Coalbed methane (CBM, also called coal-seam gas or coalbed gas) is natural gas — mostly methane — that is held on the internal surfaces of coal rather than in the pore space of a sandstone or shale. It is produced by drilling into the coal seam and pumping off the water that holds the gas in place; as pressure in the seam falls, the methane releases from the coal and flows to the wellbore.
In a conventional gas reservoir the gas sits in pore space under pressure. In a coal seam most of the gas is adsorbed — held on the enormous internal surface area of the coal — and kept there by the pressure of water in the seam's natural fractures (called cleats). Coal can hold several times more gas per unit volume this way than a sandstone of the same size.
To produce it, an operator drills into the coal (vertically, or with horizontal laterals in the thicker seams), completes the well, and pumps water out. Lowering the water level lowers the pressure, the gas desorbs from the coal, and it flows through the cleats to the well. The water is the key: without dewatering, there is no gas.
A shale well produces its highest volumes in the first months and declines steeply. A coalbed-methane well does the opposite. It produces mostly water first, gas production ramps up over months to a few years as the seam depressures, and it then declines slowly — often over decades. Peak gas can arrive one to three years after first production, and early royalty checks can understate what the well will eventually pay.
The flip side is that a CBM well's economics depend on the cost of handling water. Produced water must be treated and discharged under permit, reinjected, or hauled, and in a mature field the operator's dewatering cost per unit of gas rises as volumes fall. Which wells stay on line is therefore as much a water-handling decision as a gas-price decision.
Commercial CBM production began in the 1970s and early 1980s in the Black Warrior Basin of Alabama, where the Pottsville coal groups (Pratt, Mary Lee, and Black Creek) around the Oak Grove, Blue Creek, and Brookwood fields became the first large-scale coalbed-methane development in the country. The San Juan Basin of New Mexico and Colorado (Fruitland Coal) became the largest CBM field in the world, and the Powder River Basin of Wyoming added thousands of shallow CBM wells in the 2000s. Smaller plays include the Raton Basin, the Cherokee Basin of Kansas and Oklahoma, the Uinta Basin, and the central Appalachian coalfields of Virginia and West Virginia.
The U.S. Geological Survey's 2002 assessment of the Black Warrior Basin estimated a mean of about 8.5 trillion cubic feet of undiscovered technically recoverable gas across the basin's conventional and continuous plays, with the Pottsville coalbed-methane play a large part of it (USGS Fact Sheet 038-03; the Pottsville coalbed play alone was assessed at about 7.1 Tcf in Fact Sheet 2004-3092). Most U.S. CBM production peaked in the mid-to-late 2000s and has declined since as gas prices fell and fields matured.
Any buyer evaluating a coalbed-methane interest will check which wells on the tract are still on line at the state regulator, what they currently produce and how that has trended, who operates them and how that operator handles water, whether mining is planned through the seam, and how the coal and gas estates were severed in the chain of title. Owners in the Black Warrior Basin can read how those factors play out locally on the basin page or go straight to the Black Warrior Basin sell page.
Black Warrior Basin Mineral Rights (Alabama & Mississippi)
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Powder River Basin Mineral Rights
Split Estates: Surface and Minerals Owned Separately
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Educational information only — not legal, tax, or investment advice. Consult a qualified attorney, CPA, or landman about your specific situation.
Coalbed methane is natural gas, mostly methane, that is held on the internal surfaces of coal seams rather than in the pore space of a sandstone or shale. It is produced by drilling into the coal and pumping off the water that holds the gas in place; as pressure falls, the gas releases from the coal and flows to the well.
The gas is held in the coal by the pressure of water in the seam's natural fractures. Pumping the water out lowers the pressure, which lets the methane desorb from the coal. Gas production typically ramps up over months to a few years as the seam dewaters, then declines slowly.
A shale well pays most in its first year and declines steeply. A coalbed-methane well pays little at first, ramps as the seam depressures, and then declines slowly over decades. Early checks understate a CBM well; a very old CBM well may still pay a small, steady amount.
The Black Warrior Basin of Alabama was the first large-scale commercial coalbed-methane development in the United States. The San Juan Basin (New Mexico and Colorado) became the largest CBM field in the world, and the Powder River Basin of Wyoming, the Raton Basin, the Cherokee Basin, the Uinta Basin, and the central Appalachian coalfields also produce it.
It depends on the deed language that severed the estates and on the state's case law. Some courts have held that gas still in the coal belongs to the coal owner while gas that migrates out belongs to the gas owner; others have reached different results on different instruments. It is a title question, and a qualified oil and gas attorney can confirm what your documents convey.
Yes, at a reduced level. Alabama coalbed-methane production held a plateau of roughly 100–120 billion cubic feet a year from the mid-1990s through 2007 and has declined steadily since (EIA), but thousands of wells in Tuscaloosa, Jefferson, Walker, and neighboring Alabama counties remain on the state regulator's books, and several operators continue to produce and permit wells in the Pottsville coal groups.
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