A systematic set of flume tests was developed to explore the relation between soil water content and soil detachment capacity for a coarse-grained soil and a fine-grained soil. The experiments included aging treatments (three volumetric water contents of 4.0, 11.5, and 21.7% for the sandy loam soil and 5.0, 10.5, and 17.4% for the silt loam soil, and seven aging durations of 0, 12, 24, 36, 48, 60, and 72 h) and drying treatments (saturated soil samples oven-dried for 0, 12, 24, 36, 48, 60, and 72 h). Results showed that soil detachment capacity for these two soils presented unique patterns as soil water content increased: the fine-grained soil presented an increasing and then a decreasing trend under aging treatments, whereas the coarse-grained soil showed a continuous increasing trend as soil water content increased. Both patterns could be fitted by quadratic equations. The effect of soil water content on soil detachment capacity was mainly reflected by water-stable aggregate content. Higher soil water content results in weaker bonds for fine-grained soil but in less slaking for coarse-grained soil. Lower soil water content leads to less slaking for fine-grained soil but more particle deposition and cementation for coarse-grained soil. Future work will include additional soil textures and focus on soil erodibility and critical shear stress to expand our understanding of soil detachment influenced by soil water content.