Three Western Canadian coals with different ranks have been upgraded b
y evaporative drying in several atmosphere at temperatures up to 500-d
egrees-C. Data from proximate and ultimate analyses, along with equili
brium moistures and heating values, have been evaluated by principal c
omponent analysis. The results indicate that significant changes in th
e products occur above 400-degrees-C for lignite and above 300-degrees
-C for subbituminous B and high-volatile C bituminous coals. No signif
icant differences are observed when the data for the upgraded coals ar
e compared with published data for naturally occurring Western Canadia
n and US coals of the same rank.