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Jake W. Riedel, Eric W. Peterson, Toby J. Dogwiler and Wondwosen M. Seyoum
The flux of water through the hyporheic zone (HZ) is controlled by stream bedforms, sinuosity, surface water velocity, local water table, seasonality, and hydraulic conductivity (K) of the bed material. Dependent on both the kinematic viscosity and densi...
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