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Volatile matter characterization of birch biochar produced under pressurized conditions
The volatile matter (VM) content and composition of birch biochars produced at 320 °C under elevated pressure (0.1–11 MPa) and constant pressure or constant volume reactor conditions were characterized by thermogravimetry/mass spectrometry (TG/MS) and pyrolysis–gas chromatography/mass spectrometry (...
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Published in: | Journal of thermal analysis and calorimetry 2024-10, Vol.149 (19), p.10915-10926 |
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container_title | Journal of thermal analysis and calorimetry |
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creator | Babinszki, Bence Czirok, István Sándor Johnson, Robert Sebestyén, Zoltán Jakab, Emma Wang, Liang Turn, Scott Skreiberg, Øyvind Czégény, Zsuzsanna |
description | The volatile matter (VM) content and composition of birch biochars produced at 320 °C under elevated pressure (0.1–11 MPa) and constant pressure or constant volume reactor conditions were characterized by thermogravimetry/mass spectrometry (TG/MS) and pyrolysis–gas chromatography/mass spectrometry (Py–GC/MS). Some of the thermal properties of the biochars and the composition of the VMs varied as a function of the maximal pressure applied during carbonization. The samples prepared at higher pressures released more volatiles up to 320 °C, while the maximal rate of thermal decomposition at around 440 °C showed decreasing tendency with the carbonization pressure. In terms of VM composition, the most apparent effect was the significant increase of the amounts of apoallobetulins from biochars prepared at elevated pressures, which were formed by dehydration, ring closure and rearrangement from the betulin content of birch. The change in the ratio of the evolved guaiacol and 4-methylguaiacol as well as that of syringol and 4-methylsyringol as a function of the maximal pressure of carbonization indicated a modification of the lignin decomposition mechanism. |
doi_str_mv | 10.1007/s10973-024-13381-4 |
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Some of the thermal properties of the biochars and the composition of the VMs varied as a function of the maximal pressure applied during carbonization. The samples prepared at higher pressures released more volatiles up to 320 °C, while the maximal rate of thermal decomposition at around 440 °C showed decreasing tendency with the carbonization pressure. In terms of VM composition, the most apparent effect was the significant increase of the amounts of apoallobetulins from biochars prepared at elevated pressures, which were formed by dehydration, ring closure and rearrangement from the betulin content of birch. The change in the ratio of the evolved guaiacol and 4-methylguaiacol as well as that of syringol and 4-methylsyringol as a function of the maximal pressure of carbonization indicated a modification of the lignin decomposition mechanism.</description><identifier>ISSN: 1388-6150</identifier><identifier>EISSN: 1588-2926</identifier><identifier>DOI: 10.1007/s10973-024-13381-4</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Analytical Chemistry ; Carbonization ; Chemistry ; Chemistry and Materials Science ; Composition effects ; Dehydration ; Gas chromatography ; Inorganic Chemistry ; Mass spectrometry ; Measurement Science and Instrumentation ; Physical Chemistry ; Polymer Sciences ; Pressure effects ; Pyrolysis ; Scientific imaging ; Thermal decomposition ; Thermodynamic properties ; Thermogravimetry</subject><ispartof>Journal of thermal analysis and calorimetry, 2024-10, Vol.149 (19), p.10915-10926</ispartof><rights>The Author(s) 2024</rights><rights>The Author(s) 2024. 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Some of the thermal properties of the biochars and the composition of the VMs varied as a function of the maximal pressure applied during carbonization. The samples prepared at higher pressures released more volatiles up to 320 °C, while the maximal rate of thermal decomposition at around 440 °C showed decreasing tendency with the carbonization pressure. In terms of VM composition, the most apparent effect was the significant increase of the amounts of apoallobetulins from biochars prepared at elevated pressures, which were formed by dehydration, ring closure and rearrangement from the betulin content of birch. 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subjects | Analytical Chemistry Carbonization Chemistry Chemistry and Materials Science Composition effects Dehydration Gas chromatography Inorganic Chemistry Mass spectrometry Measurement Science and Instrumentation Physical Chemistry Polymer Sciences Pressure effects Pyrolysis Scientific imaging Thermal decomposition Thermodynamic properties Thermogravimetry |
title | Volatile matter characterization of birch biochar produced under pressurized conditions |
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