Lignite
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Lignite (derived from Latin lignum meaning 'wood'), often referred to as brown coal,[1] is a soft, brown, combustible sedimentary rock formed from naturally compressed peat. It has a carbon content around 25–35%[1][2] and is considered the lowest rank of coal due to its relatively low heat content. When removed from the ground, it contains a very high amount of moisture, which partially explains its low carbon content. Lignite is mined all around the world and is used almost exclusively as a fuel for steam-electric power generation.
Lignite combustion produces less heat for the amount of carbon dioxide and sulfur released than other ranks of coal. As a result, lignite is the most harmful coal to human health.[3] Depending on the source, various toxic heavy metals, including naturally occurring radioactive materials, may be present in lignite and left over in the coal fly ash produced from its combustion, further increasing health risks.[4]
Characteristics
[edit]
Lignite is brownish-black in color and has a carbon content of 60–70 percent on a dry ash-free basis. However, its inherent moisture content is sometimes as high as 75 percent[1] and its ash content ranges from 6–19 percent, compared with 6–12 percent for bituminous coal.[5] As a result, its carbon content on the as-received basis (i.e., containing both inherent moisture and mineral matter) is typically just 25-35 percent.[2]

The energy content of lignite ranges from 10 to 20 MJ/kg (9 to 17 million BTU/short ton) on a moist, mineral-matter-free basis. The energy content of lignite consumed in the United States averages 15 MJ/kg (13 million BTU/short ton), on the as-received basis.[6] The energy content of lignite consumed in Victoria, Australia, averages 8.6 MJ/kg (7.4 million BTU/short ton) on a net wet basis.[7]
Lignite has a high content of volatile matter which makes it easier to convert into gas and liquid petroleum products than higher-ranking coals. Its high moisture content and susceptibility to spontaneous combustion can cause problems in transportation and storage. Processes which remove water from brown coal reduce the risk of spontaneous combustion to the same level as black coal, increase the calorific value of brown coal to a black coal equivalent fuel, and significantly reduce the emissions profile of 'densified' brown coal to a level similar to or better than most black coals.[8][9] However, removing the moisture increases the cost of the final lignite fuel.
Lignite rapidly degrades when exposed to air, in a process called slacking (or slackening).[10]
Uses
[edit]
Most lignite is used to generate electricity.[2] However, small amounts are used in agriculture, in industry, and even, as jet, in jewelry. Its historical use as fuel for home heating has continuously declined and is now of lower importance than its use to generate electricity.
As fuel
[edit]
Lignite is often found in thick beds located near the surface, making it inexpensive to mine. However, because of its low energy density, tendency to crumble, and typically high moisture content, brown coal is inefficient to transport and is not traded extensively on the world market compared with higher coal grades.[1][7] It is often burned in power stations near the mines, such as in Poland's Bełchatów plant and Turów plant, Australia's Latrobe Valley and Luminant's Monticello plant and Martin Lake plant in Texas. Primarily because of latent high moisture content and low energy density of brown coal, carbon dioxide emissions from traditional brown-coal-fired plants are generally much higher per megawatt-hour generated than for comparable black-coal plants, with the world's highest-emitting plant being Australia's Hazelwood Power Station[11] until its closure in March 2017.[12] The operation of traditional brown-coal plants, particularly in combination with strip mining, is politically contentious due to environmental concerns.[13][14]
The German Democratic Republic relied extensively on lignite to become energy self-sufficient, and eventually obtained 70% of its energy requirements from lignite.[15] Lignite was also an important chemical industry feedstock via Bergius process or Fischer-Tropsch synthesis in lieu of petroleum,[16] which had to be imported for hard currency following a change in policy by the Soviet Union in the 1970s, which had previously delivered petroleum at below market rates.[17] East German scientists even converted lignite into coke suitable for metallurgical uses (high temperature lignite coke) and much of the railway network was dependent on lignite either through steam trains or electrified lines mostly fed with lignite derived power.[17] As per the table below, East Germany was the largest producer of lignite for much of its existence as an independent state.
