Mansueto Library: Drama below Ground and Above

"The recently opened Mansueto Library at the University of Chicago campus was a 2012 OPA runner-up. The dramatic elliptical shaped dome of this structure tells only part of this structure’s story. The underground automated storage and book retrieval system below ground required excavations as deep as 55 ft (17 m). The system that allows the University to store many of its publications well below grade also required an approximately 50 ft (15 m) clear span for the perimeter walls between the lower level and street level slabs. The latter requirement allows the conveyors to operate freely to retrieve and transport publications up to the lobby level. The design-assist-build team worked together to develop the most cost-effective solution for below-grade work in this challenging urban and geologic environment.The perimeter of the new oval-shaped library is over 620 ft (189 m) long and sits in a central location on campus—adjacent to the Regenstein Library and two city streets and the Henry Moore sculpture, which commemorates the location of the first self-sustaining controlled nuclear reaction. The new library construction not only had to meet challenging structural and geotechnical requirements, but also had to be sensitive to its active and historic surroundings. The soils at the site consist of about 25 ft (7.6 m) of sand, followed by lean clay, generally increasing in stiffness to the top of the dolomitic limestone. Five to 10 ft (1.5 to 3 m) pockets of saturated sand also lie on the north side of the site at about 45 ft (13.7 m) below grade. The top of weathered rock varies in elevation from 59 ft (18 m) below grade in the south to 69 ft (21 m) in the north. There is 1 to 2 ft (30 to 60 cm) of weathered rock. Groundwater at the site is about 7 ft (2 m) below grade.The new structure would extend 55 ft (17 m) below grade through saturated sand strata and into weathered rock for part of the structure’s footprint, so it was critical that the new permanent retention system minimize groundwater seepage laterally through the structure’s wall as well as piping through the weathered rock below the structure. The perimeter walls had to be very stiff to minimize ground movement around the structure’s perimeter due to the significant clear span between slabs."