2021
DOI: 10.1016/j.envpol.2021.117822
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Impact of fate properties, groundwater fluctuations and the presence of worm burrows on pesticide leaching assessments through golf areas

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Cited by 5 publications
(2 citation statements)
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“…The boundary condition, bgrad, being among the parameters with the largest contribution to the prediction uncertainty, controls the percolation out of the model domain (Equation 7). Obviously, the boundary conditions can affect the simulation results and as shown by, for example, Karan et al (2021) the choice in lower boundary condition may affect simulated concentrations, especially when estimating concentrations at or near the boundary. It was evident that the information content in the available observation data was sufficient to constrain bgrad as seen from the identifiability that was dominated by low singular value indices (Figure S2A in Supporting Information S1).…”
Section: Parameter Contribution To Prediction Uncertaintymentioning
confidence: 99%
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“…The boundary condition, bgrad, being among the parameters with the largest contribution to the prediction uncertainty, controls the percolation out of the model domain (Equation 7). Obviously, the boundary conditions can affect the simulation results and as shown by, for example, Karan et al (2021) the choice in lower boundary condition may affect simulated concentrations, especially when estimating concentrations at or near the boundary. It was evident that the information content in the available observation data was sufficient to constrain bgrad as seen from the identifiability that was dominated by low singular value indices (Figure S2A in Supporting Information S1).…”
Section: Parameter Contribution To Prediction Uncertaintymentioning
confidence: 99%
“…Models are needed to quantify these fluxes, however, the inherent complexity of subsurface processes presents substantial challenges for numerical modeling and associated predictions (e.g., Beven, 2018;Gassmann, 2021), particularly in clay till settings characterized by preferential flows (Badawi et al, 2023;Villholth & Jensen, 1998). The presence of preferential flow pathways, such as macropores and root channels, creates a heterogeneous and non-uniform water content, leading to faster solute transport with less likelihood for degradation and thus potential for contamination of groundwater resources (Badawi et al, 2023;Brown et al, 2000;Karan et al, 2021;Nimmo, 2012;Rosenbom et al, 2014). A major challenge in numerical modeling of the variably saturated zone in settings with preferential flow paths is a lack of data to constrain the models adequately (N. Jarvis et al, 2007;Šimůnek et al, 2003).…”
Section: Introductionmentioning
confidence: 99%