Micropiles Take Off at Dulles Airport

"An expansion plan for Washington Dulles International Airport is currently underway to prepare for growth at this northern Virginia facility in the future. While Dulles currently serves more than 20 million passengers a year, when the Master Plan for the Airport is fulfilled, it will be capable of handling approximately 55 million passengers a year. The current Capital Construction Program underway at Dulles will take the Airport one step closer to its full potential.As planned, work includes a new Airport Traffic Control Tower, expansion to existing concourses, a fourth runway, additional parking, and other improvements. One of the most interesting features of this project is the construction of a two-track passenger train system (Automated People Mover, or APM) linking the main terminal and concourses, which will largely replace the Mobile Lounge transportation system, thus greatly reducing surface traffic. Construction of the APM system involves deep excavations along the tunnels and at the transfer stations. This poses special challenges because the settlement-sensitive terminal, original Airport Traffic Control Tower, and concourse buildings, as well as other facilities, exist near the proposed below-ground stations. The site is also underlain by a tight grid of underground utilities that include jet fuel, gas and central communication lines, in addition to more mundane electric, sewer and water mains.One of the most interesting features of this project was the extensive and skillful utilization of micropiles for support of existing structures adjacent to the excavations. Without the use of micropiles, the cost and difficulty of the excavations would likely have been much more. Several important lessons were learned about the use of micropiles, which advance that technology.Throughout the project site, bedrock was generally encountered at 25-ft depths or more. The rock consists of micaceous and highly calcareous siltstone rock. This rock is typical of the sedimentary component of the Culpeper Basin, a Triassic Age geologic feature extending from south central Virginia to western Maryland. The siltstone beds dip gently to the west at about 10 to 20 degrees. Joint planes typically dip 60 degrees to vertical. The rock underlies a sequence of fill materials and residual soils of varying thickness."