Detailed Characterization of the Savage Superfund Site, New Hampshire
The U.S. Geological Survey (USGS), in cooperation with the U.S. Environmental Protection Agency and the New Hampshire Department of Environmental Services, is conducting advanced site characterization activities at the Savage Municipal Water Supply Superfund site in Milford, New Hampshire, and implementing new remediation efforts based on USGS science and tools.
The program includes studying contaminant occurrence, long-term water quality monitoring, and groundwater flow and transport modeling to assess remediation strategies. USGS staff have also mapped site geologic and hydrogeologic units. This 20-year collaboration is facilitating the implementation and evaluation of new and updated remediation strategies.
Transverse cross section showing hydrostratigraphic units at the Savage Municipal Well Superfund site.
The Savage Municipal Water Supply Superfund site includes a plume of contaminated groundwater that connects with several water bodies. From the 1940s to the 1980s, four major industrial facilities were located hydraulically upgradient of the Savage Municipal Well, which provided potable water to the town’s approximately 10,000 residents. In 1983, the well was sampled for volatile organic compounds (VOCs) for the first time as mandated by the Safe Drinking Water Act. VOCs were identified in the well at concentrations exceeding drinking water standards and the well was shut down. Shortly thereafter, in September 1984, the site was added to the National Priorities List. Sixteen constituents of concern (COCs) have been identified, including heavy metals in addition to VOCs.
The hydrogeology of the site is complex: a river and a brook drain the site, and these and an unconfined overburden glacial outwash aquifer are hydraulically connected with a fractured crystalline bedrock aquifer. Flowpaths are complex and the interactions of COCs with underground rock and water (subsurface media) are affected by diverse material properties and fracture networks. Since 2001, USGS contributions to work at this site include:
- Implementing and conducting long-term monitoring of water quality parameters and COCs;
- Mapping hydrostratigraphic units and fracture networks;
- Simulating solute transport for multiple COCs in overburden and bedrock aquifers;
- Simulating the effectiveness of proposed remedies prior to implementation; and
- Monitoring the effectiveness of remedies after installation.
Groundwater well ejects water from air sparging at Savage Municipal Water Supply Superfund Site.
MODFLOW-2005, MODPATH, and MOC3D used for groundwater flow simulation, pathlines analysis, and solute transport in the crystalline-rock aquifer in the vicinity of the Savage Municipal Water-Supply Well Superfund Site, Milford, New Hampshire MODFLOW-2005, MODPATH, and MOC3D used for groundwater flow simulation, pathlines analysis, and solute transport in the crystalline-rock aquifer in the vicinity of the Savage Municipal Water-Supply Well Superfund Site, Milford, New Hampshire
Numerical modeling of groundwater flow in the crystalline-rock aquifer in the vicinity of the Savage Municipal Water-Supply Well Superfund site, Milford, New Hampshire Numerical modeling of groundwater flow in the crystalline-rock aquifer in the vicinity of the Savage Municipal Water-Supply Well Superfund site, Milford, New Hampshire
Bedrock geology and outcrop fracture trends in the vicinity of the Savage Municipal Well Superfund site, Milford, New Hampshire Bedrock geology and outcrop fracture trends in the vicinity of the Savage Municipal Well Superfund site, Milford, New Hampshire
Geochemical, isotopic, and dissolved gas characteristics of groundwater in a fractured crystalline-rock aquifer, Savage Municipal Well Superfund site, Milford, New Hampshire, 2011 Geochemical, isotopic, and dissolved gas characteristics of groundwater in a fractured crystalline-rock aquifer, Savage Municipal Well Superfund site, Milford, New Hampshire, 2011
Evaluation of modeling for groundwater flow and tetrachloroethylene transport in the Milford-Souhegan glacial-drift aquifer at the Savage Municipal Well Superfund site, Milford, New Hampshire, 2011 Evaluation of modeling for groundwater flow and tetrachloroethylene transport in the Milford-Souhegan glacial-drift aquifer at the Savage Municipal Well Superfund site, Milford, New Hampshire, 2011
Time series geophysical monitoring of permanganate injections and in situ chemical oxidation of PCE, OU1 area, Savage Superfund Site, Milford, NH, USA Time series geophysical monitoring of permanganate injections and in situ chemical oxidation of PCE, OU1 area, Savage Superfund Site, Milford, NH, USA
