![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhR3RNcEnMOy7OQxTAr_xEtuy-ThlLt5i9QX1h__RlePtyLQnYhsoeOSlQGne4ffm5oOYlRgiUHBPUM4vpHpt4igFfIECZXycADvmTwvxxl59HaFtjvV9dKRcFD-_rkV3qf7Ipcsf5xVHLB/s320/Coal.jpg)
Coal begins as layers of plant matter accumulate at the bottom of a body of water. For the process to continue the plant matter must be protected from biodegradation and oxidization, usually by mud or acidic water. The wide shallow seas of the Carboniferous period provided such conditions. This trapped atmospheric carbon in the ground in immense peat bogs that eventually were covered over and deeply buried by sediments under which they metamorphosed into coal. Over time, the chemical and physical properties of the plant remains (believed to mainly have been fern-like species antedating more modern plant and tree species) were changed by geological action to create a solid material.
Coal, a fossil fuel, is the largest source of energy for the generation of electricity worldwide, as well as one of the largest worldwide anthropogenic sources of carbon dioxide emissions. Gross carbon dioxide emissions from coal usage are slightly more than those from petroleum and about double the amount from natural gas.Coal is extracted from the ground by mining, either underground or in open pits.
No comments:
Post a Comment