PLATTE RIVER RESTORATION
The data and analyses from our study associate the channel narrowing with substantial reductions in river flow and the resulting expansion of vegetation, primarily caused by water development and drought, and by a decrease in sediment supply and resulting channel incision. Reductions in river flow account for most of the narrowing. Vegetation growing on sandbars creates wooded islands, dividing the river into narrow channels.
Clear water from dams and canals causes channel incision, which initially has maximum scour impact near the sources of clear water. Local bed coarsening causes the erosion to migrate downstream over time. Channel narrowing and bed coarsening are geomorphic consequences of incision. Significant incision can currently be found in the reach immediately downstream from the Johnson-2 Canal Return, while smaller amounts of incision have been noted as far downstream as Kearney. With no additional changes to flow or sediment, it is anticipated that this channel narrowing will continue downstream to Chapman.
The proposed plan for channel restoration includes: 1) the clearing and lowering of vegetated islands, and 2) annual pulse flows of short (3 day) duration from Kingsley Dam. The clearing and lowering of fine-grained river islands would immediately increase the area of wide, open channel, and add finer sand to the riverbed. The annual pulse flows would build sandbars for summer nesting and would keep the sandbars clear from the previous year's seedlings. Implementation would occur by adaptive-management to ensure habitat improvement and avoidance of adverse impacts.