Dam Removal
Dam removal and downstream transport of reservoir sediments create exciting experiments and research opportunities in sediment transport, channel evolution, and habitat response. My group addresses several related questions pertaining to dam removal: How do downstream channels respond to increases in sediment supply, including both short-term increases from downstream transport of reservoir sediments and long-term restoration of supplies from upstream drainage basins? How do pulses of sediment travel through river systems? What are the effective discharges for redistributing reservoir sediments? How do aquatic habitats respond to dam removal?
I participated in the John Wesley Powell Center working group on "Dam removal: Synthesis of ecological and physical responses." This group brought together dam-removal researchers from around the country to synthesize what we have learned from individual dam-removal studies; the effort produced a dam-removal science database and several synthesis papers about the state of dam-removal science.
![Condit Dam](https://images.apps.umt.edu/storage/umt/center/630/410/wilcox/images/dam.jpg)
![Condit Dam](https://images.apps.umt.edu/storage/umt/center/320/320/wilcox/images/dam.jpg)
Condit Dam Removal
The Condit Dam removal entailed dynamiting of a 4m by 5.5m hole at the base of the dam, in October 2011, which produced rapid and dramatic draining of fine reservoir sediments within hours of the blast. We are investigating the downstream geomorphic response to develop insight into spatial and temporal variation in recovery from sediment-pulse disturbance. You can view our publication about the initial geomorphic response.
![milltown reservoir](https://images.apps.umt.edu/storage/umt/center/630/410/wilcox/images/milltown-dam.jpg)
![milltown reservoir](https://images.apps.umt.edu/storage/umt/center/320/320/wilcox/images/milltown-dam.jpg)
Milltown Dam Removal
My students and I have taken advantage of the fantastic natural experiment created by this dam removal to (1) investigate the upstream channel responses to dam removal in both the Blackfoot and Clark Fork arms of the former Milltown reservoir; (2) construct a sediment budget for the Milltown reservoir area, including measurements of bedload transport into and out of the reservoir, to document volumetric erosion of reservoir sediments; (3) analyze downstream geomorphic changes related to sediment deposition in channel-bed interstices [PDF] and on the channel bed and floodplain; and (4) examine the historical range of variability of channel morphology of the Clark Fork River in the vicinity of the dam removal [PDF].