Mercury emission is an important issue during in-situ gasification chemical-looping combustion ( i G-CLC) of coal. This work focused on experimentally “isolating” two elementary subprocesses (coal pyrolysis and char gasification) during i G-CLC of coal, identifying mercury distribution within the two subprocesses, and examining the effects of a hematite oxygen carrier (OC) on the mercury fate. The mercury measurement accuracy was carefully ensured by comparing online measurements (by a VM 3000 instrument) and benchmark measurements (by the standard Ontario Hydro Method, ASTM D6784) as well as repeated tests (10 times for each case). The mercury mass balance was 115% for the entire i G-CLC. A total of 44.7% of the mercury was released as the gas phase form within the coal pyrolysis process at a typical CLC operation temperature (950 °C), whereas 13.4% was released during the char gasification process. The release rate and amount of mercury were minimally affected by the presence of OC; however, the OC promoted the conversion of Hg 0 (g) to Hg 2+ (g). Only a small amount of mercury was absorbed by the OC and transported into the air reactor along with carbon residue, released as Hg 0 (g) and Hg 2+ (g) or remained in the OC and coal ash as particulate mercury.
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Ma et al. (2019) studied this question.
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