Final instrumentation is checked prior to full bridge aeroelastic wind tunnel testing at NRC labs in Ottawa, Canada.
The current, much safer Tacoma Narrows Bridge, situated on State Route 16 in Pierce County, opened on October 14, 1950. It is the primary link between the Seattle-Tacoma metropolitan area on the eastern shore of Puget Sound and the scenic residential and recreational areas on the Olympic Peninsula to the west. After 53 years of operation, it has been nominated for the National Register of Historic Places.
In recent years, population and traffic growth have increased congestion along State Route 16, especially on the Tacoma Narrows Bridge. During peak periods, the four-lane bridge operates at or beyond its design capacity. Congestion lasts for three to four hours—during both morning and evening rush hours—costing motorists a significant amount of lost time every year.
View of wind tunnel models.
The new Tacoma Narrows Bridge, set to open in 2007, is only the second suspension bridge to be built in the United States in the past 40 years—the first was California’s new Carquinez Bridge for which Parsons provided design services and engineering support during construction. The new Tacoma Narrows Bridge is in the top five in the United States in terms of its span, behind the likes of the Golden Gate Bridge and the Mackinac Straits Bridge. Its caissons are some of the largest ever built—they are equivalent to an underwater 20-story building supporting the 510-foot-tall towers. They are being constructed under environmentally extreme conditions—150-foot-deep water, currents up to 7 knots, 50-degree waters, and 50-mph winds are routine.
To ensure that currents do not erode the soil around the caissons, Parsons performed extensive scour analysis of the channel bottom using field measurements combined with physical modeling to accurately portray the channel bed behavior. Tidal conditions and the existing bridge’s caissons complicated the analysis.