Peat gatherers at Westhay, Somerset Levels in 1905

Peat stacks and cutting at Westhay, Somerset Levels

Harvesting the peat at Westhay, Somerset Levels

Peat in Lewis, Scotland

Peat (turf) is an accumulation of partially decayed vegetation. One of the most common components is Sphagnum moss, although many other plants can contribute. Soils that contain mostly peat are known as a histosol. Peat forms in wetland conditions, where flooding obstructs flows of oxygen from the atmosphere, reducing rates of decomposition.^[1] Bogs are the most important source of peat,^[2] but other less common wetland types also deposit peat, including fens, pocosins, and peat swamp forests. There are a good many other words for lands dominated by peat including moors, muskeg or mires. Landscapes covered in peat also have specific kinds of plants, particularly Sphagnum moss, ericaceous shrubs, and sedges (see bog for more information on this aspect of peat). Since organic matter accumulates over thousands of years, peat deposits also provide records of past vegetation and climates stored in plant remains, particularly pollen. Hence they allow humans to reconstruct past environments and changes in human land use.^[3] Peat is harvested as an important source of fuel in certain parts of the world. By volume, there are about 4 trillion m³ of peat in the world covering a total of around 2% of global land area (about 3 million km²), containing about 8 billion terajoules of energy.^[4]

Geographic distribution[link]

Peat extraction in East Frisia, Germany

Peatlands are areas of land with a naturally accumulated layer of peat. Peatlands are found in at least 175 countries and cover around 4 million km² or 3% of the world’s land area. In Europe, peatlands extend to ca. 515,000 km².^[5]

Peat deposits are found in many places around the world, including northern Europe, and North America, principally in Canada and the northern United States. Here, too, occur some of the worlds largest peatlands, including The West Siberian Lowland, the Hudson Bay Lowland, and the Mackenzie River Valley^[6]. The amount of peat is smaller in the southern hemisphere, partly because there is less land, yet South America (Southern Patagonia/Tierra del Fuego) has one of the world's largest wetlands, the vast Magellanic Moorland, with extensive peat dominated landscapes^[7]. Peat can be found in New Zealand, Kerguelen, and the Falkland Islands, Indonesia (Kalimantan (Sungai Putri, Danau Siawan, Sungai Tolak, Rasau Jaya (West Kalimantan), and Sumatra). Indonesia has more tropical peat land and mangrove forests than any other nation on earth, but Indonesia is losing wetlands by 100,000 hectares per year.^[8]

Approximately 60% of the world's wetlands are peat. About 7% of total peatlands have been exploited for agriculture and forestry.^{[citation needed]} Under proper conditions, peat will turn into lignite coal over geologic periods of time.

Formation[link]

Peat forms when plant material, usually in wet areas, is inhibited from decaying fully by acidic and anaerobic conditions. It is composed mainly of wetland vegetation: principally bog plants including mosses, sedges and shrubs. As it accumulates, the peat can hold water, thereby slowly creating wetter conditions, and allowing the area of wetland to expand. Peatland features can include ponds, ridges, and raised bogs. For more information on this process, refer to wetland in general and bog in particular.^[9]

Most modern peat bogs formed in high latitudes after the retreat of the glaciers at the end of the last ice age some 12,000 years ago.^[10] Peat usually accumulates slowly, at the rate of about a millimetre per year.^[11]

The peat in the world's peatlands has been forming for 360 million years and contains 550 Gt of carbon.^[12]

Under the appropriate circumstances, peat could be considered an early component in the formation of coal.

Types of peat material[link]

Peat material is either fibric, hemic, or sapric. Fibric peats are the least decomposed, and comprise intact fiber. Hemic peats are somewhat decomposed, and sapric are the most decomposed. Phragmites peat is one composed of reed grass, Phragmites australis, and other grasses. It is denser than many other types of peat. Engineers may describe a soil as peat which has a relatively high percentage of organic material. This soil is problematic because it exhibits poor consolidation properties.

