by Clyde Howard on Thu Nov 19, 2009 7:55 pm
Stole this from Wiki, but did check it against a print encyclopedia I trust (1970 edition of Britannica) and it looks pretty straight factually:
Types of coal
Believed approximate position of the proto-continents toward the end of the Carboniferous period; the light blue represents shallow seas where many of today's coal deposits are found, as opposed to deeper waters which gave rise to oil bearing rocks derived from marine species. The ice caps were known to be very large, lowering sea levels extensively by locking up oceanic waters into solid ice, though how large the ice caps became is a matter of debate. The position of most continental foundations in lower latitudes definitely created a series of successive shallow swamplike seas we burn for today's coal sourced electricity.As geological processes apply pressure to dead biotic matter over time, under suitable conditions it is transformed successively into
Peat, considered to be a precursor of coal, has industrial importance as a fuel in some regions, for example, Ireland and Finland.
Lignite, also referred to as brown coal, is the lowest rank of coal and used almost exclusively as fuel for electric power generation. Jet is a compact form of lignite that is sometimes polished and has been used as an ornamental stone since the Iron Age.
Sub-bituminous coal, whose properties range from those of lignite to those of bituminous coal are used primarily as fuel for steam-electric power generation. Additionally, it is an important source of light aromatic hydrocarbons for the chemical synthesis industry.
Bituminous coal, dense mineral, black but sometimes dark brown, often with well-defined bands of bright and dull material, used primarily as fuel in steam-electric power generation, with substantial quantities also used for heat and power applications in manufacturing and to make coke.
Anthracite, the highest rank; a harder, glossy, black coal used primarily for residential and commercial space heating. It may be divided further into metamorphically [b]altered bituminous coal and petrified oil, as from the deposits in Pennsylvania.
Graphite, technically the highest rank, but difficult to ignite and is not so commonly used as fuel: it is mostly used in pencils and, when powdered, as a lubricant.
The classification of coal is generally based on the content of volatiles. However, the exact classification varies between countries. According to the German classification, coal is classified as follows:[2]
Name Volatiles % C Carbon % H Hydrogen % O Oxygen % S Sulfur % Heat content kJ/kg
Braunkohle (Lignite) 45-65 60-75 6.0-5.8 34-17 0.5-3 <28470
Flammkohle (Flame coal) 40-45 75-82 6.0-5.8 >9.8 ~1 <32870
Gasflammkohle (Gas flame coal) 35-40 82-85 5.8-5.6 9.8-7.3 ~1 <33910
Gaskohle (Gas coal) 28-35 85-87.5 5.6-5.0 7.3-4.5 ~1 <34960
Fettkohle (Fat coal) 19-28 87.5-89.5 5.0-4.5 4.5-3.2 ~1 <35380
Esskohle (Forge coal) 14-19 89.5-90.5 4.5-4.0 3.2-2.8 ~1 <35380
Magerkohle (Non baking coal) 10-14 90.5-91.5 4.0-3.75 2.8-3.5 ~1 35380
Anthrazit (Anthracite) 7-12 >91.5 <3.75 <2.5 ~1 <35300
Percent by weight
The middle six grades in the table represent a progressive transition from the English-language sub-bituminous to bituminous coal, while the last class is an approximate equivalent to anthracite, but more inclusive (the U.S. anthracite has < 6% volatiles).[/b]
Sorry the table for the German classifications didn't format as it does in the article.
The Reading and some other anthracite burning (and hauling) roads like the Lackawana (the famous road of anthracite travelled by Phoebe Snow) actually burned anthracite waste, known a "culm" IIRC, which burned clean and and hot, but had problems requiring a shallow fire-box that was also wide to get enough heating surface exposed.
Absent comrades (Sound of breaking glass)