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SPME Coupled with GC-FID for the Detection of n-Propyl Alcohol and Its Use as a Geothermal Tracer. Michael Mella 1,2 1 Energy and Geoscience Institute - University of Utah, 2 Chemical Engineering Department – University of Utah Senior Projects Lab I - 2006. Why n-propanol?.
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SPME Coupled with GC-FID for the Detection of n-Propyl Alcohol and Its Use as a Geothermal Tracer Michael Mella1,2 1 Energy and Geoscience Institute - University of Utah, 2 Chemical Engineering Department – University of Utah Senior Projects Lab I - 2006
Why n-propanol? • Liquid phase only tracers and vapor phase only tracers are in common use • Two-phase tracers are needed to better trace water • n-Propanol has a similar partition coefficient to water, similar two-phase characteristics to water
Objectives • Lab work - Develop an analytical method to reduce the limit of detection of n-propanol • Field work - Validate method with a field test
Lab Development • Solid Phase MicroExtraction (SPME) was used to help lower the limit of detection over previous methods by 30 fold • Gas Chromatography with a Flame Ionization Detector used to analyze n-propanol solutions
SPME basics • A flexible fiber coated with 85µm thick Carboxen/PDMS layer • A needle that houses the fiber and an injection assembly
GC analysis • Needle injected into 300°C GC inlet • Separation by HP-5 capillary column • Detection by FID • Analysis of signal using HP-CHEM software
Analytical method results • Limit of detection at 1 ppb • Reduction by a factor of 30 from previous methods • Lower limit of detection means less n-propanol needed for test • Method can be extended to other alcohols and aldehydes
Objectives • Lab work - Develop an analytical method to reduce the limit of detection of n-propanol • Field work - Validate method with a field test
Field test • Injector 34-9RD2 of Coso East Flank tagged with 165 gallons n-propanol • Samples taken from surrounding East Flank producers
Field Work • Alcohol returns • Comparison with a liquid tracer test
Alcohol returns • Raw results • E(t) scaled results and recovery • Liquid phase tracer results
Alcohol returns • Raw results • E(t) scaled results and recovery • Liquid phase tracer results
E(t) • E(t) residence-time distribution function • E(t) is a way to normalize for mass of tracer injected and flow rates • E(t) required for future assessment of return data, an example is the convolution integral and tracer recovery
Tracer Recovery • Use E(t) to calculate the amount of tracer recovered in both the liquid phase and the vapor phase.
Alcohol returns • Raw results • E(t) scaled results and recovery • Liquid phase tracer return
Liquid phase tracer return • 2 months prior 100 kg 1,3,5-NTS injected into 34-9RD2 • Samples from the same area were taken and analyzed by HPLC with a fluorescence detector
Return comparisons • Normalized n-propanol and 1,3,5-NTS return curves were plotted together with a common x-axis of days after their respective injection date.
Return comparisons • Tracer recovery of n-propanol = 3.5% • Tracer recover of 1,3,5-NTS = 74.8%
Conclusions • Similar arrival times for 1,3,5-NTS and n-propanol in well 38C-9 • Appearance of n-propanol in 38D-9 but not 1,3,5-NTS • 38B-9 seems to have been “skipped” by both tracers • Less return of n-propanol than of 1,3,5-NTS
Conclusions • Similar arrival times for 1,3,5-NTS and n-propanol in well 38C-9 • Appearance of n-propanol in 38D-9 but not 1,3,5-NTS • 38B-9 seems to have been “skipped” by both tracers • Less return of n-propanol than of 1,3,5-NTS
Conclusions • Similar arrival times for 1,3,5-NTS and n-propanol in well 38C-9 • Appearance of n-propanol in 38D-9 but not 1,3,5-NTS • 38B-9 seems to have been “skipped” by both tracers • Less return of n-propanol than of 1,3,5-NTS
Conclusions • Similar arrival times for 1,3,5-NTS and n-propanol in well 38C-9 • Appearance of n-propanol in 38D-9 but not 1,3,5-NTS • 38B-9 seems to have been “skipped” by both tracers • Less return of n-propanol than of 1,3,5-NTS
Conclusion • Lab work - n-propanol is appropriate as a geothermal tracer in smaller volume by using SPME-GC-FID • Lab work - Alcohols can be a powerful tool in determining two-phase pathways in reservoirs
Acknowledgements This work was supported by grants from the Department of Energy. Done with the support of Coso Operating Company, LLC; and the Geothermal Program Office of the Naval Air Weapons Station.
Acknowledgements Peter Rose1, Nick Dahdah1, Michael Adams1, Jess McCulloch2, Cliff Buck2, and G. Michael Shook3 1 Energy and Geoscience Institute – University of Utah 2 Coso Operating Company – Catihness Energy LLC 3 Idaho National Laboratory
References Adams, M.C., Yamada, Y., Yagi, M., Kondo, T., and Wada, T. (2000), “Stability of Methanol, Propanol, and SF6 as High-Temperature Tracers,” World Geothermal Congress p. 3015-3019 Adams, M.C., Yamada, Y., Yagi, M., Kasteler, C., Kilbourn, P., and Dahdah, N. (2004), “Alcohols as Two-Phase Tracers,” Proceedings, Twenty-Ninth Workshop on Geothermal Reservoir Engineering Fogler, H.S. Elements of Chemical Reaction Engineering. 3rd Edition, New Jersey: Prentice Hall, 1999, chapter 13. Fukuda, D., Asanuma, M., Hishi, Y., Kotanaka, K. (2005), “Alcohol Tracer Testing at the Matsukawa Vapor-Dominated Geothermal Field, Northeast Japan,” Proceedings, Thirtieth Workshop on Geothermal Reservoir Engineering
References Mella, M.J., Rose, P.E., McCulloch, J., Buck, C., Adams, M.C., Dahdah, N.F. (2006), “The Use of n-Propanol as a Tracer at the site of the Coso Engineered Geothermal System,” PROCEEDINGS, Thirty-First Workshop on Geothermal Reservoir Engineering Stanford University,SGP-TR-179 Rose, P.E., Mella, M.J., Kasteler, C. (2003), “A New Tracer For Use in Liquid-Dominated, High-Temperature Geothermal Reservoirs,” GRC Transactions, 27, pp. 403-406 Supelco (2003), Chromatography Products for analysis and Purification. Supelco p. 348-358