Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method

The thermal maturity of shale is often measured by vitrinite reflectance (VRo). VRo measurements for the Devonian–Mississippian black shale source rocks evaluated herein predicted thermal immaturity in areas where associated reservoir rocks are oil-producing. This limitation of the VRo method led to...

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Main Authors: Jason S. Lupoi, Luke P. Fritz, Thomas M. Parris, Paul C. Hackley, Logan Solotky, Cortland F. Eble, Steve Schlaegle
Format: Article
Language:English
Published: Frontiers Media S.A. 2017-09-01
Series:Frontiers in Energy Research
Subjects:
Online Access:http://journal.frontiersin.org/article/10.3389/fenrg.2017.00024/full
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spelling doaj-18d6b35f62a848b5b77035066c3b23d02020-11-24T22:57:51ZengFrontiers Media S.A.Frontiers in Energy Research2296-598X2017-09-01510.3389/fenrg.2017.00024284690Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting MethodJason S. Lupoi0Luke P. Fritz1Thomas M. Parris2Paul C. Hackley3Logan Solotky4Cortland F. Eble5Steve Schlaegle6RJ Lee Group, Inc., Monroeville, PA, United StatesRJ Lee Group, Inc., Monroeville, PA, United StatesKentucky Geological Survey, University of Kentucky, Lexington, KY, United StatesU.S. Geological Survey, Reston, VA, United StatesRJ Lee Group, Inc., Monroeville, PA, United StatesKentucky Geological Survey, University of Kentucky, Lexington, KY, United StatesRJ Lee Group, Inc., Monroeville, PA, United StatesThe thermal maturity of shale is often measured by vitrinite reflectance (VRo). VRo measurements for the Devonian–Mississippian black shale source rocks evaluated herein predicted thermal immaturity in areas where associated reservoir rocks are oil-producing. This limitation of the VRo method led to the current evaluation of Raman spectroscopy as a suitable alternative for developing correlations between thermal maturity and Raman spectra. In this study, Raman spectra of Devonian–Mississippian black shale source rocks were regressed against measured VRo or sample-depth. Attempts were made to develop quantitative correlations of thermal maturity. Using sample-depth as a proxy for thermal maturity is not without limitations as thermal maturity as a function of depth depends on thermal gradient, which can vary through time, subsidence rate, uplift, lack of uplift, and faulting. Correlations between Raman data and vitrinite reflectance or sample-depth were quantified by peak-fitting the spectra. Various peak-fitting procedures were evaluated to determine the effects of the number of peaks and maximum peak widths on correlations between spectral metrics and thermal maturity. Correlations between D-frequency, G-band full width at half maximum (FWHM), and band separation between the G- and D-peaks and thermal maturity provided some degree of linearity throughout most peak-fitting assessments; however, these correlations and those calculated from the G-frequency, D/G FWHM ratio, and D/G peak area ratio also revealed a strong dependence on peak-fitting processes. This dependency on spectral analysis techniques raises questions about the validity of peak-fitting, particularly given the amount of subjective analyst involvement necessary to reconstruct spectra. This research shows how user interpretation and extrapolation affected the comparability of different samples, the accuracy of generated trends, and therefore, the potential of the Raman spectral method to become an industry benchmark as a thermal maturity probe. A Raman method devoid of extensive operator interaction and data manipulation is quintessential for creating a standard method.http://journal.frontiersin.org/article/10.3389/fenrg.2017.00024/fullRaman spectroscopyshalethermal maturityvitrinite reflectancepeak-fitting
collection DOAJ
language English
format Article
sources DOAJ
author Jason S. Lupoi
Luke P. Fritz
Thomas M. Parris
Paul C. Hackley
Logan Solotky
Cortland F. Eble
Steve Schlaegle
spellingShingle Jason S. Lupoi
Luke P. Fritz
Thomas M. Parris
Paul C. Hackley
Logan Solotky
Cortland F. Eble
Steve Schlaegle
Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
Frontiers in Energy Research
Raman spectroscopy
shale
thermal maturity
vitrinite reflectance
peak-fitting
author_facet Jason S. Lupoi
Luke P. Fritz
Thomas M. Parris
Paul C. Hackley
Logan Solotky
Cortland F. Eble
Steve Schlaegle
author_sort Jason S. Lupoi
title Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
title_short Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
title_full Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
title_fullStr Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
title_full_unstemmed Assessment of Thermal Maturity Trends in Devonian–Mississippian Source Rocks Using Raman Spectroscopy: Limitations of Peak-Fitting Method
title_sort assessment of thermal maturity trends in devonian–mississippian source rocks using raman spectroscopy: limitations of peak-fitting method
publisher Frontiers Media S.A.
series Frontiers in Energy Research
issn 2296-598X
publishDate 2017-09-01
description The thermal maturity of shale is often measured by vitrinite reflectance (VRo). VRo measurements for the Devonian–Mississippian black shale source rocks evaluated herein predicted thermal immaturity in areas where associated reservoir rocks are oil-producing. This limitation of the VRo method led to the current evaluation of Raman spectroscopy as a suitable alternative for developing correlations between thermal maturity and Raman spectra. In this study, Raman spectra of Devonian–Mississippian black shale source rocks were regressed against measured VRo or sample-depth. Attempts were made to develop quantitative correlations of thermal maturity. Using sample-depth as a proxy for thermal maturity is not without limitations as thermal maturity as a function of depth depends on thermal gradient, which can vary through time, subsidence rate, uplift, lack of uplift, and faulting. Correlations between Raman data and vitrinite reflectance or sample-depth were quantified by peak-fitting the spectra. Various peak-fitting procedures were evaluated to determine the effects of the number of peaks and maximum peak widths on correlations between spectral metrics and thermal maturity. Correlations between D-frequency, G-band full width at half maximum (FWHM), and band separation between the G- and D-peaks and thermal maturity provided some degree of linearity throughout most peak-fitting assessments; however, these correlations and those calculated from the G-frequency, D/G FWHM ratio, and D/G peak area ratio also revealed a strong dependence on peak-fitting processes. This dependency on spectral analysis techniques raises questions about the validity of peak-fitting, particularly given the amount of subjective analyst involvement necessary to reconstruct spectra. This research shows how user interpretation and extrapolation affected the comparability of different samples, the accuracy of generated trends, and therefore, the potential of the Raman spectral method to become an industry benchmark as a thermal maturity probe. A Raman method devoid of extensive operator interaction and data manipulation is quintessential for creating a standard method.
topic Raman spectroscopy
shale
thermal maturity
vitrinite reflectance
peak-fitting
url http://journal.frontiersin.org/article/10.3389/fenrg.2017.00024/full
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