Characteristics and uses[link]

A peat stack in Ness in the Isle of Lewis (Scotland).

Worked bank in blanket bog, near Ulsta, Yell, Shetland Islands

Falkland Islanders shovelling peat in the 1950s

Peat is soft and easily compressed. Under pressure, water in the peat is forced out. Upon drying, peat can be used as a fuel. It has industrial importance as a fuel in some countries, such as Ireland and Finland, where it is harvested on an industrial scale. In many countries, including Ireland and Scotland, where trees are often scarce, peat is traditionally used for cooking and domestic heating. Stacks of drying peat dug from the bogs can still be seen in some rural areas.

Peat's insulating properties make it of use to industry.

In Scotland[link]

Some Scotch whisky distilleries, such as those on Islay, use peat fires to dry malted barley. This gives some Scotch whisky a distinctive smoky flavour, often called "peatiness".^[13]

Although peat has many uses for humans, it also presents severe problems at times. Wet or dry, it can be a major fire hazard, as peat fires can burn almost indefinitely (or at least until the fuel is exhausted). Peat fires can even burn underground, reigniting after the winter, provided there is a source of oxygen. Peat deposits also pose major difficulties to builders of structures, roads, and railways, as they are highly compressible under even small loads. When the West Highland Line was built across Rannoch Moor in western Scotland, its builders had to float the tracks on a mattress of tree roots, brushwood and thousands of tons of earth and ashes.

Peat bogs had considerable ritual significance to Bronze Age and Iron Age peoples, who considered them to be home to (or at least associated with) nature gods or spirits. The bodies of the victims of ritual sacrifices have been found in a number of locations in Scotland, England, Ireland, and especially northern Germany and Denmark, almost perfectly preserved by the tanning properties of the acidic water. (See Tollund Man for one of the most famous examples of a bog body).

Peat wetlands formerly had a degree of metallurgical importance as well. During the Dark Ages, peat bogs were the primary source of bog iron, used to create the swords and armour of the Vikings.

Many peat swamps along the coast of Malaysia serve as a natural means of flood mitigation. The peat swamps serve like a natural form of water catchment whereby any overflow will be absorbed by the peat. However, this is effective only if the forests are still present, since they prevent peat fires.

In Ireland[link]

Industrial milled peat production in a section of the Bog of Allen in the Irish Midlands. The turf in the foreground is machine produced for domestic use

In Ireland, large-scale domestic and industrial peat usage is widespread. Specifically in the Republic of Ireland, a state-owned company called Bord na Móna is responsible for managing peat production. It produces milled peat which is used in power stations. It sells processed peat fuel in the form of peat briquettes which are used for domestic heating. These are oblong bars of densely compressed, dried and shredded peat. Briquettes are largely smokeless when burned in domestic fireplaces and as such are widely used in Irish towns and cities where burning non-smokeless coal is banned. Peat moss is a manufactured product for use in garden cultivation. Turf (dried out peat sods) is very commonly used in rural areas.

In England[link]

The extraction of peat from the Somerset Moors is known to have taken place during Roman times, and has been carried out since the Levels were first drained.^[14] On Dartmoor there were several commercial distillation plants formed and run by the British Patent Naphtha Company in 1844. These produced Naphtha on a commercial scale from the high quality local peat.^[15]

In Finland[link]

The Toppila Power Station, a peat-fired facility in Oulu, Finland.

The climate, geography and environment of Finland favour bog and peat bog formation. Peat is available in considerable quantities: Some estimates put the amount of peat in Finland alone to be twice the size of the North Sea oil reserves.^[16] This abundant resource (often mixed with wood at an average of 2.6%) is burned to produce heat and electricity. Peat provides approximately 6.2% of Finland's annual energy production, second only to Ireland.^[17] The contribution of peat to greenhouse gas emissions of Finland can exceed a yearly amount of 10 million tonnes carbon dioxide, equal to the total emissions of all passenger car traffic in Finland.