In 2014, about 12 percent of Germany's energy and, specifically, 27 percent of Germany's electricity came from lignite power plants,[18] while in 2014 in Greece, lignite provided about 50 percent of its power needs. Germany has announced plans to phase out lignite by 2038 at the latest.[19][20][21][22] Greece has confirmed that the last coal plant will be shut in 2025 after receiving pressure from the European Union[23] and plans to heavily invest in renewable energy.[24]
Home heating
[edit]Lignite was and is used as a replacement for or in combination with firewood for home heating. It is usually pressed into briquettes for that use.[25][26] Due to the smell it gives off when burned, lignite was often seen as a fuel for poor people compared to higher value hard coals. In Germany, briquettes are still readily available to end consumers in home improvement stores and supermarkets.[27][28][29][30]
In agriculture
[edit]An environmentally beneficial use of lignite is in agriculture. Lignite may have value as an environmentally benign soil amendment, improving cation exchange and phosphorus availability in soils while reducing availability of heavy metals,[31][32] and may be superior to commercial K humates.[33] Lignite fly ash produced by combustion of lignite in power plants may also be valuable as a soil amendment and fertilizer.[34] However, rigorous studies of the long-term benefits of lignite products in agriculture are lacking.[35]
Lignite may also be used for the cultivation and distribution of biological control microbes that suppress plant pests. The carbon increases the organic matter in the soil while the biological control microbes provide an alternative to chemical pesticides.[36]
Leonardite is a soil conditioner rich in humic acids that is formed by natural oxidation when lignite comes in contact with air.[37] The process can be replicated artificially on a large scale.[38] The less matured xyloid (wood-shaped) lignite also contains high amounts of humic acid.[39]
In drilling mud
[edit]Reaction with quaternary amine forms a product called amine-treated lignite (ATL), which is used in drilling mud to reduce fluid loss during drilling.[40]
As an industrial adsorbent
[edit]Lignite may have potential uses as an industrial adsorbent. Experiments show that its adsorption of methylene blue falls within the range of activated carbons currently used by industry.[41]
In jewellery
[edit]Jet is a form of lignite that has been used as a gemstone.[42] The earliest jet artifacts date to 10,000 BCE[43] and jet was used extensively in necklaces and other ornamentation in Britain from the Neolithic until the end of Roman Britain.[44] Jet experienced a brief revival in Victorian Britain.[45]
Geology
[edit]

Lignite begins as partially decayed plant material, or peat. Peat tends to accumulate in areas with high moisture, slow land subsidence, and no disturbance by rivers or oceans – under these conditions, the area remains saturated with water, which covers dead vegetation and protects it from atmospheric oxygen. Otherwise, peat swamps are found in a variety of climates and geographical settings. Anaerobic bacteria may contribute to the degradation of peat, but this process takes a long time, particularly in acidic water. Burial by other sediments further slows biological degradation, and subsequent transformations are a result of increased temperatures and pressures underground.[46]
Lignite forms from peat that has not been subjected to deep burial and heating. It forms at temperatures below 100 °C (212 °F),[1] primarily by biochemical degradation. This includes the process of humification, in which microorganisms extract hydrocarbons from peat and form humic acids, which decrease the rate of bacterial decay. In lignite, humification is partial, coming to completion only when the coal reaches sub-bituminous rank.[47] The most characteristic chemical change in the organic material during formation of lignite is the sharp reduction in the number of C=O and C-O-R functional groups.[48]
Lignite deposits are typically younger than higher-ranked coals, with the majority of them having formed during the Tertiary period.[1]
Extraction
[edit]Lignite is often found in thick beds located near the surface.[1][7] These are inexpensive to extract using various forms of surface mining, though this can result in serious environmental damage.[49] Regulations in the United States and other countries require that land that is surface mined must be restored to its original productivity once mining is complete.[50]
Strip mining of lignite in the United States begins with drilling to establish the extent of the subsurface beds. Topsoil and subsoil must be properly removed and either used to reclaim previously mined-out areas or stored for future reclamation. Excavator and truck overburden removal prepares the area for dragline overburden removal to expose the lignite beds. These are broken up using specially equipped tractors (coal ripping) and then loaded into bottom dump trucks using front loaders.[51]
Once the lignite is removed, restoration involves grading the mine spoil to as close an approximation as practical of the original ground surface (Approximate Original Contour or AOC). Subsoil and topsoil are restored and the land reseeded with various grasses. In North Dakota, a performance bond is held against the mining company for at least ten years after the end of mining operations to guarantee that the land has been restored to full productivity.[50] A bond (not necessary in this form) for mine reclamation is required in the US by the Surface Mining Control and Reclamation Act of 1977.[52]
Resources and reserves
[edit]List of countries by lignite resources
[edit]| Countries | Lignite resources (millions of tons) |
|---|---|
| United States | 1,368,124 |
| Russia | 541,353 |
| Australia | 407,430 |
| China | 323,849 |
| Poland | 222,392 |
| Vietnam | 199,876 |
| Pakistan | 176,739 |
| Mongolia | 119,426 |
| Canada | 118,270 |
| India | 38,830 |
| Germany | 36,500 |
Australia
[edit]The Latrobe Valley in Victoria, Australia, contains estimated reserves of some 65 billion tonnes of brown coal.[53] The deposit is equivalent to 25 percent of known world reserves. The coal seams are up to 98 m (322 ft) thick, with multiple coal seams often giving virtually continuous brown coal thickness of up to 230 m (755 ft). Seams are covered by very little overburden (10 to 20 m (33 to 66 ft)).[53]
A partnership led by Kawasaki Heavy Industries and backed by the governments of Japan and Australia has begun extracting hydrogen from brown coal. The liquefied hydrogen will be shipped via the transporter Suiso Frontier to Japan.[54]
North America
[edit]The largest lignite deposits in North America are the Gulf Coast lignites and the Fort Union lignite field. The Gulf Coast lignites are located in a band running from Texas to Alabama roughly parallel to the Gulf Coast. The Fort Union lignite field stretches from North Dakota to Saskatchewan. Both are important commercial sources of lignite.[10]
Types
[edit]Lignite can be separated into two types: xyloid lignite or fossil wood, and compact lignite or perfect lignite.
