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The goals of the Stream Restoration Project are to: 1)
construct a stable, meandering stream channel
from the end of the concrete flume to the Rio Grande River; 2) vegetate the
riparian corridor with regionally
appropriate grasses and trees; 3) monitor the channel morphology, vegetation
success, and biologic re-colonization
following construction; and 4) produce data, maps, and reports for dissemination
of information regarding the approach to stream restoration and success.
Lower Willow Creek is located on an alluvial fan that was
likely created during paleoflood events. At
some point the stream corridor was disturbed from its natural (and likely
stable) condition; a braided stream
resulted and has since existed. Potential causes of this braiding include
vegetation removal during settlement and heavy sediment loading during
mining operations. The lack of braiding in local reference streams, as
identified by similar geomorphology, indicates that this stream pattern is
not due to natural processes.
During high flows in this braided Rosgen D3 channel, the
bars and islands alternatingly aggrade and degrade with the constantly
changing flow dynamics. Since the braided bankfull channel is wide and
shallow, the sediment transport rate per unit width is relatively low for a
mountain stream, and the stream is inefficient at carrying the sediment that
has been mobilized from the watershed. In a braided stream, the prevalence
of high velocity gradients means that more bank and bed is subject to
near-bank stress than in a narrower, deeper Rosgen C3 channel. This, in
addition to the lack of bank vegetation, greatly facilitates mobilization of
bank and bed material.
Additionally, in profile Willow Creek lacks the riffle-pool
morphology typical in reference streams. It is, in essence, just one long
riffle. Transforming this type of
braided channel into a more stable form will greatly decrease local erosion.
A vegetation-armored, hydraulically efficient cross-section will transport
the sediment mobilized from the watershed while greatly minimizing
mobilization of bank and bed material. Cross-vanes and J-hooks will also
decrease bank shear stress and provide energy dissipation.
Since 1999, the WCRC has worked in
cooperation with the Natural Resources Conservation Service, US Forest
Service, Colorado Forest Service, and Colorado State University Cooperative
Extension to evaluate revegetation options for riparian and floodplain
areas. These trials have incorporated various species of trees,
shrubs, and grasses, as well as soil amendments. Discussions of these
trials and preliminary evaluations are provided in the report, Re-vegetation
Trials, Willow Creek Floodplain, 1999-2003.
In April 2007, the USDA Natural Resources Conservation Service
finalized Willow Creek Stream Restoration: Planning Study. The
purpose of this study was "to collect and present available data and
publications on the [Willow Creek] floodplain into one package, to provide
informed alternatives and recommendations for a restoration". In
addition, this report also characterizes the watershed, and provides cost
estimates for the various alternatives presented. To view this report please
click here.
Based on the NRCS conceptual design
presented in the report, the WCRC has applied for, and successfully been
granted CO Non-point source funds to improve water quality and fish habitat
in the Lower Willow Creek floodplain. The Committee is currently seeking
additional funding for
other environmental and programmatic goals not covered by the CO Non-point
source grant. Local support has been
tremendous for such an effort, and over $280,000 in In Kind and cash
contributions have been pledged.
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