2019
DOI: 10.3390/ma12121946
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Surface Chemical Changes of Sugar Maple Wood Induced by Thermo-Hygromechanical (THM) Treatment

Abstract: The aim of this study was to investigate the effects of heat and steam on the chemical properties of thermo-hygromechanical (THM)-densified sugar maple wood. The THM densification process was performed at two different temperatures (180 °C and 200 °C) with and without steam. The functional groups, surface chemical composition and internal structure and components of the control and densified samples were investigated using attenuated total reflection Fourier transform infrared (ATR-FTIR), X-ray photoelectron (… Show more

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Cited by 15 publications
(2 citation statements)
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“…In the region of 1733 cm -1 it is possible to notice the lower intensity of peaks as a function of the increase in densification temperature. This change is attributed to the elongation of carbonyl groups (C=O) in hemicelluloses, lignin and extractives (Fu et al 2019, Alqrinawi et al 2024. Decreasing intensity peaks suggest the cleavage of ester groups associated with the decomposition of hemicellulose polysaccharides (Inari et al 2006),…”
Section: Changes In Chemical Constituentsmentioning
confidence: 99%
“…In the region of 1733 cm -1 it is possible to notice the lower intensity of peaks as a function of the increase in densification temperature. This change is attributed to the elongation of carbonyl groups (C=O) in hemicelluloses, lignin and extractives (Fu et al 2019, Alqrinawi et al 2024. Decreasing intensity peaks suggest the cleavage of ester groups associated with the decomposition of hemicellulose polysaccharides (Inari et al 2006),…”
Section: Changes In Chemical Constituentsmentioning
confidence: 99%
“…In terms of the investigation of flow in porous media, Darcy’s law was the earliest linear seepage model to emerge [6,7]. Since its emergence, numerous experiments and theoretical investigations on gas flow and transport properties in various porous media have been performed and reported for single-phase, multiphase, saturated, and partially saturated domains [8,9,10]. However, because of the complex structure of porous media and the limitations of considering real geological conditions, conventional experiments and theoretical achievements fail in describing the uncertainties of flow and transport properties in porous media.…”
Section: Introductionmentioning
confidence: 99%