4.6 Article

Thermal simulation experimental study on the difference of molecular structure evolution between vitrinite and inertinite in low-rank coal

Journal

FRONTIERS IN EARTH SCIENCE
Volume 10, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2022.992017

Keywords

vitrinite; inertinite; macromolecular structure; thermal simulation; coalification

Funding

  1. National Key Research and Development Plan of China
  2. National Natural Science Foundation of China
  3. [2021YFC2902004]
  4. [42072197]
  5. [41902170]
  6. [41972174]

Ask authors/readers for more resources

The study revealed significant differences in the chemical structure evolution of vitrinite and inertinite during coalification. The structure parameters of inertinite were consistently larger than vitrinite, while certain parameters were consistently smaller in inertinite compared to vitrinite.
In order to carry out an in-depth study of the differences in the molecular structure evolution of the vitrinite and the inertinite during coalification, the chemical structure of 13 groups of vitrinite and inertinite with different coal ranks were comprehensively characterized using X-ray diffraction (XRD), Fourier transform infrared (FTIR) spectroscopy, and C-13 nuclear magnetic resonance (C-13 NMR). The correlation of structure parameters and vitrinite random reflectance (R (o, ran)) were analyzed. The results show that three evolution stages of vitrinite were observed with R (o, ran) at 0.35%-0.90%, 1.20%-2.67%, and 3.03%-4.20%, and two evolution stages of inertinite were marked with R (o, ran) at 0.35%-2.07% and 2.07%-4.20%. The f (a), DOC, I, f (a)', f (a) (H), f (a) (N), f (a) (B), X-b, L-a, L-c, and N-ave of inertinite are always larger than vitrinite, whereas the A(CH2)/(CH3), f (al), f (al) *, f (al) (H), d(002) of inertinite are always smaller than vitrinite. When R (o, ran) = 0.35%-0.90%, the oxygen-containing functional groups and aliphatic structure of vitrinite fall off rapidly, the condensation degrees of the aromatic ring, L-a, L-c, and N-ave increase, whereas the lengths of side chains and d(002) decrease. When R (o, ran) = 1.20%-2.67%, the vitrinite structure variation follows the same trend as the first stage, but the evolution rate is significantly lower. When R (o, ran) = 0.35%-2.07%, the oxygen-containing functional groups, methyl groups, and methylene groups of inertinite fall off at a slower rate than those of vitrinite. The aromaticity, condensation degree, aromatic carbon content, and order degree of microcrystalline structure also increase at a rate less than that of vitrinite. The vitrinite and inertinite structure variation becomes flat, and the structures of both macerals are similar in the high metamorphic stage. The content of oxygen-containing functional groups and aliphatic chain length decrease to the lowest, whereas the aromaticity increases to the maximum. This study contributes to a comprehensive understanding of the chemical structure differences between vitrinite and inertinite, which can provide a theoretical reference for the clean utilization of coal and coalbed methane (CBM) exploration and development.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.6
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available