Obama sides with coal over clean energy

The Sierra Club is troubled by the Obama Administration’s support of the Susquehanna-Roseland project. The transmission line will be part of a pilot program to fast-track federal permitting on major power line projects. However, the unnecessary Susquehanna-Roseland line will bring dirty coal power into New Jersey while cutting across our public lands. The project is being used by PSE&G to increase exports of cleaner energy produced in state to New York City, where they can charge higher rates.

The president is wrong. The Susquehanna-Roseland project is not about renewable energy and will not create long-term jobs. The Susquehanna-Roseland line undermines green energy jobs as we invest in antiquated technology instead of a smart grid, energy efficiency and demand response programs.

President Obama is moving us in the wrong direction on energy issues. This is the third disappointment in the past two months. First, the approval of the Keystone pipeline to carry tar sands oil across the country, then scrapping the smog rule, and now promoting the expanded exportation of coal-fired energy through this pilot program and the Susquehanna-Roseland line.

The Susquehanna-Roseland line is unnecessary. Energy demand has dropped significantly and energy efficiency programs, local renewable generation, and grid reliability have increased in New Jersey. We do not need the power line and investing in clean energy programs in New Jersey would create many more jobs than shipping our money to Pennsylvania for dirty coal.

The National Park Service is currently reviewing the environmental impacts of the project as it crosses our federal public lands at the Delaware Water Gap National Recreation Area, the Middle Delaware Scenic and Recreational River, and the Appalachian Trail. This new pilot program could jeopardize the NPS environmental review and put our public lands at risk. The NPS review could ultimately dramatically alter the route of the line or determine that the project is not needed at all under the “No Build” alternative and an expedited review under this pilot program would interfere with that process. The NPS review must not be rushed. They are examining eight alternatives, including three that would move the project entirely outside of the Delaware Water Gap.


Environmental Effects of Coal Burning

There are a number of adverse health and environmental effects of coal burning especially in power stations, and of coal mining. These effects include:

  • Coal-fired power plants shorten nearly 24,000 lives a year in the United States, including 2,800 from lung cancer
  • Generation of hundreds of millions of tons of waste products, including fly ash, bottom ash, flue gas desulfurization sludge, that contain mercury, uranium, thorium, arsenic, and other heavy metals
  • Acid rain from high sulfur coal
  • Interference with groundwater and water table levels
  • Contamination of land and waterways and destruction of homes from fly ash spills such as Kingston Fossil Plant coal fly ash slurry spill
  • Impact of water use on flows of rivers and consequential impact on other land-uses
  • Dust nuisance
  • Subsidence above tunnels, sometimes damaging infrastructure
  • Uncontrollable underground fires which may burn for decades or centuries.
  • Coal-fired power plants without effective fly ash capture are one of the largest sources of human-caused background radiation exposure
  • Coal-fired power plants emit mercury, selenium, and arsenic which are harmful to human health and the environment
  • Release of carbon dioxide, a greenhouse gas, which causes climate change and global warming according to the IPCC and the EPA. Coal is the largest contributor to the human-made increase of CO2 in the air

Carbon Intensity of Coal

Commercial coal has a carbon content of at least 70%. Coal with a heating value of 6.67 kWh per kilogram as quoted above has a carbon content of roughly 80%, which is

 \frac{0.8 \ \mathrm{kg}}{\mathrm{12} \cdot \mathrm{kg/kmol}} = \frac{2}{30} \ \mathrm{kmol} , where 1 mol equals to NA (Avogadro Number) atoms.

Carbon combines with oxygen in the atmosphere during combustion, producing carbon dioxide, with an atomic weight of (12 + 16 × 2 = 44 kg/kmol). The CO2 released to air for each kilogram of incinerated coal is therefore

\frac{2}{30} \ \mathrm{kmol} \cdot \frac{44 \ \mathrm{kg}}{\mathrm{kmol}} = \frac{88}{30} \ \mathrm{kg} \approx 2.93 \ \mathrm{kg}.

This can be used to calculate an emission factor for CO2 from the use of coal power. Since the useful energy output of coal is about 30% of the 6.67 kWh/kg(coal), the burning of 1 kg of coal produces about 2 kWh of electrical energy. Since 1 kg coal emits 2.93 kg CO2, the direct CO2 emissions from coal power are 1.47 kg/kWh, or about 0.407 kg/MJ.

