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Structure Evolution of Organic Compounds in Shale Plays by Spectroscopy (1H & 13C−NMR, XPS, and FTIR) Analysis

preprint
revised on 04.03.2020 and posted on 06.03.2020 by Hyeonseok Lee, Nuri Oncel, Mohammadreza Shokouhimehr, Mehdi Ostadhassan, Bo Liu, Rajender S. Varma
Amorphous organic matter in geomaterials also known as kerogen undergoes significant alteration in chemical structure during thermal maturation which is characterized using a combination of solid−state 1H & 13C−NMR, X−ray photoelectron spectroscopy (XPS), and Fourier transform infrared (FTIR) techniques.

History

Email Address of Submitting Author

hlee104@hawk.iit.edu

Institution

University of North Dakota

Country

United States

ORCID For Submitting Author

0000-0002-9808-2272

Declaration of Conflict of Interest

no conflict of interest

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