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Making chemistry data meaningful
“Geo-CSI” in the oil patch – how
advanced geochemistry solves real
world problems
© 2015
Chemistry Matters Inc.
Scott Mundle* and Court Sandau
WBPC, Regina, SK, April 28-30, 2105
Presented at the Williston Basin Petroleum Conference, Regina, SK
April 28-30, 2015
o  Geochemical characterization of sources to identify ‘fugitive’
gas migration in the oil/gas sector
“Geo-CSI”
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 2
o  Surface casing used to protect
shallow (potable) aquifers
o  Gas (and water) in SCVs migrate
from deeper zones (cement failure)
o  Irregular and low flow rates (can be
difficult to sample/monitor)
o  How can you determine the
source(s) of the leaks?
Surface casing vent flow
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 3
Geochemical characterizations & forensics
o  Gases/fluids for different zones can
be ‘fingerprinted’
o  But why do you keep getting
burned with this approach?
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 4
The geochemistry is never wrong, but the
interpretation is often incorrect
o  Common problems:
o  Sample degraded prior to
analysis
o  Either the wrong ‘end-
members’, or no ‘end-
members are used to
identify sources
o  Numbers are reported that
are at or below the
detection limits of the
instrument
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 5
Don’t make assumptions based on regional
geochemistry
o  Where do the ‘fingerprints’
originate?
o  Commercial isotope
“databases” often use
regional values rather than
local values that can
mislead interpretations
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 6
Need high quality SCV samples
o  Can separate and collect gas and liquid
o  Gas can be purged to remove “breathing”
gas from well
o  Need low atmospheric content in gas
samples for compositional and isotopic
characterization
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 7
Sampling can affects water chemistry
0.0001$
0.001$
0.01$
0.1$
1$
10$
100$
1000$
10000$
100000$
Lithium$
Sodium$
Potassium$
Rubidium$
Cesium$
Beryllium$
Magnesium$
Calcium$
Stron=um$
Barium$
Boron$
Aluminum$
Gallium$
Indium$
Thallium$
Silicon$
Germanium$
Tin$
Lead$
Phosphorus$
Arsenic$
An=mony$
Bismuth$
Sulphur$
Selenium$
Tellurium$
Chlorine$
Bromine$
Iodine$
Scandium$
YDrium$
Titanium$
Zirconium$
Vanadium$
Niobium$
Tantalum$
Chromium$
Molybdenum$
Tungsten$
Manganese$
Iron$
Cobalt$
Nickel$
Palladium$
Pla=num$
Copper$
Silver$
Gold$
Zinc$
Cadmium$
Mercury$
Lanthanum$
Cerium$
Praseodymium$
Neodymium$
Samarium$
Europium$
Gadolinium$
Terbium$
Dysprosium$
Holmium$
Erbium$
YDerbium$
Thorium$
Uranium$
BleedNbarrel$
FlowNthrough$Cell$
1 2 3 4 5 6 7 d-block f-block
Group 2 metals and f-block metals lower in bleed barrels
- suspended solids settle out in bleed barrel (low energy environment)
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 8
Sample integrity: The gas bag
•  Over time isotopic composition of methane and CO2 changes
•  Methane artificially appears more ‘thermogenic’
•  Shift in CO2 is less predictable
•  Manufacturer recommendations - analyze within 48 hours
© 2015
Chemistry Matters Inc.
*Arrows not to
scale
WBPC, Regina, SK, April 28-30, 2105 9
How can you get it right every time?
Mudgas Geochemical Profile
Characterized stratigraphy
Production and Potential Source
Zones:
1.) Fluids
2.) Gases
Characterized end-members
Shallow Fluids
1.) Surface water
2.) Groundwater
Characterized inputs
SCVs:
What are the Source(s)?
1.) Fluid
2.) Gas
GEOCHEMISTRY:
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 10
Complex case study: Fluid and gas flows
•  Collected four samples from each location:
–  SCV gas sample
–  SCV liquid sample
–  Production casing gas sample
–  Production casing liquid sample
•  Used local groundwater and deep aquifer wells in region for
comparison
•  Used perforated wells with DST samples to acquire ‘end-
members’ for other potential source zones
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 11
No insight from water isotopes
o  Water isotopes implicated groundwater sources that
conflicted with other indicators (chlorides, TDS, etc.)
