Recently, the Hg0 re-emission from flue scrubbing solutions
has become a research focus. The objective of this study was to evaluate
the influence of arsenite on Hg0 re-emission by investigating
critical important parameters, including the arsenite ion concentration,
pH values, solution temperature, fluorine ion concentration, and chlorine
ion concentration. The experimental results indicate that arsenite
could directly reduce Hg2+ to Hg0 and promote
the decomposition of Hg(SO3)2
2–. High pH, temperature, and chlorine ion concentration contributed
to the inhibition of Hg0 re-emission, but the fluorine
ions had little effect. The mechanism research suggests that the formation
of unstable HgH2AsO3
+ at low arsenite
concentration accelerates Hg0 re-emission. For the Hg(II)–As(III)–S(VI)
system, the formation of unstable HgSO3H2AsO3
– than Hg(SO3)2
2– could increase Hg0 re-emission. With an
increase in arsenite concentration, the formation of Hg(H2AsO3)2 (which comes from the reaction between
HgSO3H2AsO3
– and
H2AsO3
–) contributes to the
suppression of Hg0 re-emission. The results of this study
are conducive to providing new insight into Hg0 re-emission
and mercury control.