Oil shale in Belarus is a large, but undeveloped energy resource. [1] While the reserves have been known for decades, they remain unexplored due to the oil shale's high ash and sulphur content, low heat of combustion and high cost of extraction and processing. However, depletion of conventional petroleum and natural gas reserves, as well as high degree of reliance on imported hydrocarbons (from Russia), have recently renewed interest in oil shale exploration in the country.
Belarus is estimated to contain 5–11 billion tonnes of oil shale. [2] [3] [4] Up to 3.6 billion tonnes of recoverable reserves are concentrated within the Pripyat Basin, occupying western Homiel, southern Minsk and eastern Brest voblasts. [5]
Oil shales are found in Podlasie-Brest Depression, Orsha Depression, Belarusian anteclise, Zhlobin Saddle and the Pripyat Basin. [3] The main resource is located in the Pripyat Basin which covers an area of 10,000–20,000 square kilometres (3,900–7,700 sq mi) and contains oil shale of Upper Devonian to Lower Carboniferous age. [2] [3] Within the Pripyat Basin, two potentially exploitable deposits, Lyuban and Turov, have been identified, estimated to contain 0.9 and 2.7 billion tonnes of oil shale in place respectively. [1] [2] However, recoverable reserves of Turov deposit are identified to be 0.33–0.47 billion tonnes. [6] [7] The smaller deposits in the other parts of the country were found to be of negligible economic value. [3]
Belarusian oil shales contain 10–28% of organic matter, their thermal energy of combustion is 4.2–9.5 MJ/kg, while the ash content ranges from 58 to 87%. [8] Due to these properties, Belarusian oil shale cannot be burned directly for power generation; the rock must first undergo the process of pyrolysis, which results in production of shale oil, oil shale gas and other factions that can then be used like the conventionally produced hydrocarbons. Furthermore, a significant depth of seams (64–514 m) excludes the possibility of open-pit mining, adding to the cost of production. For these reasons, fossil fuel extraction in Belarus has been limited to the more easily accessible and cheaply produced conventional oil and gas. Though this was insufficient for the total energy needs of the republic, additional resources were supplied from elsewhere in the Soviet Union.
In 1963, oil shale was discovered in the Pripyat Basin, Minsk and Homiel voblasts. [2] The Pripyat Basin has been extensively studied during the 1970s–1980s, while the smaller deposits in the other parts of the country were found to be of negligible economic value. [3] Unlike nearby Estonia with its large reserves, where extensive oil shale industry was constructed, the Belarusian deposits were deemed inexpedient to develop.
After the Soviet collapse, the newly independent Belarus became highly reliant on imported hydrocarbons from Russia, while the production of domestic oil and gas peaked in the 1970s and has been steadily declining ever since. As of 2010, relations with Russia have deteriorated significantly, largely, due to numerous energy disputes. As a part of its energy security, Belarus has renewed interest in oil shale exploration. In December 2010, Belarus companies Belaruskali, BelorusNeft and Belgorkhimprom established a joint venture for the oil shale development. [9] International tender was announced in March 2011. [10]
One of its main obstacles is the problem of complex utilization of large volumes of waste products. It has been suggested to use the oil shale ash in production of concrete and ceramics, as well as in soil liming. [3] In 2010, the Belarusian government decided on a construction of an oil shale processing plant, though financing of the project remains in question: a Luxembourgian company withdrew from the endeavour, forcing Belarus to start negotiations with the Chinese investors. [6] Belarus also seeks to build cooperation with Estonia, which has one of the most developed oil shale industries in the world. [11]
Oil shale is an organic-rich fine-grained sedimentary rock containing kerogen from which liquid hydrocarbons can be produced. In addition to kerogen, general composition of oil shales constitutes inorganic substance and bitumens. Based on their deposition environment, oil shales are classified as marine, lacustrine and terrestrial oil shales. Oil shales differ from oil-bearing shales, shale deposits that contain petroleum that is sometimes produced from drilled wells. Examples of oil-bearing shales are the Bakken Formation, Pierre Shale, Niobrara Formation, and Eagle Ford Formation. Accordingly, shale oil produced from oil shale should not be confused with tight oil, which is also frequently called shale oil.
