| Groundwater
subsidence poses a significant challenge to the City of Boston.
Most buildings
constructed in Boston prior to 1920 are supported by wood pilings.
When groundwater levels drop below the level of the pilings, the
wood is exposed to air and pilings rot, which can lead to building
collapse. Over 2,000 acres in Beacon Hill, Back Bay, South End,
Fenway, Chinatown, Bay Village, and parts of the North End and
Charlestown are exposed to this risk.
Infrastructure
developed in Boston over the past century has permanently altered
the flow of groundwater. The largest sources of groundwater
loss
in Boston include sewers, drains, subways, underpasses, building
foundations,
other structures below the water table, and pumping from sumps. Although
the significance of groundwater subsidence is
well-known, no former policy has been implemented by the city in
order to prevent future subsidence.
This project examines the development history of Copley Square in
order to better understand the relationship between groundwater and
development in Boston. Copley Square is surrounded by several significant
sources of groundwater loss. Moreover, because Copley Square is built
entirely on filled land, buildings in the area are especially susceptible
to lowered groundwater levels. Using Copley Square as an example,
this project will answer the following questions:
• How does
groundwater flow in Boston?
• How has the last century of development in and around Copley Square
affected groundwater subsidence?
• How have specific incidents of dewatering been addressed in Copley
Square and what strategies have been effective?
• What can be learned from Copley Square in order to better address
groundwater subsidence in all of Boston?
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