The U.S. Energy Information Agency's 1999 report on CO2 emissions for energy generation, quotes a lower emission factor of 0.963 kg CO2/kWh for coal power. The same source gives a factor for oil power in the U.S. of 0.881 kg CO2/kWh, while natural gas has 0.569 kg CO2/kWh. Estimates for specific emission from nuclear power, hydro, and wind energy vary, but are about 100 times lower.

Energy Density of Coal

The energy density of coal, i.e. its heating value, is roughly 24 megajoules per kilogram.

The energy density of coal can also be expressed in kilowatt-hours, the units that electricity is most commonly sold in, per units of mass to estimate how much coal is required to power electrical appliances. One kilowatt-hour is 3.6 MJ, so the energy density of coal is 6.67 kW·h/kg. The typical thermodynamic efficiency of coal power plants is about 30%, so of the 6.67 kW·h of energy per kilogram of coal, 30% of that—2.0 kW·h/kg—can successfully be turned into electricity; the rest is waste heat. So coal power plants obtain approximately 2.0 kW·h per kilogram of burned coal.

As an example, running one 100-watt lightbulb for one year requires 876 kW·h (100 W × 24 h/day × 365 day/year = 876000 W·h = 876 kW·h). Converting this power usage into physical coal consumption:

\frac{876 \ \mathrm{kW \cdot h}}{2.0 \ \mathrm{kW} \cdot \mathrm{h/kg}} = 438 \ \mathrm{kg \ of \ coal} = 966 \ \mathrm{pounds \ of \ coal}

It takes 325 kg (714 lb) of coal to power a 100 W lightbulb for one year. One should also take into account transmission and distribution losses caused by resistance and heating in the power lines, which is in the order of 5–10%, depending on distance from the power station and other factors.

Refined Coal

Refined coal is the product of the application of a coal upgrading technology that removes moisture and certain pollutants from lower-rank coals such as sub-bituminous and lignite (brown) coals and raising their calorific values. Coal refining or upgrading technologies are typically pre-combustion treatments and/or processes that alter the characteristics of a coal before it is burned. The goals of pre-combustion coal upgrading technologies are to increase efficiency and reduce emissions when coal is burned. Depending on the situation, pre-combustion technology can be used in place of or as a supplement to post-combustion technologies to control emissions from coal-fueled boilers. A primary benefit of refined coal is the capacity to reduce the net volume of carbon emissions that is currently emitted from power generators and would reduce the amount of emissions that is proposed to be managed via emerging carbon sequestration methodologies. Refined coal technologies have primarily been developed in the United States, several similar technologies have been researched, developed and tested in Victoria, Australia, including the Densified coal technology (Coldry Process) developed to alter the chemical bonds of brown coal to create a product that is cleaner, stable (not prone to spontaneous combustion), exportable and of sufficiently high calorific value to be a black coal equivalent.

Commercial Development of Refined Coal

United States

Evergreen Energy constructed a full-scale coal refinery near Gillette, Wyoming that began operation in late 2005. Designed originally to be a commercial plant, the facility encountered design and operational problems. Evergreen idled the facility in March 2008 and instead used the plant as a process development platform with its engineering, construction and procurement contractor Bechtel Power Corporation.

Evergreen is now seeking to construct a coal refinery using the improved Bechtel design at locations in the Midwestern United States and in Asia.


Calleja Group constructed a full-scale 16,000 tonne per annum pilot demonstration plant at JBD Business Park at Maddingley Mine near Bacchus Marsh, Victoria that began operation in early 2004. From 2005 ECT Limited upgraded the facility, added a water recovery process with Victorian Government funding in 2007 and operated the plant as a process development platform with its engineering partner ARUP. In 2009 ECT Limited secured and agreement with Thang Long Investment Company (Tincom) of Vietnam to finalise commercial feasibility ahead of construction of a 2 million tonne pa export plant by 2014 and 20 million tonne pa export by 2020. ECT Limited is using the ARUP improved design to secure technology licensing agreements with brown coal suppliers in China, India, Indonesia, Poland, Greece and Russia.

Coal Liquefaction Methods

Coal liquefaction is the process of producing synthetic liquid fuels from coal.

