3D Site Characterization and Autonomous Remedial Process Monitoring - - PowerPoint PPT Presentation

3d site characterization and autonomous remedial process
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3D Site Characterization and Autonomous Remedial Process Monitoring - - PowerPoint PPT Presentation

3D Site Characterization and Autonomous Remedial Process Monitoring Using High Performance Electrical Resistivity and Induced Polarization Tomographic Imaging Tim Johnson, Mike Truex, Jason Greenwood, Chris Strickland, Dawn Wellman: Pacific


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3D Site Characterization and Autonomous Remedial Process Monitoring Using High Performance Electrical Resistivity and Induced Polarization Tomographic Imaging

Tim Johnson, Mike Truex, Jason Greenwood, Chris Strickland, Dawn Wellman: Pacific Northwest National Laboratory Roelof Versteeg: Sky Research Fred Day-Lewis and John Lane: U.S. Geological Survey William Major: NAVFAC

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Acknowledgements

ESTCP – Environmental Resotoration Optimized Enhanced Bioremediation Through Four- Dimensional Geophysical Monitoring and Dimensional Geophysical Monitoring and Autonomous Data Collection, Processing, and Analysis, ER-2001717 Andrews AFB Andrews AFB CH2MHILL Plateau Remediation Company

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Outline

Autonomous Electrical Resistivity Tomography (ERT) Autonomous Electrical Resistivity Tomography (ERT) characterization and monitoring systms. What and how we measure How we monitor spatial and temporal changes in electrical properties (time-lapse inversion) What does it mean in terms of properties we’re What does it mean in terms of properties we re interested in Examples

Brandywine MD DRMO Superfund Bioremediation Monitoring Soil desiccation characterization and monitoring at the H f d BC C ib Hanford BC Cribs

Concluding comments

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  • ELECTRIC GEOPHYSICAL MONITORING

COMPONENTS

Automated & on demand results Server: Data QA/QC, Management Data Electrical geophysical Hydrologic Geochemical Time Time-lapse lapse Amendment Maps Time-lapse Inversion

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Field scale electrical geophysical measurements measurements

Surface electrodes Measurement 1

Current Electrodes: 55,77 Potential Electrodes: 46,49 Current: 150 mA

Borehole electrodes

Voltage: 112 mV

112 mV Current Source Current Sink

150 mA

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  • de
  • de
  • =

3D characterization and monitoring flowchart

Baseline Characterization Inversion

Starting

M0

Reference model model

se data Electrical Resistivity / I d d Time-laps Induced Polarization Tomography Inversion

=

D1 D2 D3 . M1 M2 M3 ∆M DN

  • M0

. . . . . . . . M ∆M1 ∆M2 ∆M3 MN ∆M4

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Pore-scale current conduction mechanisms

Ionic Conduction is sensitive to: Pore fluid conductivity + Electric Field

  • Saturation

Temperature Electronic Conduction is sensitive to: Mineral conductivity Temperature Interfacial Conduction is sensitive to: Interfacial electrochemistry T t Temperature

Total Conductivity = ionic + electronic + interfacial

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Brandywine

Brandywine MD DRMO Superfind Site

Andrews AFB Site location Brandywine DRMO (green box)

  • Primary groundwater contaminant is TCE

Primary groundwater contaminant is TCE

  • Primary soil contaminants PCB
  • Plume has spread from Air force property to

residential property

  • Contamination resides in upper 30 feet, sandy

gravel, aquitard at 30 ft bgs

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DRMO Enhanced Bioremediation

Site location Site location Brandywine DRMO (green box) Remedial Action

  • Amendment injections at ~1000 injection

points points

  • Injection point spacing ~ 20 ft
  • Dem/Val effort monitored two of the

injections at edge of March/April 2008 treatment area Dem/Val study area (injections B6 & B7)

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ERT/IP Monitoring Systems Details

  • 8 Chem sample wells
  • 7 ERT/Chem wells
  • 7 ERT/Chem wells
  • ERT wells: 15 electrodes @

2 feet spacing. 2 inch Sampling ports at 11,19 and 26 feet 26 feet

  • Sampling wells: sampling

ports at 11 and 19 feet. Well screen at bottom (26 feet) screen at bottom (26 feet)

  • 45 total sampling ports
  • ERT data acquisition: repeat

3D survey with 35000 3D survey with 35000 measurements

Sample Well

Injection Well

ERT/IP Well Sample Well

Injection Well (3/10/08)

Electrodes Sample Ports Groundwater Flow to West ~60 ft/year

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Time-lapse ERT imaging results

Baseline Characterization Sodium dominated 6/18/08 12/17/08 3/18/08 Aquifer 3/23/09 6/16/09 3/18/09 Confining Unit Biological processes Unit 1/22/10 4/09/10 effect Simplified description: initially “conservative tracer” (first year) Simplified description: initially conservative tracer (first year) (signal results from changes in fluid conductivity) followed by changes in solid phase conductivity resulting from

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precipitation

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Relating changes in bulk conductivity to changes in geochemistry

~3.5 m bgs ~6.0 m bgs ~8.5 m bgs Note:

  • Dots are ERT inversion

Dots are ERT inversion results at sample ports.

  • Triangles are fluid

conductivity measurements taken at sample ports March 2008 to Jan. 2009 summary:

  • Little microbial activity
  • Rise and fall in bulk conductivity due primarily to

sodium transport and subsequent dilution.

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Relating changes in bulk conductivity to changes in geochemistry

~3.5 m bgs ~6.0 m bgs ~8.5 m bgs Note:

  • Dots are ERT inversion

Dots are ERT inversion results at sample ports.

  • Triangles are fluid

conductivity measurements taken at sample ports

Jan 2009 to April 2010 summary

  • Geochemical data suggest vigorous microbial activity
  • Fluid conductivity decreases, bulk conductivity increases

suggesting increase in interfacial conductivity (iron-sulfide precipitation)

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Hanford BC Cribs Desiccation Treatability Test

Historical liquid waste crib. Primary vadose zone contaminants ERT Array Plan View Nitrate, Tc99, Uranium Liquid nitrogen system ERT Array y Instrument panels Extraction Blower

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Background ERT Characterization

Section View Oblique View High electrical conductivity contaminated zones

  • high sat. and/or ionic strength
  • low permeability (fine)

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4D desiccation induced changes in bulk conductivity

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4 days 1 week 2 weeks

Other example applications

Vadose zone infiltration monitoring Hyporheic exchange monitoring at Hanford along the Columbia River 0.22 in @ t=0 1 day 2 days y Depth (m) 6 weeks 9 weeks Distance (m) Paleochannel Paleochannel

River Stage / Conductivity Correlation

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Conclusions

Changes in subsurface electrical conductivity obtained from ERT inversions coupled with sparse supporting data from sampling can be interpreted with high confidence in from sampling can be interpreted with high confidence in terms of spatiotemporal information on remedial processes. Capability to ‘ ‘see’ ’ in 4D Petrophysics are important Automation for long term monitoring is feasible Automation for long term monitoring is feasible

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