Flow properties (permeability and diffusivity) of subbituminous to high volatile bituminous coals from the Horseshoe Canyon and Mannville formations of the Western Canada Sedimentary Basin have been investigated using both solid coal plugs and samples crushed to between 0.8 mm and 0.6 mm (20-30 mesh). The coals examined have contents of vitrinite between 65%-98%, inertinite up to 31% and rare liptinite macerals. Permeability of crushed coal ranges from 1.46.10(-5) md to 7.60.10(-3) md whereas coal plug permeability is between 0.38 md to 0.01 md. Average diffusivity of crushed coal is estimated to be on the order of 10(-11) m(2)/s. This difference of up to four orders of magnitude between crushed and coal plug permeability is attributed to different stress conditions during sample testing and the influence of coal cleat and coal fractures on coal plug permeability. The permeability of crushed coal is influenced by coal matrix properties including maceral content and micro fabric. The coals with greatest amount of inertinite have the greatest matrix permeability and diffusivity due to the greater macro- and meso- porosity of inertinite. Increasing effective stress, with all other factors kept constant, leads to a decrease in coal plug permeability. Coal plug permeability declines exponentially with increasing effective stress which is attributed to the closure of permeability pathways due to compaction of coal at high effective stress levels. Probe gas type influences plug permeability. Helium permeability measurements are higher than permeability measured with methane or nitrogen. Permeability difference with probe gas is attributed to a combination of different probe gas molecule size, relative swelling effects of probe gas on coal and associated changes at in-situ stress during tests. (C) 2011 Elsevier B.V. All rights reserved.