The Coal liquefaction processes are classified as direct conversion to liquids processes and indirect conversion to liquids processeses. Direct processes are carbonization and hydrogenation.

Pyrolysis and carbonization processes

There are a number of carbonization processes. The carbonization conversion occurs through pyrolysis or destructive distillation, and it produces condensable coal tar, oil and water vapor, non-condensable synthetic gas, and a solid residue-char. The condensed coal tar and oil are then further processed by hydrogenation to remove sulfur and nitrogen species, after which they are processed into fuels.

The typical example of carbonization is the Karrick process. The process was invented by Lewis Cass Karrick in the 1920s. The Karrick process is a low-temperature carbonization process, where coal is heated at 680 °F (360 °C) to 1,380 °F (750 °C) in the absence of air. These temperatures optimize the production of coal tars richer in lighter hydrocarbons than normal coal tar. However, the produced liquids are mostly a by-product and the main product is semi-coke, a solid and smokeless fuel.

The COED Process, developed by FMC Corporation, uses a fluidized bed for processing, in combination with increasing temperature, through four stages of pyrolysis. Heat is transferred by hot gases produced by combustion of part of the produced char. A modification of this process, the COGAS Process, involves the addition of gasification of char. The TOSCOAL Process, an analogue to the TOSCO II oil shale retorting process and Lurgi-Ruhrgas process, which is also used for the shale oil extraction, uses hot recycled solids for the heat transfer.

Liquid yields of pyrolysis and Karrick processes are generally low for practical use for synthetic liquid fuel production. Furthermore, the resulting liquids are of low quality and require further treatment before they can be used as motor fuels. In summary, there is little possibility that this process will yield economically viable volumes of liquid fuel.

Hydrogenation processes

One of the main methods of direct conversion of coal to liquids by hydrogenation process is the Bergius process. The Bergius process was developed by Friedrich Bergius in 1913. In this process, dry coal is mixed with heavy oil recycled from the process. Catalyst is typically added to the mixture. The reaction occurs at between 400 °C (752 °F) to 5,000 °C (9,030 °F) and 20 to 70 MPa hydrogen pressure. The reaction can be summarized as follows:

n C + (n + 1) H2 → CnH2 n + 2

After World War I several plants were built in Germany; these plants were extensively used during World War II to supply Germany with fuel and lubricants. The Kohleoel Process, developed in Germany by Ruhrkohle and VEBA, was used in the demonstration plant with the capacity of 200 ton of lignite per day, built in Bottrop, Germany. This plant operated from 1981 to 1987. In this process, coal is mixed with a recycle solvent and iron catalyst. After preheating and pressurizing, H2 is added. The process takes place in a tubular reactor at the pressure of 300 bar and at the temperature of 470 °C (880 °F). This process was also explored by SASOL in South Africa.

In 1970-1980s, Japanese companies Nippon Kokan, Sumitomo Metal Industries and Mitsubishi Heavy Industries developed the NEDOL process. In this process, coal is mixed with a recycled solvent and a synthetic iron-based catalyst; after preheating H2 is added. The reaction takes place in a tubular reactor at temperature between 430 °C (810 °F) and 465 °C (870 °F) at the pressure 150-200 bar. The produced oil has low quality and requires intensive upgrading. H-Coal process, developed by Hydrocarbon Research, Inc., in 1963, mixes pulverized coal with recycled liquids, hydrogen and catalyst in the ebullated bed reactor. Advantages of this process are that dissolution and oil upgrading are taking place in the single reactor, products have high H/C ratio, and a fast reaction time, while the main disadvantages are high gas yield (this is basically a thermal cracking process), high hydrogen consumption, and limitation of oil usage only as a boiler oil because of impurities.

The SRC-I and SRC-II (Solvent Refined Coal) processes developed by Gulf Oil and implemented as pilot plants in the United States in the 1960s and 1970s. The Nuclear Utility Services Corporation developed hydrogenation process which was patented by Wilburn C. Schroeder in 1976. The process involved dried, pulverized coal mixed with roughly 1wt% molybdenum catalysts. Hydrogenation occurred by use of high temperature and pressure synthesis gas produced in a separate gasifier. The process ultimately yielded a synthetic crude product, Naphtha, a limited amount of C3/C4 gas, light-medium weight liquids (C5-C10) suitable for use as fuels, small amounts of NH3 and significant amounts of CO2. Other single-stage hydrogenation processes are the Exxon Donor Solvent Process, the Imhausen High-pressure Process, and the Conoco Zinc Chloride Process.