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 12
A clearer picture with advanced analyses
o  Different sources had characteristic ranges of concentrations
and isotope values
o  Provided first line of evidence to indicate that different source
zones can be identified
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 13
Identifying source zones
o  Fluids provide a line of evidence for potential sources, but
they do not provide a refined interpretation
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 14
Combined fluid and gas characterization
*Exact values property of client, shift in isotope values indicated
δ13C Values
GASES C1 C2 C3
SCV A - 1.9 B - 2.3 C
Casing A* B* C*
o  Gases provide a second line of evidence for potential sources
and help confirm a production zone leak
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 15
Complete geochemistry = complete picture
δ13C Values
GASES C1 C2 C3
SCV A - 1.9 B - 2.3 C
Casing A* B* C*
*Exact values property of client, shift in isotope values indicated
δ13C Values
GASES C1 C2 C3
SCV A - 13.1 B - 8.1 bdl
Casing A* B* C*o  Gases provide a second line of
evidence to confirm a cretaceous
zone leak
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 16
δ13C Values
GASES C1 C2 C3
SCV A - 13.1 B - 8.1 bdl
Casing A* B* C*
Identification of depth of source zone
o  Mudgas log can refine cretaceous
leak to within 200-300m range
© 2015
Chemistry Matters Inc.
WBPC, Regina, SK, April 28-30, 2105 17
Where can it go wrong?
•  Similar isotope
‘fingerprints can be
expected
•  Need to account for
this complexity in the
interpretation
WBPC, Regina, SK, April 28-30, 2105 18
Best practices for ‘geoforensics’
•  Collect high quality samples
•  Collect samples for potential source(s) and from the
production casing (if possible)
•  Ask the right questions and get it right !
–  What source zone characterizations were used in the interpretation?
–  Where were these source zones characterized (geographically)?
–  What are the reliable detection limits for your instrumentation?
High quality samples, isotope analysis and accurate
interpretation of microbial effects provide more
conclusive source determination.
WBPC, Regina, SK, April 28-30, 2105 19
Thank You
csandau@chemistry-matters.com
www.chemistry-matters.com
403.669.8569

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GeoCSI solving gas migration problems WBPC 2015

  • 1. Making chemistry data meaningful “Geo-CSI” in the oil patch – how advanced geochemistry solves real world problems © 2015 Chemistry Matters Inc. Scott Mundle* and Court Sandau WBPC, Regina, SK, April 28-30, 2105 Presented at the Williston Basin Petroleum Conference, Regina, SK April 28-30, 2015
  • 2. o  Geochemical characterization of sources to identify ‘fugitive’ gas migration in the oil/gas sector “Geo-CSI” © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 2
  • 3. o  Surface casing used to protect shallow (potable) aquifers o  Gas (and water) in SCVs migrate from deeper zones (cement failure) o  Irregular and low flow rates (can be difficult to sample/monitor) o  How can you determine the source(s) of the leaks? Surface casing vent flow © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 3
  • 4. Geochemical characterizations & forensics o  Gases/fluids for different zones can be ‘fingerprinted’ o  But why do you keep getting burned with this approach? © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 4
  • 5. The geochemistry is never wrong, but the interpretation is often incorrect o  Common problems: o  Sample degraded prior to analysis o  Either the wrong ‘end- members’, or no ‘end- members are used to identify sources o  Numbers are reported that are at or below the detection limits of the instrument © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 5
  • 6. Don’t make assumptions based on regional geochemistry o  Where do the ‘fingerprints’ originate? o  Commercial isotope “databases” often use regional values rather than local values that can mislead interpretations © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 6
  • 7. Need high quality SCV samples o  Can separate and collect gas and liquid o  Gas can be purged to remove “breathing” gas from well o  Need low atmospheric content in gas samples for compositional and isotopic characterization © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 7
