Abstract

In order to study the evolution of the mechanical properties and macromolecular structures in different macerals of tectonically deformed coal (TDC), vitrinite and inertinite samples were handpicked from six block TDCs in the same coal seam with an increasing deformation degree (unaltered, cataclastic, porphyroclast, scaly and powdery coal). The micro mechanical properties were tested by the nanoindentation experiment and the macromolecular structures were measured using 13C nuclear magnetic resonance (NMR) and Fourier transform infrared spectroscopy (FTIR). The results show that the range of hardness and elastic modulus of inertinite is 0.373–1.517 GPa and 4.339–12.158 GPa, respectively, which is significantly higher than that of vitrinite with values of 0.278–0.456 GPa and 4.857–7.810 GPa, respectively. From unaltered coal to powdery coal, the hardness of vitrinite and inertinite gradually decreases, with the difference between these macerals becomes smaller and the elastic modulus of vitrinite shows an increasing trend, while that of inertinite was more variable. Both the NMR and FITR results reveal that the macromolecular structure of inertinite has similar structural transitions as vitrinite. As the degree of deformation increases, the aliphatic side chains become shorter and the aromaticity is increasing. Macromolecular alterations caused by tectonic stress is expected to produce defects in the TDCs, therefore there should be more interspacing among the macromolecular groups for the extrusion of macromolecules caused by the indenter of the nanoindentation experiment, thereby reducing the hardness. The elastic modulus of coal is believed to be related to intermolecular forces, which are positively correlated to the dipole moment. By calculating the dipole moments of the typical aromatic molecular structures with aliphatic side chains, the detachment of the aliphatic side chains and the growth of benzene rings can both increase the dipole moment, which can promote elastic modulus. In addition, the increasing number of benzene rings can create more π-π bonds between the molecules, which can lead to an increase in the intermolecular forces, further increasing the elastic modulus.

Highlights

  • The physical and chemical properties of tectonically deformed coal (TDC) are significantly different from those of unaltered coal [1]

  • The indentation depth indentation depth increases from F1-I to F6-I, indicating the hardness decreases with the increasing increases from F1-I to F6-I, indicating the hardness decreases with the increasing deformation degree

  • The micromechanical properties and macromolecular structural evolution of vitrinite and inertinite in TDC with different degrees of deformation were quantified through nanoindentation experiments, nuclear magnetic resonance (NMR) and Fourier transform infrared spectroscopy (FTIR) and the following conclusions are obtained: (1) The evolution of the mechanical properties of vitrinite and inertinite in TDC have been quantitatively described at the microscale

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Summary

Introduction

The physical and chemical properties of tectonically deformed coal (TDC) are significantly different from those of unaltered coal [1]. TDC can be classified in different types with increasing deformation, such as cataclastic, porphyroclast, scaly, powdery, heterogeneous structure and mylonitic coal [14]. Godyńand and Kožušníková [15] studied the microhardness of TDC using the Vickers hardness test in Silesian Coal Basin, Poland and found the lowest values in cataclastic coal and the highest values in unalerted coal, which was a valuable discovery for TDC research. There should be more quantitative descriptions for studies of TDC with different degrees of deformation. Fengfeng coal coal mine area is located to. TheThe coal-bearing strata in the mining area to northern Taihangshanfault faultzone zone[3], [3],North

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