Contenu connexe Similaire à Methane forensics techniques for source allocation (20) Plus de Chemistry Matters Inc. (20) Methane forensics techniques for source allocation1. Use of Forensics to Identify
Sources of Methane
Presented by: Court Sandau, PhD, PChem
November 15, 2007
Air and Waste Management Association’s
Vapour Intrusion – A Rapidly Developing Environmental Challenge
1
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3. When to use Environmental Forensics
• When contamination may not
be yours (remove liability)
• When contamination is from
multiple sources (share
liability)
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4. Implicate or Vindicate?
• It may demonstrate your own
responsibility
• It may show dual responsibility
(share the liability)
• It may vindicate a party
completely
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5. Issues of Concern
The client (municipality) has identified fugitive
methane gas in the subsurface soils of several
different areas of the city
• Unknown source
• Concerned residents
• Possible health risks
• Potential legal action
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6. Health Region Guidelines
Subsurface Action Levels
• Further investigation
• Evaluation of indoor levels
• Source removal or ventilation system
• Further investigation
• Monitoring, ventilation recommended
• Immediate building evacuation, call 911
• Further investigation
• Alarm, ventilation system, evacuation
plan for nearby buildings
50,000
(100% LEL)
Indoor Methane
Concentration
(ppm)
5,000
1,000
0
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7. Forensic Geo-Gas Investigation (FGI)
• Collect gas samples
from various origins
• Characterize each
source and create a
reference library
• Establish the
composition and
source of the fugitive
gases through
comparisons with the
reference library
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8. Forensic Geo-gas Investigation
Multidisciplinary Approach to develop lines of
evidence
Measurement and interpretation of
physical and chemical sampling data
Historical documents
Witness and knowledgeable individuals Area of highest
confidence
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12. Case History
Pre 1940’s 1950’s 1960’s 1970’s 1980’s 1990’s 2000’s
1953:
nuisance ground
operation began
1963:
nuisance ground
operation closed
2001-2005:
Phase I&II Site
Investigations
indicate elevated
CH4 Levels
Borrow
Pit/
Natural
Vegetation
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13. Investigation
• Sampling location chosen based on historical data
• 1L gas samples taken from 4 sample locations
• Tiered Forensic Approach adopted to identify
potential sources
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14. Tiered Forensic Approach
Calorific Value (BTU Ft3
)
Hydrocarbon Content
Volatile Organic Carbon Content
Level1
Fixed Gas
Radio Active Isotope (14
C)
Stable Isotope Analysis of CH4
Level2
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15. QA-QC
• Duplicate sample collected at reference library
sampling point
• Relative Percent Differences <20% indicates good
precision
• Lab reported accuracy to within 2% of reference
standards
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16. Level 1: Fixed Gas
Results
Methane and Fixed Gas Data Library
0
10
20
30
40
50
60
70
80
90
100
H
istoric
Landfill
Landfill
Landfill
Sew
age
Sew
age
N
aturalG
as
N
aturalG
as
U
nknow
n
#1
U
nknow
n
#2
Sampling Location
Volume(%)
O2 %
CO2 %
N2 %
CH4%
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17. Level 1: Hydrocarbon Fingerprinting
Results
0
10
20
30
40
50
60
C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15
Alkane
s
Concentrationmg/m3
Natural Gas
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18. Level 1: Hydrocarbon Fingerprinting
Results
0
10
20
30
40
50
60
C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15
Alkanes
Concentrationmg/m3
Landfill
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19. Level 1: Hydrocarbon Fingerprinting
Results
0
10
20
30
40
50
60
C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15
Alkanes
Concentrationmg/m3
Sewage
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20. Level 1: Hydrocarbon Fingerprinting
Results
0
10
20
30
40
50
60
C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15
Alkanes
Concentrationmg/m3
Unknown #1
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21. Level 1: Hydrocarbon Fingerprinting
Results
0
10
20
30
40
50
60
C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15
Alkanes
Concentrationmg/m3
Unknown #2
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22. Level 1: Hydrocarbon Fingerprinting
Results
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23. Level 1: VOC Fingerprinting
Results
0
10
20
30
40
50
60
Volatile Organic Compounds
Concentrationmg/m3
Natural Gas: Alkanes
and Alkenes
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24. Level 1: VOC Fingerprinting
Results
0
10
20
30
40
50
60
Volatile Organic Compounds
Concentrationmg/m3
Sewage: Sulfide
Compounds
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25. Level 1: VOC Fingerprinting
Results
0
10
20
30
40
50
60
Volatile Organic Compounds
Concentrationmg/m3
Landfill: Chlorinated
Compounds
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26. Level 1: VOC Fingerprinting
Results
0
10
20
30
40
50
60
Volatile Organic Compounds
Concentrationmg/m3
Unknown #1
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27. Level 1: VOC Fingerprinting
Results
0
10
20
30
40
50
60
Volatile Organic Compounds
Concentrationmg/m3
Unknown #2
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28. Summary of Level 1 Findings
• 2 locations had elevated levels of CH4
• Based on calorific and fixed gas data
Thermogenic sources were ruled out
• Unable to differentiate landfill, sewage sources
using level 1 investigation
• Need to progress to Level 2
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29. Radio Carbon Isotope Dating 14
C
•Naturally occurring isotope with a half life of
5730 yrs
•The ratio of 14
C contained within CH4 is indicative
of age
50%
Age 5730 yr
100%
Age 0
…
….
