Statistical and physical analysis of soil detachment by raindrop impact: Rain erosivity indices and threshold energy

Laboratory experiments have been conducted to study the effects of various simulated rain properties on soil detachment due to raindrop impact. Two so il materials were tested: a fine sand and a silt loam. The mass of detached sediment was measured with the splash cup technique. The splash cups fille d with soil material were exposed to simulated rain intensities ranging bet ween 10 and 140 mm h-l. The detached sediment was collected and weighed, wh ereas rain intensity, drop diameter, and fall velocity of each raindrop wer e measured with an optical spectropluviometer. A statistical analysis has b een made in order to evaluate which rain parameter best predicts the splash detachment rate. Linear fits between the rate of detached sediment and the product of drop size (D) and drop velocity (V), that is, (DVbeta)-V-alpha with values of a varying between 1 and 6 and values of beta varying between 0 and 2, have been computed. The results indicate that values for a rangin g between 3 and 6 and for beta smaller than or equal to 2 best describe the rate of detached sediment. Although all indices containing the mass of wat er (i.e., D-3) predicted splash detachment rates relatively well, the produ ct of momentum and drop diameter ((DV)-V-4) was slightly superior in descri bing splash detachment. The existence of a rain erosivity threshold (critic al kinetic energy) to initiate soil detachment is confirmed. This threshold energy equals 5 mu J for the fine sand and 12 mu J for the silt loam and c ompares relatively well with the threshold energy data for other soils repo rted in the literature.