Oil shale reserves

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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.

Contents

As source rocks for most conventional oil reservoirs, oil shale deposits are found in all world oil provinces, although most of them are too deep to be exploited economically. [1] There are more than 600 known oil shale deposits around the world. [2] [3] Although resources of oil shale occur in many countries, only 33 countries possess known deposits of possible economic value. [2] [4] [5]

Many deposits need more exploration to determine their potential as reserves. Well-explored deposits, which could ultimately be classified as reserves, include the Green River deposits in the western United States, the Tertiary deposits in Queensland, Australia, deposits in Sweden and Estonia, the El-Lajjun deposit in Jordan, and deposits in France, Germany, Brazil, China, and Russia. It is expected that these deposits would yield at least 40 liters (0.25 bbl) of shale oil per metric ton of shale, using the Fischer Assay. [6] [7]

A 2016 conservative estimate set the total world resources of oil shale equivalent to yield of 6.05 trillion barrels (962 billion cubic metres) of shale oil, with the largest resource deposits in the United States accounting for more than 80% of the world total resource. [2] For comparison, at the same time the world's proven oil reserves are estimated to be 1.6976 trillion barrels (269.90 billion cubic metres). [8]

Oil shale geology

Oil shale formation takes place in a number of depositional settings and has considerable compositional variation. Oil shales can be classified by their composition (carbonate minerals such as calcite or detrital minerals such as quartz and clays) or by their depositional environment (large lakes, shallow marine, and lagoon/small lake settings). Much of the organic matter in oil shale 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. [9] Some oil-shale deposits also contain metals which include vanadium, zinc, copper, and uranium. [10] [7]

Most oil shale deposits were formed during Middle Cambrian, Early and Middle Ordovician, Late Devonian, Late Jurassic, and Paleogene times through burial by sedimentary loading on top of the algal swamp deposits, resulting in conversion of the organic matter to kerogen by diagenetic processes. [10] [11] The largest deposits are found in the remains of large lakes such as the deposits of the Green River Formation of Wyoming and Utah, USA. Oil-shale deposits formed in the shallow seas of continental shelves generally are much thinner than large lake basin deposits. [12]

Definition of reserves

Estimating shale oil reserves is complicated by several factors. Firstly, the amount of kerogen contained in oil shale deposits varies considerably. Secondly, some nations report as reserves the total amount of kerogen in place, including all kerogen regardless of technical or economic constraints; these estimates do not consider the amount of kerogen that may be extracted from identified and assayed oil shale rock using available technology and under given economic conditions. By most definitions, "reserves" refers only to the amount of resource which is technically exploitable and economically feasible under current economic conditions. The term "resources", on the other hand, may refer to all deposits containing kerogen. Thirdly, shale oil extraction technologies are still developing, so the amount of recoverable kerogen can only be estimated. [3] [13]

There are a wide variety of extraction methods, which yield significantly different quantities of useful oil. As a result, the estimated amounts of resources and reserves display wide variance. The kerogen content of oil shale formations differs widely, and the economic feasibility of its extraction is highly dependent on international and local costs of oil. Several methods are used to determine the quantity and quality of the products extracted from shale oil. At their best, these methods give an approximate value to its energy potential. One standard method is the Fischer Assay, which yields a heating value, that is, a measure of caloric output. This is generally considered a good overall measure of usefulness. The Fischer Assay has been modified, standardized, and adapted by the American Petroleum Institute. It does not, however, indicate how much oil could be extracted from the sample. Some processing methods yield considerably more useful product than the Fischer Assay would indicate. The Tosco II method yields over 100% more oil, and the Hytort process yields between 300% and 400% more oil. [7]

Size of the resource

The size of the oil shale resources is highly dependent on which grade cut-off is used. [14] A 2008 estimate set the total world resources of oil shale at 689 gigatones—equivalent to yield of 4.8 trillion barrels (760 billion cubic metres) of shale oil, with the largest reserves in the United States, which is thought to have 3.7 trillion barrels (590 billion cubic metres), though only a part of it is recoverable. [15] According to the 2010 World Energy Outlook by the International Energy Agency, the world oil shale resources may be equivalent of more than 5 trillion barrels (790 billion cubic metres) of oil in place of which more than 1 trillion barrels (160 billion cubic metres) may be technically recoverable. [1]

