Zh. Ding et al., Preliminary study on the mode of occurrence of arsenic in high arsenic coals from southwest Guizhou Province, SCI CHINA D, 42(6), 1999, pp. 655-661
Coal samples from high arsenic coal areas have been analyzed by electron mi
croprobe analyzer (EMPA), scanning electron microscopy with an energy dispe
rsive X-ray analyzer (SEM-EDX), X-ray diffraction analysis (XRD), low tempe
rature ashing (LTA), transmission electron microscopy (TEM), X-ray absorpti
on fine structure (XAFS), instrument neutron activation analysis (INAA) and
wet chemical analysis. Although some As-bearing minerals such as pyrite, a
rsenopyrite, realgar(?), As-bearing sulfate, and As-bearing clays are found
in the high arsenic coals, their contents do not account for the abundance
of arsenic in the some coals. Analysis of the coal indicates that arsenic
exists mainly in the form of As5+ and As3+ , combined with compounds in the
organic matrix. The occurrence of such exceptionally high arsenic contents
in coal and the fact that the arsenic is dominantly organically associated
are unique observations. The modes of occurrence of arsenic in high As-coa
ls are discussed.