THE PROBLEM
Loss of natural flow regime:
Diversion of the Smoky Hill River into the 1.1-mile cut-off channel resulted in loss of a natural flow regime and sediment transport function in the Old Channel. Before the cut-off channel, the Old Channel would have received runoff from 8,341 square miles of drainage, contributing 80,000 acre-feet of water annually. Currently, the Old Channel receives run-off from a 4.6 square mile urban drainage that contributes 6,300 acre-feet of runoff. Current flow is insufficient for maintaining quality aquatic and riparian habitat.
Sedimentation in Old Channel:
The upstream culvert is filled entirely with sediment and inhibits free discharge of flows (only 1-2 cfs of water seeps through.) Reduced flow has caused sedimentation, which further reduces channel capacity and flow rates. It's easy for sediment to deposit because reduced flows can't remobilize sediment and the channel has a very mild slope. Sedimentation has degraded stream habitat function and features, including loss of stream flow areas, loss of stream depth and loss of riffle/pool sequences. Sediment deposition upstream of the weir is about seven feet deep.
Loss of quality habitat and connectivity:
Aquatic, wetland and riparian habitat features have been degraded or eliminated by loss of flow and sedimentation. Floodplain encroachment and development has had an adverse impact on habitat and connectivity, resulting in loss of riparian forest and off-channel emergent wetland habitats. There is currently limited connectivity between the wetlands and Lakewood Lake and the Old Channel, which has resulted in loss of aquatic passage.