A 2016 conservative estimate by the World Energy Council set the total world resources of oil shale equivalent to yield of 6.05 trillion barrels (962 billion cubic metres). [2] For comparison, at the same time the world's proven oil reserves are estimated to be 1.6976 trillion barrels (269.90 billion cubic metres). [8]

Geographical allocation

There is no comprehensive overview of oil shale geographical allocation around the world. Around 600 known oil shale deposits are diversely spread throughout the earth, and are found on every continent with the possible exception of Antarctica, which has not yet been explored for oil shale. [3] [10] Oil shale resources can be concentrated in a large confined deposit such as the Green River formations, which were formed by a large inland lake. These can be many meters thick but limited by the size of the original lake. They may also resemble the deposits found along the eastern American seaboard, which were the product of a shallow sea, in that they may be quite thin but laterally expansive, covering thousands of square kilometers.

Largest oil shale deposits (over 1 billion metric tons) (Dyni 2006) [7]
DepositCountryPeriodIn-place shale oil resources (million barrels)In-place oil shale resources (million metric tons)
Green River Formation United States Paleogene 1,466,000213,000
Phosphoria Formation United States Permian 250,00035,775
Eastern DevonianUnited States Devonian 189,00027,000
Heath FormationUnited States Early Carboniferous 180,00025,578
Olenyok BasinRussia Cambrian 167,71524,000
CongoDemocratic Republic of Congo?100,00014,310
Irati Formation Brazil Permian 80,00011,448
SicilyItaly?63,0009,015
Tarfaya Morocco Cretaceous 42,1456,448
Volga BasinRussia?31,4474,500
Leningrad deposit, Baltic Oil Shale Basin Russia Ordovician 25,1573,600
Vychegodsk BasinRussia Jurassic 19,5802,800
Wadi MagharJordan Cretaceous 14,0092,149
Graptolitic argillite Estonia Ordovician 12,3861,900
Timahdit Morocco Cretaceous 11,2361,719
Collingwood ShaleCanada Ordovician 12,3001,717
ItalyItaly Triassic 10,0001,431

The table below reports reserves by estimated amount of shale oil. Shale oil refers to synthetic oil obtained by heating organic material (kerogen) contained in oil shale to a temperature which will separate it into oil, combustible gas, and the residual carbon that remains in the spent shale. All figures are presented in barrels and metric tons.

Shale oil: resources and production at end-2008 by regions and countries with resources over 10 billion barrels of in-place shale oil (Dyni 2010) [15]
RegionIn-place shale oil resources (million barrels)In-place oil shale resources (million metric tons)Production in 2008 (thousand metric tons (oil))
Africa159,24323,317-
Democratic Republic of the Congo100,00014,310-
Morocco53,3818,167-
Asia613,14583,836375
China354,43047,600375
Pakistan91,00012,236-
Russia167,71524,000-
Europe368,15652,845355
Russia247,88335,470-
Italy73,00010,446-
Estonia16,2862,494355
Middle East38,1725,792-
Jordan34,1725,242-
North America3,722,066539,123-
United States3,706,228536,931-
Canada15,2412,192-
Oceania31,7484,534-
Australia31,7294,531-
South America82,42111,794157
Brazil82,00011,734159
World total4,786,131689,227930

Africa

Major oil shale deposits are located in the Democratic Republic of Congo (equal to 14.31 billion metric tons of shale oil) and Morocco (12.3 billion metric tons or 8.16 billion metric tons of shale oil). Deposits in Congo are not properly explored yet. [7] In Morocco, oil shale deposits have been identified at ten localities with the largest deposits in Tarfaya and Timahdite. Although reserves in Tarfaya and Timahdit are well explored, the commercial exploitation has not started yet and only a limited program of laboratory and pilot-plant research has been undertaken. [16] There are also oil shale reserves in Egypt, South Africa, Madagascar, and Nigeria. The main deposits of Egypt are located in Safaga-Al-Qusayr and Abu Tartour areas. [7]

