Coal contains three classes of Sulfur. These are Pyretic, Sulfate, and Organic. Pyretic and Organic Sulfur are the most volatile of the three. Sulfate is a dormant form of sulfur and is not found to be particularly harmful to the environment. During combustion, Organic Sulfur and Pyretic Sulfur are oxidized to form Sulfur dioxide (S02), and with the right combustion conditions, some small amount of sulfur trioxide (S03) can be formed. The sulfate forms usually represent a small percentage of the total Sulfur in coal and have little to do with the combustion or contributions to SOX emissions. Under the laboratory test conditions, the sulfates seem to have increased at levels higher than the mass loss levels observed.
Combustion conditions often change the more volatile types of sulfur discussed; pyretic and organic. The amount emitted of SOx is complicated due to combustion conditions differing from plant to plant. Our tests show in the case of the lignite and PRB coal that the Pyretic Sulfur values showed significant loss while sulfate and organic species increased. It appears some Pyretic Sulfur was converted to Sulfate. The organic species appear to have been mostly retained during the mass reduction by charring.
It has been determined that a slower heating process tends to bind the Sulfur and turn higher percentages into Sulfate, a better form of Sulfur. It is also possible to add Calcium to the process. Calcium will bind the Sulfur and keep much of it from forming into SOx.
During the charring process, it was found that some of the more volatile forms of Sulfur were still residing long enough in the gas streams to recombine with elements such as calcium to form stable Sulfates.