Although xyloid lignite may sometimes have the tenacity and the appearance of ordinary wood, it can be seen that the combustible woody tissue has experienced a great modification. It is reducible to a fine powder by trituration, and if submitted to the action of a weak solution of potash, it yields a considerable quantity of humic acid.[39] Leonardite is an oxidized form of lignite, which also contains high levels of humic acid.[55]
Jet is a hardened, gem-like form of lignite used in various types of jewelry.[42]
Production
[edit]This article needs to be updated. (January 2023) |
Germany is the largest producer of lignite,[56] followed by China, Russia, and United States.[57] Lignite accounted for 8% of all U.S. coal production in 2019.[2]
| Country or territory | 1970 | 1980 | 1990 | 2000 | 2010 | 2011 | 2012 | 2013 | 2014 | 2015 |
|---|---|---|---|---|---|---|---|---|---|---|
| 261 | 258.1 | 280 | [a] | |||||||
| 108[b] | 129.9[b] | 107.6[b] | 167.7 | 169 | 176.5 | 185.4 | 183 | 178.2 | 178.1 | |
| – | 24.3 | 45.5 | 47.7 | 125.3 | 136.3 | 145 | 147 | 145 | 140 | |
| 145[c] | 141[c] | 137.3[c] | 87.8 | 76.1 | 76.4 | 77.9 | 73 | 70 | 73.2 | |
| [d] | 2.6 | 7.3 | 8.4 | 5.5 | 6.5 | 6.6 | – | |||
| 2.5 | 3.4 | 3.8 | 3.8 | – | – | – | ||||
| 5 | 42.8 | 79.9 | 77.6 | 71.0 | 73.6 | 71.6 | 70.1 | 72.1 | 64.7 | |
| – | 36.9 | 67.6 | 59.5 | 56.5 | 62.8 | 64.3 | 66 | 63.9 | 63.1 | |
| – | 14.5 | 44.4 | 60.9 | 70.0 | 72.5 | 68.1 | 57.5 | 62.6 | 50.4 | |
| – | 32.9 | 46 | 67.3 | 68.8 | 66.7 | 69.1 | 59.9 | 58.0 | 63.0 | |
| – | 23.2 | 51.9 | 63.9 | 56.5 | 58.7 | 61.8 | 54 | 48 | 46 | |
| – | 5 | 14.1 | 24.2 | 37.7 | 42.3 | 43.5 | 45 | 47.2 | 43.9 | |
| – | – | – | – | 40.0 | 51.3 | 60.0 | 65.0 | 60.0 | 60.0 | |
| 82 | 87 | 71 | [e] | |||||||
| [f] | 50.1 | 43.8 | 46.6 | 43.5 | 40 | 38.3 | 38.3 | |||
| 3.7 | 2.4 | 2.4 | 2.3 | – | – | – | ||||
| – | 33.7 | 64.1 | 35.5[g] | [h] | ||||||
| [i] | [j] | 37.8 | 40.6 | 38 | 40.1 | 29.7 | 37.3 | |||
| [j] | 8.7[k] | 9[k] | 8.7[k] | 8.2[k] | 7.2[k] | 8.2[k] | ||||
| 7.5 | 6.7 | 8.2 | 7.5 | – | – | – | ||||
| 3.4 | 11 | 7.1 | 7 | 6.2 | 6.2 | 6.5 | ||||
| 3.7 | 4 | 4.1 | 4 | – | – | – | ||||
| [j] | 1.9 | 2 | 2 | – | – | – | ||||
| – | 26.5 | 33.7 | 29 | 31.1 | 35.5 | 34.1 | 24.7 | 23.6 | 25.2 | |
| – | 30 | 31.5 | 26.3 | 29.4 | 37.1 | 32.5 | 26.5 | 31.3 | 35.9 | |
| – | 1.4 | 2.1 | 30 | 14 | 9 | 20 | – | – | – | |
| – | 1.5 | 12.4 | 17.8 | 18.3 | 21.3 | 18.3 | 18.1 | 18 | 15.2 | |
| – | 4.4 | 6.6 | 5.1 | 8.5 | 8.3 | 9.9 | – | – | – | |
| – | 6 | 9.4 | 11.2 | 10.3 | 9.7 | 9.5 | 9.0 | 8.5 | 10.5 | |
| – | 22.6 | 17.3 | 14 | 9.1 | 9.6 | 9.3 | 9.6 | 9.6 | 9.3 | |
| – | 10 | 10.6 | 7.2 | 6.7 | 6.8 | 6.8 | 7 | 7 | 7 | |
| Source: World Coal Association[58] · U.S. Energy Information Administration[59] · BGR bund.de Energiestudie 2016[60] · 1970 data from World Coal (1987)[61]
– no data available | ||||||||||
- ^ East Germany became a part of Germany as a result of German reunification in 1990.
- ^ a b c Data prior to 2000 are for West Germany only.
- ^ a b c Data prior to 2000 represent the Soviet Union.
- ^ Country was a part of the Soviet Union during this time.
- ^ Czechoslovakia dissolved in 1993.
- ^ Country was a part of Czechoslovakia during this time.
- ^ 2000 data is for Federal Republic of Yugoslavia.
- ^ Yugoslavia broke up in a process that concluded in 1992.
- ^ Country was a part of Yugoslavia during this time.
- ^ a b c Country was a part of Federal Republic of Yugoslavia during this time.
