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1

Bedrock CharacterizationMottolo Pig Farm Superfund Site

Andrew “Drew” Hoffman, PE

NH Department of Environmental Services

andrew.hoffman@des.nh.gov

603.271.6778

1

Acknowledgments

� GZA GeoEnvironmental (lead consultant)

� Hager-Richter (sub for geophysics)

� EPA, Region 1

� NH Geological Survey (regional bedrock)

� USGS (geochemistry / arsenic expertise)

2

2

� Site Orientation & Defining the Problem

� TCE Investigation

� Geophysical Surveys

� 3D Model (Representation)

� Groundwater Hydraulics & Geochemical Studies

� Results

� Questions & Discussion

What’s Ahead

3

Site Location & Orientation

Randy Lane

North

4

3

Former Piggery Buildings

FORMER DRUM

DISPOSAL AREA

SHALLOW BEDROCK

FLOW TO BROOK A

SHALLOW BEDROCK MWs

Site Features & EPA Cleanup Actions

5

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

6

4

Residential sampling

began in 2003

2009 Expanded Residential Well Sampling

7

2009 TCE Concentrations

Detected

below

standard

Detected

above DW

standard

Non-Detect

8

5

Arsenic Concentrations

9

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?

10

6

� 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

11

Bedrock Groundwater Contours

12

Brook A

7

� 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

13

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

14

8

Surface Geophysical Methods:VLF & EM34 Fracture Interpretation

Former DrumDisposal Area

N

15

Former DrumDisposal Area

Perspective View

Looking Northwest

Surface Geophysical Methods:Earth Resistivity Imaging

16

9

Geophysically Logged Wells

17

Blue Fracture Plane

in 3D Model

Borehole Geophysical LoggingFracture & Flow Interpretation

18

10

Perspective View

Looking Northeast

Former DrumDisposal Area

3D Geophysical Conceptual Model

Well or Borehole Logged by Hager-Richter or USGS

19

North

Area of

concentrated

groundwater

withdrawals

Former DrumDisposal Area

Surface Traces of Modeled

Fracture Planes

N

20

11

� Site Orientation & Defining the Problem

� TCE Investigation

� Geophysical Surveys

� 3D Model (Representation)

� Groundwater Hydraulics & Geochemical Studies

� Results

� Questions & Discussion

What’s Ahead

21

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

22

12

Pump Test Drawdown

Pumping well

5’ 10’15’

23

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

24

13

Area 1 – Remedial Area

25

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

26

14

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

27

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

28

15

Questions and Discussion

29

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