STUDENT EXPERIMENTS IN SEDIMENT TRANSPORT, LANDFORM MIGRATION, AND CHANNEL MODIFICATION IN NONCOHESIVE RIVER CHANNELS USING A LARGE SCALE LABORATORY STREAM MODEL
Sets of two-hour experiments were designed for students to observe a stream response to base level changes, and tectonism. During the exercises, students replicated straight and meandering stream patterns, and observed sediment movement along the channel; also, they examined sediment redistribution along meander bends and point bars. Changes in stream bed elevation were measured along three fixed cross-sections; these allowed for determining shifting of sand bars and alluvial terraces after modification of base level or axis tilt. To replicate tectonism, the lateral inclination of the table was modified, causing re-routing of the stream followed by channel scouring and formation of alluvial terraces. Furthermore, upon adjustment of the axial tilt, changes in the stream channel extended from lower reaches to the middle of the simulated stream. After completion of formal exercises, students were encouraged and engaged into creating their own science experiments, thus increasing their curiosity on towards science projects.
Through these activities, students had hands on experience on the response of fluvial systems to natural and man made changes. The results obtained on these experiments demonstrate the advantages of using large scale movable bed river models to teach and demonstrate geomorphologic concepts in laboratory settings.