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Coal bed methane (CBM) is an unconventional form of natural gas found in coal deposits or coal seams. It is a primary clean energy source of natural gas. The development and utilization of CBM is of great social and economic benefit.
The majority of samples contained ethane, propane, and butane; hydrogen and helium were found in some samples. Oxygen and nitrogen were usually present, possibly as a result of air contamination.
CBM is a hydrocarbon gas that is chiefly composed of CH4 and is generated and stored in coal beds in the adsorbed state.
CBM reservoirs are characterized by low mechanical strength, presence of developed cleats, heterogeneity and anisotropy, and a larger surface area as compared to the conventional gas reservoirs. Therefore, potential damage in coal may occur during drilling, completion, and production.
CBM is naturally created during the geologic process of converting plant material to coal (coalification). To extract the methane, CBM operators drill wells into coal seams and pump out ground water (produced water or CBM wastewater).
Generally, it consists predominantly of methane gas (CH4) although it can contain trace amounts of ethane (C2H6), carbon dioxide (CO2) and water (H2O).
CBM is a significant resource of unconventional gas in the world. Natural gas, chiefly methane, is trapped in coal seams and micropores of coal and is extracted by drilling vertical and horizontal wells. Large deposits of coal are found in basins and produced commercially.
Coal seam gas (CSG), also known as coal bed methane, is a mixture of a number of gases but is mostly made up of methane (generally 95-97 per cent pure methane). It is typically attached by adsorption to the coal matrix, and is held in the coal by the pressure of formation water in the coal cleats and fractures.