25%
Age 11,460 yr
Natural Gas Landfill Sewage Unknown
14
C (pMc) 0 >100 100-110 141
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30. Stable Isotope Analysis
• Highly variable in nature and generally endemic of every
organic compound
• Have been used with petroleum exploration for many
decades, advance is isotope techniques has led to new
areas of applications e.g. archaeology, biomedical
sciences, biosynthesis and environmental forensics
pp
ee--
Hydrogen,1
H
nn
pp
ee--
Deuterium,Deuterium,22
H, DH, D
nn
pp nn
ee--
Tritium,Tritium,33
H, TH, T
99
%
~1
%
<1
%
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31. Clarke Diagram for 2D Fingerprinting
δ13
C-CH4(‰)
Bacterial MF
δ2
H-CH4 (‰)
Bacterial
Carbonate
Reduction
Bacterial
M
ixand
Transition
Early Mature
Thermogenic
migration
Bacterial Oxidation
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32. Combination of Techniques
δ13
C-CH4 (‰)
C1/[C2+C3]
Sewage
Plant
Sewage
Plant
Unknown
Unknown
Landfill
Landfill
Historic
Landfill
Natural Gas
Natural Gas
Bacterial consumption of Methane will cause a
reduction in Methane concentration and
isotopic shift
Migration will cause a change in methane
concentration but not a large isotopic shift
Migration
Migration
Oxidation
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33. Summary
Source
Calorifi
c Value
(BTU/Ft
3
)
CH4
/CO
2
GC Carbon
Analysis
VOC
14
C –
pMC
δ13
C and δ2
H of CH4
Thermogenic ~ 1000 + CH4
Low C1
/C1
– C5 Odorants 0 pMC
δ13
C = -48‰ to -40‰
δ2
H = -250‰ to -200‰
Landfill ~600
CO2
=
CH4
High C1
/C1
– C5
chlorinated
compounds
>100
pMC
δ13
C = -60‰ to -52‰
δ2
H = -400‰ to
-350‰
Sewage ~600
CO2
=
CH4
High C1
/C1
– C5
Sulphur
containing
100
-110
pMC
δ13
C = -52‰ to -48‰
δ2
H = -425‰ to
-375‰
Unknown1 ~447
CO2
<
CH4
High C1
/C1
– C5 ND
141
pMC
δ13
C = -54.5‰
δ2
H = -346‰
Unknown2 ~26
CO2
=
CH4
High C1
/C1
– C5 ND
101
pMC
δ13
C = -51.5‰
δ2
H = -341‰
Level 1 Level 2
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34. Summary
Source
Calorifi
c Value
(BTU/Ft
3
)
CH4
/CO
2
GC Carbon
Analysis
VOC
14
C –
pMC
δ13
C and δ2
H of CH4
Thermogenic ~ 1000 + CH4
Low C1
/C1
– C5 Odorants 0 pMC
δ13
C = -48‰ to -40‰
δ2
H = -250‰ to -200‰
Landfill ~600
CO2
=
CH4
High C1
/C1
– C5
chlorinated
compounds
>100
pMC
δ13
C = -60‰ to -52‰
δ2
H = -400‰ to
-350‰
Sewage ~600
CO2
=
CH4
High C1
/C1
– C5
Sulphur
containing
100
-110
pMC
δ13
C = -52‰ to -48‰
δ2
H = -425‰ to
-375‰
Unknown1 ~447
CO2
<
CH4
High C1
/C1
– C5 ND
141
pMC
δ13
C = -54.5‰
δ2
H = -346‰
Unknown2 ~26
CO2
=
CH4
High C1
/C1
– C5 ND
101
pMC
δ13
C = -51.5‰
δ2
H = -341‰
Level 1 Level 2
Potentially a mixed source
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35. Conclusion
• Main Issue for client was identification of potential sources of
fugitive methane emissions
• Outcomes
– Generation of Library
– Use of historical data and Level 1 analysis eliminated
thermogenic sources
– Level 2 data indicate degradation of landfill material may be
responsible for methane found at sampling point with highest
concentration
– Second sampling point likely to be of a mixed source with landfill
and organic soils contributing
• Further monitoring may determine the fate and behavior of
elevated methane which will help clients to make decision
regarding any action needed
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36. Contact Info:
Chemistry Matters Inc.
Court Sandau
Cell: 1.403.669.8566
Email: csandau@chemistry-matters.com
URL: chemistry-matters.com
Twitter: @Chem_Matters
Slideshare: www.slideshare.net/csandau
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