Finland classifies peat as a slowly renewing biomass fuel^[18] and that position has also been taken by the European Union. The Intergovernmental Panel on Climate Change has taken the position that peat is not a fossil fuel. Peat producers in Finland often claim that peat is a special form of biofuel, because of the relatively fast retake rate of released CO₂ if the bog is not forested for the following 100 years. Also, agricultural and forestry-drained peat bogs actively release more CO₂ annually than is released in peat energy production in Finland. The average regrowth rate of a single peat bog, however, is indeed slow, from 1,000 up to 5,000 years. Furthermore it is a common practice to forest used peat bogs instead of giving them a chance to renew, leading to lower levels of CO₂ storage than the original peat bog.

At 106 g CO₂/MJ,^[19] the carbon dioxide emissions of peat are higher than those of coal (at 94.6 g CO₂/MJ) and natural gas (at 56.1) (IPCC). According to one study, increasing the average amount of wood in the fuel mixture from the current 2.6% to 12.5% would take the emissions down to 93 g CO₂/MJ, though little effort is made to achieve this.^[20]

Peat extraction is also seen by some conservationists^[who?] as the main threat to mire biodiversity in Finland. The International Mire Conservation Group (IMCG) in 2006 urged the local and national governments of Finland to protect and conserve the remaining pristine peatland ecosystems. This includes the cessation of drainage and peat extraction in intact mire sites and the abandoning of current and planned groundwater extraction that may affect these sites.

In Russia[link]

Shatura Power Station, Russia has the largest peat power capacity in the world

Use of peat for energy production was prominent during the Soviet Union, with the peak occurring in 1965 and declining from that point. In 1929, over 40% of the Soviet Union's electric energy came from peat, which dropped to 1% by 1980.

In the 1960s, larger sections of swamps and bogs in Western Russia were drained for agricultural use and to generate peat fields for mining.^[21] Plans are underway to increase peat output and increase peat's contribution to Russian energy generation.^[22] However, there is concern about the environmental impact as peat fields are flammable, drainage degrades eco-systems, and burning of peat releases carbon dioxide.^[22] Due to 2010 forest and peat fires the Russian government is under heavy pressure to finance re-flooding of the previously drained bogs around Moscow. The initial costs for the programme are estimated to be about 20 to 25 billion rubles, which is close to 500 million euros.

Currently, Russia is responsible for 17% of the world's peat production, and 20% of the peat that it produces, 1.5 million tons, is used for energy purposes.^[23][24] Shatura Power Station in Moscow Oblast and Kirov Power Station in Kirov Oblast are the two largest peat power stations in the world.

Use in agriculture[link]

Peat is important for farmers and gardeners, who mix it into soil to improve its structure and to increase acidity. The most important property of peat is retaining moisture in soil when it is dry and yet preventing the excess of water from killing roots when it is wet. Peat can store nutrients although it is not fertile itself.

Peat is discouraged as a soil amendment by the Royal Botanic Gardens, Kew, England, and has been since 2003.^[25]

Peat is an important raw material in horticulture. However, it is recommended to treat peat thermally, e.g. through soil steaming, in order to kill inherent pest and reactivate nutrients.

Freshwater aquaria[link]

Peat is sometimes used in freshwater aquaria, most commonly in soft water or blackwater river systems, such as those mimicking the Amazon River basin. In addition to being soft in texture and therefore suitable for demersal (bottom-dwelling) species such as Corydoras catfish, peat is reported to have a number of other beneficial functions in freshwater aquaria. It softens water by acting as an ion exchanger; it also contains substances that are beneficial for plants, and for the reproductive health of fishes. It can even prevent algae growth and kill microorganisms. Peat often stains the water yellow or brown due to the leaching of tannins.^[26]

Water filtration[link]

Peat is used in water filtration, such as for the treatment of septic tank effluent, as well as for urban runoff.

