MÖSSBAUER SPECTROSCOPY OF AMPHIBOLE-ASBESTOS FROM LIBBY, MONTANA: IMPLICATIONS FOR ASBESTOS CLASSIFICATION
The Fe3+ content of Libby amphiboles is important to their characterization and chemical classification as pointed out by Wylie and Verkouteren (2000). Mössbauer spectroscopy at 12-300 K is used to measure the Fe3+/Fe2+ in the amphibole. Ferric iron contents ranged from 56%-76% of the total Fe in the five samples studied. Thus, it is apparent that previous wet chemical (bulk) analyses of these samples, such as that by Larsen (1942), probably underestimated the Fe3+ contents of these samples because impurities were not recognized. When considered along with uranium extraction data for hydrogen contents and EMPA results of Gunter et al. (2001) showing significant Na and K contents, these data allow the proper formulas for various samples of Libby amphibole to be determined. The resultant formulas support the suggestion of Wylie and Verkouteren (2000) that these samples are winchite. Winchite is not currently considered "asbestos" by any regulatory agency, but it should be.