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Deliberate tracer releases in Groundwater
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Why deliberate tracer experiments?
Determine: flow paths residence times (< few years) dispersion coefficients reactive transport (e.g. push/pull) presence of multiple phases (CO2 seq, oil, natural gas, air)
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Borden aquifer Br-
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Scale dependency of dispersivity
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Push/pull experiments
Sedimentary aquifer fractured rock aquifer Matter et al., 2006
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Artificial recharge Clark et al., 2005
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Clark et al., 2005
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Tracer release 900L of SF6 1L of 3He 8 days
Injection by bubbling through a diffusion stone that was placed in a water depth of about 1.2 m into pond #2. Clark et al., 2005
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Clark et al., 2005
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Clark et al., 2005
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Findings: Trapped air => excess air formation
Breakthrough curves of 3He and SF6 very similar => not much loss during recharge maximum conc. was 25% of the mean pond concentration ~24 days residence time 50% recovery over 18 months Clark et al., 2005
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Winthrop landfill, ME LANDFILL As plume 50 meters (horizontal)
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Landfill History 1930 Dump operations begin including local industrial wastes 1972 Landfilling begins and serves adjacent towns 1979 Buried drums found at landfill 1982 Landfilling ceases 1987 Landfill cover system installed 1995 SVE and P&T remediation commences N. Nikolaidis, UCon
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2 tracer experiments Is oxidation of the subsurface a viable option?
ORC (oxygen release compound, MgO2, REGENESIS) single point injection tracer experiment (11/00) flow direction,velocities is treated water captured by EW2? ORC injection experiment (1/01) identification of zones influenced by ORC
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Tracers NaBr, NaCl, SF6 advantages of SF6: high dynamic range, extreme sensitivity (~1 fm/L), inert, conservative?
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SF6 injection, 1st exp.
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sampling
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sampling 2nd exp.
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American Museum of Natural History, 2001
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SF6
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N Existing well (5-10ft screen) New well (long screen) Extraction well
OW7 OW9 OW19 OW10 OW20 EW2 OW1 5’ OW8 OW12 OW13 OW16 OW18 OW17 OW14 OW11 OW6 OW15 P2-D OW2 N Existing well (5-10ft screen) New well (long screen) Extraction well ORC injection point
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Hydraulic head distribution
=> flow towards EW2 Harding, ESE
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1st tracer experiment 120 L of 5g/L NaCl salt solution
100,000 pptv SF6 (~5*10-7 moles total) if equally distributed: 3 ppt
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EW2, 1st tracer experiment
1/29/01
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N Existing well (5-10ft screen) New well (long screen) Extraction well
OW7 OW9 OW19 OW10 OW20 EW2 OW1 5’ OW8 OW12 OW13 OW16 OW18 OW17 OW14 OW11 OW6 OW15 P2-D OW2 N Existing well (5-10ft screen) New well (long screen) Extraction well ORC injection point
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Sf6/Br comparison - OW12 L3 OW12 L 3 relative concentration
Relative time => average Sf6/Br ratio = 294ppt/(mg/L) => tracers behave similarly
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Sf6/Br comparison - EW2 relative concentration Relative time
ppt/(mg/L)
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Why was the recovery rate lower during the second experiment?
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1st tracer experiment waste
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2nd tracer experiment waste
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OW12 OW11 OW14 OW13
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Maximum SF6 concentrations measured at all levels, level at which
Maximum SF6 concentrations measured at all levels, level at which it was measured fence 49 4500,5 ? 4400,3 1400,1 7600,2 5500,2 840,2 10,3 After Harding ESE, Inc., hand drawn map by BKB, 10/26/00 MS, LDEO Existing well (5-10ft screen) New well (long screen) Extraction well ORC injection point 50,2 N Approximate scale 20 feet 2/10/01
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N Existing well (5-10ft screen) New well (long screen) Extraction well
OW7 OW9 OW19 OW10 OW20 EW2 OW1 5’ OW8 OW12 OW13 OW16 OW18 OW17 OW14 OW11 OW6 OW15 P2-D OW2 N Existing well (5-10ft screen) New well (long screen) Extraction well ORC injection point
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As concentrations => little change
Injection
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