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"Untangling Hyporheic Residence time Distributions and Whole Stream" "Metabolism Using a Hydrological Process Model"
2016
Procedia Engineering
The interaction of the water residence time (RT) in hyporheic sediments with the sediment metabolic rates is believed to be a key factor controlling whole stream metabolism. However, due to the methodological difficulties, there is little data that investigates this fundamental theory of aquatic ecology. Here, we report on progress made to combine numerical modelling with a series of modification to laboratory flumes overcoming methodological difficulties e.g. by creating steady flow paths for
doi:10.1016/j.proeng.2016.07.598
fatcat:22vxd77evjhbpg5izhbujbz4dq