Journal
INTERNATIONAL JOURNAL OF COAL GEOLOGY
Volume 82, Issue 3-4, Pages 135-146Publisher
ELSEVIER
DOI: 10.1016/j.coal.2009.10.017
Keywords
Coalbed methane; Gas saturation; Hydrogeology; Adsorption; Black Warrior Basin
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Gas saturation is highly variable in Carboniferous coalbed methane reservoirs of the Black Warrior Basin (USA), and diverse geologic data derived from more than three decades of exploration and development provides insight into the origin of this variability and the consequences for production performance Coalbed methane is produced from numerous thin (similar to 03 to <4 m) coal seams that are distributed through 700 to 1200 m of stratigraphic section Gas content tends to increase with depth, and gas saturation typically ranges from <10 to >95% Importantly, this range of variation is commonly developed among closely spaced seams within the same well Exploration has to date been successful where coal seams are in the thermogenic gas window Geochemical evidence indicates that thermogenic gases have been altered by subsurface water movement and may have been augmented with late-stage biogenic gases, particularly in areas affected by fresh-water recharge Adsorption isotherms of coal samples in the Black Warrior Basin typically have Langmuir volume between 15 and 30 cm(3)/g and Langmuir pressure between 2 and 6 MPa Both Langmuir pressure and Langmuir volume correlate significantly with coal rank In deep, normally pressured coal beds where reservoir pressure is substantially above Langmuir pressure, even a small degree of undersaturation can necessitate prolonged dewatenng before a large reservoir volume can reach the critical desorption pressure Permeability, moreover, decreases exponentially with depth, which can make dewatering coal seams deeper than 800 m difficult Where reservoir pressure is relatively low, however. isotherm geometry indicates that significantly undersaturated reservoirs can be near the critical desorption pressure Consequently, areas of underpressure favoi high gas production along with minimal water production. (C) 2009 Elsevier B V All rights reserved
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