The influence of aluminium substitution on the absorption of gamma-rays in hematite
Abstract
In aluminous hematites, α-(Fe, Al) 2O 3, absorption of the 14.4 keV gamma-ray used in 57Fe Mössbauer spectroscopy increases with substitution of Fe 3+ by Al 3+. This trend may be masked by a superimposed dependence of absorption on particle size in the microcrystal range below about 400 nm.
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118076
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doi:10.1016/0375-9601(85)90809-6
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