The condition at Fee Fee Creek before the project was a severly eroded stream filled with debris.Homes had been built along Fee Fee Creek’s north bank in the 1960s and 1970s, before the city was incorporated in 1985. This development – as well as residential and commercial development farther upstream – increased the imperviousness of the watershed feeding Fee Fee Creek, which in turn increased the runoff and velocity of water flowing in the creek. Through the years, homeowners began dumping grass clippings and other debris down Fee Fee Creek’s banks, killing vegetation that had held soil in place.Fast-forward a couple of decades, and the once-attractive, meandering stream had changed dramatically. Because of the increase in stream flow, the creek began to undergo entrenchment, a process by which the stream bottom drops, which caused the banks to slide into the stream. Several hundred feet of embankment had a near-vertical face because of the erosion. A number of outfall pipes from an existing drainage system had been undermined and were in varying states of disrepair. Many trees with trunks as large as 3 ft. in diameter had fallen victim to Fee Fee Creek’s destructive forces and had plunged into the water.The entrenchment of Fee Fee Creek was so advanced that residents were losing their backyards; some fences were ready to tumble into the water. Left unchecked, the creek threatened to claim sheds and swimming pools. In 2001, the City of Maryland Heights stepped in to stabilize a 1,900-ft. section of Fee Fee Creek. The city hired Woolpert LLP, a national consulting firm that provides engineering and environmental planning and design, to study the creek’s problems and recommend a sustainable stream design solution. Woolpert assembled a team of surveyors, geotechnical engineers, hydraulic engineers, and environmental scientists to perform the project, which included the following:Topographic and boundary surveysHydrologic and hydraulic modelingBiostabilization designPlans and specifications preparationCost estimatingEasement plat preparationBid servicesTechnical support during constructionAt the center of Woolpert’s recommendations was the use of certain instream and on-bank design techniques, including the J-hook weir, Newbury riffle pool, wrapped earth, and root wads. These techniques have been used in other regions of the United States but were relatively new to the St. Louis region. They are part of a sustainable stream design movement that takes a natural and holistic approach to stream stabilization.Although the City of Maryland Heights is considered progressive when it comes to stormwater management, some city officials and local homeowners still were a little skeptical of the techniques that Woolpert was recommending. Convincing stakeholders that sustainable stream design is as effective as traditional stream improvement methods – not to mention healthier for water quality and wildlife – was part of the educational process that included public presentations describing the process and benefits.“We’re taking a different approach to creek stabilization,” says L.G. Loos, P.E., assistant director of public works for the City of Maryland Heights. “We’re looking at Fee Fee as an overall unit – as an entire ecosystem – instead of doing spot fixes. We’re learning what caused problems to form in the first place and remedying them with sustainable solutions.”The Beginning
Constructing a Newbury riffleA total of six J-hook weirs, so called because the placement of rocks involved resembles a “J,” will be developed around bends in Fee Fee Creek. The technique was pioneered by Dave Rosgen, a geomorphologist and founder of Wildland Hydrology based in Pagosa Springs, CO. It has been used for about a decade throughout the US but still is gaining acceptance in the St. Louis region.The J-hook weir is a series of strategically placed rocks designed to redirect the flow of water to the center of the stream. The J-hook is embedded approximately 5 ft. into the bank and curves out into the water, gradually sloping downward. The rocks are placed without gaps between them closer to the bank (to slow the water and direct it toward the center of the stream) and with gaps between them nearer the center and end of the J-hook (where the swirl of water is more beneficial, creating deeper, oxygenated pools for aquatic life). Rocks should be square; their size depends on the size and velocity of the stream. At Fee Fee Creek, the size of rocks will vary from 2.5 to 3.5 ft. across, weighing from 1,000 to 4,000 lb.The Newbury riffle pool – also gaining popularity in the St. Louis region – was chosen as another way to slow the velocity of water and to improve water quality by aerating the water with riffles and providing deeper pools for aquatic life. A total of 11 Newbury riffle pools are being installed at Fee Fee Creek.Created by Robert Newbury of Newbury Hydraulics in British Columbia, Canada, the technique is based on the principle that riffles and pools can be created to mimic naturally occurring riffle-pool complexes. Similar to their naturally occurring counterparts, the manmade riffles at Fee Fee Creek are being strategically placed to create upstream pools through the bends.To create this system, the riffle crest first is built across the stream using large-diameter boulders. At Fee Fee Creek, stones from 2.5 to 3.5 ft. in diameter (1,000-4,000 lb.) will be used to create the crest, which spans the width of the stream and embeds into the bank. The goal is to set the crest stones at the proper elevation to create the desired pool elevation upstream of the crest. Next, support stones ranging from 1 to 2.5 ft. in diameter (75-1,000 lb.) will be set in place behind and in front of the crest. Each riffle will have a 4:1 sloped upstream face and a 20:1 sloped downstream face. Smaller stone is used to fill the remaining gaps.Special Considerations at Fee Fee Creek