There is also a number of two-stage direct liquefaction processes; however, after 1980s only the Catalytic Two-stage Liquefaction Process, modified from the H-Coal Process; the Liquid Solvent Extraction Process by British Coal; and the Brown Coal Liquefaction Process of Japan have been developed.

Shenhua, the Chinese coal miner, decided in 2002 to build a direct liquefaction plant in Inner Mongolia, with barrel capacity of 20 thousand barrels per day (3.2×103 m3/d). First tests were implemented at the end of 2008. A second and longer test campaign was started in October 2009.

Chevron Corporation developed a process invented by Joel W. Rosenthal called the Chevron Coal Liquefaction Process (CCLP). It is unique due the close-coupling of the non-catalytic dissolver and the catalytic hydroprocessing unit. The oil produced had properties that were unique when compared to other coal oils; it was lighter and had far fewer heteroatom impurities. The process was scaled-up to the 6 ton per day level, but not proven commercially.

Indirect conversion processes

The main indirect process is the Fischer-Tropsch process. In this process, coal is first gasified to make syngas (a balanced purified mixture of CO and H2 gas). Next, Fischer-Tropsch catalysts are used to convert the syngas into light hydrocarbons (like ethane) which are further processed into gasoline and diesel. This method was used on a large technical scale in Germany between 1934 and 1945 and is currently being used by Sasol in South Africa. In addition to creating gasoline, syngas can also be converted into methanol, which can be used as a fuel, or into a fuel additive.

Syngas may be converted to liquids through conversion of the syngas to methanol which is subsequently polymerized into alkanes over a zeolite catalyst. This process, named as the Mobil MTG Process, was developed by Mobil in early 1970s.

Environmental Effects of Coal Gasification

Environmental Effects of Coal Gasification: From its original development until the wide-scale adoption of natural gas, more than 50,000 manufactured gas plants were in existence in the United States alone. The process of manufacturing gas usually produced a number of by-products that contaminated the soil and groundwater in and around the manufacturing plant, so many former town gas plants are a serious environmental concern, and cleanup and remediation costs are often high. Manufactured gas plants (MGPs) were typically sited near or adjacent to waterways that were used to transport in coal and for the discharge of wastewater contaminated with tar, ammonia and/or drip oils, as well as outright waste tars and tar-water emulsions.

In the earliest days of MGP operations, coal tar was considered a waste and often disposed into the environment in and around the plant locations. While uses for coal tar developed by the late-19th century, the market for tar varied and plants that could not sell tar at a given time could store tar for future use, attempt to burn it as fuel for the boilers, or dump the tar as waste. Commonly, waste tars were disposed of in old gas holders, adits or even mine shafts (if present). Over time, the waste tars degrade with phenols, benzene (and other mono-aromatics – BTEX) and polycyclic aromatic hydrocarbons released as pollutant plumes that can escape into the surrounding environment. Other wastes included "blue billy", which is a ferroferricyanide compound—the blue colour is from Prussian blue, which was commercially used as a dye. Blue billy is typically a granular material and was sometimes sold locally with the strap line "guaranteed weed free drives". The presence of blue billy can give gas works waste a characteristic musty/bitter almonds or marzipan smell which is associated with cyanide gas.

The shift to the CWG process initially resulted in a reduced output of water gas tar as compared to the volume of coal tars. The advent of automobiles reduced the availability of naphtha for carburetion oil, as that fraction was desirable as motor fuel. MGPs that shifted to heavier grades of oil often experienced problems with the production of tar-water emulsions, which were difficult, time consuming, and costly to break. (The cause of tar-water emulsions is complex and was related to several factors, including free carbon in the carburetion oil and the substitution of bituminous coal as a feedstock instead of coke.) The production of large volumes of tar-water emulsions quickly filled up available storage capacity at MGPs and plant management often dumped the emulsions in pits, from which they may or may not have been later reclaimed. Even if the emulsions were reclaimed, the environmental damage from placing tars in unlined pits remained. The dumping of emulsions (and other tarry residues such as tar sludges, tank bottoms, and off-spec tars) into the soil and waters around MGPs is a significant factor in the pollution found at FMGPs today.

