Environmental Forensics R Paul Philp School of Geology
- Slides: 56
Environmental Forensics R. Paul Philp, School of Geology and Geophysics, University of Oklahoma, Norman, OK. 73019
Environmental Forensics • What is “Environmental Forensics”? • “Environmental Forensics” can be defined as a scientific methodology developed for identifying petroleum-related and other potentially hazardous environmental contaminants and for determining their sources and time of release. It combines experimental analytical procedures with scientific principles derived from the disciplines of organic geochemistry and hydrogeology. Environmental Forensics provides a valuable tool for obtaining scientifically proven, court admissible evidence in environmental legal disputes. • Much of the information required in this approach will not be obtained from the data obtained using the conventional EPA methods 2
Crude Oils and Related Products
Basic Environmental Forensic Questions • What is the product? • Is there more than one source and, if so, which one caused the problem? • How long has it been there? • Is it degrading?
Fingerprinting and Correlation • What are the most commonly used techniques for such purposes? Gas chromatography Mass Spectrometry Gas chromatography-Isotope Ratio Mass Spectrometry (GCIRMS) 5
GC Fingerprints of Different Products Condensate 0 7 14 21 28 35 42 49 56 JP 4 63 70 70 0 7 14 21 28 35 Gasoline 0 7 14 21 28 35 42 49 56 63 70 Minutes Diesel 56 63 0 7 14 21 28 35 42 Minutes 49 56 63 70
GC Fingerprints of different products • Although GC permits product identification, many gasoline samples, for example, will be chromatographically similar, even if from different sources. • Refined products generally do not contain biomarkers making GCMS of little consequence. • If refined products are from different sources, stable isotopes may provide a potential solution. Minutes
Crude Oil Chromatogram C 17 Pristane Phytane 0 C 35
Biomarker Distributions
Utilization of Stable Isotopes • What is the product? NO • Is there more than one source and, if so, which one caused the problem? YES • How long has it been there? NO • Is it degrading? YES
Utilization of Stable Isotopes Why do compounds derived from different feedstocks have different isotope values?
Carbon Isotopes • Carbon in fossil fuels is initially derived from atmospheric CO 2. During photosynthesis, fractionation of the two isotopes occurs with preferential assimilation of the lighter isotopes. 12
Carbon Isotopes • Extent of fractionation during photosynthesis depends on factors such as: plant type; marine v. terrigenous; C 3 v. C 4 plant types; temperature; sunlight intensity; water depth. • (C 3 Temperate plants; trees; not grasses; 95% plant species -22 to -30; C 4 plants grasses; sugar cane; corn; higher temps and sunlight 10 to -14 per mil) 13
Stable Isotope Determinations ISOTOPIC VALUES CAN BE MEASURED IN TWO WAYS: • BULK ISOTOPES • ISOTOPIC COMPOSITIONS OF INDIVIDUAL COMPOUNDS 14
Isotope Values of Crude Oils Vary with Source d 13 C -35 -30. 06 -30 -29. 52 -29. 68 -29. 50 -25. 66 -25 -23. 45 -23. 27 -20 Monterey Crude Katalla Crude Cook Inlet Crude North Slope Crude Unknown Source Monterey Source NSC Source Petroleum Source 15
d 13 C of Saturates (‰, PDB) Correlations Using Carbon Isotopes BP “American Trader” Accident 5/7/90 - Huntington Beach, CA California Crude Oils Other Southern California Beach Tars Alaska Crude Oils Huntington Beach Tars and Spilled Oil d 13 C of Aromatics (‰, PDB) 16
Correlation Using Bulk Isotope Ratios MW-2 d. D (‰) MW-5 MW-11 MW-4 Brand A Gasoline Brand B Gasoline d 13 C (‰) Contamination in monitoring wells had two possible sources; GC fingerprints were similar since both were contemporary gasolines; isotopically distinct since derived from different crude oils
EXXON VALDEZ • March 24 th, 1989 • 258, 000 barrels of Alaskan North Slope crude oil spilled into Prince William Sound
Residues from Prince William Sound
Terpanes in Prince William Sound Residues -24. 5 -24. 1 -29. 1 -28. 7
Stable Isotope Determinations ISOTOPIC VALUES CAN BE MEASURED IN TWO WAYS: • BULK ISOTOPES • ISOTOPIC COMPOSITIONS OF INDIVIDUAL COMPOUNDS 21
GCIRMS System
Crude Oil Chromatogram C 17 Pristane Phytane C 35 0 23
GCIRMS DATA FOR SELECTED OILS 36 D 24 D C 35 C 33 C 31 C 29 C 27 C 25 C 23 C 21 C 19 C 17 C 15 C 13 n-alkanes -25 -26 -27 -28 d 13 C (‰) -29 -30 -31 -32 U 8 -106 -1 Paris Basin Middle East -33 Oklahoma -34 -35 Mahakam 24
Hydrocarbon Spills and Weathering • Major effects of weathering from a geochemical perspective are : – Evaporation – Water washing – Biodegradation 25
Tar Ball Chromatograms 26
Terpanes in Tar Ball Samples C 29 -Hop. C 30 -Hop. 18 a-Oleanane 27
GCIRMS – Tar Balls 28
The Erika Oil Spill. Sampling locations of oil residues and oiled bird feathers collected along the Atlantic Coast of France after the Erika oil spill. Mazeas et al. , EST, 36(2), 130 -137, 2002 29
The Erika Oil Spill. Bulk isotope values 30
The Erika Oil Spill. Molecular n-alkane isotopic compositions of the oil residues collected in the north Atlantic shoreline (mean of S 2 -S 12), on the Crohot Beach (S 13), in the Arcachon Bay area (mean of S 14 -S 18), and of bird feathers (mean of S 19 -S 28) are compared with 31 Erika oil.
