Effect of soil thickness on rainfall infiltration and runoff generation from karst hillslopes during rainstorms (vol 73, e13288, 2022)

Knowledge of water movement from the hillslope critical zone is important for water management. However, the runoff process resulting from extreme rainfall events remains unclear due to rare field-based natural monitoring data. We investigated rainwater infiltration and runoff generation processes in two plots with deep and relatively shallow soil thicknesses (66 vs. 35 cm depth on average, respectively) on karst hillslopes. Rainwater, soil water and lateral discharge runoff in the soil-epikarst system were monitored using hydrometric and O-18 isotope methods in September 2020, which was the wettest month on record at the study s, including three normal rainfalls (29.6 mm in 8.5 h, 25 mm in 8.5 h, and 27.4 in 3.5 h) and three extreme rainstorms (335 mm in 11.5 h, 77.8 mm in 9 h, and 129.2 mm in 5 h). Soil moisture and water table responded rapidly (<30 min) during the extreme rainfall. However, the soil-epikarst interface exhibited the strongest stability (coefficient variation [CV] < 8.18%) and collected more pre-event water, reflected by the isotopic signature of the soil water. Accordingly, low permeability at the soil-epikarst interface played an important role in buffering rainwater infiltration. Controlled by infiltration-excess and saturation-excess runoff mechanisms, the contribution of surface runoff to total discharge was less than 3% during normal rainfall events, which was significantly less than that during extreme rainfall events (13%-60%). This was supported by the evolution of delta O-18 values of surface runoff that were similar to rainwater and more O-18-depleted than that of subsurface runoff. Higher rainfall intensity which exceeded soil permeability during extreme rainstorms further increased the possibility of exceeding infiltration-saturation processes. For the deep soil plot (DSP), surface runoff (>44%) dominated the extreme rainfall process; while for the shallow-soil plot (SSP), surface runoff (60%) dominated only during the maximum rainfall events. Moreover, the surface runoff contribution to total runoff in DSP was greater than that in SSP. Surface runoff from slopes with thicker soil layers is an important part of karst watershed flood processes in extreme rainfall events, which should be considered carefully for water resource management. Highlights Hydrometric and isotope methods are used to assess extreme hydrological processes. The surface runoff of extreme rainfalls is much higher than that of normal rainfall. The infiltration-excess mechanism dominates the surface runoff of extreme rainfall. Slopes with thicker soil layers are more vulnerable to flooding in the karst region.