Bunker Fuel Oil - Heavy, residual fuel oil used in ships.
yep..
Centigrade - Temperature based on 0 for the temperature at which water freezes and 100 for the temperature at which water boils.
Europeans do not accept this term for Celcius. See that term above. This term is accepted and used in North American chemical texbrooks, so which term you use may depend on your location, but both are abbreviated with a degree symbol and capital C, so at least you now know what it means.
Centipoise - 0.01 poise or centistokes times specific gravity at the test temperature.
Centistoke - 0.01 stoke (see stoke)
Centrifuge - A machine using centrifugal force produced by high-speed rotation for separating materials of different densities.
Applied to Diesel engine fuels and lubricating oils to remove moisture and other extraneous materials.
Cetane Index - An empirical measure of ignition quality. Defined as the percentage by volume of cetane in a mixture of cetane and methyl naphthalene which has the same ignition quality when used in an engine as a fuel under test.
The proportion of hydrocarbons in the mixture is highly variable and ranges from as much as 97% by weight in the lighter oils to as little as 50% in the heavier oils and bitumens.
The hydrocarbons in crude oil are mostly alkanes, cycloalkanes and various aromatic hydrocarbons while the other organic compounds contain nitrogen, oxygen and sulfur, and trace amounts of metals such as iron, nickel, copper and vanadium.
Crude oil varies greatly in appearance depending on its composition. It is usually black or dark brown (although it may be yellowish or even greenish). In the reservoir it is usually found in association with natural gas, which being lighter forms a gas cap over the petroleum, and saline water, which being heavier generally floats underneath it. Crude oil may also be found in semi-solid form mixed with sand, as in the Athabasca oil sands in ..:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />Canada, where it may be referred to as crude bitumen.
Petroleum is used mostly, by volume, for producing fuel oil and gasoline (petrol), both important "primary energy" sources.
84% by volume of the hydrocarbons present in petroleum is converted into energy-rich fuels (petroleum-based fuels), including gasoline, diesel, jet, heating, and other fuel oils, and liquefied petroleum gas.
Due to its high energy density, easy transportability and relative abundance, it has become the world's most important source of energy since the mid-1950s. Petroleum is also the raw material for many chemical products, including pharmaceuticals, solvents, fertilizers, pesticides, and plastics; the 16% not used for energy production is converted into these other materials.
Fuel oil is a fraction obtained from petroleum distillation, either as a distillate or a residue. Broadly speaking, fuel oil is any liquid petroleum product that is burned in a furnace or boiler for the generation of heat or used in an engine for the generation of power, except oils having a flash point of approximately 40 °C (104 °F) and oils burned in cotton or wool-wick burners. In this sense, diesel is a type of fuel oil. Fuel oil is made of long hydrocarbon chains, particularly alkanes, cycloalkanes and aromatics. The term fuel oil is also used in a stricter sense to refer only to the heaviest commercial fuel that can be obtained from crude oil, heavier than gasoline and naphtha.
Petroleum is found in porous rock formations in the upper strata of some areas of the Earth's crust. There is also petroleum in oil sands (tar sands). Known reserves of petroleum are typically estimated at around 140 km³ (1.2 trillion (short scale) barrels) without oil sands, or 440 km³ (3.74 trillion barrels) with oil sands.
Consumption is currently around 84 million barrels (13.4×106 m3) per day, or 3.6 km³ per year. Because the energy return over energy invested (EROEI) ratio of oil is constantly falling as petroleum recovery gets more difficult, recoverable oil reserves are significantly less than total oil-in-place.
However, there are factors which may extend or reduce this estimate, including the rapidly increasing demand for petroleum in China, India, and other developing nations; new discoveries; energy conservation and use of alternative energy sources; and new econonomically viable exploitation of non-conventional oil sources.
Petroleum is a mixture of a very large number of different hydrocarbons ; the most commonly found molecules are alkanes (linear or branched), cycloalkanes, aromatic hydrocarbons, or more complicated chemicals like asphaltenes. Each petroleum variety has a unique mix of molecules, which define its physical and chemical properties, like color and viscosity.
The alkanes, also known as paraffins, are saturated hydrocarbons with straight or branched chains which contain only carbon and hydrogen and have the general formula CnH2n+2 They generally have from 5 to 40 carbon atoms per molecule, although trace amounts of shorter or longer molecules may be present in the mixture.
The alkanes from pentane (C5H12) to octane (C8H18) are refined into gasoline (petrol), the ones from nonane (C9H20) to hexadecane (C16H34) into diesel fuel and kerosene (primary component of many types of jet fuel), and the ones from hexadecane upwards into fuel oil and lubricating oil. At the heavier end of the range, paraffin wax is an alkane with approximately 25 carbon atoms, while asphalt has 35 and up, although these are usually cracked by modern refineries into more valuable products. Any shorter hydrocarbons are considered natural gas or natural gas liquids.
