| Coal Education |
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| What is Coal? |
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| Most European and North Americal coals are of the warm climate type and date from a period when a great southern continent (Gondwana) was enveloped in ice. This ice melted about 300 million years ago, allowing cool climate coals like most Australian coals to develop over large tracts of Gondwana. Gondwana later broke up to form South America, Africa, Inda, Antactica and Australia. | |
| Plants are most made of carbon, hydrogen amd oxygen; these elements are preserved in the organic part of coal. The physical and chemical structure undergoes massive changes in the coal development process, caused by the pressure of later sediments from above, and by geothermal heat from below. Coal also contains impurities in the form of water from plants and swamp, and mineral grains from sand and silt. | |
| Can you comprehend a period of 300 million years? Imagine walking back through time to a place 300 kilometres away, and think of this distance as representing that time. Each millimetre of your journey would represent a year and the width of your hand more than most people's lifespan. | |
| Within your first half dozen steps civilization would disappear; within a few hundred metres there would be no sign of mankind itself. You would have to walk for 65 kilometres before you would see a dinosaur! | |
| Why coal burns? |
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| A megajoule(MJ) is a unit of energy, about equivalent to that needed to boil three litres of water. More energy is available if the steam is condensed, but this is rarely practical. | |
| What is coal used for? |
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| Coal Types There are several different types of coal, that different properties usually dependent on their age and the depth to which they have been buried under other rocks. |
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| In some parts of the world, coal development is accelerated by volcanic heat or crustal stresses. The degree of coal development is referred to as a coal's "rank," with peat being the lowest rank coal and anthracite the highest. | |
| Peat |
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| Lignite |
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| Black coal |
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| Coals that get more deeply buried by other rocks lose more moisture and start to lose their oxygen and hydrogen. These coals are harder and shinier (bituminous coal), which have energy contents around 24 to 28 megajoules per kilogram. These coals generally have less than 3% moisture. | |
| Anthracite |
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| Coal rank has little to do with quality; as a coal matures its ash content actually increases as a proportion because of the loss of moisture and volatiles. Lower rank coals may have lower energy contents, but they tend to be more reactive (they burn faster) because of their porosity and resultant higher surface area. |