The Channel Source Hypothesis
Researchers Steve Wondzell and Adam Ward propose the “channel-source hypothesis” in which the stream channel itself should be considered as a potential source of DOC to stream water during storms. Data collected during a small storm in the H. J. Andrews’ Watershed 1 could not be explained by existing conceptual models of stormflow generation. Simply put, DOC concentrations in the water samples collected from both the riparian and hillslope wells were lower than the concentrations in stream water so these areas could not be the primary source of DOC to the stream.
