4.5 Article

Experimental study on transformation of alkali and alkaline earth metals during biomass gasification

期刊

JOURNAL OF THE ENERGY INSTITUTE
卷 103, 期 -, 页码 117-127

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.joei.2022.06.003

关键词

Biomass gasification; AAEMs; Transformation; CO2 gasification; Particle size

资金

  1. National Natural Science Foundation of China [51406147]

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A fixed-bed reactor was used to simulate CO2 gasification and examine the transformation of alkali and alkaline earth metals (AAEMs) in biomass. The study found that the release of AAEMs followed a specific sequence and the alkali metals mainly appeared as water-soluble inorganic salts. Higher temperatures led to the formation of compounds with other elements. Larger particle sizes were beneficial for the transformation of potassium from water-soluble to organic forms, particularly in candlenut wood.
To gain an in-depth understanding of AAEMs (alkali and alkaline earth metals) transformation during biomass gasification, a fixed-bed reactor is built to simulate the CO2 gasification at 500-900 degrees C. The influences of biomass species, gasification temperature, and particle size are examined. The results show that the AAEMs release follow a sequence of candlenut wood > wheat straw > corn stalk. The alkali metals mainly appear as water-soluble inorganic salts and the contents are more than 80%. K mainly occurs as KCl and KClO4. At higher temperatures, K could combine with Al and Si to form K(AlSi3)O8. For candlenut wood, a bigger particle size is beneficial to the transformation of water-soluble K to organic K. For candlenut wood with centimeter-scale, K mainly occurs as organic K in the biochar during 600-700 degrees C. When the gasification is carried out at 700 degrees C, K concentrates at the center and its content is even higher than that on the outer surface. While for biochar samples obtained from gasification at 600 and 900 degrees C, the K content at the center is lower than that on the outer surface due to the continuous outward transformation of K from the central biochar.

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