资源环境科技发展态势分析平台

Streambed erosion and deposition are fundamental geomorphic processes in riverbeds, and monitoring their evolution is important for ecological system management and in-stream infrastructure stability. Previous research showed proof of concept that analysis of paired temperature signals of stream and pore waters can simultaneously provide monitoring scour and deposition, stream sediment thermal regime, and seepage velocity information. However, it did not address challenges often associated with natural systems, including nonideal temperature variations (low-amplitude, nonsinusoidal signal, and vertical thermal gradients) and natural flooding conditions on monitoring scour and deposition processes over time. Here we addressed this knowledge gap by testing the proposed thermal scour-deposition chain (TSDC) methodology, with laboratory experiments to test the impact of nonideal temperature signals under a range of seepage velocities and with a field application during a pulse flood. Both analyses showed excellent match between surveyed and temperature-derived bed elevation changes even under very low temperature signal amplitudes (less than 1 degrees C), nonideal signal shape (sawtooth shape), and strong and changing vertical thermal gradients (4 degrees C/m). Root-mean-square errors on predicting the change in streambed elevations were comparable with the median grain size of the streambed sediment. Future research should focus on improved techniques for temperature signal phase and amplitude extractions, as well as TSDC applications over long periods spanning entire hydrographs.

Plain Language Summary Sediment transport in stream causes erosion and depositional processes, which are difficult to monitor continuously. These processes are typically monitored with surveys, which may be several days apart if not years. Here we tested a new method, which can monitor point scour and deposition at the daily time scale over years. This method will help quantify how dynamic and changing are streambeds with implication for hydraulic structure risk and constrain the interaction between stream and pore waters.