A fossil fuel is a hydrocarbon-containing material formed underground from the remains of dead plants and animals that humans extract and burn as fuel. The main fossil fuels are coal, petroleum and natural gas, which humans extract through mining and drilling. Fossil fuels may be burnt to provide heat for use directly, to power engines, or to generate electricity.
Unconventional oil is petroleum produced or extracted using techniques other than the conventional method. Industry and governments across the globe are investing in unconventional oil sources due to the increasing scarcity of conventional oil reserves. Unconventional oil and gas have already made a dent in international energy linkages by reducing US energy import dependency.
Brazil is the largest energy consumer in South America. It is the most important oil and gas producer in the region and the world's largest ethanol fuel producer. The government agencies responsible for energy policy are the Ministry of Mines and Energy (MME), the National Council for Energy Policy (CNPE), the National Agency of Petroleum, Natural Gas and Biofuels (ANP) and the National Agency of Electricity (ANEEL). State-owned companies Petrobras and Eletrobras are the major players in Brazil's energy sector, as well as Latin America's.
Oil shale geology is a branch of geologic sciences which studies the formation and composition of oil shales–fine-grained sedimentary rocks containing significant amounts of kerogen, and belonging to the group of sapropel fuels. Oil shale formation takes place in a number of depositional settings and has considerable compositional variation. Oil shales can be classified by their composition or by their depositional environment. Much of the organic matter in oil shales is of algal origin, but may also include remains of vascular land plants. Three major type of organic matter (macerals) in oil shale are telalginite, lamalginite, and bituminite. Some oil shale deposits also contain metals which include vanadium, zinc, copper, and uranium.
Oil shale reserves refers to oil shale resources that are economically recoverable under current economic conditions and technological abilities. Oil shale deposits range from small presently economically unrecoverable to large potentially recoverable resources. Defining oil shale reserves is difficult, as the chemical composition of different oil shales, as well as their kerogen content and extraction technologies, vary significantly. The economic feasibility of oil shale extraction is highly dependent on the price of conventional oil; if the price of crude oil per barrel is less than the production price per barrel of oil shale, it is uneconomic.
The oil shale industry is an industry of mining and processing of oil shale—a fine-grained sedimentary rock, containing significant amounts of kerogen, from which liquid hydrocarbons can be manufactured. The industry has developed in Brazil, China, Estonia and to some extent in Germany and Russia. Several other countries are currently conducting research on their oil shale reserves and production methods to improve efficiency and recovery. Estonia accounted for about 70% of the world's oil shale production in a study published in 2005.
Shale oil extraction is an industrial process for unconventional oil production. This process converts kerogen in oil shale into shale oil by pyrolysis, hydrogenation, or thermal dissolution. The resultant shale oil is used as fuel oil or upgraded to meet refinery feedstock specifications by adding hydrogen and removing sulfur and nitrogen impurities.
Environmental impact of the oil shale industry includes the consideration of issues such as land use, waste management, and water and air pollution caused by the extraction and processing of oil shale. Surface mining of oil shale deposits causes the usual environmental impacts of open-pit mining. In addition, the combustion and thermal processing generate waste material, which must be disposed of, and harmful atmospheric emissions, including carbon dioxide, a major greenhouse gas. Experimental in-situ conversion processes and carbon capture and storage technologies may reduce some of these concerns in future, but may raise others, such as the pollution of groundwater.
The history of the oil shale industry started in ancient times. The modern industrial use of oil shale for oil extraction dates to the mid-19th century and started growing just before World War I because of the mass production of automobiles and trucks and the supposed shortage of gasoline for transportation needs. Between the World Wars oil shale projects were begun in several countries.