  • 8. Sampling can affects water chemistry 0.0001$ 0.001$ 0.01$ 0.1$ 1$ 10$ 100$ 1000$ 10000$ 100000$ Lithium$ Sodium$ Potassium$ Rubidium$ Cesium$ Beryllium$ Magnesium$ Calcium$ Stron=um$ Barium$ Boron$ Aluminum$ Gallium$ Indium$ Thallium$ Silicon$ Germanium$ Tin$ Lead$ Phosphorus$ Arsenic$ An=mony$ Bismuth$ Sulphur$ Selenium$ Tellurium$ Chlorine$ Bromine$ Iodine$ Scandium$ YDrium$ Titanium$ Zirconium$ Vanadium$ Niobium$ Tantalum$ Chromium$ Molybdenum$ Tungsten$ Manganese$ Iron$ Cobalt$ Nickel$ Palladium$ Pla=num$ Copper$ Silver$ Gold$ Zinc$ Cadmium$ Mercury$ Lanthanum$ Cerium$ Praseodymium$ Neodymium$ Samarium$ Europium$ Gadolinium$ Terbium$ Dysprosium$ Holmium$ Erbium$ YDerbium$ Thorium$ Uranium$ BleedNbarrel$ FlowNthrough$Cell$ 1 2 3 4 5 6 7 d-block f-block Group 2 metals and f-block metals lower in bleed barrels - suspended solids settle out in bleed barrel (low energy environment) © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 8
  • 9. Sample integrity: The gas bag •  Over time isotopic composition of methane and CO2 changes •  Methane artificially appears more ‘thermogenic’ •  Shift in CO2 is less predictable •  Manufacturer recommendations - analyze within 48 hours © 2015 Chemistry Matters Inc. *Arrows not to scale WBPC, Regina, SK, April 28-30, 2105 9
  • 10. How can you get it right every time? Mudgas Geochemical Profile Characterized stratigraphy Production and Potential Source Zones: 1.) Fluids 2.) Gases Characterized end-members Shallow Fluids 1.) Surface water 2.) Groundwater Characterized inputs SCVs: What are the Source(s)? 1.) Fluid 2.) Gas GEOCHEMISTRY: © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 10
  • 11. Complex case study: Fluid and gas flows •  Collected four samples from each location: –  SCV gas sample –  SCV liquid sample –  Production casing gas sample –  Production casing liquid sample •  Used local groundwater and deep aquifer wells in region for comparison •  Used perforated wells with DST samples to acquire ‘end- members’ for other potential source zones © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 11
  • 12. No insight from water isotopes o  Water isotopes implicated groundwater sources that conflicted with other indicators (chlorides, TDS, etc.) © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 12
  • 13. A clearer picture with advanced analyses o  Different sources had characteristic ranges of concentrations and isotope values o  Provided first line of evidence to indicate that different source zones can be identified © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 13
  • 14. Identifying source zones o  Fluids provide a line of evidence for potential sources, but they do not provide a refined interpretation © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 14
  • 15. Combined fluid and gas characterization *Exact values property of client, shift in isotope values indicated δ13C Values GASES C1 C2 C3 SCV A - 1.9 B - 2.3 C Casing A* B* C* o  Gases provide a second line of evidence for potential sources and help confirm a production zone leak © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 15
  • 16. Complete geochemistry = complete picture δ13C Values GASES C1 C2 C3 SCV A - 1.9 B - 2.3 C Casing A* B* C* *Exact values property of client, shift in isotope values indicated δ13C Values GASES C1 C2 C3 SCV A - 13.1 B - 8.1 bdl Casing A* B* C*o  Gases provide a second line of evidence to confirm a cretaceous zone leak © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 16
  • 17. δ13C Values GASES C1 C2 C3 SCV A - 13.1 B - 8.1 bdl Casing A* B* C* Identification of depth of source zone o  Mudgas log can refine cretaceous leak to within 200-300m range © 2015 Chemistry Matters Inc. WBPC, Regina, SK, April 28-30, 2105 17
  • 18. Where can it go wrong? •  Similar isotope ‘fingerprints can be expected •  Need to account for this complexity in the interpretation WBPC, Regina, SK, April 28-30, 2105 18
  • 19. Best practices for ‘geoforensics’ •  Collect high quality samples •  Collect samples for potential source(s) and from the production casing (if possible) •  Ask the right questions and get it right ! –  What source zone characterizations were used in the interpretation? –  Where were these source zones characterized (geographically)? –  What are the reliable detection limits for your instrumentation? High quality samples, isotope analysis and accurate interpretation of microbial effects provide more conclusive source determination. WBPC, Regina, SK, April 28-30, 2105 19