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AGRA Foundations, Inc. Richmond/San Rafael Bridge HIGH CAPACITY MICROPILE CONSTRUCTION. Photograph courtesy of California Department Transportation. Richmond/San Rafael Bridge. Completed in 1956, the 5.5 mile long bridge sits between two fault lines in the San Francisco Bay.
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AGRA Foundations, Inc. Richmond/San Rafael Bridge HIGH CAPACITY MICROPILE CONSTRUCTION
Photograph courtesy of California Department Transportation Richmond/San Rafael Bridge Completed in 1956, the 5.5 mile long bridge sits between two fault lines in the San Francisco Bay. The bridge connects the cities of Richmond and San Rafael as part of Interstate 580.
Site Location Richmond/San Rafael Bridge San Francisco SAN ANDREAS FAULT HAYWARD FAULT
Project Hierarchy Date bid: August 08, 1999 Owner: California Department of Transportation General Contractor: A Joint Venture of Tutor Saliba/Koch/Tidewater Prime Subcontractor: AGRA Foundations, Inc.
AGRA’s Scope of Work 66” Dia. CIDH Piles 150” Dia. CIDH Piles Substructure Micropiles Superstructure Micropiles ``
Substructure Micropiles Pile Data Micropiles This table represents 31 pier locations with 476 production piles and 5 performance piles. Load range from 290 kips to 1140 kips
Substructure Micropile Note Spirals at base of pile and rings at Micropile top (inside the bell) Typical CRIP
Prerequisites to Micropiles Work Platforms
Hinge Locations Micropile Installation Templates Templates were constructed to accurately locate the micropiles
Completed Templates and Conductor Casing Micropile Installation Templates Template Connector Templates in place on Bridge
Foundation Bell Pipe Reinforcement Conductor Casing Steel Bell Casing 14” Dia. Cored Hole with Groves Rubber Seat Mud line Seal Coring Bed Rock Grooving Permanent Steel Casing Bedrock Socket Pipe placed from bottom of bell and socketted into bedrock (not shown) Bell 12” Dia. Micropile Installation
Geological Description The Franciscan Formation is a heterogeneous unit of sedimentary and volcanic rock deposited in an offshore, deep-marine trough at the base of the continental slope. The formation consists of massive graywackesandstone, dark shale, minorchert and limestone, altered volcanic rock, and various metamorphic rocks. All of the rock is intruded by serpentine. The Franciscan Formation is believed to be as thick as 50,000 feet and typically found as fault-bound blocks accreted onto the western shoreline of California by plate movement .
Log of Test Bore Working Drawing Load Capacity Calculations
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