2009
DOI: 10.1016/j.jconhyd.2008.09.001
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Numerical analysis of water and solute transport in variably-saturated fractured clayey till

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Cited by 36 publications
(33 citation statements)
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“…Monitoring began at the Tylstrup, Jyndevad and Faardrup fields in 1999 and at the Silstrup and Estrup fields in 2000 (Table 1). The three loamy fields are characterized by preferential transport through macropores (biopores, fractures) in a low permeable soil matrix (Rosenbom et al, 2009b), while other forms of preferential transport in the soil matrix may be found in the sandy fields (Rosenbom et al, 2009a). These hydraulic conditions result in groundwater table fluctuations exceeding 2.5 m in the loamy fields and being less than 2 m in the sandy fields.…”
Section: Selection Of the Five Fieldsmentioning
confidence: 99%
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“…Monitoring began at the Tylstrup, Jyndevad and Faardrup fields in 1999 and at the Silstrup and Estrup fields in 2000 (Table 1). The three loamy fields are characterized by preferential transport through macropores (biopores, fractures) in a low permeable soil matrix (Rosenbom et al, 2009b), while other forms of preferential transport in the soil matrix may be found in the sandy fields (Rosenbom et al, 2009a). These hydraulic conditions result in groundwater table fluctuations exceeding 2.5 m in the loamy fields and being less than 2 m in the sandy fields.…”
Section: Selection Of the Five Fieldsmentioning
confidence: 99%
“…It is well documented (Aschonitis and Antonopoulos, 2013) that the effective porosity in loamy soil corresponding to connected discontinuities, such as wormholes and fractures, is low compared to that of sandy soil, with the result that climatic conditions have a greater impact on the pore system. The consequences are: (i) immediate response to a precipitation or snowmelt event causing rapid flow and transport through discontinuities (Rosenbom et al, 2008(Rosenbom et al, , 2009bVryzas et al, 2012), which may sometimes be directly connected to drains (Nielsen, 2010); and (ii) seasonal fluctuations of up to 4 m in the groundwater table with resultant drainage, primarily in periods when the groundwater table is located above the drains (above 1.1e1.2 m b.g.s.). This very dynamic hydrogeological setting enables a larger variety of pesticides and their degradation products to reach groundwater in intense pulses, before being diluted or retarded to varying degrees.…”
Section: Impact Of Fate Processes and Hydrogeological Setting On Leacmentioning
confidence: 99%
“…The flow velocities in the discontinuities are determined by the commonly used cubic law [7]. Retention and relative permeability curves for both the fractures and the matrix can be expressed from van Genuchten's function [8] or can be specified in a tabular form. In the model, the porous medium is discretized with 3D finite elements and fractures are discretized with 2D finite elements.…”
Section: Hydro-geosphere Codementioning
confidence: 99%
“…The applied HydroGeoSphere model (Therrien et al, 2006) is a non-commercial code available to the interested user under http://hydrogeosphere.org/. The model has been extensively used for various studies involving dual porosities such as Mclaren et al (2000), Rosenbom et al (2009) and Schwartz et al (2010). The governing equation in the applied model is the Richards equation (Richards, 1931), which is slightly modified to account for inter-continuum water exchange:…”
Section: Modeling Approachmentioning
confidence: 99%