4.7 Article

Distribution and evolution of organic matter phases during biochar formation and their importance in carbon loss and pore structure

Journal

CHEMICAL ENGINEERING JOURNAL
Volume 250, Issue -, Pages 240-247

Publisher

ELSEVIER SCIENCE SA
DOI: 10.1016/j.cej.2014.04.053

Keywords

Biochar; Organic matter phases; Sequential fractionations; Carbon loss; Pore structure

Funding

  1. National Natural Science Foundation of China [21107070, 21377081]
  2. Young Teacher's Project of Shanghai Jiaotong University
  3. State Key Laboratory of Pollution Control and Resource Reuse Foundation [PCRRF12009]

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This study investigated the distribution and evolution of organic phases during biochar formation from twelve waste biomass and at the highest heating temperatures between 200 degrees C and 650 degrees C. Relation of the organic phase transformation to the carbon loss and pore structure was also analyzed. The organic phases in both feedstock biomass and the derived biochar were sequentially separated into four fractions: neutral detergent soluble fraction, hemicellulose, cellulose, and lignin. Plant-based residues mainly contained cellulose (25.8-64.6%), while municipal solid wastes had a large fraction of neutral detergent soluble fraction (22.9-65.0%). Transformation of cellulose into detergent soluble fraction and hemicellulose initially happened at the charring temperature between 100 degrees C and 200 degrees C, and the complete transformation was observed at the higher temperatures from 200 degrees C to 350 degrees C. The high lignin amount in biochar may be partly formed from the aromatization of cellulose fraction in addition to the contribution from the existing lignin in feedstock. All biochars had small total pore volumes ranging from 0.009 cm(3) g(-1) to 0.278 cm(3) g(-1) and were a type of mesoporous material with the pore sizes between 2 nm and 30 nm. The decrease of detergent soluble fraction, hemicellulose, and cellulose fractions had little effect on pore formation, but it was positively related to the C loss during pyrolysis. Pore volume and surface area seemed to have a positive relationship with lignin percentage and insoluble minerals in feedstock. This study provided insight into the mechanism of biochar formation related to the C loss and pore structure evolution. It will help produce the designated biochar with different environmental functions. (C) 2014 Elsevier B.V. All rights reserved.

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