Stereological Conversion from Linear and Areal Grade Distribution Measurements

Any serious study of stereological conversion procedures must be based on an as accurate as possible complete fractionation of a real mineralogical texture. The original work on the Dolomite- Sphalerite Magstream? separation provided excellent data for establishing a working stereological conversion procedure, which has been successfully applied to a number of ores since its implementation. The linear grade distributions measured from these fractionated particles have been published and are accessible. The procedure for stereological conversion from areal measurements is exactly equal to the procedure for linear measurements. Particle composition from the dolomite-sphalerite density-fractionated particle sets, derived from both linear and areal data (Figures 1 and 2, respectively) are redundant, after proper transformation, and match the particle’s compositional range (plotted against S.G.) expected from Magstream?; direct density measurements by Hemicropicnometry plots within the ranges. Linear data cannot be used without conversion, but areal measurements are often directly applied as liberation spectra. Our areal measurements, without stereological conversion (Figure 3), differ completely from the results after transformation, and its density range falls mostly out of the expected/measured values. Therefore non-transformed areal data cannot be directly applied as useful liberation information.