Asia

Major oil shale deposits are located in China, which has an estimated total of 32 billion metric tons, of which 4.4 billion metric tons are technically exploitable and economically feasible. [7] [5] In 2008, the amount of potential shale oil was estimated at 354 billion barrels (5.63×1010 cubic metres) and in 2016 at 330 billion barrels (5.2×1010 cubic metres). [15] [14] The principal Chinese oil shale deposits and production lie in Fushun and Liaoning; others are located in Maoming in Guangdong, Huadian in Jilin, Heilongjiang, and Shandong. [5] Professor Alan R. Carroll of University of Wisconsin–Madison estimates that Upper Permian lacustrine oil shale deposits of northwest China, absent from previous global oil shale assessments, are comparable to the Green River Formation. [17]

In addition to China, major deposits are located in Thailand (18.7 billion metric tons), Pakistan (227 billion metric tons, of which 9.1 billion metric tons are technically exploitable and economically feasible), Kazakhstan (several deposits; major deposit at Kenderlyk Field with 4 billion metric tons), and Turkey (2.2 billion metric tons). [6] [7] Thailand's oil shale deposits are near Mae Sot, Tak Province, and at Li, Lamphun Province. [18] Deposits in Turkey are found mainly in middle and western Anatolia. [7] According to some reports, also Uzbekistan has major oil shale deposits of 47 billion metric tons, mainly located at Sangruntau but also at Baysun, Jam, Urtabulak, Aktau, Uchkyr and Kulbeshkak. [19] Smaller oil shale reserves have also been found in India, Turkmenistan, Myanmar, Armenia, and Mongolia.

Europe

Outcrop of Ordovician kukersite oil shale, northern Estonia OilShaleEstonia.jpg
Outcrop of Ordovician kukersite oil shale, northern Estonia

The biggest oil shale reserves in Europe are located in Russia (equal to 35.47 billion metric tons of shale oil). Major deposits are located in the Volga-Petchyorsk province and in the Baltic Oil Shale Basin. Other major oil shale deposits in Europe are located in Italy (10.45 billion metric tons of shale oil), Estonia (2.49 billion metric tons of shale oil), France (1 billion metric tons of shale oil), Belarus (1 billion metric tons of shale oil), Sweden (875 million metric tons of shale oil), Ukraine (600 million metric tons of shale oil) and the United Kingdom (500 million metric tons of shale oil). There are oil shale reserves also in Germany, Luxembourg, Spain, Bulgaria, Hungary, Poland, Serbia, Austria, Albania, and Romania. [7] [15]

Middle East

Significant oil shale deposits are located in Israel (equal to about 250 billion barrels (4.0×1010 cubic metres) of shale oil) and in Jordan (equal to about 102 billion barrels (1.62×1010 cubic metres) of shale oil). [14] In 2008, these resources were estimated 4 billion barrels (640,000,000 cubic metres) of shale oil and 34.172 billion barrels (5.4329×109 cubic metres) of shale oil correspondingly. [15] Jordan oil shales are high quality, comparable to western US oil shale, although their sulfur content is high. The best-explored deposits are El Lajjun, Sultani, and the Juref ed Darawish are located in west-central Jordan, while the Yarmouk deposit, close to its northern border, extends into Syria. [7] [20] Most of Israel's deposits are located in the Rotem Basin region of the northern Negev desert near the Dead Sea. Israeli oil shale is relatively low in heating value and oil yield. [7] [21]

North America

Oil shale from the Mahogany Zone of the Green River Formation, Colorado. Weathered surface on right; fresh surface on left. Colorado Oil Shale.jpg
Oil shale from the Mahogany Zone of the Green River Formation, Colorado. Weathered surface on right; fresh surface on left.

