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The BBC, along with USEPA Region I, the New Hampshire
Department of Environmental Services (NHDES) and the New Hampshire/Vermont
District of the U.S. Geological Survey (USGS), evaluated many field
sites where the BBC could conduct its research.
Field Site Criteria:
In order to rank these sites, six criteria were
established that would be desirable for the BBC's research:
- Bedrock aquifer readily accessible (e.g., depth to bedrock not
excessive),
- Good understanding of the site's hydrogeological and physical
characteristics,
- Good understanding of the specific contaminants present and
their distribution and concentrations in situ,
- Existing network of monitoring wells,
- Site readily accessible for several years
without fear
that remediation/litigation will impact the BBC's work,
- Good understanding of the type of bedrock present (competent
vs. highly fractured (weathered) bedrock, fracture characterization,
sorption, permeability).
Pease History
Ultimately, it was decided that Site 32 in Zone 3 at the Pease
International Tradeport in Portsmouth, NH was best suited for the
BBC's field site.
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| Site 32, Zone
3, Pease International Tradeport in Portsmouth, NH |
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Site 32 is in an area formerly known as the Industrial Shop/Parking
Area. The BBC is working at Site 32 under the auspices of
the Federal Facilities Agreement (FFA) between the U.S. Air
Force (USAF), Pease Development Authority (PDA), USEPA and
NHDES. Building 113, located at Site 32, was used for equipment
maintenance, which included degreasing operations. A 1,200-gallon
concrete tank buried beneath the northeastern corner of the
building served as a reservoir for degreasing wastes, primarily
TCE. The tank contained an overflow discharge pipe that released
contaminants associated with the degreasing wastes directly
into the soil (overburden). The TCE migrated downward into
the groundwater. A contaminant plume containing primarily
TCE and its degradation products cis- and trans-1,2-DCE and
VC now extends ~0.5 kilometers beyond the identified source
area. The plume has migrated with the groundwater into the
weathered and competent bedrock.
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