Rights statement: ©2011. American Geophysical Union. All Rights Reserved.
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Research output: Contribution to Journal/Magazine › Journal article › peer-review
Modeling the dynamics of soil erosion and size-selective sediment transport over nonuniform topography in flume-scale experiments. / Heng, B. C. P.; Sander, G. C.; Armstrong, A. et al.
In: Water Resources Research, Vol. 47, No. 2, W02513, 10.02.2011.Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - Modeling the dynamics of soil erosion and size-selective sediment transport over nonuniform topography in flume-scale experiments
AU - Heng, B. C. P.
AU - Sander, G. C.
AU - Armstrong, A.
AU - Quinton, John
AU - Chandler, J. H.
AU - Scott, C. F.
N1 - 721BQ Times Cited:1 Cited References Count:51 ©2011. American Geophysical Union. All Rights Reserved.
PY - 2011/2/10
Y1 - 2011/2/10
N2 - Soil erosion and the associated nutrient fluxes can lead to severe degradation of surface waters. Given that both sediment transport and nutrient sorption are size selective, it is important to predict the particle size distribution (PSD) as well as the total amount of sediment being eroded. In this paper, a finite volume implementation of the Hairsine-Rose soil erosion model is used to simulate flume-scale experiments with detailed observations of soil erosion and sediment transport dynamics. The numerical implementation allows us to account for the effects of soil surface microtopography (measured using close range photogrammetry) on soil erosion. An in-depth discussion of the model parameters and the constraints is presented. The model reproduces the dynamics of sediment concentration and PSD well, although some discrepancies can be observed. The calibrated parameters are also consistent with independent data in the literature and physical reason. Spatial variations in the suspended and deposited sediment and an analysis of model sensitivity highlight the value of collecting distributed data for a more robust validation of the model and to enhance parametric determinacy. The related issues of spatial resolution and scale in erosion prediction are briefly discussed.
AB - Soil erosion and the associated nutrient fluxes can lead to severe degradation of surface waters. Given that both sediment transport and nutrient sorption are size selective, it is important to predict the particle size distribution (PSD) as well as the total amount of sediment being eroded. In this paper, a finite volume implementation of the Hairsine-Rose soil erosion model is used to simulate flume-scale experiments with detailed observations of soil erosion and sediment transport dynamics. The numerical implementation allows us to account for the effects of soil surface microtopography (measured using close range photogrammetry) on soil erosion. An in-depth discussion of the model parameters and the constraints is presented. The model reproduces the dynamics of sediment concentration and PSD well, although some discrepancies can be observed. The calibrated parameters are also consistent with independent data in the literature and physical reason. Spatial variations in the suspended and deposited sediment and an analysis of model sensitivity highlight the value of collecting distributed data for a more robust validation of the model and to enhance parametric determinacy. The related issues of spatial resolution and scale in erosion prediction are briefly discussed.
KW - Soil erosion
KW - particle size distribution
KW - microtopography
KW - Model calibration
KW - sediment transport
UR - http://www.scopus.com/inward/record.url?scp=79951806387&partnerID=8YFLogxK
U2 - 10.1029/2010wr009375
DO - 10.1029/2010wr009375
M3 - Journal article
VL - 47
JO - Water Resources Research
JF - Water Resources Research
SN - 0043-1397
IS - 2
M1 - W02513
ER -