Octadecane (C18H38) is an aliphatic hydrocarbon
that is abundant in carbonaceous chondritic meteorites. It is debated
whether these hydrocarbons found in the meteorite are pristine or
are a result of subsequent modifications as these meteorites are delivered
to the Earth. It is well-known that meteorites are often subjected
to extreme pressures and temperatures upon entering the Earth’s
atmosphere. To explore the behavior of octadecane at high pressures,
that is, how its molecular structure responds to compression, we use
a diamond anvil cell in conjunction with Raman spectroscopy. We find
that at room temperatures, upon compression to ∼5 GPa, a linear-chain
octadecane molecule transforms into a bent-chain configuration. Similar
transitions from linear to a bent configuration in other hydrocarbons
have been documented. We find a linear correlation between the transition
pressure from linear to bent configuration, and the chain length of
the alkane, that is, longer chain lengths, is likely to be less stable
in the linear configuration under compression. These kinks in the
bent-chain configuration are likely sites for the dissociation of
the longer chain hydrocarbons to smaller hydrocarbons. The octadecane
sample examined in this study did not undergo any additional transition
to the highest pressure (∼18 GPa) explored in this study.