Commonly associated with former manufactured gas plants (known as "FMGPs" in environmental remediation) are contaminants including:

  • BTEX
    • Diffused out from deposits of coal/gas tars
    • Leaks of carburetting oil/light oil
    • Leaks from drip pots, that collected condensible hydrocarbons from the gas
  • Coal tar waste/sludge
    • Typically found in sumps of gas holders/decanting ponds.
    • Coal tar sludge has no resale value and so was always dumped.
  • Volatile organic compounds
  • Polycyclic aromatic hydrocarbons (PAHs)
    • Present in coal tar, gas tar, and pitch at significant concentrations.
  • Heavy metals
    • Leaded solder for gas mains, lead piping, coal ashes.
  • Cyanide
    • Purifier waste has large amounts of complex ferrocyanides in it.
  • Lampblack
    • Only found where crude oil was used as gasification feedstock.
  • Tar emulsions

Coal tar and coal tar sludges are frequently denser than water and are present in the environment as a dense non-aqueous phase liquid.

In the UK, former gasworks have commonly been developed over for residential and other uses (including the Millennium Dome), being seen as prime developable land in the confines of city boundaries. Situations such as these are now lead to problems associated with planning and the Contaminated Land Regime and have recently been debated in the House of Commons.

The more modern coal gasification processes (circa 1970 to 2006) also have environmental problems requiring various available technologies for mitigation.

UCG Environmental and Social Impacts

Underground Coal Gasification Environmental and Social Impacts

Eliminating mining eliminates mine safety issues. Compared to traditional coal mining and processing the underground coal gasification eliminates surface damage and solid waste discharge, and reduces sulfur dioxide (SO2) and nitrogen oxide (NOx) emissions. For comparison, the ash content of UCG syngas is estimated to be approximately 10 mg/m³ compared to smoke from traditional coal burning where ash content may be up to 70 mg/m³. However, UCG operations cannot be controlled as precisely as surface gasifiers. Variable include the rate of water influx, the distribution of reactants in the gasification zone, and the growth rate of the cavity. These can only be estimated from temperature measurements, and analyzing product gas quality and quantity.

Subsidence is a common issue with all forms of extractive industry. While UCG leaves the ash behind in the cavity, the depth of the void left after UCG is typically more than other methods of coal extraction.

Underground combustion produces NOx and SO2 and lowers emissions, including acid rain. The process has advantages for geologic carbon storage. Combining UCG with CCS technology allows re-injecting some of the CO2 on-site into the highly permeable rock created during the burning process, i.e. where the coal used to be. Contaminants such as ammonia and hydrogen sulfide can be removed from product gas at a relatively low cost.

Aquifer contamination is a potential environmental concerns. Organic and often toxic materials (such as phenol) remain in the underground chamber after gasification and therefore are likely to leach into ground water, absent appropriate site selection. Phenol leachate is the most significant environmental hazard due to its high water solubility and high reactiveness to gasification. Livermore conducted a burn at Hoe Creek, Wyoming, producing operating pressure in the burn cavity greater than the surrounding rock, forcing contaminants (including the carcinogen benzene) into potable groundwater. However, some research has shown that the persistence of such substances in the water is short and that ground water recovers within two years

Underground Coal Gasification

Underground coal gasification (UCG) is an industrial process, which converts coal into product gas. UCG is an in-situ gasification process carried out in non-mined coal seams using injection of oxidants, and bringing the product gas to surface through production wells drilled from the surface. The product gas could to be used as a chemical feedstock or as fuel for power generation. The technique can be applied to resources that are otherwise unprofitable or technically complicated to extract by traditional mining methods and it also offers an alternative to conventional coal mining methods for some resources.

Process of Underground Coal Gasification

Underground coal gasification converts coal to gas while still in the coal seam (in-situ). Gas is produced and extracted through wells drilled into the unmined coal–seam. Injection wells are used to supply the oxidants (air, oxygen, or steam) to ignite and fuel the underground combustion process. Separate production wells are used to bring the product gas to surface. The high pressure combustion is conducted at temperature of 700–900 °C (1290–1650 °F), but it may reach up to 1,500 °C (2,730 °F). The process decomposes coal and generates carbon dioxide (CO2), hydrogen (ḥ), carbon monoxide (CO) and small quantities of methane (CH4) and hydrogen sulfide(H2S). As the coal face burns and the immediate area is depleted, the oxidants injected are controlled by the operator.