The Erika Oil Spill. Compound specific isotopic composition of oil residues and oiled bird feathers collected along the Atlantic Coast of France compared with Erika oil isotopic composition. 32
Diesel Fingerprints 33
Isoprenoid Isotope Fingerprints California Oklahoma 34
Forensic Geochemistry B Site A MW 1 Groundwater flow direction C MW 6 Site B 35
Weathered and Unweathered Diesel MW 1 * * * Diesel MW 6 Pr* * Ph* C 17 36
Carbon Isotope Values for Isoprenoids 37
Gasolines • Gasolines from different sources often have very similar chromatograms, making it difficult to distinguish such samples • Gasolines are also devoid of biomarkers, further limiting correlation possibilities • One solution here is to use GCIRMS for both the hydrocarbons and additives
Comparison of Gasolines by GC 39
Gasoline Database 117 122 30 83 144 94 31 97 78 52 102 6667 62 90 89 91 148 126 118 135 109 107 133113 151 152 123 119 Retail stations locations 143 149 150 114 136 Aromatics δ 13 C + d. D, oxygenates (MTBE, TBA) 108 138 Samples provided by Dr. J. Graham Rankin, Marshall University, WV 138 Aromatics δ 13 C only 108 40
δ 13 C Fingerprints of 39 Gasolines -22 Crude oil feedstock variable Trend reflects the manufacturing process -23 δ 13 C offset reflects the crude oil feedstock -25 -26 -27 -28 H A ap h N z pr o. B B TM 1, 2, 3 - 3 e Bz 1 m 2 e Bz 1 m EB o. X TM B L 1, 2, 4 - TO /p -X m TM B -29 1, 3, 5 - δ 13 C (‰) -24 41
CSIA of Gasoline 1, 2, 4 trimethylbenzene δ 13 C = – 26. 7 ‰ ethylbenzene δ 13 C = – 24. 6 ‰ m, p-xylene δ 13 C = – 26. 0 ‰ o-xylene δ 13 C = – 25. 1 ‰
Gasolines – GC Signals mp-Xyl A B 1, 2, 4 -TMB
1, 1, 44 H A ap h N z pr o. B B -T M 3 e Bz 1 m 2, 3 EB o. X 2 e Bz 1 m L B -T M 2, 4 TO /p -X m B -T M 3, 5 δ 13 C (‰) Gasolines – Different δ 13 C Fingerprints -22 A -23 -24 -25 B -26 -27 -28 -29 -30
PCE Degradation Site Study Hunkeler et al. , J. Contaminant Hydrology, 74, 265 -282, 2004.
PCE Source Evaluation Study -33 -27 Hunkeler et al. , J. Contaminant Hydrology, 74, 265 -282, 2004. -25
PCBs • Study by Yanik et al. , OG, 239 -253, 34, 2003 showed that different Aroclors may be isotopically different and thus useful for source discrimination although there is some slight enrichment from degradation. 47
M/z 44 Chromatogram for Aroclor 1245 48
Variations in Isotopic Composition of Various Congeners 49
PAHs and Stable Isotopes • Current interest is centered around whether carbon isotopes can be used to discriminate PAHs derived from former manufactured gas plant (MGP) wastes versus those from general urban background aromatics • Urban backgrounds have a fairly narrow range and small differences may be related to source differences 50
Sources of PAHs to Urban Background Mixed Pyrogenic and Petrogenic Sources 51
PAHs-Combined GC and GCIRMS Data 08 07 52
Benzo(G, H, I) perylene Pyrene Acenaphthalene Naphthalene PAHs-Combined GC and GCIRMS Data 02 08 08
CSIRs of NAPL Samples 54
PAH Fingerprints and Isotopes Show No MGP Contribution to Background MT 03, MT 07, MT 09, MT 10 – background soil samples from town MT NAPL – tar from MGP site in town TPAH-ug/kg Fl/Py MT 03 2, 510 1. 177 MT 07 11, 100 1. 136 MT 09 3, 880 1. 194 MT 10 6, 940 1. 208 MT NAPL 0. 64 55
Summary • Environmental Forensics combines a variety of analytical tools to typically provide information on origin and state of contaminants in the environment. • One of these tools involves utilization of stable isotopes. • In some situations stable isotope data compliments other analytical data. In other cases may be only tool available.
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