TY - JOUR
T1 - Molecular structure controls on micropore evolution in coal vitrinite during coalification
AU - Liu, Yu
AU - Zhu, Yanming
AU - Liu, Shimin
AU - Chen, Shangbin
AU - Li, Wu
AU - Wang, Yang
N1 - Funding Information:
The authors are sincerely thankful for the financial support of the National Natural Science Foundation of China (No. 41472135 , No. 41702167 , No. 41772141 ), the National Postdoctoral Program for Innovative Talents ( BX201700282 ), the Natural Science Foundation of Jiangsu Province ( BK20181362 ), the China Postdoctoral Science Foundation ( 2017M621870 ), and the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD).
Publisher Copyright:
© 2018 Elsevier B.V.
PY - 2018/11/1
Y1 - 2018/11/1
N2 - Micropores (<2 nm) play an important role in coalbed methane adsorption, desorption, and diffusion. However, the mechanisms of micropore formation and evolution still need further study. This study primarily focuses on molecular structure controls on micropore evolution during coalification. CO2 adsorption experiments were employed to characterize micropore structure in coals, and 13C nuclear magnetic resonance (13C NMR) and X-ray diffraction (XRD) were employed to characterize the molecular structures of those coal samples. The results demonstrated that micropore evolution during laboratory simulated coalification was similar to that in geo-time-scale natural maturation. This suggests that laboratory simulated coalification can be an effective method for studying micropore evolution during coalification. Micropore evolution in laboratory simulated coalification and natural maturation both exhibited a parabolic curvature with coal rank, with a minimum at ~1.4%. When vitrinite reflectance (Ro) was <1.4%, micropores were mainly controlled by the aliphatic part of the coal samples, and micropore volume decreased with decreasing aliphatic functional groups. When Ro varied from 1.4% to 4.0%, micropore structure was mainly controlled by aromatic parts and coal crystallite structure. In this coalification stage, micropore volume showed linear correlation with the fraction of aromatic bridgehead carbon, the fraction of protonated aromatic carbon, and the ratio of aromatic bridge carbon to aromatic peripheral carbon (XBP). Moreover, the increase in lateral sizes (La) and the decrease in interlayer spacing (d002) both resulted in the increase in micropore volume. In conclusion, the coal microporosity and its evolution were primarily determined by coal molecular structure. In different coalification stages, microporosity and its evolution were controlled by different sub-portions of the whole molecular structure. These findings can provide mechanistic insights of gas sorption and diffusion, as gas sorption and diffusion behaviors are simultaneously controlled by both pore structure and molecular structure.
AB - Micropores (<2 nm) play an important role in coalbed methane adsorption, desorption, and diffusion. However, the mechanisms of micropore formation and evolution still need further study. This study primarily focuses on molecular structure controls on micropore evolution during coalification. CO2 adsorption experiments were employed to characterize micropore structure in coals, and 13C nuclear magnetic resonance (13C NMR) and X-ray diffraction (XRD) were employed to characterize the molecular structures of those coal samples. The results demonstrated that micropore evolution during laboratory simulated coalification was similar to that in geo-time-scale natural maturation. This suggests that laboratory simulated coalification can be an effective method for studying micropore evolution during coalification. Micropore evolution in laboratory simulated coalification and natural maturation both exhibited a parabolic curvature with coal rank, with a minimum at ~1.4%. When vitrinite reflectance (Ro) was <1.4%, micropores were mainly controlled by the aliphatic part of the coal samples, and micropore volume decreased with decreasing aliphatic functional groups. When Ro varied from 1.4% to 4.0%, micropore structure was mainly controlled by aromatic parts and coal crystallite structure. In this coalification stage, micropore volume showed linear correlation with the fraction of aromatic bridgehead carbon, the fraction of protonated aromatic carbon, and the ratio of aromatic bridge carbon to aromatic peripheral carbon (XBP). Moreover, the increase in lateral sizes (La) and the decrease in interlayer spacing (d002) both resulted in the increase in micropore volume. In conclusion, the coal microporosity and its evolution were primarily determined by coal molecular structure. In different coalification stages, microporosity and its evolution were controlled by different sub-portions of the whole molecular structure. These findings can provide mechanistic insights of gas sorption and diffusion, as gas sorption and diffusion behaviors are simultaneously controlled by both pore structure and molecular structure.
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U2 - 10.1016/j.coal.2018.09.012
DO - 10.1016/j.coal.2018.09.012
M3 - Article
AN - SCOPUS:85054176190
SN - 0166-5162
VL - 199
SP - 19
EP - 30
JO - International Journal of Coal Geology
JF - International Journal of Coal Geology
ER -