As coal varies considerably in its resistance to flow, depending on its age, composition and geological history, the natural permeability of the coal to transport the gas is generally not adequate. For high pressure break-up of the coal, hydro-fracturing, electric-linkage, and reverse combustion may be used in varying degrees.

Two methods are commercially available. One uses vertical wells and a method of reverse combustion to open internal pathways in the coal. The process was used in the Soviet Union and was later modified by Ergo Exergy. It was tested in Chinchilla site in 1998–2003. Livermore developed another method that creates dedicated inseam boreholes, using drilling and completion technology adapted from oil and gas production. It has a movable injection point known as CRIP (controlled retraction injection point) and generally uses oxygen or enriched air for gasification.

According to the Commonwealth Scientific and Industrial Research Organisation the following coal seam characteristics are most suitable for the underground coal gasification:

  • Depth of 100–600 metres (330–2,000 ft)
  • Thickness more than 5 metres (16 ft)
  • Ash content less than 60%
  • Minimal discontinuities
  • No nearby aquifers (to avoid polluting supplies of drinking water).

Types of Coal

As geological processes apply pressure to dead biotic material 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. In its dehydrated form, peat is a highly effective absorbent for fuel and oil spills on land and water
  • 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 Upper Palaeolithic
  • 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 sedimentary rock, 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
  • Steam coal is a grade between bituminous coal and anthracite, once widely used as a fuel for steam locomotives. In this specialized use it is sometimes known as sea-coal in the U.S. Small steam coal (dry small steam nuts or DSSN) was used as a fuel for domestic water heating
  • Anthracite, the highest rank; a harder, glossy, black coal used primarily for residential and commercial space heating. It may be divided further into metamorphically 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:

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).

Cannel coal (sometimes called "candle coal"), is a variety of fine-grained, high-rank coal with significant hydrogen content. It consists primarily of "exinite" macerals, now termed "liptinite".

Largest Coal Importers by Country

Countries with annual import higher than 30 million tonnes are shown.

Imports of Coal by Country and year (million short tons)
Country 2006 2007 2008 2009 Share
Japan 199.7 209.0 206.0 182.1 17.5%
China 42.0 56.2 44.5 151.9 14.5%
South Korea 84.1 94.1 107.1 109.9 10.6%
India 52.7 29.6 70.9 76.7 7.4%
Taiwan 69.1 72.5 70.9 64.6 6.2%
Germany 50.6 56.2 55.7 45.9 4.4%
United Kingdom 56.8 48.9 49.2 42.2 4.1%
Total 991.8 1,056.5 1,063.2 1,039.8 100%

Largest Coal Exporters by Country

Countries with annual export higher than 10 million tonnes are shown.

Exports of Coal by Country and year (million short tons)
Country 2007 2008 2009 Share
Australia 268.5 278.0 288.5 26.5%
Indonesia 221.9 228.2 261.4 24.0%
Russia 112.2 115.4 130.9 12.0%
Colombia 74.5 74.7 75.7 6.9%
South Africa 72.6 68.2 73.8 6.8%
USA 60.6 83.5 60.4 5.5%
China 75.4 68.8 38.4 3.5%
Canada 33.4 36.5 31.9 2.9%
Vietnam 35.1 21.3 28.2 2.6%
Kazakhstan 32.8 47.6 25.7 2.4%
Poland 20.1 16.1 14.6 1.3%
Total 1,073.4 1,087.3 1,090.8 100%

Coal Production by Country

The reserve life is an estimate based only on current production levels and proved reserves level for the countries shown, and makes no assumptions of future production or even current production trends. This is a list of countries by coal production in 2009 based mostly on Statistical Review of World Energy 2010 published in 2010 by BP ranks countries with coal production larger than 100 millions tonnes.

