Dynamics of Various Size Particle Distribution in Slope Washout Products
DOI:
https://doi.org/10.52575/2712-7443-2024-48-4-515-525Keywords:
soil erosion, granulometry, experiment, slope, sprinkling, soils, groundAbstract
The article interprets the results of the analysis of soil washout product granulometric composition. The problem is considered within the framework of constructing a theoretical model of sediment movement by surface runoff. During the study, the granulometric composition of sediments formed by the method of full-scale experiment at the test site was compared to that of the material on the slope in its natural state, which shows surface runoff only. It is shown that in the conditions of a full-scale experiment, on a site composed of sandy material, the proportion of larger fractions increases towards the bottom. On the slope of a complex structure in its natural state, there are no pronounced patterns in the change in the granulometric composition of sediments. It is assumed that deluvium fraction distribution patterns that are characteristic of slopes with a homogeneous composition are smoothed by the arrival of eluvial material which is heterogeneous in terms of composition and erosion resistance.
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Hairsine P.B, Sander G.C., Rose C.W., Parlange J.-Y., Hogarth W.L., Lisle I., Rouhipour H. 1999. Unsteady Soil Erosion Due to Rainfall Impact: a Model of Sediment Sorting on the Hillslope. Journal of Hydrology, 220(3–4): 115–128. https://doi.org/10.1016/S0022-1694(99)00068-2
Issa O.M., Bissonnais Y.L., Planchon O., Favis-Mortlock D., Silvera N., Wainwright J. 2006. Soil Detachment and Transport on Field- and Laboratory-Scale Interrill Areas: Erosion Processes and the Size-Selectivity of Eroded Sediment. Earth Surface Processes and Landforms, 31(8): 929–939.
Kinnell P.I.A. 2020. The Influence of Time and Other Factors on Soil Loss Produced by Rain-Impacted Flow Under Artificial Rainfall. Journal of Hydrology, 587: 125004. https://doi.org/10.1016/j.jhydrol.2020.125004
Lin J., Huang Y., Zhao G., Jiang F., Wang M.-K., Ge H. 2017. Flow-Driven Soil Erosion Processes and the Size Selectivity of Eroded Sediment on Steep Slopes Using Colluvial Deposits in a Permanent Gully. Catena, 157: 47–57. https://doi.org/10.1016/j.catena.2017.05.015
Neal T.H. 1938. Effect of Degree of Slope and Rainfall Characteristics on Runoff and Soil Erosion. Agricultural Engeneering. Research Bulletin, 280: 45 p.
Rienzi E.A., Fox J.F., Grove J.H., Matocha C.J. 2013. Interrill Erosion in Soils with Different Land Uses: The Kinetic Energy Wetting Effect on Temporal Particle Size Distribution. Catena, 107: 130–138. https://doi.org/10.1016/j.catena.2013.02.007
Zhang P., Yao W., Liu G., Xiao P., Sun W. 2020. Experimental Study of Sediment Transport Processes and Size Selectivity of Eroded Sediment on Steep Pisha Sandstone Slopes. Geomorphology, 363: 107211. https://doi.org/10.1016/j.geomorph.2020.107211
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