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Resistivity Profile in an Urban Setting


          Bill Montgomery
  Dept of Geoscience / Geography
    New Jersey City University
Background
• NJCU is a Federally designated Minority and Hispanic –
  Serving Institution in Jersey City, NJ (near Miss Liberty)
• Approx 5000 students FTE, primarily undergraduate
• 40% Caucasian, 30% Hispanic, 20% Afr-American
• Feds (NSF et al.) screaming for more bodies & more
  diversity in STEM
• Need to expand inquiry & activity-based learning across
  the Science curriculum to attract more Science students
• Our GIS success at NJCU suggests that hands-on,
  student-centered learning improves outcomes,
  regardless of discipline
• Geophysics re-introduced in Sp 2006 after 7-yr hiatus,
  plan was to get the students into the field
• Enter Dr. Lee Slater from Rutgers-Newark (!)
Jersey City History
• Geologic backbone = tilted edge (hogback?) of the
  Palisades Sill, world-famous layered intrusion
  associated with opening of the current Atlantic Ocean
• Industrial sites dating back to 18th century, many on
  sites created with artificial fill from tailings associated
  with chrome processing
• Artificial fill frequently contains Cr VI (nasty heavy
  metal), along with Pb, petroleum, BTEX, timber
  fragments, concrete block, metallic debris, etc.
• The shallow exploration geophysicist’s paradise (?)
Site Location
• Former industrial site
• Part of a larger area designated to become largest park
  (8+ acres) in Jersey City
• Larger issue: area will experience massive
  redevelopment as part of residential housing boom (NYC
  spilling over into JC)
• NJDEP historic fill map shows no fill at the site, but
  nearby well control to NE and SW suggests otherwise:
   –   Chromate waste
   –   Wood & concrete fragments
   –   Fly ash
   –   Miscellaneous debris, including steel
Site Location Map
Exercise Goals
• Reinforce student concepts:
   – Conductivity
   – Resistivity
• Introduce / reinforce use of multiple data sources
  (geological & geophysical) to analyze and solve
  problems
• Begin to familiarize students with modern equipment and
  field data collection techniques
• Embrace multiple working hypotheses to explain
  resistivity profile
• Reinforce student use of “cross-sectional view” of
  subsurface
Exercise
• One resistivity line (thus far), parallel & extended from
  Berry Road, 400+ feet long
   – Discernible differences in resistivity with depth
   – Suggestive of layering / stratigraphy
• 2 sets of well control, 500 & 1000 feet away
   – Shallow water table (~ 5 feet below grade)
   – No reliable “depth to bedrock”, perhaps because of:
       • Similarities between artificial fill and Pleistocene deposits (sand/silt)
       • Poor sample descriptions (hint: hire more geoscientists….)
• Students instructed to take available data & construct a
  hydrostratigraphic cross-section
The Profile
NE                            SW




                   Water Table?




                     Base Fill ?
Student Learning Outcomes
• TBD (To Be Determined)
  – Initial use of line on Sp 2006 Exam w/o well control
    and instructor mention of possible metallic debris in fill
    led to student answer of “metal” when asked why the
    low resistivity….
• Initial results (get them out of the lecture room
  and into the field) encouraging in terms of
  student attitude
• Students clearly are interested in, and motivated
  by, local problems and community issues
Epilogue
• Stay tuned for further additions to the new
  “Geophysics in the NJ Urban Jungle” series
• Check out “Find the UST with GPR”
• Thanks to Lee Slater and all of you real
  geophysicists who are helping me help NJCU
  students
• Questions?

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Resistivity Profile in an Urban Setting

  • 1. Resistivity Profile in an Urban Setting Bill Montgomery Dept of Geoscience / Geography New Jersey City University
  • 2. Background • NJCU is a Federally designated Minority and Hispanic – Serving Institution in Jersey City, NJ (near Miss Liberty) • Approx 5000 students FTE, primarily undergraduate • 40% Caucasian, 30% Hispanic, 20% Afr-American • Feds (NSF et al.) screaming for more bodies & more diversity in STEM • Need to expand inquiry & activity-based learning across the Science curriculum to attract more Science students • Our GIS success at NJCU suggests that hands-on, student-centered learning improves outcomes, regardless of discipline • Geophysics re-introduced in Sp 2006 after 7-yr hiatus, plan was to get the students into the field • Enter Dr. Lee Slater from Rutgers-Newark (!)
  • 3. Jersey City History • Geologic backbone = tilted edge (hogback?) of the Palisades Sill, world-famous layered intrusion associated with opening of the current Atlantic Ocean • Industrial sites dating back to 18th century, many on sites created with artificial fill from tailings associated with chrome processing • Artificial fill frequently contains Cr VI (nasty heavy metal), along with Pb, petroleum, BTEX, timber fragments, concrete block, metallic debris, etc. • The shallow exploration geophysicist’s paradise (?)
  • 4. Site Location • Former industrial site • Part of a larger area designated to become largest park (8+ acres) in Jersey City • Larger issue: area will experience massive redevelopment as part of residential housing boom (NYC spilling over into JC) • NJDEP historic fill map shows no fill at the site, but nearby well control to NE and SW suggests otherwise: – Chromate waste – Wood & concrete fragments – Fly ash – Miscellaneous debris, including steel
  • 6. Exercise Goals • Reinforce student concepts: – Conductivity – Resistivity • Introduce / reinforce use of multiple data sources (geological & geophysical) to analyze and solve problems • Begin to familiarize students with modern equipment and field data collection techniques • Embrace multiple working hypotheses to explain resistivity profile • Reinforce student use of “cross-sectional view” of subsurface
  • 7. Exercise • One resistivity line (thus far), parallel & extended from Berry Road, 400+ feet long – Discernible differences in resistivity with depth – Suggestive of layering / stratigraphy • 2 sets of well control, 500 & 1000 feet away – Shallow water table (~ 5 feet below grade) – No reliable “depth to bedrock”, perhaps because of: • Similarities between artificial fill and Pleistocene deposits (sand/silt) • Poor sample descriptions (hint: hire more geoscientists….) • Students instructed to take available data & construct a hydrostratigraphic cross-section
  • 8. The Profile NE SW Water Table? Base Fill ?
  • 9. Student Learning Outcomes • TBD (To Be Determined) – Initial use of line on Sp 2006 Exam w/o well control and instructor mention of possible metallic debris in fill led to student answer of “metal” when asked why the low resistivity…. • Initial results (get them out of the lecture room and into the field) encouraging in terms of student attitude • Students clearly are interested in, and motivated by, local problems and community issues
  • 10. Epilogue • Stay tuned for further additions to the new “Geophysics in the NJ Urban Jungle” series • Check out “Find the UST with GPR” • Thanks to Lee Slater and all of you real geophysicists who are helping me help NJCU students • Questions?