Production of Coal by Country and year (million tonnes)
Country 2007 2008 2009 Share Reserve Life (years)
China 2526.0 2782.0 3050.0 45.6 % 38
USA 1040.2 1062.8 973.2 15.8 % 245
India 478.4 521.7 557.6 6.2 % 105
EU 593.4 587.7 536.8 4.6 % 55
Australia 399.0 401.5 409.2 6.7 % 186
Russia 314.2 326.5 298.1 4.3 % 150+
Indonesia 217.4 229.5 252.5 3.6 % 17
South Africa 247.7 250.4 250.0 3.6 % 122
Germany 201.9 192.4 183.7 2.6 % 37
Poland 145.9 143.9 135.1 1.7 % 56
Kazakhstan 97.8 111.1 101.5 1.5 % 308
Total World 6,421.2 6,781.2 6,940.6 100 % 119

World Coal Reserves

The 930 billion short tons of recoverable coal reserves estimated by the Energy Information Administration are equal to about 4,116 BBOE (billion barrels of oil equivalent). The amount of coal burned during 2007 was estimated at 7.075 billion short tons, or 133.179 quadrillion BTU's. This is an average of 18.8 million BTU per short ton. In terms of heat content, this is about 57,000,000 barrels (9,100,000 m3) of oil equivalent per day. By comparison in 2007, natural gas provided 51,000,000 barrels (8,100,000 m3) of oil equivalent per day, while oil provided 85,800,000 barrels per day.

BP, in its 2007 report, estimated at 2006 end that there were 909,064 million tons of proven coal reserves worldwide, or 147 years reserves-to-production ratio. This figure only includes reserves classified as "proven"; exploration drilling programs by mining companies, particularly in under-explored areas, are continually providing new reserves. In many cases, companies are aware of coal deposits that have not been sufficiently drilled to qualify as "proven". However, some nations haven't updated their information and assume reserves remain at the same levels even with withdrawals. Collective projections generally predict that global peak coal production may occur sometime around 2025 at 30 percent above current production in the best case scenario, depending on future coal production rates.

Of the three fossil fuels, coal has the most widely distributed reserves; coal is mined in over 100 countries, and on all continents except Antarctica. The largest reserves are found in the USA, Russia, China, India and Australia. Note the table below.

Proved recoverable coal reserves (million tons (teragrams))
Country Bituminous & Anthracite SubBituminous Lignite TOTAL Percentage of World Total
United States 108,501 98,618 30,176 237,295 22.6
Russia 49,088 97,472 10,450 157,010 14.4
China 62,200 33,700 18,600 114,500 12.6
Australia 37,100 2,100 37,200 76,500 8.9
India 56,100 0 4,500 60,600 7.0
Germany 99 0 40,600 40,699 4.7
Ukraine 15,351 16,577 1,945 33,873 3.9
Kazakhstan 21,500 0 12,100 33,600 3.9
South Africa 30,156 0 0 30,156 3.5
Serbia 9 361 13,400 13,770 1.6
Colombia 6,366 380 0 6,746 0.8
Canada 3,474 872 2,236 6,528 0.8
Poland 4,338 0 1,371 5,709 0.7
Indonesia 1,520 2,904 1,105 5,529 0.6
Brazil 0 4,559 0 4,559 0.5
Greece 0 0 3,020 3,020 0.4
Bosnia and Herzegovina 484 0 2,369 2,853 0.3
Mongolia 1,170 0 1,350 2,520 0.3
Bulgaria 2 190 2,174 2,366 0.3
Pakistan 0 166 1,904 2,070 0.3
Turkey 529 0 1,814 2,343 0.3
Uzbekistan 47 0 1,853 1,900 0.2
Hungary 13 439 1,208 1,660 0.2
Thailand 0 0 1,239 1,239 0.1
Mexico 860 300 51 1,211 0.1
Iran 1,203 0 0 1,203 0.1
Czech Republic 192 0 908 1,100 0.1
Kyrgyzstan 0 0 812 812 0.1
Albania 0 0 794 794 0.1
North Korea 300 300 0 600 0.1
New Zealand 33 205 333-7,000 571-15,000 0.1
Spain 200 300 30 530 0.1
Laos 4 0 499 503 0.1
Zimbabwe 502 0 0 502 0.1
Argentina 0 0 500 500 0.1
All others 3,421 1,346 846 5,613 0.7
Total world 404,762 260,789 195,387 860,938 100