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The effect of hedgerow wild-margins on topsoil hydraulic properties, and overland-flow incidence, magnitude and water-quality

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The effect of hedgerow wild-margins on topsoil hydraulic properties, and overland-flow incidence, magnitude and water-quality. / Wallace, E.E.; McShane, G.; Tych, W. et al.
In: Hydrological Processes, Vol. 35, No. 3, e14098, 31.03.2021.

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@article{1a588c49d5764d5988b0e034b4ea6dad,
title = "The effect of hedgerow wild-margins on topsoil hydraulic properties, and overland-flow incidence, magnitude and water-quality",
abstract = "Overland and shallow-subsurface flows from agricultural catchments are believed to contribute towards flood-risk and water-quality degradation across the globe. Hedgerows are commonplace agricultural features that may disrupt these rapid hydrological pathways. Research into the hydrological functioning of hedgerows is very limited however, with no field-based quantitative comparison of overland-flows within hedgerows versus other land-uses. This research is the first globally to observe changes in overland-flow incidence, volume and water-quality, alongside topsoil hydraulic and physico-chemical properties, induced by a hedgerow and adjoining wild-margin within a grassland landscape. Observations were conducted within two replicated paired-plots between a hedgerow wild-margin and a bordering pasture, within Cumbria, UK. Compared to adjacent pasture, hedge-margins significantly reduced topsoil dry bulk-density and increased porosity, and significantly increased the topsoil median permeability by a factor of 22–27. Overland-flow models, based on direct observations, highlight that hedge-margins are slower to produce overland-flows than pastures, requiring an equal or greater amount of saturation before the onset of overland-flow generation. Hedge-margins resultantly produced less overland-flow volume, likely due to increased infiltration, percolation and/or evapotranspiration. Soil saturation models, also based on direct observations, confirm pastures saturate faster than hedge-margins, with hedge-margins having extremely variable dynamics in relation to precipitation, whereas pastures have more moderate and consistent dynamics. Overland-flow water-quality from {\textquoteleft}wash-off{\textquoteright} experiments highlight that hedge-margins may store substantially more nitrate (70–260%), nitrate-nitrite (640–650%), and loose sediment (540–3970%) on the ground surface compared to pastures; although further experimentation is needed to determine contaminant mobilization potential. ",
keywords = "grassland hydrology, hedgerow hydrology, natural flood-risk management, overland-flow, rainfall-runoff processes, transfer-function modelling, Agricultural robots, Agriculture, Catchments, Floods, Land use, Nitrates, Solvents, Water quality, Agricultural catchments, Direct observations, Dry bulk densities, Hydraulic properties, Mobilization potential, Quantitative comparison, Shallow subsurface, Water quality degradation, Wooden fences, flood, grassland, hedgerow, hydraulic property, overland flow, rainfall-runoff modeling, topsoil, water quality, Cumbria, England, United Kingdom",
author = "E.E. Wallace and G. McShane and W. Tych and A. Kretzschmar and T. McCann and N.A. Chappell",
year = "2021",
month = mar,
day = "31",
doi = "10.1002/hyp.14098",
language = "English",
volume = "35",
journal = "Hydrological Processes",
issn = "0885-6087",
publisher = "John Wiley and Sons Ltd",
number = "3",

}

RIS

TY - JOUR

T1 - The effect of hedgerow wild-margins on topsoil hydraulic properties, and overland-flow incidence, magnitude and water-quality

AU - Wallace, E.E.

AU - McShane, G.

AU - Tych, W.

AU - Kretzschmar, A.

AU - McCann, T.

AU - Chappell, N.A.