Kukersite is a light-brown marine type oil shale of Ordovician age. It is found in the Baltic Oil Shale Basin in Estonia and North-West Russia. It is of the lowest Upper Ordovician formation, formed some 460 million years ago. It was named after the German name of the Kukruse Manor in the north-east of Estonia by the Russian paleobotanist Mikhail Zalessky in 1917. Some minor kukersite resources occur in sedimentary basins of Michigan, Illinois, Wisconsin, North Dakota, and Oklahoma in North America and in Amadeus and Canning basins Australia.
Energy in Russia describes energy and electricity production, consumption and export from Russia. Energy policy of Russia describes the energy policy in the politics of Russia more in detail. Electricity sector in Russia is the main article of electricity in Russia.
Belarus is a landlocked, generally flat country without natural borders, that occupies an area of 207,600 square kilometers (80,200 sq mi). Its neighbors are Russia to the east and northeast, Latvia to the north, Lithuania to the northwest, Poland to the west, and Ukraine to the south. Its extension from north to south is 560 km (350 mi), from west to east is 650 km (400 mi).
Oil shale in China is an important source of unconventional oil. A total Chinese oil shale resource amounts of 720 billion tonnes, located in 80 deposits of 47 oil shale basins. This is equal to 48 billion tonnes of shale oil. At the same time there are speculations that the actual resource may even exceed the oil shale resource of the United States.
Oil shale in Jordan represents a significant resource. Oil shale deposits in Jordan underlie more than 70% of Jordanian territory. The total resources amounts to 31 billion tonnes of oil shale.
There are two kinds of oil shale in Estonia, both of which are sedimentary rocks laid down during the Ordovician geologic period. Graptolitic argillite is the larger oil shale resource, but, because its organic matter content is relatively low, it is not used industrially. The other is kukersite, which has been mined for more than a hundred years. Kukersite deposits in Estonia account for 1.1% of global oil shale deposits.
The Galoter process is a shale oil extraction technology for a production of shale oil, a type of synthetic crude oil. In this process, the oil shale is decomposed into shale oil, oil shale gas, and spent residue. A decomposition is caused by mixing raw oil shale with a hot oil shale ash, generated by combustion of carbonaceous residue (semi-coke) in the spent residue. The process was developed in 1950s and it is used commercially for the shale oil production in Estonia. There are projects for further development of this technology and for expansion of its usage, e.g. in Jordan and USA.
The Alberta Taciuk process is an above-ground dry thermal retorting technology for extracting oil from oil sands, oil shale and other organics-bearing materials, including oil contaminated soils, sludges and wastes. The technology is named after its inventor William Taciuk and the Alberta Oil Sands Technology and Research Authority.
Oil shale in Serbia is a large, but undeveloped energy resource. Serbia is estimated to have a total resource of 4.81 billion tonnes of oil shale, with up to 3.6 billion tonnes of recoverable reserves, all concentrated within the Aleksinac, Vranje, Senonian Tectonic Trench, Valjevo, Western Morava, Kruševac, Babušnica, Kosanica, Niš and Levač basins, which are all located in the Central - Eastern part of the country. Serbia has around 21 oil shale deposits of various qualities and oil content. The biggest deposits of commercial potential are near Aleksinac and Vina-Zubetin. Serbian oil shale is of sapropel type and sapropel-coaly type.
The Bazhenov Formation or Bazhenov Shale is a geological stratum in the West Siberian basin. It was formed from sediment deposited in a deep-water sea in Tithonian–early Berriasian time. The sea covered more than one million square kilometers in the central basin area. Highly organic-rich siliceous shales were deposited during this time in anoxic conditions on the sea bottom. The sea was connected to the world's oceans and contains trace minerals derived from dissolved minerals and organic materials similar to sapropel sediments in the Black Sea.