
Gregory Okolo
Address: Potchefstroom, North-West, South Africa
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Papers by Gregory Okolo
> tip active sites. The mean DFT–DNP values for the activation energy of 233 kJ mol1 at the reactive carbon edge was in agreement with the experimental 191 ± 25 kJ mol1 and 210 ± 8 kJ mol1 for the respective chars.
The chemical-structural properties of four South African bituminous coals were investigated using wide angle X-ray diffraction-carbon fraction analysis (WAXRD-CFA), attenuated total reflection Fourier transform infra-red spectroscopy (ATR-FTIR), solid state 13C nuclear magnetic resonance spectroscopy (ss 13C NMR), and high resolution transmission electron microscopy (HRTEM). The aromaticity of the samples determined by solid state 13C NMR ranged from 0.74 to 0.87 and compared well with the WAXRD-CFA results (0.73-0.86). WAXRD-CFA, ATR-FTIR and 13C NMR data showed that the lower iso-rank coal samples contained more aliphatic moieties; while the higher rank sample contained higher fractions of polyaromatic moieties and saturated long chain hydrocarbons. The lattice parameters determined from WAXRD-CFA show that lower rank coals investigated are structurally less well-ordered than the higher rank coal. Also, its fringes were quantified as having the greatest preferential alignment of the coals examined. HRTEM aromatic fringe image analysis revealed that the carbon lattice of the samples consist of aromatic fringes of varying lengths, L (3Å ≤ L ≤ 95Å), which corresponded to a molecular weight distribution ranging from 75 to 1925 amu, assuming circular catenation. The coal with the highest volatile matter yield was found to exhibit a higher frequency of lower molecular weight fringes; while the higher rank coal possessed the most higher molecular weight fringes. The average molecular weights determined for the samples from 13C NMR varied between 504 to 544 amu; and compared well with the values from HRTEM aromatic fringe image analysis data. Thus, there was good agreement and consistency between the different techniques. It was demonstrated that, for the characterisation methods used in this study; that vitrinite reflectance impacts more on the chemical-structural properties of these coals than maceral composition does.
underestimated the surface area and porosity of the samples compared to results obtained using the other techniques, but it provided a good insight into the pore size distribution of mesopores. The surface areas and porosities of the samples determined from SAXS were found to be larger than any of the values obtained using the other techniques. This is attributed to SAXS probing a wider range of pores, including pores that are closed to, or restricted in access by, gas adsorption or mercury intrusion and also capturing the properties of pores of diameters between 5 and 17 Å, which are not readily measured by any of the other techniques used in this investigation. However, we show here that because each technique probes
different pore size ranges in coal, a combination of SAXS with other techniques (gas adsorption, MIP, etc.) provides a richer picture of the nature of the porosity in coals.
> tip active sites. The mean DFT–DNP values for the activation energy of 233 kJ mol1 at the reactive carbon edge was in agreement with the experimental 191 ± 25 kJ mol1 and 210 ± 8 kJ mol1 for the respective chars.
The chemical-structural properties of four South African bituminous coals were investigated using wide angle X-ray diffraction-carbon fraction analysis (WAXRD-CFA), attenuated total reflection Fourier transform infra-red spectroscopy (ATR-FTIR), solid state 13C nuclear magnetic resonance spectroscopy (ss 13C NMR), and high resolution transmission electron microscopy (HRTEM). The aromaticity of the samples determined by solid state 13C NMR ranged from 0.74 to 0.87 and compared well with the WAXRD-CFA results (0.73-0.86). WAXRD-CFA, ATR-FTIR and 13C NMR data showed that the lower iso-rank coal samples contained more aliphatic moieties; while the higher rank sample contained higher fractions of polyaromatic moieties and saturated long chain hydrocarbons. The lattice parameters determined from WAXRD-CFA show that lower rank coals investigated are structurally less well-ordered than the higher rank coal. Also, its fringes were quantified as having the greatest preferential alignment of the coals examined. HRTEM aromatic fringe image analysis revealed that the carbon lattice of the samples consist of aromatic fringes of varying lengths, L (3Å ≤ L ≤ 95Å), which corresponded to a molecular weight distribution ranging from 75 to 1925 amu, assuming circular catenation. The coal with the highest volatile matter yield was found to exhibit a higher frequency of lower molecular weight fringes; while the higher rank coal possessed the most higher molecular weight fringes. The average molecular weights determined for the samples from 13C NMR varied between 504 to 544 amu; and compared well with the values from HRTEM aromatic fringe image analysis data. Thus, there was good agreement and consistency between the different techniques. It was demonstrated that, for the characterisation methods used in this study; that vitrinite reflectance impacts more on the chemical-structural properties of these coals than maceral composition does.
underestimated the surface area and porosity of the samples compared to results obtained using the other techniques, but it provided a good insight into the pore size distribution of mesopores. The surface areas and porosities of the samples determined from SAXS were found to be larger than any of the values obtained using the other techniques. This is attributed to SAXS probing a wider range of pores, including pores that are closed to, or restricted in access by, gas adsorption or mercury intrusion and also capturing the properties of pores of diameters between 5 and 17 Å, which are not readily measured by any of the other techniques used in this investigation. However, we show here that because each technique probes
different pore size ranges in coal, a combination of SAXS with other techniques (gas adsorption, MIP, etc.) provides a richer picture of the nature of the porosity in coals.