- ^ a b c d e f Albanians unilaterally declared independence from Serbia, but the country it is not member of UN and its status is heavily disputed.
Gallery
[edit]See also
[edit]- Coal analysis – Measurement of properties of coal
- Dakota Gasification Company
- Energy value of coal
- International Humic Substances Society
- Karrick process
- Kemper Project – Power station in Mississippi, US
- Orders of magnitude (specific energy) – Physical quantity representing energy content per unit mass
- Subcoal – Coal substitute made from recycled waste
- Torrefaction – Thermochemical process
References
[edit]- ^ a b c d e f g Kopp, Otto C. "Lignite" Archived 2019-06-03 at the Wayback Machine in Encyclopædia Britannica
- ^ a b c d "Coal explained". Energy Information Administration. Archived from the original on 31 January 2021. Retrieved 26 September 2020.
- ^ "Lignite coal – health effects and recommendations from the health sector" (PDF). Health and Environment Alliance. December 2018. Archived (PDF) from the original on 9 October 2022.
- ^ Holdinghausen, Heike. "Gesundheit: Feiner Staub, großer Schaden". Heinrich Böll Stiftung. Archived from the original on 17 January 2022. Retrieved 12 March 2022.
- ^ Ghassemi, Abbas (2001). Handbook of Pollution Control and Waste Minimization. CRC Press. p. 434. ISBN 0-8247-0581-5.
- ^ "Lignite". Glossary. U.S. Energy Information Agency. Retrieved 4 May 2021.
- ^ a b c Victoria, Australia: A principal brown coal province (PDF). Department of Primary Industries Melbourne. July 2010. ISBN 978-1-74199-835-1. Archived from the original (PDF) on 17 March 2011.
- ^ George, A.M. (1975). State Electricity Victoria, Petrographic Report No 17 (Report).
- ^ Perry, G.J.; Allardice, D.J. Paper R4.1. Coal Resources Conference, NZ 1987 (Report). Proc. 1, Sec. 4.
- ^ a b Schobert, Harold H., ed. (1995). "Chapter 1 The principal lignite deposits of North America". Coal Science and Technology. 23: 1–50. doi:10.1016/S0167-9449(06)80002-9. ISBN 9780444898234.
- ^ "Hazelwood tops international list of dirty power stations". World Wide Fund for Nature Australia. Archived from the original on 13 October 2008. Retrieved 2 October 2008.
- ^ "End of generation at Hazelwood". Engie. Archived from the original on 31 March 2017. Retrieved 30 June 2017.
- ^ "The Greens Won't Line Up For Dirty Brown Coal In The Valley". Australian Greens Victoria. 18 August 2006. Archived from the original on 13 August 2011. Retrieved 28 June 2007.
- ^ "Greenpeace Germany Protests Brown Coal Power Stations". Environment News Service. 28 May 2004. Archived from the original on 30 September 2007. Retrieved 28 June 2007.
- ^ Irfan, Ulmair (3 November 2014). "How East Germany Cleaned Up Dirty Power". Scientific American. Springer Nature America, Inc. Archived from the original on 12 November 2020. Retrieved 4 May 2021.
- ^ "Liquid fuel revival". Chemistry and Industry. No. 22. SCI. 2009. Archived from the original on 4 May 2021. Retrieved 4 May 2021.
- ^ a b "The history of energy in Germany". Planete energies. Total Foundation. 29 April 2015. Archived from the original on 14 June 2021. Retrieved 4 May 2021.
- ^ "Statistics on energy production in Germany 2014, Department of Energy (in german, lignite = "Braunkohle")" (PDF). 1 October 2014. Archived from the original (PDF) on 6 December 2015. Retrieved 10 December 2015.
- ^ "Interview zum Kohlekompromiss: "Damit ist es nicht getan"". Tagesschau.de.
- ^ "Was der Kohlekompromiss für Deutschland bedeutet". Erneuerbareenergien.de. 13 August 2019. Archived from the original on 13 August 2020. Retrieved 8 December 2020.
- ^ "Teurer Kohlekompromiss". Zdf.de. Retrieved 30 June 2022.
- ^ "Kommentar zum Kohleausstieg: Der Kohlekompromiss ist ein Meisterstück". Ksta.de. 26 January 2019.
- ^ "Greece confirms last coal plant will be shut in 2025". Euractiv.com. 26 April 2021.
- ^ "Σκρέκας: Προετοιμάζουμε και σχεδιάζουμε την πράσινη πολιτική της χώρας | ΣΚΑΪ". Skai.gr. 18 May 2021. Archived from the original on 20 May 2021. Retrieved 20 May 2021.
- ^ Francis, Wilfrid (1980). Fuels and fuel technology : a summarized manual (2d (SI) ed.). Oxford: Pergamon Press. pp. 4–5. ISBN 9781483147949.
- ^ Thuβ, U.; Popp, P.; Ehrlich, Chr.; Kalkoff, W.-D. (July 1995). "Domestic lignite combustion as source of polychlorodibenzodioxins and -furans (PCDD/F)". Chemosphere. 31 (2): 2591–2604. Bibcode:1995Chmsp..31.2591T. doi:10.1016/0045-6535(95)00132-R.
- ^ "Briketts kaufen bei". Obi.de. Archived from the original on 29 July 2021. Retrieved 29 July 2021.
