It can be seen that the main parameter controlling the residual CaS is the size of
the grain, the smaller the grain lesser the residual CaS with all other conditions
remaining the same. The greater oxygen concentration favours a lower residual
CaS but increases the CaO/CaSO
4
, indicating a greater SO
2
emission. With regard
to temperature, the best one seems to be the one around 850C, as the amount of
residual CaS increases noticeably at 700 or 950C.
In the cases already commented, oxidation was performed just with the O
2
and
N
2
mixture, but the reactions change if an attempt is made to use a combustion flue
gas as the oxidising gas. In a fixed bed, oxygen, particularly in low concentrations
(4–8%), is depleted because of its fast reaction with CaS to give SO
2
and, after-
wards, this gas (SO
2
) plus CO
2
and H
2
O, which react much more slowly, are the
ones reaching the next CaS layers, then causing the reactions to inverse to (3),
generating H
2
S, and to (5), generating COS.
Álvarez-Rodríguez and Clemente-Jul [23], oxidising CaS previously obtained
in a calcined dolomite sulphidisation stage, with a 21% CO
2
and 79% N
2
mixture
at 850C, found, Fig. 9, that a strong emission of COS occurs initially, meaning
that the inverse reaction of (5) takes place, although it drops quickly, becoming
substituted by a SO
2
emission that rises initially and then drops, stabilising at a
relatively high value of 100 ppmv for hours. This change in behaviour could be
explained by the fact that, initially, the entire surface of the grains is CaS, and the
inverse reaction of (5) takes place in competition with reaction (14), the main one
being the former.
The check for the existence of this reaction is that the similar reaction (18)
CaS þ COS $ CS
2
þ CaO DH
0
¼ 93:4 kJ mol
1
ð18Þ
also occurs at first (when the grains surface are only CaS and there is a great
quantity of COS generated in previous grains), detecting a small CS
2
peak,
Fig. 10. As the reactions are scarcely intense, the CO
2
consumption is very low
and, therefore, reaches the entire column of grains from the beginning, with the
entire external surface of the grains becoming loaded with CaO. During the fol-
lowing moments, the COS produced finds CaO on the surface of other grains and
reacts according to reaction (5), regenerating CaS. The same occurs when the COS
produced inside the grains must go through areas with CaO. In this way, the COS
0
200
400
600
800
1000
1200
1400
1600
0 40 80 120 160 200 240 280 320 360 400
minutes
COS and SO2 ppm.
Fig. 9 COS and SO
2
trend in
oxidation with 21% CO
2
(79% N
2
), grain size
2–2.5 mm, 850C,
COS (filled circle) and
SO
2
(filled square)
Emerging Technologies on Syngas Purification: Process Intensification 133