2014
DOI: 10.1016/j.saa.2014.04.046
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Structure evolution characterization of Anyang anthracites via H2O2 oxidization and HF acidification

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Cited by 18 publications
(9 citation statements)
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“…The FTIR spectra of raw and MA are shown in Figure . We observe stretching vibrations and in‐plane vibrations of the hydroxyl bonds (OH) at the spectral peaks at 3100–3600 and 1400 cm −1 , respectively . After modification of the coal, the strength of these peaks is decreased, which corresponds to a decrease in the hydroxyl content on the coal surface; silanol formed by the hydrolysis of the silane coupling agent can react with and consume hydroxyl groups or cover their signals.…”
Section: Resultsmentioning
confidence: 96%
See 1 more Smart Citation
“…The FTIR spectra of raw and MA are shown in Figure . We observe stretching vibrations and in‐plane vibrations of the hydroxyl bonds (OH) at the spectral peaks at 3100–3600 and 1400 cm −1 , respectively . After modification of the coal, the strength of these peaks is decreased, which corresponds to a decrease in the hydroxyl content on the coal surface; silanol formed by the hydrolysis of the silane coupling agent can react with and consume hydroxyl groups or cover their signals.…”
Section: Resultsmentioning
confidence: 96%
“…Anthracite has aromatic rings as the basic structural unit; these are usually linked by aliphatic or heteroaliphatic bridges; it also has some oxygen‐containing functional groups, such as carboxyl (COOH), hydroxyl (OH), and ester (COOR) groups, with small amounts of thiol–mercaptan (RSH), sulfoether, disulfide, and heterocyclic sulfur groups . The side‐chain structures and active oxygen‐containing functional groups endow anthracite particles with good chemical reactivity . Considering the preparation of coal‐based functional fillers, anthracite has potential advantages, including its high carbon content, moderate oxygen functional groups, and aromatic lamellar structure similar to that of graphite .…”
Section: Introductionmentioning
confidence: 99%
“…Compared to those of FC0, the contents of the C═C and C═O functional groups decrease from 64.04 and 11.37% in FC0 to 62.40 and 7.18% in FC5 after the addition of silica sol, respectively while that of the CO and CC groups increase from 10.78 and 13.80% in FC0 to 13.83 and 16.59% in FC5, respectively. The reason may be that the particle fragmentation of humic acid under the mechanochemical forces (ball milling) leads to partial C═C double bond breakage and thus to the formation of new active sites that can be bound to hydroxyl groups (mainly contributed by silica hydroxyl groups or water) 47,48 . The reduction of C═O is mainly caused by the volatilization of small molecule side chains in humic acid during carbonation by cleavage 49 .…”
Section: Resultsmentioning
confidence: 99%
“…Sulfates are barite, gypsum, and anhydrite, 4,5 while organic sulfur exists in the form of thiophene heterocyclic compounds, mercaptan, thioether, and so forth. It is mainly embedded in the macromolecular structure of coals, which is more difficult to be removed by using the conventional physical desulfurization method 6 . Although the chemical method can effectively remove organic sulfur, it requires high temperature and pressure associated with expensive operating costs 7–9 .…”
Section: Introductionmentioning
confidence: 99%