- ^ "Briketts kaufen bei". Hornbach.de. Archived from the original on 29 July 2021. Retrieved 29 July 2021.
- ^ "Braunkohlebriketts 10kg bei REWE online bestellen!". Shop.rewe.de. Archived from the original on 25 May 2022. Retrieved 30 June 2022.
- ^ "Briketts kaufen bei Bauhaus". Bauhaus.info. Archived from the original on 11 April 2022. Retrieved 9 March 2022.
- ^ Kim Thi Tran, Cuc; Rose, Michael T.; Cavagnaro, Timothy R.; Patti, Antonio F. (November 2015). "Lignite amendment has limited impacts on soil microbial communities and mineral nitrogen availability". Applied Soil Ecology. 95: 140–150. Bibcode:2015AppSE..95..140K. doi:10.1016/j.apsoil.2015.06.020.
- ^ Li, Changjian; Xiong, Yunwu; Zou, Jiaye; Dong, Li; Ren, Ping; Huang, Guanhua (March 2021). "Impact of biochar and lignite-based amendments on microbial communities and greenhouse gas emissions from agricultural soil". Vadose Zone Journal. 20 (2). Bibcode:2021VZJ....2020105L. doi:10.1002/vzj2.20105.
- ^ Lyons, Graham; Genc, Yusuf (28 October 2016). "Commercial Humates in Agriculture: Real Substance or Smoke and Mirrors?". Agronomy. 6 (4): 50. Bibcode:2016Agron...6...50L. doi:10.3390/agronomy6040050.
- ^ Ram, Lal C.; Srivastava, Nishant K.; Jha, Sangeet K.; Sinha, Awadhesh K.; Masto, Reginald E.; Selvi, Vetrivel A. (September 2007). "Management of Lignite Fly Ash for Improving Soil Fertility and Crop Productivity". Environmental Management. 40 (3): 438–452. Bibcode:2007EnMan..40..438R. doi:10.1007/s00267-006-0126-9. PMID 17705037. S2CID 1257174.
- ^ Patti, Antonio; Rose, Michael; Little, Karen; Jackson, Roy; Cavagnaro, Timothy (2014). "Evaluating Lignite-Derived Products (LDPs) for Agriculture – Does Research Inform Practice?". EGU General Assembly Conference Abstracts: 10165. Bibcode:2014EGUGA..1610165P. Archived from the original on 11 April 2022. Retrieved 4 May 2021.
- ^ Jones, Richard; Petit, R; Taber, R (1984). "Lignite and stillage:carrier and substrate for application of fungal biocontrol agents to soil". Phytopathology. 74 (10): 1167–1170. doi:10.1094/Phyto-74-1167.
- ^ "Youngs, R.W. & Frost, C.M. 1963. Humic acids from leonardite – a soil conditioner and organic fertilizer. Ind. Eng. Chem., 55, 95–99" (PDF). Archived (PDF) from the original on 9 October 2022. Retrieved 30 June 2022.
- ^ Gong, Guanqun; Xu, Liangwei; Zhang, Yingjie; Liu, Weixin; Wang, Ming; Zhao, Yufeng; Yuan, Xin; Li, Yajun (3 November 2020). "Extraction of Fulvic Acid from Lignite and Characterization of Its Functional Groups". ACS Omega. 5 (43): 27953–27961. doi:10.1021/acsomega.0c03388. PMC 7643152. PMID 33163778.
- ^ a b Mackie, Samuel Joseph (1861). The Geologist. Original from Harvard University: Reynolds. pp. 197–200.
- ^ Elgibaly, A.; Farahat, M.; Abd El Nabbi, M. (1 December 2018). "The Optimum Types and Characteristics of Drilling Fluids Used During Drilling in The Egyption Western Desert". Journal of Petroleum and Mining Engineering. 20 (1): 89–100. doi:10.21608/jpme.2018.40453.
- ^ Qi, Ying; Hoadley, Andrew F.A.; Chaffee, Alan L.; Garnier, Gil (April 2011). "Characterisation of lignite as an industrial adsorbent". Fuel. 90 (4): 1567–1574. Bibcode:2011Fuel...90.1567Q. doi:10.1016/j.fuel.2011.01.015.
- ^ a b Neuendorf, K. K. E. Jr.; Mehl, J. P.; Jackson, J. A., eds. (2005). Glossary of Geology (5th ed.). Alexandria, Virginia: American Geological Institute. p. 344.
- ^ "Venus figures from Petersfels". Archived from the original on 29 September 2016. Retrieved 9 August 2016.
- ^ Allason-Jones, Lindsay (1996). Roman Jet in the Yorkshire Museum. The Yorkshire Museum. pp. 8–11. ISBN 0905807170.
- ^ Muller, Helen (1987). Jet. Butterworths. pp. 59–63. ISBN 0408031107.
- ^ Schweinfurth, Stanley P.; Finkelman, Robert P. (2002). "Coal – A complex natural resource". U.S. Geological Survey Circular. 1143. doi:10.3133/cir1143. hdl:2027/umn.31951d02181642b.
- ^ "Coal types, formation, and methods of mining". Eastern Pennsylvania Coalition for Abandoned Mine Reclamation. 2016. Archived from the original on 17 July 2020. Retrieved 5 May 2021.
