) more effectively.
LanguageEnglish
Pages3504-3518
JournalHydrological Processes
Volume29
DOIs
Publication statusPublished - 20 Jul 2015

Fingerprint

flow control
catchment
phosphorus
soil
runoff
land use
baseflow
mobilization
streamflow
soil surface
partitioning
grassland
loss
well
rainfall

Keywords

  • diffuse pollution
  • agriculture
  • eutrophication
  • high-frequency water quality monitoring
  • nutrient management
  • climate

Cite this

Mellander, P.-E. ; Jordan, P. ; Shore, M. ; Melland, A.R. ; Shortle, G. / Flow paths and phosphorus transfer pathways in two agricultural streams with contrasting flow controls. In: Hydrological Processes. 2015 ; Vol. 29. pp. 3504-3518.
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Flow paths and phosphorus transfer pathways in two agricultural streams with contrasting flow controls. / Mellander, P.-E.; Jordan, P.; Shore, M.; Melland, A.R.; Shortle, G.

In: Hydrological Processes, Vol. 29, 20.07.2015, p. 3504-3518.

Research output: Contribution to journalArticle

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T1 - Flow paths and phosphorus transfer pathways in two agricultural streams with contrasting flow controls

AU - Mellander, P.-E.

AU - Jordan, P.

AU - Shore, M.

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AB - In this paper we analyze four years of data from simultaneous high-frequency monitoring of streamflow and phosphorus (P) concentration. This was to investigate hydrolological flow paths and P transfer pathways from diffuse sources in two intensively farmed river catchments (ca. 10km2) with contrasting flow controls and dominating flow paths. Catchment scale P loss was viewed on an annual and event flow basis and related to hydrological flow paths. A grassland catchment with mostly poorly drained soils, and a higher Q10:Q90 ratio (60 compared to 24), had three times higher annual P loss than an arable catchment with mostly well-drained soils (1.04kg TP ha-1 compared to 0.34 kg TP ha-1) despite the arable catchment having larger areas with high soil P status and more discharge. Neither of the catchments indicated supply limitations. The magnitude of the P losses from the two catchments were not defined by land use, source pressure or discharge volume, but rather by more basic rainfall-to-runoff partitioning influences that determine proportions of quickflow and slowflow. There were larger differences between the years than between the catchments and the P loss of the arable catchment appeared more sensitive to climate. The results confirmed the need to manage the quickflow components of runoff to moderate P transfers. In order to further reduce diffuse pollution it may, therefore, be necessary to account for the contrast in hydrological function before or in addition to any of the other factors known to influence P losses from catchments (such as soil P and land use). Schemes designed to attenuate diffuse P after mobilization from soil surfaces can then be targeted (and resourced) more effectively.

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KW - agriculture

KW - eutrophication

KW - high-frequency water quality monitoring

KW - nutrient management

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SN - 0885-6087

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