Nitrogen is an important component of petroleum systems.
However,
nitrogen loss and fractionation processes during the thermal evolution
of organic matter are not conclusive. Moreover, current studies have
focused mainly on single components, such as bulk rock, kerogen, or
crude oil, but the relationships between them have not been systematically
studied. A series of hydrothermal experiments were conducted, and
data were collected from 69 geological samples. The results illustrate
that the nitrogen isotope compositions (δ15N) of
different nitrogen-containing components vary with simulated temperature.
The δ15Nex‑bulk (δ15N of bulk rock after extraction) continuously increased, with the
largest change reaching 2.4‰. The δ15Nkerogen (δ15N of kerogen) basically remained
constant until 400 °C (R
o < 1.78%),
and the δ15Noil (δ15N
of expelled oil) changed by only 0.6‰ throughout the oil generation
phase. A comparison of the data for δ15Nex‑bulk and δ15Nkerogen reveals that the relationship
between them is affected by thermal evolution. Below 400 °C,
the δ15Nkerogen value is greater than
δ15Nex‑bulk, and these differences
decrease with increasing temperature. However, above 400 °C,
the relationship reverses to δ15Nkerogen lower than δ15Nex‑bulk, and the
difference between them increases with the temperature. The difference
between them can serve as a rough maturity indicator. In addition,
the comparison of δ15Noil and δ15Nkerogen reveals that thermal evolution has little
effect on the δ15Noil, which indicates
that the δ15Noil has the potential to
preserve the original information on organic matter.