- ^ Ibarra, JoséV.; Muñoz, Edgar; Moliner, Rafael (June 1996). "FTIR study of the evolution of coal structure during the coalification process". Organic Geochemistry. 24 (6–7): 725–735. Bibcode:1996OrGeo..24..725I. doi:10.1016/0146-6380(96)00063-0.
- ^ Turgeon, Andrew; Morse, Elizabeth (22 December 2012). "Coal". National Geographic. Archived from the original on 25 September 2021. Retrieved 25 September 2021.
- ^ a b "Reclamation Process". Mining Lignite Coal for our Energy Future. BNI Coal. Archived from the original on 25 September 2021. Retrieved 25 September 2021.
- ^ "Mining Process". Mining Lignite Coal for our Energy Future. BNI Coal. Retrieved 25 September 2021.
- ^ "Reclamation Bonds". Office of Surface Mining Reclamation and Enforcement. Archived from the original on 2 March 2022. Retrieved 18 March 2022.
- ^ a b Department of Primary Industries, Victorian Government, Australia, ‘Victoria Australia: A Principle Brown Coal Province’ (Fact Sheet, Department of Primary Industries, July 2010).
- ^ "Kawasaki Heavy says liquefied hydrogen carrier departs Japan for Australia". Asia Pacific. Reuters. 24 December 2021. Archived from the original on 24 December 2021. Retrieved 24 December 2021.
- ^ Tan, Kim H. (22 April 2003). Humic Matter in Soil and the Environment: Principles and Controversies. CRC Press. ISBN 9780203912546. Retrieved 30 June 2022 – via Google Books.
- ^ "Deutschland ‒Rohstoffsituation 2015" (PDF). Bundesanstalt für Geowissenschaften und Rohstoffe (in German). 1 November 2016. Archived from the original (pdf) on 6 July 2019. Retrieved 6 July 2019.
- ^ Appunn, Kerstine (7 August 2018). "Germany's three lignite mining regions". The Clean Energy Wire. Archived from the original on 26 November 2018. Retrieved 5 July 2019.
Germany has been the largest lignite producer in the world since the beginning of industrial lignite mining. It still is, followed by China, Russia, and the United States. The softer and moister lignite (also called brown or soft coal) has a lower calorific value than hard coal and can only be mined in opencast operations. When burned, it is more CO2 intensive than hard coal.
- ^ "Resources". World Coal Association. 2014. Archived from the original on 23 December 2015. Retrieved 22 December 2015.
- ^ "Production of Lignite Coal". U.S. Energy Information Administration. 2012. Archived from the original on 24 December 2015. Retrieved 23 December 2015.
- ^ "Energiestudie 2016 Tabellen". Archived from the original on 20 October 2017. Retrieved 19 April 2017.
- ^ Gordon, Richard (1987). World coal: economics, policies and prospects. Cambridge: Cambridge University Press. p. 44. ISBN 0521308275. OCLC 506249066.
External links
[edit]- "Coal and lignite domestic consumption". Global Energy Statistical Yearbook. 2016.
- Geography in action – an Irish case study
- Photograph of lignite
- Coldry:Lignite Dewatering Process
Lignite
View on GrokipediaPhysical and Chemical Characteristics
Composition and Properties
Lignite consists primarily of carbonized vegetal matter in an early stage of coalification, with a typical carbon content of 25% to 35% on an as-received basis, reflecting its low rank and incomplete carbonization.[7] Hydrogen content ranges from 4% to 5%, oxygen from 20% to 30%, and nitrogen around 1%, while sulfur levels vary geographically but average 0.5% to 3%, predominantly in organic form.[8][9] Ash content is generally low at 4% to 15%, derived from inorganic minerals such as silica, alumina, and iron oxides incorporated during deposition.[10] Volatile matter exceeds 45%, facilitating easy ignition but contributing to inefficient combustion without preprocessing. Physically, lignite is soft, friable, and brownish-black in color, with a blocky or earthy texture that crumbles readily due to its high inherent moisture content of 25% to 40%.[3][11] This moisture, held in open pores, results in bulk densities of 0.8 to 1.0 g/cm³ and high porosity (often 50% or more), enhancing its susceptibility to oxidation and spontaneous heating.[12] The as-received heating value is low, typically 10 to 18 MJ/kg (4,300 to 7,700 Btu/lb), limited by moisture and volatiles, compared to higher-rank coals.[6][8] On a dry, mineral-matter-free basis, the calorific value rises to 15 to 25 MJ/kg, underscoring its potential for upgrading via drying.[9]Comparison to Other Coals
Lignite represents the lowest rank in the coal classification system, distinguished by its high moisture content, typically ranging from 25% to 45%, and low fixed carbon content of 25% to 35%, which yield a gross calorific value of approximately 4,000 to 8,300 British thermal units per pound (Btu/lb).[13][1] In comparison, higher-rank coals undergo progressive coalification, resulting in reduced moisture, increased carbon content, and elevated heating values; sub-bituminous coal features 35% to 45% carbon and 8,300 to 13,000 Btu/lb, bituminous coal contains 45% to 86% carbon with 10,500 to 15,500 Btu/lb, and anthracite exhibits 86% to 97% carbon exceeding 15,000 Btu/lb.[7][14] These differences stem from varying degrees of geological pressure, heat, and time during formation, with lignite retaining more volatile matter (up to 65%) and oxygen, rendering it softer and more prone to spontaneous combustion than denser, harder anthracite.[1] Lignite's elevated moisture and lower energy density necessitate larger volumes for equivalent energy output compared to bituminous or anthracite, often limiting its transport and favoring local use.[2]| Coal Type | Carbon Content (%) | Moisture Content (%) | Heating Value (Btu/lb) | Volatile Matter (%) |
