final mottolo geophysics - newmoa
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Bedrock CharacterizationMottolo Pig Farm Superfund Site
Andrew “Drew” Hoffman, PE
NH Department of Environmental Services
andrew.hoffman@des.nh.gov
603.271.6778
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Acknowledgments
� GZA GeoEnvironmental (lead consultant)
� Hager-Richter (sub for geophysics)
� EPA, Region 1
� NH Geological Survey (regional bedrock)
� USGS (geochemistry / arsenic expertise)
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� Site Orientation & Defining the Problem
� TCE Investigation
� Geophysical Surveys
� 3D Model (Representation)
� Groundwater Hydraulics & Geochemical Studies
� Results
� Questions & Discussion
What’s Ahead
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Site Location & Orientation
Randy Lane
North
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Former Piggery Buildings
FORMER DRUM
DISPOSAL AREA
SHALLOW BEDROCK
FLOW TO BROOK A
SHALLOW BEDROCK MWs
Site Features & EPA Cleanup Actions
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EPA’s 3rd Five-Year Review
� Completed August 2008
� Questioned the Protectiveness of Remedy– Increasing concentrations of TCE & arsenic in
several on-site monitoring wells
– Increased residential development
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Residential sampling
began in 2003
2009 Expanded Residential Well Sampling
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2009 TCE Concentrations
Detected
below
standard
Detected
above DW
standard
Non-Detect
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Arsenic Concentrations
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Unanswered Questions
1. Does the TCE found in residential wells
originate from the Mottolo Site?
2. Any of the arsenic Site-related?
3. Extent of remedy?
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� Site Orientation & Defining the Problem
� TCE Investigation
� Geophysical Surveys
� 3D Model (Representation)
� Groundwater Hydraulic Studies
� Conclusions & Findings
� Lessons Learned & Options for Scale-Down
� Questions & Discussion
What’s Ahead
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Bedrock Groundwater Contours
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Brook A
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� Site Orientation & Defining the Problem
� TCE Investigation
� Geophysical Surveys� Surface geophysical methods
� Borehole geophysical methods
� 3D Model (Representation)
� Groundwater Hydraulic Studies
� Conclusions & Findings
� Lessons Learned & Options for Scale-Down
� Questions & Discussion
What’s Ahead
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Geophysical Surveys
Surface Geophysical Methods:
� Very Low Frequency Electromagnetics (VLF)
� Electromagnetic Induction - EM34
� Earth Resistivity Imaging (ERI)
Borehole Geophysical Methods:
� Optical Televiewer (OTV)
� Acoustic Televiewer (ATV)
� Fluid Temperature & Fluid Resistivity
� Heat Pulse Flow Meter (HPFM) Ambient & Pumped Conditions
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Surface Geophysical Methods:VLF & EM34 Fracture Interpretation
Former DrumDisposal Area
N
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Former DrumDisposal Area
Perspective View
Looking Northwest
Surface Geophysical Methods:Earth Resistivity Imaging
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Geophysically Logged Wells
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Blue Fracture Plane
in 3D Model
Borehole Geophysical LoggingFracture & Flow Interpretation
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Perspective View
Looking Northeast
Former DrumDisposal Area
3D Geophysical Conceptual Model
Well or Borehole Logged by Hager-Richter or USGS
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North
Area of
concentrated
groundwater
withdrawals
Former DrumDisposal Area
Surface Traces of Modeled
Fracture Planes
N
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� Site Orientation & Defining the Problem
� TCE Investigation
� Geophysical Surveys
� 3D Model (Representation)
� Groundwater Hydraulics & Geochemical Studies
� Results
� Questions & Discussion
What’s Ahead
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Pump Test
� Pumped from Site Well
� 30 gpm for First Two Days; 50 gpm Remaining Five Days
� Treated Extracted Water for VOCs and Arsenic
� Measured Groundwater Level Response at 27 Locations
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Pump Test Drawdown
Pumping well
5’ 10’15’
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Perspective View to the
Southeast Looking Down-Dip
Of Modeled Green Fracture Plane
Pumped WellMOT_MW-103
Former DrumDisposal Area
3D Geophysical Conceptual ModelWith Pump Test Results
Well with Immediate Drawdown
Well with Delayed or No Drawdown
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Area 1 – Remedial Area
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Results
� Bedrock groundwater flow and contaminant migration largely influenced by a dominant set of fractures and pumping of residential wells
� TCE generally detected in wells intersecting the dominant bedrock fractures
� Water line remedy addressed residences that were impacted or likely to be impacted
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Results (continued)
� Predictions of plume contraction since 2012
� 9 of 25 former drinking water wells became additional site monitoring wells
� Have not detected site-related VOCs since pre-water line
� Continued sampling of residential wells and site wells support remedy decision
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Lessons Learned
� Data from residential wells critical
� Multiple lines of evidence inform decisions
� 3D model can be kept simple to explain the primary bedrock fracture network
� Integration of multidiscipline team was key to decision making process
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Questions and Discussion
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