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The presentation examines excavation-induced ground movement, focusing on deep excavations in the greater Boston area. It distinguishes local movement, caused by retaining-wall deflection, from broader “global” movement associated with heave and strain softening in Boston’s thick blue clay. Reviewing 21 projects, the speaker found settlement effects extending farther than conventional predictions—up to roughly five to five-and-a-half excavation depths, and farther when measured from adjacent foundations. Larger excavation footprints were associated with greater wall movement, potentially because of longer bracing spans and construction duration. The talk emphasizes that reliable predictions require good information on geology, soil properties, groundwater, nearby structures, construction sequence, and project methods; sophisticated models cannot compensate for poor inputs. A final case study describes a Seaport District excavation and measured movements: the wall moved about 2–3.5 inches, while a nearby building 74 feet away settled up to about half an inch.
Keywords
deep excavation
ground movement
Boston blue clay
retaining wall deflection
settlement
geotechnical monitoring
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