Effect of rainfall intensity and slope steepness on the development of soil erosion in the Southern Cis-Ural region (A model experiment)

• Published in: Eurasian soil science 2017-09, Vol.50 (9), p.1098-1104
• Main Authors: Sobol, N. V., Gabbasova, I. M., Komissarov, M. A.
• Format: Article
• Language: English
• Subjects: Calcareous soils; Clay; Clay soils; Computer simulation; Conservation of Soils; Decomposing organic matter; Degradation; Duration; Earth and Environmental Science; Earth Sciences; Entrapment; Erosion; Erosion resistance; Geotechnical Engineering & Applied Earth Sciences; Humus; Inclination; Rain; Rain and rainfall; Rainfall; Rainfall intensity; Regions; Rehabilitation; Runoff; Silt; Slope; Slope stability; Slopes; Soil; Soil erosion; Soil resistance; Tillage; Vegetation type
• ISSN: 1064-2293; 1556-195X
• DOI: 10.1134/S106422931709006X

The effect of rainfall intensity on the erosion of residual calcareous agrogray soils and clay-illuvial agrochernozems in the Southern Cis-Ural region on slopes of different inclination and vegetation type has been studied by simulating with a small-size sprinkler. It has been shown that soil loss linearly depends on rainfall intensity (2, 4, and 6 mm/min) and slope inclination (3° and 7°). When the rainfall intensity and duration, and the slope inclination increase, soil loss by erosion from agrogray soils increases higher than from agrochernozems. On the plowland with a slope of 3°, runoff begins 12, 10, and 5 min, on the average, after the beginning of rains at these intensities. When the slope increases to 7°, runoff begins earlier by 7, 6, and 4 min, respectively. After the beginning of runoff and with its increase by 1 mm, the soil loss from slopes of 3° and 7° reaches 4.2 and 25.7 t/ha on agrogray soils and 1.4 and 4.7 t/ha on agrochernozems, respectively. Fallow soils have higher erosion resistance, and the soil loss little depends on the slope gradient: it gradually increases to 0.3–1.0 t/ha per 1 mm of runoff with increasing rainfall intensity and duration. The content of physical clay in eroded material is higher than in the original soils. Fine fractions prevail in this material, which increases their humus content. The increase in rainfall intensity and duration to 4 and 6 mm/min results in the entrapment of coarse silt and sand by runoff.