Balneotherapy[link]

Peat is widely used in balneotherapy (the use of bathing to treat disease). Many traditional spa treatments include peat as part of peloids. Such health treatments have a very long tradition in Europe, especially in the Czech Republic, Germany and Austria. Some of these old spas go back to the 18th century, and they are still active today. The most common types of peat application in balneotherapy are peat muds, poultices, and suspension baths.^[27]

Environmental and ecological issues[link]

Because of the distinctive ecological conditions of peat wetlands, they provide habitat for a distinctive fauna and flora. For example, Whooping Cranes nest in North American peatlands, while Siberian Cranes nest in the West Siberian peatland. Such habitats also have many species of wild orchids and carnivorus plants. It takes centuries for a peat bog to recover from disturbance. For more on biological communities, see wetland, bog or fen.

Recent studies indicate that the world's largest peat bog, located in Western Siberia and the size of France and Germany combined, is thawing for the first time in 11,000 years. As the permafrost melts, it could release billions of tons of methane gas into the atmosphere.

The world's peatlands are thought to contain 180 to 455 billion metric tons of sequestered carbon, and they release into the atmosphere 20 to 45 million metric tons of methane annually. The peatlands' contribution to long-term fluctuations in these atmospheric gases has been a matter of considerable debate.^[28]

Peat drainage[link]

Large areas of organic wetland (peat) soils are currently drained for agriculture, forestry, and peat extraction. This process is taking place all over the world. This not only destroys the habitat of many species, but also heavily fuels climate change. As a result of peat drainage, the organic carbon that was built up over thousands of years and is normally under water, is suddenly exposed to the air. It decomposes and turns into carbon dioxide (CO₂), which is released into the atmosphere.^[29] The global CO₂ emissions from drained peatlands have increased from 1,058 Mton in 1990 to 1,298 Mton in 2008 (>20%). This increase has particularly taken place in developing countries, of which Indonesia, China, Malaysia, and Papua New Guinea, are the fastest growing top emitters. This estimate excludes emissions from peat fires (conservative estimates amount to at least 4,000 Mton/CO₂-eq./yr for south-east Asia. With 174 Mton/CO₂-eq./yr the EU is after Indonesia (500 Mton) and before Russia (161 Mton) the World's 2nd largest emitter of drainage related peatland CO₂ (excl. extracted peat and fires). Total CO₂ emissions from the worldwide 500,000 km² of degraded peatland may exceed 2.0 Gtons (including emissions from peat fires) which is almost 6% of all global carbon emissions.^[30]

Fires[link]

Smoke and ozone pollution from Indonesian fires, 1997.

Peat has a high carbon content and can burn under low moisture conditions. Once ignited by the presence of a heat source (e.g. a wildfire penetrating the subsurface), it smolders. These smoldering fires can burn undetected for very long periods of time (months, years and even centuries) propagating in a creeping fashion through the underground peat layer. Peat fires are emerging as a global threat with significant economic, social and ecological impacts.^{[citation needed]} Recent burning of peat bogs in Indonesia, with their large and deep growths containing more than 50 billion tons of carbon, has contributed to increases in world carbon dioxide levels.^{[citation needed]} Peat deposits in Southeast Asia could be destroyed by 2040.^[31][32]

It is estimated, that in 1997, peat and forest fires in Indonesia released between 0.81 and 2.57 Gt of carbon; equivalent to 13–40 percent of the amount released by global fossil fuel burning, and greater than the carbon uptake of the world's biosphere. These fires may be responsible for the acceleration in the increase in carbon dioxide levels since 1998.^[33][34] More than 100 peat fires in Kalimantan and East Sumatra have continued to burn since 1997. Each year, the peat fires in Kalimantan and East Sumatra ignite new forest fires above the ground.