PY - 2021/3/31

Y1 - 2021/3/31

N2 - Overland and shallow-subsurface flows from agricultural catchments are believed to contribute towards flood-risk and water-quality degradation across the globe. Hedgerows are commonplace agricultural features that may disrupt these rapid hydrological pathways. Research into the hydrological functioning of hedgerows is very limited however, with no field-based quantitative comparison of overland-flows within hedgerows versus other land-uses. This research is the first globally to observe changes in overland-flow incidence, volume and water-quality, alongside topsoil hydraulic and physico-chemical properties, induced by a hedgerow and adjoining wild-margin within a grassland landscape. Observations were conducted within two replicated paired-plots between a hedgerow wild-margin and a bordering pasture, within Cumbria, UK. Compared to adjacent pasture, hedge-margins significantly reduced topsoil dry bulk-density and increased porosity, and significantly increased the topsoil median permeability by a factor of 22–27. Overland-flow models, based on direct observations, highlight that hedge-margins are slower to produce overland-flows than pastures, requiring an equal or greater amount of saturation before the onset of overland-flow generation. Hedge-margins resultantly produced less overland-flow volume, likely due to increased infiltration, percolation and/or evapotranspiration. Soil saturation models, also based on direct observations, confirm pastures saturate faster than hedge-margins, with hedge-margins having extremely variable dynamics in relation to precipitation, whereas pastures have more moderate and consistent dynamics. Overland-flow water-quality from ‘wash-off’ experiments highlight that hedge-margins may store substantially more nitrate (70–260%), nitrate-nitrite (640–650%), and loose sediment (540–3970%) on the ground surface compared to pastures; although further experimentation is needed to determine contaminant mobilization potential. 

AB - Overland and shallow-subsurface flows from agricultural catchments are believed to contribute towards flood-risk and water-quality degradation across the globe. Hedgerows are commonplace agricultural features that may disrupt these rapid hydrological pathways. Research into the hydrological functioning of hedgerows is very limited however, with no field-based quantitative comparison of overland-flows within hedgerows versus other land-uses. This research is the first globally to observe changes in overland-flow incidence, volume and water-quality, alongside topsoil hydraulic and physico-chemical properties, induced by a hedgerow and adjoining wild-margin within a grassland landscape. Observations were conducted within two replicated paired-plots between a hedgerow wild-margin and a bordering pasture, within Cumbria, UK. Compared to adjacent pasture, hedge-margins significantly reduced topsoil dry bulk-density and increased porosity, and significantly increased the topsoil median permeability by a factor of 22–27. Overland-flow models, based on direct observations, highlight that hedge-margins are slower to produce overland-flows than pastures, requiring an equal or greater amount of saturation before the onset of overland-flow generation. Hedge-margins resultantly produced less overland-flow volume, likely due to increased infiltration, percolation and/or evapotranspiration. Soil saturation models, also based on direct observations, confirm pastures saturate faster than hedge-margins, with hedge-margins having extremely variable dynamics in relation to precipitation, whereas pastures have more moderate and consistent dynamics. Overland-flow water-quality from ‘wash-off’ experiments highlight that hedge-margins may store substantially more nitrate (70–260%), nitrate-nitrite (640–650%), and loose sediment (540–3970%) on the ground surface compared to pastures; although further experimentation is needed to determine contaminant mobilization potential. 

KW - grassland hydrology

KW - hedgerow hydrology

KW - natural flood-risk management

KW - overland-flow

KW - rainfall-runoff processes

KW - transfer-function modelling

KW - Agricultural robots

KW - Agriculture

KW - Catchments

KW - Floods

KW - Land use

KW - Nitrates

KW - Solvents

KW - Water quality

KW - Agricultural catchments

KW - Direct observations

KW - Dry bulk densities

KW - Hydraulic properties

KW - Mobilization potential

KW - Quantitative comparison

KW - Shallow subsurface

KW - Water quality degradation

KW - Wooden fences

KW - flood

KW - grassland

KW - hedgerow

KW - hydraulic property

KW - overland flow

KW - rainfall-runoff modeling

KW - topsoil

KW - water quality

KW - Cumbria

KW - England

KW - United Kingdom

U2 - 10.1002/hyp.14098

DO - 10.1002/hyp.14098

M3 - Journal article

VL - 35

JO - Hydrological Processes

JF - Hydrological Processes

SN - 0885-6087

IS - 3

M1 - e14098

ER -