Thiols
(or mercaptans) in crude oils have been considered to be
associated with thermochemical sulfate reduction (TSR). However, the
molecular composition and the formation mechanism of thiols in crude
oils are not clear. This study provides the molecular composition
of thiols in several deep strata condensate oils (condensates) from
the Tarim Basin. Selective Michael addition products of thiols were
characterized using Fourier transform ion cyclotron resonance mass
spectrometry (FT-ICR MS) and comprehensive two-dimensional gas chromatography–MS
(GC × GC MS). The carbon numbers and double bond equivalents
of the thiols ranged between 4–20 and 0–10, respectively.
Abundant diamondoidthiols found in two condensates were from high-temperature
reservoirs. Various thiol compounds with multiple heteroatoms (S2, S3, S1O1, S1O2, and S2O1 class species) were
detected in two other condensates, and low reservoir temperature made
it possible to prevent the depletion of the multiple-heteroatom thiols.
The pronounced 34S enrichment in H2S and high
abundance of thiadiamondoids indicate that four condensates were originally
sourced from Cambrian strata and suffered severe TSR alteration. The
pathway of thiol formation was speculated as follows: TSR-generated
H2S reacts with petroleum hydrocarbons. Deep Cambrian strata
in the Tarim Basin has the potential of being a huge hydrocarbon resource,
although the high maturity and TSR alteration may negatively impact
the quantity and quality of reserves and lead to a high H2S content. The results presented here provide new insights into the
TSR reaction, which may assist deep oil exploration and facilitate
evaluation of the extent of TSR alteration.