Sediment transport through self‐adjusting, bedrock‐walled waterfall plunge pools

Many waterfalls have deep plunge pools that are often partially or fully filled with sediment. Sediment fill may control plunge‐pool bedrock erosion rates, partially determine habitat availability for aquatic organisms, and affect sediment routing and debris flow initiation. Currently, there exists no mechanistic model to describe sediment transport through waterfall plunge pools. Here we develop an analytical model to predict steady‐state plunge‐pool depth and sediment‐transport capacity by combining existing jet theory with sediment transport mechanics. Our model predicts plunge‐pool sediment‐transport capacity increases with increasing river discharge, flow velocity, and waterfall drop height and decreases with increasing plunge‐pool depth, radius, and grain size. We tested the model using flume experiments under varying waterfall and plunge‐pool geometries, flow hydraulics, and sediment size. The model and experiments show that through morphodynamic feedbacks, plunge pools aggrade to reach shallower equilibrium pool depths in response to increases in imposed sediment supply. Our theory for steady‐state pool depth matches the experiments with an R2 value of 0.8, with discrepancies likely due to model simplifications of the hydraulics and sediment transport. Analysis of 75 waterfalls suggests that the water depths in natural plunge pools are strongly influenced by upstream sediment supply, and our model provides a mass‐conserving framework to predict sediment and water storage in waterfall plunge pools for sediment routing, habitat assessment, and bedrock erosion modeling. Key Points Waterfall plunge pools are dynamic and transient repositories for sediment Plunge pools self‐adjust their depth to pass the upstream sediment load Sediment‐transport capacity increases for larger waterfalls and shallower pools