Bank
Stabilization Using Bankform Roughness--Johns Demonstration Project
Barry Duff, ARCO Environmental
Remediation, LLC
The purpose of the demonstration project was
to stabilize the streambank by increasing bankform roughness using natural
materials (large willows, small shrubs, and willow cuttings). The bankform was
intermittently cutback at a 25-foot
interval to create a “scalloped” shape.
Additional shade was provided with large willows, reducing water
temperature and improving aquatic habitat.
The design draws from research of Dr. J. Duncan Smith of the U.S.
Geological Survey (USGS). This
voluntary demonstration project was undertaken by ARCO Environmental
Remediation, LLC with the cooperation and assistance of the local landowner
(Allen Johns), the U.S. Environmental Protection Agency, USGS, the Montana
Department of Fish Wildlife and Parks, and other agencies.
Construction began on December 15, 1999 and was
completed on January 24, 2000. Approximately 664-lineal feet of streambank were
stabilized. A total of 20
“scallops”, on approximately 25-foot centers, were constructed. One hundred twenty-five large willows and 100
containerized shrubs were installed. Sod was cut prior to excavation and
re-installed afterwards, and disturbed areas were seeded with a native riparian
grasses seed mix. Willow stakes
will be cut and planted in spring, 2000. Coconut
fabric and geo-coir fabric were installed to provide short-term erosion
protection until vegetation is established.
Riprap was installed at the toe of the bank to anchor the geo-coir fabric
and provide additional erosion protection.
Riprap was installed below the water surface to preserve a natural look.
Less riprap was used than typically associated with a “hardened toe”
approach. Fencing was installed to prevent disturbance from livestock until
vegetation is established. Work was completed at a unit cost of $127 per lineal
foot, including design, oversight, and construction.
To evaluate effectiveness of the technique, monitoring will quantify
erosion rates, based on surveys after ice-flow and spring runoff 2000.