Spatial Variations in Channel Morphology at Segment and Reach Scales, Middle Fork John Day River, Northeastern Oregon

نویسنده

  • Patricia F. McDowell
چکیده

Like many montane rivers in the western U. S., the Middle Fork of the John Day River is characterized by alternating narrowand wide-valley segments. Although the river has a low gradient (generally < 0.01) alluvial channel, changes in valley width exert a clear infl uence on channel morphology. A spatial hierarchical model of channel morphology was applied to the Middle Fork to understand reach-level and segment-level patterns of morphologic variation. Channel unit data for a 55-km long section of the mainstem channel and detailed profi les at segment transitions where the valley width widens or narrows sharply were used in the analysis. Wide-valley segments, where not signifi cantly modifi ed by human activities, have higher sinuosity, 80% more pool area, and pools up to 40% deeper, on average, than narrow-valley segments. Going downstream from a wide-valley segment to a narrow-valley segment, channel morphology changes relatively abruptly from pool-riffl e morphology, coarse pebble bed-material, and a gradient of less than 0.005, to plane bed morphology, cobble bed material, and a gradient of 0.005 to 0.010. Within one wide-valley segment, distinct reaches were delineated based on channel pattern and valley position. The more sinuous mid-valley reaches have several times more pool area, and pools more than 25% deeper, than the less sinuous valley-edge reaches. Segment-level differences appear to be related primarily to long term geologic controls, but these differences have been modifi ed by human impacts. Observed reach-level differences are related to both geomorphic controls and human impacts. In this montane setting, the hierarchical spatial model is a useful way of analyzing and understanding spatial patterns of channel morphology and aquatic habitat.

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تاریخ انتشار 2005