摘要
Aliphatic organics are reactive components of biomass in activation, playing important roles in pore development. They could be consumed with progress of activation while introducing external O 2 might create additional aliphatic structures via oxidation, probably facilitating generation of extra pores in resulting activated carbon (AC). This was investigated herein by activation of spring jasmine wood with ZnCl 2 or K 2 C 2 O 4 in presence of 11 % or 5 % O 2 at 550 or 700 °C. The results suggested that the oxygen added diminished yield of AC O 2 ZnCl 2 by 21.7 % and yield of AC O 2 K 2 C 2 O 4 by 29.0 %, resulting from partial oxidation of carbonaceous organics on nascent AC. Nonetheless, O 2 presence promoted pore development, increasing S BET from 1833.8 m 2 g -1 for AC N 2 -ZnCl 2 to 2018.2 m 2 g -1 for AC O 2 ZnCl 2 . The S BET of AC O 2 K 2 C 2 O 4 also increased by 35.6 % with presence of O 2 . Oxidization of nascent AC generated more oxygen-containing species that actively involved in polymerization with ZnCl 2 or cracking with K 2 C 2 O 4 to form more pores. Additionally, O 2 presence generated smaller pores in AC O 2 ZnCl 2 while larger ones in AC O 2 -K 2 C 2 O 4 , enhancing the latter AC for adsorption. Oxidation reactions could also form the AC with oxygen-rice surface and hydrophilic nature, which negatively affect aromatization and reduced interplanar spacing of carbon crystals in AC.
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