At 301 billion metric tons, as estimated in 2005, the oil shale deposits in the United States are the largest in the world. There are two major deposits: the eastern US deposits, in Devonian-Mississippian shales, cover 250,000 square miles (650,000 km2); the western US deposits of the Green River Formation in Colorado, Wyoming, and Utah, are among the richest oil shale deposits in the world. [7]

More recent studies by the United States Geological Survey estimate that the resource in the United States may be bigger than previously estimated. According to these studies, three largest oil-shale deposits — all are part of the Green River Formation — are the Piceance Basin with 1.525157 trillion barrels (2.424806×1011 cubic metres), [22] the Greater Green River Basin with 1.444992 trillion barrels (2.297354×1011 cubic metres), [23] and the Uinta Basin with 1.318964 trillion barrels (2.096985×1011 cubic metres) in-place shale oil resources. [24] In 2010, it was estimated by the World Energy Council that the United States resource could be equal to 3.7 trillion barrels (590 billion cubic metres) of shale oil. [15] In 2016, their estimation was that the resource may even consist of up to 6 trillion barrels (950 billion cubic metres) of shale oil. [14]

In Canada 19 deposits have been identified. The best-examined deposits are in Nova Scotia and New Brunswick. [25]

Oceania

In 2008, Australia's oil shale resource was estimated at 4.531 billion metric tons of oil shale equal to 31.7 billion barrels (5.04×109 cubic metres) of shale oil, of which about 24 billion barrels (3.8 billion cubic metres) is recoverable. [15] The deposits are located in the eastern and southern states with the biggest potential in the eastern Queensland deposits. [7] Oil shale has also been found in New Zealand. [15]

South America

Brazil has at least nine oil shale deposits in São Mateus do Sul, Paraná, and in Vale do Paraíba. In 2008, the total oil shale resource was 11.734 billion metric tonnes, equal to 80–82 billion barrels (1.27×1010–1.30×1010 cubic metres) of shale oil. [15] Small resources are also found in Argentina, Chile, Paraguay, Peru, Uruguay, and Venezuela. [15] [26]

See also

Related Research Articles

<span class="mw-page-title-main">Oil shale</span> Organic-rich fine-grained sedimentary rock containing kerogen

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.

Shale oil is an unconventional oil produced from oil shale rock fragments by pyrolysis, hydrogenation, or thermal dissolution. These processes convert the organic matter within the rock (kerogen) into synthetic oil and gas. The resulting oil can be used immediately as a fuel or upgraded to meet refinery feedstock specifications by adding hydrogen and removing impurities such as sulfur and nitrogen. The refined products can be used for the same purposes as those derived from crude oil.

<span class="mw-page-title-main">Western Canadian Sedimentary Basin</span> Sedimentary basin of Canada

The Western Canadian Sedimentary Basin (WCSB) underlies 1.4 million square kilometres (540,000 sq mi) of Western Canada including southwestern Manitoba, southern Saskatchewan, Alberta, northeastern British Columbia and the southwest corner of the Northwest Territories. This vast sedimentary basin consists of a massive wedge of sedimentary rock extending from the Rocky Mountains in the west to the Canadian Shield in the east. This wedge is about 6 kilometres (3.7 mi) thick under the Rocky Mountains, but thins to zero at its eastern margins. The WCSB contains one of the world's largest reserves of petroleum and natural gas and supplies much of the North American market, producing more than 450 million cubic metres per day of gas in 2000. It also has huge reserves of coal. Of the provinces and territories within the WCSB, Alberta has most of the oil and gas reserves and almost all of the oil sands.

<span class="mw-page-title-main">Oil shale geology</span> Branch of geology

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.

<span class="mw-page-title-main">Piceance Basin</span>

The Piceance Basin is a geologic structural basin in northwestern Colorado, in the United States. It includes geologic formations from Cambrian to Holocene in age, but the thickest section is made up of rocks from the Cretaceous Period. The basin contains reserves of coal, natural gas, and oil shale. The name likely derives from the Shoshoni word /piasonittsi/ meaning “tall grass”.

<span class="mw-page-title-main">Kukersite</span> Light-brown marine type oil shale of Ordovician age

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 the Amadeus and Canning basins of Australia.

<span class="mw-page-title-main">Bakken Formation</span> Geological rock formation known for crude oil and gas production

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<span class="mw-page-title-main">Bend Arch–Fort Worth Basin</span> Major petroleum producing region in Texas and Oklahoma

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<span class="mw-page-title-main">Natural gas in Iran</span> Overview of proven natural gas reserves in Iran

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As of 2017, Azerbaijan produced a range of metals and industrial minerals, including aluminum, bentonite, copper, gold, iodine, limestone, silver and steel.