In North America, peat fires can occur during severe droughts throughout their occurrence, from boreal forests in Canada to swamps and fens in subtropical southern Florida.^{[citation needed]} Once a fire has burnt through the area, hollows in the peat are burnt out, and hummocks are desiccated but can contribute to Sphagnum recolonization.^[35]

In the summer of 2010, an unusually high heat wave of up to 40 °C (104 °F) ignited large deposits of peat in Central Russia, burning thousands of houses and covering the capital of Moscow with a toxic smoke blanket. The situation remained critical until the end of August 2010.^[36][37]

Wise use and protection[link]

In June 2002, the United Nations Development Programme launched the Wetlands Ecosystem and Tropical Peat Swamp Forest Rehabilitation Project. This project was targeted to last for 5 years until 2007 and brings together the efforts of various non-government organisations.

In November 2002, the International Peat Society and the International Mire Conservation Group (IMCG) published guidelines on the "Wise Use of Mires and Peatlands — Backgrounds and Principles including a framework for decision-making". The aim of this publication is to develop mechanisms that can balance the conflicting demands on the global peatland heritage, to ensure its wise use to meet the needs of humankind.

In June 2008, the International Peat Society published the book Peatlands and Climate Change, summarizing the currently available knowledge on the topic.

See also[link]

• Acid sulfate soil
• Acrotelm
• Histosols
• Irish Peatland Conservation Council
• List of bogs
• Peat-fired power stations
• Tropical peat
• Turbary
• Unified Soil Classification System

References[link]

External links[link]

Wikimedia Commons has media related to: Peat

Look up peat in Wiktionary, the free dictionary.

• Industry - Peat
• Equipment for peat extraction
• International Peat Society
• International Mire Conservation Group
• Gardening without peat information supplied by Kew gardens in London
• Peat-free gardens from the RSPB
• Massive peat burn is speeding climate change From The New Scientist
• Cutover and Cutaway bogs from IPCC
• King Class Torf in Turkey
• Meadowview Biological Research Station

Steve Peat

Steve Peat at Fort William World Cup 2004
Personal information
Full name	Steve Peat
Nickname	Peaty, Sheffield Steel
Born	(1974-06-17) June 17, 1974 (age 38) England  United Kingdom
Height	6'3"
Weight	14 stone
Team information
Current team	Steve Peat Syndicate
Discipline	MTB
Role	Rider
Rider type	DH and 4X
Professional team(s)
1995 Mid 1990s Late 1990s 2002–2005 2006 –	Saracen Team MBUK GT Bikes Orange Bikes Santa Cruz Syndicate
Major wins
GBR DH National Champion (8 Wins) EUR DH European Champion (3 Wins) UCI DH World Cup (17 Wins) UCI DH World Cup Overall (3 Wins) UCI DH World Champion (1 Win)
Medal record Competitor for  United Kingdom Mountain Bike World Championships Silver 2000 Sierra Nevada Downhill Silver 2001 Vail Downhill Silver 2002 Kaprun Downhill Silver 2008 Val Di Sol Downhill
Infobox last updated on 19 May 2009

Steve Peat (born 17 June 1974 in Chapeltown, South Yorkshire), nicknamed "Sheffield Steel" or more commonly just plain "Peaty", is a professional downhill mountain biker who was born and lives in Chapeltown, Sheffield, England. Prior to his career as a professional downhill cyclist Peat was employed as a plumber by James Lamb. He is married to Adele Croxon and has two sons, Jake and George Peat.

Peat began his career with little success riding for the Saracen team alongside Rob Warner, before moving in the mid 90s to Team MBUK. He rode for GT Bicycles in the late 90s and for the Orange team between 2002 and 2005, winning the Fort William downhill world cup round in 2005. He then joined the Santa Cruz Syndicate team for the 2006 season, which saw him finish 1st overall, and has continued with it since.

