Variable response of particles and inorganic carbon of two different soils during splash erosion

Splash erosion caused by raindrops is the first stage of water erosion that detaches and transports soil particles. As an important component of soil particles, soil inorganic carbon (SIC) contains little information on its redistribution during splash erosion. In this study, two soils, purple soil and loess, were selected and placed in a soil tray with a diameter of 20 cm at the center of a splash tray, and a rainfall simulator was used to simulate three raindrop energies in experiments to investigate the migration of soil particles and SIC. The results showed differences in the amount and selective migration of splashed material between the soils, which was evident in the obvious sorting of the particle size of purple soil with distance and the insignificant change of loess soil. The SIC sorting characteristic performed differently in the two soils, that is, the SIC content of purple soil increased with particle size, while that of loess was the opposite. The enrichment and depletion of SIC during splash erosion varied with soil type, and differed from the general enrichment of soil organic carbon (SOC). The SIC enrichment ratio (ERIC) of purple soil was generally > 1, whereas the ERIC values of loess were < 1. In addition, multiple linear regression (MLR) models were established to predict the SIC content of splashed material. Rainfall splash plays an important role in SIC migration and may further affect the carbon cycle. These preliminary results provide a basis for further study of SIC response to rainfall splash.

Automated summary

Splash erosion is the initial stage of water erosion and can cause detachment and transportation of soil particles. The redistribution of soil inorganic carbon (SIC) during splash erosion is not well understood. This study simulated rainfall conditions to investigate the migration of soil particles and SIC in two different types of soils. The results showed differences in the amount and selective migration of splashed material between the soils, as well as differences in SIC sorting characteristics. The enrichment and depletion of SIC during splash erosion varied with soil type, contrary to the enrichment of soil organic carbon (SOC).