Abstract
Although long-chain aliphatic hydrocarbons are documented in meteorites, their origin is poorly understood. A key question is whether they are pristine or a byproduct of terrestrial alteration? To understand if these long-chain hydrocarbons are indigenous, it will be important to explore their thermodynamic and mechanical stability at conditions experienced by extraterrestrial objects during atmospheric entry and passage. Extreme pressures and temperatures experienced by meteorites are likely to alter the molecular organization of these long-chain hydrocarbons. These structural changes associated with extreme conditions are often documented via laboratory-based Raman spectroscopic measurements. So far, Raman spectroscopic measurements have investigated the effect of static compression on the aliphatic hydrocarbons. The effect of temperature on the structural changes remains poorly explored. To bridge this gap, in this study, we have explored the behavior of two aliphatic hydrocarbons at simultaneously high pressures and temperatures. We have used a resistively heated diamond anvil cell. On compression to moderate pressures, the appearance of new vibrational modes in the low-energy region confirms prior studies and is related to the bending of the linear chains. Upon heating to ∼ 220 °C, we note that the new low-energy mode undergoes softening. The mode softening is likely due to the combination of unbending of the alkane chain and mode anharmonicity.
Original language | English |
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Pages (from-to) | 2530-2537 |
Number of pages | 8 |
Journal | Journal of Physical Chemistry B |
Volume | 126 |
Issue number | 13 |
DOIs | |
State | Published - Apr 7 2022 |
Funding
Notice of Copyright: This manuscript has been authored by UT-Battelle, LLC under contract no. DE-AC05-00OR22725 with the U.S. Department of Energy. The United States Government retains, and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a non-exclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The Department of Energy will provide public access to these results of federally sponsored research, in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ). Acknowledgments This work is funded by the National Science Foundation (NSF) (EAR 1753125, 1638752, and 1248553). A.B. acknowledges the Dean’s Teaching Postdoctoral Fellowship from the College of Arts and Sciences, Florida State University. B.H. and R.B. were supported by resources at the Spallation Neutron Source and the High Flux Isotope Reactor, DOE Office of Science User Facilities operated by the Oak Ridge National Laboratory (ORNL). This work is funded by the National Science Foundation (NSF) (EAR 1753125, 1638752, and 1248553). A.B. acknowledges the Dean???s Teaching Postdoctoral Fellowship from the College of Arts and Sciences Florida State University. B.H. and R.B. were supported by resources at the Spallation Neutron Source and the High Flux Isotope Reactor DOE Office of Science User Facilities operated by the Oak Ridge National Laboratory (ORNL).
Funders | Funder number |
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College of Arts and Sciences Florida State University | |
High Flux Isotope Reactor DOE Office of Science | |
National Science Foundation | 1248553, 1638752, EAR 1753125 |
U.S. Department of Energy | |
Office of Science | |
Oak Ridge National Laboratory | |
Florida State University | |
College of Arts and Sciences, Boston University |