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FOSSIL FUEL AND GEOTHERMAL ENERGY SOURCES FOR LOCAL USE

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FOSSIL FUEL AND GEOTHERMAL ENERGY SOURCES FOR LOCAL USE ( fossil-fuel-and-geothermal-energy-sources-for-local-use )

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Stach (1975) ASTM (1983) Scott (1995) Coal Rank lig 0.38 0.65 0.65 0.78 1.11 1.49 1.91 2.50 5.00 0.38 0.49 0.51 0.69 1.10 1.60 2.04 2.40 5.00 0.38 0.49 0.65 0.78 1.10 1.50 1.91 2.50 5.00 lignite sub subbituminous hvCb high-volatile C bituminous hvBb high-volatile B bituminous hvAb high-volatile A bituminous mvb medium-volatile bituminous lvb low-volatile bituminous sa semianthracite a anthracite ma meta-anthracite Chapter A, Introduction Fossil Fuel and Geothermal Energy Sources for Local Use in Alaska muddy offshore zone may migrate over the older beach sand, setting up a possible future stratigraphic trap. Structural traps are usually much easier to identify and generally host the initial oil and gas discoveries in a given basin. Stratigraphic traps are much harder to target, and their successful prediction normally requires more detailed mapping of the subsurface geology. This might be based on either an abundance of previously drilled wells or advanced processing and interpretation of high-quality three-dimensional seismic data. In any case, for traps to host oil and gas fields, they must be created prior to hydrocarbon generation, expulsion, and migration from ‘the kitchen.’ Additionally, they must then remain intact, uncompromised by later folding, faulting, or excessive burial. What determines whether a conventional hydrocarbon store the gas in an underground reservoir for any possibility of exploiting this potential resource. Unlike conventional natural gas, in coalbed methane the coal serves as both the source rock and the gas reservoir. Methane (when accompanied by water, nitrogen, and carbon dioxide) is formed when buried plant material is converted into coal over millions of years by heat, pressure, and chemical processes. This coalification process generates methane-rich gas, which often is held in pores and fractures in the coal reservoir and adsorbed to (attached to the surface of) coal particles. As a reservoir, coal is a microporous, carbon- rich mineral capable of holding large quantities of gas that is generated internally. However, gas cannot be extracted from the coal reservoir unless these small micropores are connected Figure A3 through a well-developed fracture system called coal ‘cleats’ Make sure the labels on the Y axis are legible at scale used. accumulation can be exploited depends on numerous geologic and economic factors, including the type of hydrocarbon, producible rate, recoverable volume, development cost, and location. In rural Alaska, either oil or gas resources would be attractive if they could provide energy at a full-cycle cost competitive with currently subsidized deliveries of diesel fuel. GEOLOGIC REQUIREMENTS FOR UNCONVENTIONAL FOSSIL FUEL RESOURCES by Ken Helmold and James G. Clough Coalbed Methane Coalbed methane is a clean- burning fuel that is comparable in heating value (~1,000 Btu/scf) to conventional natural gas. The production of coalbed methane in the lower 48 states from coal seams accounts for about 10 percent of the gas production in the United States. Coal is one of the most abundant non- renewable energy sources in the world, and Alaska has substantial coal resources in a number of sedimentary basins (refer to the description of exploitable coal in this chapter for more information on the origin of coal). The majority of Alaska’s coal is located on the North Slope, followed by the Cook Inlet region, Interior Alaska (mainly Healy), the Alaska Peninsula, Copper River basin, and numerous smaller basins and individual coal localities throughout the state (fig. A2). Within these coal basins there must exist a number of necessary and complex geologic conditions to both generate coalbed methane and to (fig. A3). Fracture permeability is the measurement of how well a fluid or gas moves through a rock when the pores are connected through a cleat or fracture system. Even if there is sufficient coalbed gas, it cannot be produced if there are very few fractures, which results in low permeability. Importantly, coals must also reach a certain critical threshold of thermal maturity or “coal rank” before very large volumes of thermogenic methane gas is generated (fig. A4). Lower-rank lignite to subbituminous coals contain mostly biogenic gas that results from bacterial action on Page 4 Figure A3. Coal rank. The numbers in the columns refer to rank as determined by vi- trinite reflectance. Significant coalbed methane generation does not occur until the high-volatile A bituminous rank is reached. Modified from figure 15 in Scott, 2004. organic material, in the same manner methane is generated by bacteria in shallow garbage landfills. It is important to note that there is no current production of biogenic gas from lignite coals because they lack a well-developed natural fracture system. Production of biogenic gas from very thick (50 to 200 feet thick) subbituminous coals is occurring in the Introduction Main-stage Early thermogenic thermogenic methane methane

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