2006
DOI: 10.1002/hyp.6190
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Incremental distributed modelling investigation in a small agricultural catchment: 2. Erosion and phosphorus transport

Abstract: Abstract:Distributed physically based erosion and phosphorus (P) transport models, run by the overland flow model described in Taskinen and Bruen (2006. Hydrological Processes 21(1)), are described. In the erosion model, the additional components to the basic model were the outflow of the particles by infiltration and a new model component, i.e. deposition when rainfall stops. Two ways of calculating the shielding factor due to the flow depth were compared. The P transport model had both dissolved P (DP) and p… Show more

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Cited by 10 publications
(3 citation statements)
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“…The same models that were best in the calibration also worked best in the verification. The fully distributed model provides a potential method for running water-quality models and testing their different processes in similar catchments and conditions, since, for example, taking into account spatial variation of slope, flow depth and velocity and different flow routes is enabled (see Nasr et al (2005) and Taskinen and Bruen (2006)). …”
Section: Discussionmentioning
confidence: 99%
“…The same models that were best in the calibration also worked best in the verification. The fully distributed model provides a potential method for running water-quality models and testing their different processes in similar catchments and conditions, since, for example, taking into account spatial variation of slope, flow depth and velocity and different flow routes is enabled (see Nasr et al (2005) and Taskinen and Bruen (2006)). …”
Section: Discussionmentioning
confidence: 99%
“…However, detachment by rainfall impact often occurs when there is little or no flow available for transport. Major factors that affect raindrop detachment are rainfall characteristics, soil characteristics, ground and canopy cover, and surface water depth (Taskinen and Bruen 2007).…”
Section: Upland Erosionmentioning
confidence: 99%
“…Where sediment is a carrier, P transfer from land to water involves three connected processes: hydrology, sediment dynamics, and P dynamics (Hutchins et al, 2002). Mathematical models describing event dynamics of P transfer usually conceptualize these compartments with a high degree of complexity, ranging from spatially semi‐distributed models with a process‐based conceptualization of each compartment (e.g., Hutchins et al, 2002) to spatially distributed models where processes are derived from small‐scale physical principles (e.g., Taskinen and Bruen, 2007). However, the compartments of these models have rarely been tested individually and usually do not include estimates of uncertainties in data and models.…”
mentioning
confidence: 99%