As last man down the hill, Peat won^[1] the La Bresse downhill world cup round 2 on May 10, 2009 with a time of 02:07.14 knocking Sam Hill out of the hot seat for his 16th world cup round win, tying at the top of the all-time leader-board with Nicolas Vouilloz. Just one week later on May 17, 2009, at the third round of the UCI World Cup in Vallnord, Peat won again^[2] (besting compatriot Gee Atherton by just 0.02 seconds) making him the most successful downhill mountain bike racer ever by number of wins.

Other successes include placing second in the Mountain Bike World Championships in 2000, 2001, 2002 and again in 2008 and becoming World Cup champion in 2002, 2004 and 2006. He has also won the Lisboa Downhill, held in Lisbon, Portugal, eight times. On September 6, 2009, Peat won the World Championships in Canberra for the first time in his career, with a winning time of 2:30.33, just 0.05 seconds ahead of his Santa Cruz team mate Greg Minnaar.

Aside from his professional riding career, Peat has other involvements with the sport, including contributing to the design and manufacture of specialist riding clothing made by Royal Racing of which he is part owner.^[3] Peat also has involvements with young cyclist academies, and is a proponent of youth involvement in the sport.

Following his recent world champ status he has released his own game 'Steve Peat - Downhill Mountain Biking' for the iPhone, iPad and iPod Touch.

Palmarès (Incomplete)[link]

References[link]

External links[link]

• Steve Peat - official site
• Steve Peat profile at Cycling Archives
• Twitter
• TwitPic (photos)

Lil Wayne
Lil Wayne in 2006
Background information
Birth name	Dwayne Michael Carter, Jr.
Born	(1982-09-27) September 27, 1982 (age 29)
Origin	New Orleans, Louisiana, U.S.
Genres	Hip hop
Occupations	Rapper, songwriter
Years active	1992–present
Labels	Cash Money, Young Money,Universal Republic
Associated acts	Birdman, Drake, Cash Money Millionaires, Hot Boys, Young Money, The B.G.'z, Nicki Minaj, Juelz Santana[1]
Website	lilwayne-online.com

Dwayne Michael Carter, Jr. (born September 27, 1982), better known by his stage name Lil Wayne, is an American rapper. At the age of nine, Lil Wayne joined Cash Money Records as the youngest member of the label, and half of the duo, The B.G.'z, with B.G.. In 1997, Lil Wayne joined the group Hot Boys, which also included rappers Juvenile, B.G., and Young Turk. Hot Boys debuted with Get It How U Live! that year. Lil Wayne gained most of his success with the group's major selling album Guerrilla Warfare, released in 1999. Also in 1999, Lil Wayne released his Platinum debut album Tha Block Is Hot, selling over one million copies in the U.S.

Although his next two albums Lights Out (2000) and 500 Degreez (2002) were not as successful (only reaching Gold status), Lil Wayne reached higher popularity in 2004 with Tha Carter, which included the single "Go D.J." Wayne also appeared on the Destiny's Child top ten single "Soldier" that year. In 2005, the sequel to Tha Carter, Tha Carter II, was released. In 2006 and 2007, Lil Wayne released several mixtapes and appeared on several popular rap and R&B singles. His most successful album, Tha Carter III, was released in 2008 and sold over 1 million copies in the U.S. its first week of release. It included the number-one single "Lollipop" featuring Static Major. It also includes the singles "A Milli" and "Got Money" featuring T-Pain and won the Grammy Award for Best Rap Album.

Lil Wayne released his debut rock album, Rebirth, in 2010 to primarily negative reception from critics. The album eventually went gold. In March 2010, Lil Wayne began serving an 8-month prison sentence in New York after being convicted of criminal possession of a weapon stemming from an incident in July 2007. While in prison he released another album entitled I Am Not a Human Being in September 2010, featuring Young Money artists such as Drake, Nicki Minaj and Lil Twist. His ninth studio album and first since being released from prison, Tha Carter IV, was released on August 29, 2011.^[2] The album includes the songs "6 Foot 7 Foot" featuring Cory Gunz, "How to Love" and "She Will" featuring Drake. It sold 964,000 copies in the U.S. its first week out.