2017
DOI: 10.1134/s106422931709006x
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Effect of rainfall intensity and slope steepness on the development of soil erosion in the Southern Cis-Ural region (A model experiment)

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Cited by 23 publications
(15 citation statements)
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“…The slope angles are one of the factors determining soil washout, and the degree of erosion manifestation depends on both the angle and the exposure of the slopes (to a greater extent) [16]. Therefore, it is advisable to form such groups by soil types considering the erosion degree, exposure and slope angles at the same time.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The slope angles are one of the factors determining soil washout, and the degree of erosion manifestation depends on both the angle and the exposure of the slopes (to a greater extent) [16]. Therefore, it is advisable to form such groups by soil types considering the erosion degree, exposure and slope angles at the same time.…”
Section: Resultsmentioning
confidence: 99%
“…The relationship between the agrochemical parameters of the soil and its soil erosion characteristics has been studied by many scientists for a long time [5][6][7][8][9][10][11][12][13][14][15][16]. However, automatic processing of agrochemical and soil erosion monitoring data is associated with certain difficulties.…”
Section: Introductionmentioning
confidence: 99%
“…e larger the slope is, the faster the runoff speed is and the greater the rainfall erosion is. e greater the slope is, the greater the influence of rainfall on slope erosion is [9][10][11][12]. When the slope gradient exceeds a certain value, the rainfall erosion of the embankment is inversely proportional to it.…”
Section: Introductionmentioning
confidence: 99%
“…The process of soil erosion is influenced by various factors including rainfall characteristics [18][19][20], topographic conditions [21,22], soil properties [23][24][25], farming methods [8,26], and vegetation cover [27,28], among which rainfall intensity (RI) and slope steepness (SS) have been widely studied and are still the focus of research [29][30][31]. For example, Sobol et al [32] investigated the effects of rainfall intensity and slope steepness on the development of soil erosion in the southern Cis-Ural region, finding that soil loss linearly depended on these two factors, and that the clay content was higher in eroded material than in the original soils. Dai et al [33] conducted field runoff plot-monitoring tests to reveal the plot-scale characteristics of surface soil erosion in the karst rocky desertification regions.…”
Section: Introductionmentioning
confidence: 99%