Hydrostratigraphic mapping of the Milford-Souhegan glacial drift aquifer, and effects of hydrostratigraphy on transport of PCE, Operable Unit 1, Savage Superfund Site, Milford, New Hampshire Hydrostratigraphic mapping of the Milford-Souhegan glacial drift aquifer, and effects of hydrostratigraphy on transport of PCE, Operable Unit 1, Savage Superfund Site, Milford, New Hampshire
Effects of a remedial system and its operation on volatile organic compound-contaminated ground water, Operable Unit 1, Savage Municipal Well Superfund Site, Milford, New Hampshire, 1998-2004 Effects of a remedial system and its operation on volatile organic compound-contaminated ground water, Operable Unit 1, Savage Municipal Well Superfund Site, Milford, New Hampshire, 1998-2004
Results of a monitoring program of continuous water levels and physical water properties at the Operable Unit 1 area of the Savage Municipal Well Superfund site, Milford, New Hampshire, water years 2000-03 Results of a monitoring program of continuous water levels and physical water properties at the Operable Unit 1 area of the Savage Municipal Well Superfund site, Milford, New Hampshire, water years 2000-03
Simulation of solute transport of tetrachloroethylene in ground water of the glacial-drift aquifer at the Savage Municipal Well Superfund Site, Milford, New Hampshire, 1960-2000 Simulation of solute transport of tetrachloroethylene in ground water of the glacial-drift aquifer at the Savage Municipal Well Superfund Site, Milford, New Hampshire, 1960-2000
Results of a monitoring program of continuous water levels, specific conductance, and water temperature at the OK Tool Facility of the Savage Municipal Well Superfund Site, Milford, New Hampshire Results of a monitoring program of continuous water levels, specific conductance, and water temperature at the OK Tool Facility of the Savage Municipal Well Superfund Site, Milford, New Hampshire
The U.S. Geological Survey (USGS), in cooperation with the U.S. Environmental Protection Agency and the New Hampshire Department of Environmental Services, is conducting advanced site characterization activities at the Savage Municipal Water Supply Superfund site in Milford, New Hampshire, and implementing new remediation efforts based on USGS science and tools.
The program includes studying contaminant occurrence, long-term water quality monitoring, and groundwater flow and transport modeling to assess remediation strategies. USGS staff have also mapped site geologic and hydrogeologic units. This 20-year collaboration is facilitating the implementation and evaluation of new and updated remediation strategies.
Transverse cross section showing hydrostratigraphic units at the Savage Municipal Well Superfund site.
The Savage Municipal Water Supply Superfund site includes a plume of contaminated groundwater that connects with several water bodies. From the 1940s to the 1980s, four major industrial facilities were located hydraulically upgradient of the Savage Municipal Well, which provided potable water to the town’s approximately 10,000 residents. In 1983, the well was sampled for volatile organic compounds (VOCs) for the first time as mandated by the Safe Drinking Water Act. VOCs were identified in the well at concentrations exceeding drinking water standards and the well was shut down. Shortly thereafter, in September 1984, the site was added to the National Priorities List. Sixteen constituents of concern (COCs) have been identified, including heavy metals in addition to VOCs.
The hydrogeology of the site is complex: a river and a brook drain the site, and these and an unconfined overburden glacial outwash aquifer are hydraulically connected with a fractured crystalline bedrock aquifer. Flowpaths are complex and the interactions of COCs with underground rock and water (subsurface media) are affected by diverse material properties and fracture networks. Since 2001, USGS contributions to work at this site include:
- Implementing and conducting long-term monitoring of water quality parameters and COCs;
- Mapping hydrostratigraphic units and fracture networks;
- Simulating solute transport for multiple COCs in overburden and bedrock aquifers;
- Simulating the effectiveness of proposed remedies prior to implementation; and
- Monitoring the effectiveness of remedies after installation.
Groundwater well ejects water from air sparging at Savage Municipal Water Supply Superfund Site.