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Factors that influence the formation and stability of hydrated ferrous sulfate in coal dusts. Possible relation to the emphysema of coal miners.

Epidemiological studies have shown that a causal relationship may exist between coal dust exposure and emphysema in coal miners. Emphysema can be considered as one of the human pathologies associated with oxidative stress, resulting from oxidant-induced alpha 1-antitrypsin (alpha 1-AT) inactivation and uncontrolled proteolysis of lung tissue. We have previously reported that certain coal dusts contained hydrated ferrous sulfate (FeSO4) that inactivated alpha 1-AT [Huang et al. (1993) Chem. Res. Toxicol. 6, 452-458]. In the present study, we have shown that the FeSO4 originated from oxidation of pyrite (FeS2), which is a typical contaminant of coal dusts. The relative humidity and microenvironment around individual pyrite particles influence the formation of FeSO4 in the coal. However, the subsequent human exposure to coal dust containing FeSO4 depends on the stability of the formed FeSO4. We found that pH played the most important role in stabilizing the FeSO4, such that a final pH < 4.5 after oxidation of pyrite stabilized FeSO4, whereas at high pH the conversion of reactive Fe2+ to Fe3+ was immediate. Sulfuric acid (H2SO4), which is also produced by the oxidation of pyrite, can lower the pH, but it can also be neutralized by other minerals in coal dusts, such as calcite (CaCO3). The stability of FeSO4 in coal dust can also be influenced by the length of exposure to air. Our studies demonstrated that coal samples differed in their capacity to stabilize FeSO4. This current study strengthens our previous reported hypothesis that emphysema, which occurs irregularly in coal miners, could be directly related to exposure to coal dust containing FeSO4.