|---|---|---|---|---|
| Lignite | 25–35 | 25–45 | 4,000–8,300 | 45–65 |
| Sub-bituminous | 35–45 | 15–30 | 8,300–13,000 | 35–45 |
| Bituminous | 45–86 | 2–15 | 10,500–15,500 | 15–45 |
| Anthracite | 86–97 | <10 | >15,000 | <8 |
Geological Formation and Deposits
Formation Processes
Lignite originates from the accumulation of partially decayed plant matter in ancient wetland environments, such as swamps and mires, where anaerobic conditions inhibit complete decomposition. Primarily composed of remains from trees, ferns, reeds, and other herbaceous vegetation, this organic debris compacts into peat, a precursor material rich in moisture and low in carbon (typically 60% or less on a dry basis).[1][16] The process begins with rapid burial of the plant material in waterlogged settings, preventing oxidation and promoting preservation through biochemical degradation by microbes.[17] Subsequent geological burial under layers of sediment initiates diagenesis, the transitional phase to lignite. Increasing overburden pressure causes physical compaction, expelling pore water and reducing peat volume by 50-70%, while mild heat from the Earth's geothermal gradient (generally 20-50°C per kilometer of depth) drives dewatering and minor chemical alterations, such as loss of oxygen and volatiles alongside modest carbon enrichment (to 25-35% on a dry, ash-free basis).[17][18] These changes occur at shallow depths (less than 1-2 km) and low temperatures (below 100°C), halting further coalification and yielding lignite's characteristic brown color, high moisture content (25-45%), and friable texture.[7] Key coalification subprocesses during the lignite stage include humification, which converts plant biopolymers into stable humic acids; gelification, forming a cohesive, gel-like matrix from microbial activity; and fusinitization, involving oxidative alteration of woody tissues into inertinite macerals.[19] Cleats—systematic fracture networks—also develop perpendicular to bedding, aiding later fluid migration but forming primarily through desiccation and tectonic stress rather than high metamorphic pressures.[17] Most lignite beds date to the Cenozoic era (66 million years ago to present), reflecting relatively recent deposition in subtropical to temperate paleoenvironments, though some occur in Mesozoic strata.[7][5]Global Distribution and Major Deposits
Lignite deposits form in low-lying sedimentary basins during the Tertiary period, primarily in continental settings with limited tectonic activity, leading to concentrations in regions like the northern Great Plains of North America, central Europe, and parts of Asia and Australia. Globally, lignite resources exceed 3 trillion metric tons, though economic reserves are smaller due to the fuel's low energy density and high moisture content, limiting extractability.[20][21] The United States holds the largest identified lignite resources at approximately 1.37 trillion metric tons as of 2022, concentrated in the Williston Basin spanning North Dakota, Montana, South Dakota, and Wyoming, where thick, extensive seams support large-scale surface mining operations.[20] Russia's lignite resources stand at 541.4 billion metric tons, with major deposits in the Kansk-Achinsk Basin in Siberia and smaller occurrences in European Russia, though extraction remains underdeveloped compared to higher-rank coals.[20] In Europe, Germany possesses significant lignite deposits totaling around 36 billion metric tons in recoverable reserves, primarily in the Rhineland (e.g., Garzweiler and Hambach mines) and Lusatian regions, which have historically supplied over 40% of the country's electricity but face phase-out pressures. Poland ranks among the top globally with over 20 billion metric tons in resources, centered at the Bełchatów complex, the world's largest lignite mine by output, while Czechia and Greece host deposits in the Most Basin and Ptolemaida-Ptolemais fields, respectively.[21][6] Asia features substantial reserves in China, estimated at over 20 billion metric tons, scattered across Inner Mongolia and Heilongjiang provinces, supporting local power generation despite transportation challenges. Indonesia's deposits in South Sumatra exceed 30 billion metric tons, while India's Neyveli lignite field in Tamil Nadu holds about 3 billion tons, integral to regional energy needs. Australia’s principal deposits lie in the Latrobe Valley of Victoria, with resources surpassing 50 billion metric tons, though utilization has declined amid energy transitions.[22][9]| Country | Estimated Lignite Resources (billion metric tons, 2022) | Key Deposits/Regions |
|---|---|---|
| United States | 1,370 | Williston Basin (North Dakota, Montana) |
| Russia | 541 | Kansk-Achinsk Basin (Siberia) |
| Australia | >50 | Latrobe Valley (Victoria) |
| China | >20 | Inner Mongolia, Heilongjiang |
| Poland | >20 | Bełchatów (Central Poland) |
| Germany | ~36 (reserves) | Rhineland, Lusatia |
Extraction and Production Methods
Mining Techniques
