Coal-Fired Power Generation Handbook. James G. Speight

Coal-Fired Power Generation Handbook - James G. Speight


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characteristics, including variability in thickness and continuity, can differ markedly from basin to basin. Therefore, any definition of geological reliability (measured, indicated, and inferred) that is intended for the entire country or for any specific region is not as precise as a system that takes into account the geological differences between regions and between coals of different geological ages. Thus, the two essential requirements that must be fulfilled before a prospective coal mine can enter the development stage are confirmation that there are (i) sufficient minable reserves of adequate quality with no unacceptable environmental or permitting risks, and (ii) confirmation of an assured or contracted market for a substantial fraction of the coal that will be mined.

      Early coal mining (i.e., the extraction of coal from the seam) was small-scale, the coal lying either on the surface, or close to the surface. Typical methods for extraction included drift mining and bell pits. In Britain, some of the earliest drift mines (in the Forest of Dean) date from the medieval period. As well as drift mines, small-scale shaft mining was used. This took the form of (i) a bell pit mining technique in which the extraction of the coal worked outward from a central shaft, or (ii) the room and pillar mining technique in which rooms of coal were extracted with pillars left to support the roofs. Both of these techniques, however, left a considerable amount of usable coal behind.

      Deep shaft mining started to develop in England in the late 18th century, and rapid expansion occurred throughout the 19th century and early 20th century. The English counties of Durham and Northumberland were the leading coal producers and they were the sites of the first deep pits. Before 1800, a great deal of coal was left in places as support pillars and, as a result in the deep pits (300 to 1,000 ft. deep) of these two northern counties (i.e., Durham and Northumberland) only approximately 40% w/w of the coal could be extracted. The use of wood props to support the roof was an innovation first introduced in 1800. The critical factor was circulation of air and control of explosive gases. In the current context, coal mining depends on the following criteria (i) the thickness of the seam, (ii) the thickness of the overburden thickness, (iii) the ease of removal of the overburden by surface mining, (iv) the ease with which a shaft can be sunk to reach the coal seam for underground mining, (v) the amount of coal extracted relative to the amount that cannot be removed, and (vi) the market demand for the coal.

      Mine plans recognize the spatial attributes of coal quality; some seams will be better than others. As a result, the plan will typically manage mining areas to balance coal quality. Mining only the highest quality seams at the outset will truncate the life of the mine. Coal quality for any given mine can also change over time, as lower seams are used or new areas exposed. Long-term relationships with a mine should recognize how quality can change and continue to be vigilant, rather than complacent.

      Exploration for coal is emerging as a future potential source for thermal coal. The process involves discovering new regions and extracting coal economically from earth. Various coal mining techniques include underground coal mining, surface coal mining and mountain top removal method (Speight, 2013).

      The most economical method of coal extraction from coal seams depends on the depth and quality of the seams, the geology of the deposit, and environmental factors. Coal mining processes are differentiated by whether they operate on the surface or underground. Coal-mining operations can be described under three main headings (i) underground or deep mining, in which the coal is extracted from a seam without removal of the overlying strata, (ii) surface mining, in which the strata – the overburden – overlying the coal seam are first removed after which the coal is extracted from the exposed seam or partially covered seam.

      Each mining technique has its own individual merits and the method eventually employed to extract the coal and the technical and economic feasibility of coal recovery are based on (i) the regional geologic conditions, (ii) the overburden characteristics, (iii) the continuity of the coal seam, (iv) the thickness of the coal seam, (v) the structure of the coal seam, (vi) the quality of the coal seam, (vii) the depth of the coal seam, (viii) the strength of the strata above and below the coal seam for roof and floor conditions, (ix) the topography – especially altitude and slope, (x) the climate, (xi) the ownership of the land as it affects the availability of land for access and subsequent mining, (xii) the surface drainage patterns, (xiii) the groundwater conditions, (xiv) the availability of labor and materials, (xv) the requirements of the coal purchaser in terms of tonnage, quality, and destination, and (xvi) the capital investment requirements (Cassidy, 1973; Lindberg and Provorse, 1977; Martin, 1978).

      There are two predominant types of mining methods that are employed for coal recovery: (i) surface mining methods, in which the strata (overburden) overlying the coal seam are first removed, after which the coal is extracted from the exposed seam, and (ii) underground mining methods which currently account for recovery of approximately 60% w/w of the available coal for use.

      3.2.1 Surface Mining

      Surface mining developed as a natural extension of the early mining techniques by which man recovered coal from a seam. In the early stages, the recovered coal would come from exposed ledges or outcrops. In time, this supply would be exhausted and the earth would be scraped away to lay bare more of the seams that led to these outcroppings, thereby exposing even larger amounts of coal. However, as the overburden to be removed became too much for the primitive equipment then in use, the workings would be abandoned and fresh outcrops sought.

      Typically, seams relatively close to the surface, at depths less than approximately 200 feet, are surface mined. Coal that occurs at depths of 200 to 300 feet is usually deep mined but, in some cases, surface mining techniques can be used. For example, some coal in the western United States (such as coal in the Powder River basin of Wyoming) that occur at depths in excess of 200 feet are mined by open pit methods – the thickness of the seam (60 to 90 feet) renders the method economically feasible.

      In surface mining, or strip mining, earth-moving equipment is used to remove the rocky overburden and then huge mechanical shovels scoop coal up from the underlying deposit (Speight, 2013). The modern coal industry has developed some of the largest industrial equipment ever made, including shovels (part of a piece of equipment known as a dragline) capable of holding in excess of 300 tons of coal.

      To reach the coal, bulldozers clear the vegetation and soil. Depending on the hardness and depth of the exposed sedimentary rocks, these rocky layers may be shattered with explosives. To do this, workers drill blast holes into the overlying sedimentary rock, fill these holes with explosives, and then blast the overburden to fracture the rock. Once the broken rock is removed, coal is shoveled from the underlying deposit into giant earth-moving trucks for transport.

      The characteristic that distinguishes open pit mining is the thickness of the coal seam insofar as it is virtually impossible to backfill the immediate mined out area with the original overburden when extremely


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