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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 3
Hydrol. Earth Syst. Sci., 17, 1003–1019, 2013
https://doi.org/10.5194/hess-17-1003-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Groundwater recharge: processes and quantification

Hydrol. Earth Syst. Sci., 17, 1003–1019, 2013
https://doi.org/10.5194/hess-17-1003-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Mar 2013

Research article | 07 Mar 2013

Linking soil moisture balance and source-responsive models to estimate diffuse and preferential components of groundwater recharge

M. O. Cuthbert1,*, R. Mackay2, and J. R. Nimmo3 M. O. Cuthbert et al.
  • 1Water Sciences Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
  • 2Geotechnical and Hydrogeological Engineering Research Group, Monash University, Churchill, Victoria, Australia
  • 3US Geological Survey, Menlo Park, California, USA
  • *present address: Water Research Laboratory, School of Civil and Environmental Engineering, University of New South Wales, 110 King St, Manly Vale, NSW, 2093, Australia

Abstract. Results are presented of a detailed study into the vadose zone and shallow water table hydrodynamics of a field site in Shropshire, UK. A conceptual model is presented and tested using a range of numerical models, including a modified soil moisture balance model (SMBM) for estimating groundwater recharge in the presence of both diffuse and preferential flow components. Tensiometry reveals that the loamy sand topsoil wets up via preferential flow and subsequent redistribution of moisture into the soil matrix. Recharge does not occur until near-positive pressures are achieved at the top of the sandy glaciofluvial outwash material that underlies the topsoil, about 1 m above the water table. Once this occurs, very rapid water table rises follow. This threshold behaviour is attributed to the vertical discontinuity in preferential flow pathways due to seasonal ploughing of the topsoil and to a lower permeability plough/iron pan restricting matrix flow between the topsoil and the lower outwash deposits. Although the wetting process in the topsoil is complex, a SMBM is shown to be effective in predicting the initiation of preferential flow from the base of the topsoil into the lower outwash horizon. The rapidity of the response at the water table and a water table rise during the summer period while flow gradients in the unsaturated profile were upward suggest that preferential flow is also occurring within the outwash deposits below the topsoil. A variation of the source-responsive model proposed by Nimmo (2010) is shown to reproduce the observed water table dynamics well in the lower outwash horizon when linked to a SMBM that quantifies the potential recharge from the topsoil. The results reveal new insights into preferential flow processes in cultivated soils and provide a useful and practical approach to accounting for preferential flow in studies of groundwater recharge estimation.

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