<span class="mw-page-title-main">Oil reserves in the United States</span> Oil reserves located in the United States

Within the petroleum industry, proven crude oil reserves in the United States was 44.4 billion barrels (7.06×109 m3) of crude oil as of the end of 2021, excluding the Strategic Petroleum Reserve.

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.

<span class="mw-page-title-main">Shale gas in the United States</span>

Shale gas in the United States is an available source of unconventional natural gas. Led by new applications of hydraulic fracturing technology and horizontal drilling, development of new sources of shale gas has offset declines in production from conventional gas reservoirs, and has led to major increases in reserves of U.S. natural gas. Largely due to shale gas discoveries, estimated reserves of natural gas in the United States in 2008 were 35% higher than in 2006.

<span class="mw-page-title-main">New Albany Shale</span>

The New Albany Shale is an organic-rich geologic formation of Devonian and Mississippian age in the Illinois Basin of the United States. It is a major source of hydrocarbons.

Oil shale in Morocco represents a significant potential resource. The ten known oil shale deposits in Morocco contain over 53.381 billion barrels of shale oil. Although Moroccan oil shale has been studied since the 1930s and several pilot plants have extracted shale oil from the local formations, commercial extraction was not underway as of 2011.

<span class="mw-page-title-main">Oil shale in Israel</span> Overview of the industry in Israel

Oil shale in Israel is widespread but an undeveloped resource, largely because of economic and technological constraints. Israeli oil shales belong to the group of Upper Cretaceous marinite deposits. Although oil-shale deposits may lie under as much as 15% of the country, only a small part of these are mineable. According to the Geological Survey of Israel, deposits that could have the biggest economic potential are located in the northern Negev, the largest being the Rotem-Yamin formation. For several decades, oil shale was used for small-scale power generation at Mishor Rotem. Several Israeli companies have proposed shale oil extraction; testing of the viability of the oil shale industry is currently being undertaken by Israel Energy Initiatives. However, as of 2011, there are no commercial oil shale operations in Israel.

There are oil shale deposits in Australia which range from small deposits to large reserves. Deposits, varying by their age and origin, are located in about a third of eastern Australia. In 2012, the demonstrated oil shale reserves were estimated at 58 billion tonnes. The easiest to recover deposits are located in Queensland.

<span class="mw-page-title-main">Bazhenov Formation</span> Oil-bearing rock formation in Russia

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.

As of 2013 the Cline Shale, also referred to as the "Wolfcamp/Cline Shale", the "Lower Wolfcamp Shale", or the "Spraberry-Wolfcamp shale", or even the "Wolfberry", is a promising Pennsylvanian oil play east of Midland, Texas which underlies ten counties: Fisher, Nolan, Sterling, Coke, Glasscock, Tom Green, Howard, Mitchell, Borden and Scurry counties. Exploitation is projected to rely on hydraulic fracturing.

an organic rich shale, with Total Organic Content (TOC) of 1-8%, with silt and sand beds mixed in. It lies in a broad shelf, with minimal relief and has nice light oil of 38-42 gravity with excellent porosity of 6-12% in thickness varying 200 to 550 feet thick.

The Timahdit oil shale deposit is an oil shale deposit located about 240 kilometres (150 mi) southeast of Rabat near Timahdite, Fès-Meknès, Morocco. It is the second largest oil-shale deposit in Morocco. Geologically, it comprises two basins: El koubbat and Angueur synclines. The oil shale formation is about 70 kilometres (43 mi) long and 4 to 10 kilometres wide. The volume of the El koubbat syncline formation is about 250 square kilometres (97 sq mi); the Angueur syncline area is about 100 square kilometres (39 sq mi).

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  26. Russell, Paul L. (1990). Oil shales of the world, their origin, occurrence and exploitation (First ed.). Pergamon Press. pp. 162–224. ISBN   0-08-037240-6.

Bibliography