Lignite deposits typically occur at shallow depths, making surface mining the predominant extraction method worldwide, as underground operations are economically and technically challenging due to the coal's high moisture content, weak structural integrity, and propensity for spontaneous combustion.[23][24] Surface mining accounts for nearly all lignite production, with techniques focused on efficient overburden removal to access thick, near-surface seams.[25] The primary technique is strip mining, where overburden—consisting of topsoil, subsoil, and rock—is systematically removed in long strips to expose the lignite seam. This process begins with exploration drilling to delineate deposit boundaries, followed by stripping and stockpiling topsoil for later reclamation. Overburden is then excavated using large draglines, truck-and-shovel systems, or continuous miners, depending on site geology and scale; for instance, massive bucket-wheel excavators, capable of moving thousands of cubic meters per hour, are employed in large-scale operations like those in Germany.[25][26][27] Once exposed, lignite is loosened via ripping or specialized machinery such as auger miners for extended seams or Easy Miners resembling asphalt milling equipment for precise recovery, then loaded onto conveyors or haul trucks for transport to processing facilities.[28][29] Depths suitable for surface mining generally do not exceed 200 feet (60 meters), beyond which costs escalate prohibitively.[18] Underground mining of lignite is exceptionally rare in modern practice, historically limited to small-scale efforts in regions like early North Dakota operations, but discontinued due to unstable roof and floor conditions, high groundwater pressure, and safety risks from auto-ignition.[23][24] Where attempted, methods like room-and-pillar were used, but these have been supplanted by surface techniques for efficiency and lower per-ton costs.[30]Global Production Trends and Statistics
Global lignite production peaked at approximately 821 million metric tons in 2017 before declining to 800 million metric tons in 2018 and further to 734 million metric tons in 2019, driven by policy-driven phase-outs in Europe and competition from natural gas and renewables.[31] The onset of the COVID-19 pandemic exacerbated the downturn, with output falling to a low of 637 million metric tons in 2020 as industrial demand weakened globally.[31] Production partially rebounded to 687 million metric tons in 2021, reflecting recovery in key Asian markets, though European declines persisted amid commitments to reduce coal dependency.[31] In 2022, the energy crisis triggered by the Russia-Ukraine conflict led to temporary production increases in parts of Europe, with EU coal output (largely lignite) rising 5% to 349 million metric tons overall.[32] By 2023, however, the trajectory reversed in the region, with EU lignite-dominated production dropping to an estimated 278 million metric tons, including 102 million metric tons from Germany alone, as phase-out schedules accelerated.[33] Globally, lignite output stabilized around 800 million metric tons annually through 2023, with projections indicating minimal growth or slight declines through 2027 due to stagnant demand in power generation and efficiency gains in alternative fuels.[33] The following table summarizes production by leading countries in 2021 (in million metric tons), highlighting China's dominance from vast domestic deposits in regions like Inner Mongolia: Data reflect primarily opencast mining for local power use, with variations attributable to national energy policies; European figures declined further post-2021, while Asian production supported baseload needs amid rapid electrification.[31] Germany's output, for instance, fell from 171 million metric tons in 2017 to 131 million metric tons in 2022, underscoring causal links between regulatory decarbonization targets and reduced extraction.[34][31]Resources and Reserves
Estimated Reserves by Country
Russia holds the largest estimated lignite reserves globally, exceeding several billion metric tons as of 2022, primarily in regions suitable for open-pit mining.[22] The United States possesses the most extensive lignite resources, totaling 1.37 trillion metric tons in 2022, with over 350 billion tons concentrated in western North Dakota alone, though proved economic reserves represent a smaller economically viable subset due to transportation constraints and moisture content limiting marketability beyond local power generation.[20][5] Australia's lignite reserves are estimated at 37 billion tons, mainly in Victoria's Gippsland Basin, supporting historical domestic energy needs but facing declining extraction amid energy transitions.[35] India's geological lignite resources reached 47.36 billion tonnes as of April 1, 2023, concentrated in Tamil Nadu, Rajasthan, and Gujarat, with proved reserves forming a portion amenable to surface mining for regional power and cement production.[36] Germany's reserves, estimated around 36-40 billion tonnes in resources terms, are distributed across the Rhenish, Lusatian, and Central districts, enabling significant historical production but subject to phasedown commitments under national climate policy.[37] Poland ranks among the top ten globally with proved lignite reserves of approximately 5.8 billion tonnes, underpinning about 20% of its electricity in recent years despite environmental pressures.[21]| Country | Estimated Reserves/Resources (billion metric tons) | Year | Notes |
|---|---|---|---|
| Russia | > several (reserves); 541 (resources) | 2022 | Largest proved reserves; resources in eastern basins.[22][20] |
| United States | 1,370 (resources); ~350 in North Dakota alone | 2022 | Primarily subbituminous-lignite in Great Plains; reserves lower due to economics.[20][5] |
| Australia | 37 (reserves) | Recent | Focused in Victoria; resources higher but utilization declining.[35] |
| India | 47 (resources) | 2023 | Geological total; proved portion supports local industry.[36] |
| Poland | 5.8 (reserves) | Recent | Tenth globally; key for baseload power.[21] |
