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The infiltration process constitutes a great part of the hydrology component in modern erosion prediction models, which mainly governs runoff production. Nevertheless, soil characteristics, surface conditions, and storm patterns create difficulties in describing or differentiating infiltration process responses analytically and numerically, especially when infiltration is taking place on gravelly-soil slopes. Therefore, the objective of this study was to experimentally assess the effects of storm patterns on a straw mat mulched slope.