The cycloalkanes, also known as napthenes, are saturated hydrocarbons which have one or more carbon rings to which hydrogen atoms are attached according to the formula CnH2n. Cycloalkanes have similar properties to alkanes but have higher boiling points.
SIGNAL OIL AND GAS
The aromatic hydrocarbons are unsaturated hydrocarbons which have one or more planar six-carbon rings called benzene rings, to which hydrogen atoms are attached with the formula CnHn. They tend to burn with a sooty flame, and many have a sweet aroma. Some are carcinogenic.
These different molecules are separated by fractional distillation at an oil refinery to produce gasoline, jet fuel, kerosene, and other hydrocarbons.
Incomplete combustion of petroleum or gasoline results in production of toxic byproducts. Too little oxygen results in carbon monoxide. Due to high temperatures and high pressures involved exhaust gases from gasoline combustion in car engines usually include nitrogen oxides which are responsible for creation of photochemical smog.
Biogenic theory
Most geologists view crude oil and natural gas as the product of compression and heating of ancient organic materials over geological time. Oil is formed from the preserved remains of prehistoric zooplankton and algae which have been settled to the sea (or lake) bottom in large quantities under anoxic conditions. Terrestrial plants, on the other hand, tend to form coal. Over geological time this organic matter, mixed with mud, is buried under heavy layers of sediment. The resulting high levels of heat and pressure cause the organic matter to chemically change during diagenesis, first into a waxy material known as kerogen which is found in various oil shales around the world, and then with more heat into liquid and gaseous hydrocarbons in a process known as catagenesis.
Geologists often refer to an "oil window" which is the temperature range that oil forms in—below the minimum temperature oil remains trapped in the form of kerogen, and above the maximum temperature the oil is converted to natural gas through the process of thermal cracking. Though this happens at different depths in different locations around the world, a typical depth for the oil window might be 4–6 km. Note that even if oil is formed at extreme depths, it may be trapped at much shallower depths where it was not formed (the Athabasca Oil Sands is one example).
Hydrocarbon trap.Because most hydrocarbons are lighter than rock or water, these often migrate upward through adjacent rock layers until they either reach the surface or become trapped beneath impermeable rocks, within porous rocks called reservoirs. However, the process is not straightforward since it is influenced by underground water flows, and oil may migrate hundreds of kilometres horizontally or even short distances downward before becoming trapped in a reservoir. Concentration of hydrocarbons in a trap forms an oil field from which the liquid can be extracted by drilling and pumping.
Three conditions must be present for oil reservoirs to form: a source rock rich in organic material buried deep enough for subterranean heat to cook it into oil; a porous and permeable reservoir rock for it to accumulate in; and a cap rock (seal) or other mechanism that prevents it from escaping to the surface. Within these reservoirs, fluids will typically organize themselves like a three-layer cake with a layer of water below the oil layer and a layer of gas above it, although the different layers vary in size between reservoirs.
The vast majority of oil that has been produced by the earth has long ago escaped to the surface and been biodegraded by oil-eating bacteria. Oil companies are looking for the small fraction that has been trapped by this rare combination of circumstances. Oil sands are reservoirs of partially biodegraded oil still in the process of escaping, but contain so much migrating oil that, although most of it has escaped, vast amounts are still present—more than can be found in conventional oil reservoirs. On the other hand, oil shales are source rocks that have never been buried deep enough to convert their trapped kerogen into oil.
The reactions that produce oil and natural gas are often modeled as first order breakdown reactions, where kerogen is broken down to oil and natural gas by a set of parallel reactions, and oil eventually breaks down to natural gas by another set of reactions. The first set was originally patented in 1694 under British Crown Patent No. 330 covering, "a way to extract and make great quantityes of pitch, tarr, and oyle out of a sort of stone."
The latter set is regularly used in petrochemical plants and oil refineries.
The idea of abiogenic petroleum origin was championed in the Western world by astronomer Thomas Gold based on thoughts from Russia, mainly on studies of Nikolai Kudryavtsev in the 1800s. Gold's hypothesis was that hydrocarbons of purely inorganic origin exist in the planet Earth. Since most petroleum hydrocarbons are less dense than aqueous pore fluids, Gold proposed that they migrate upward into oil reservoirs through deep fracture networks. Although biomarkers are found in petroleum that most petroleum geologists interpret as indicating biological origin, Gold proposed that Thermophilic, rock-dwelling microbial life-forms are responsible for their presence.
The petroleum industry generally classifies crude oil by the geographic location it is produced in (e.g. West Texas, Brent, or Oman), its API gravity (an oil industry measure of density), and by its sulfur content. Crude oil may be considered light if it has low density or heavy if it has high density; and it may be referred to as sweet if it contains relatively little sulfur or sour if it contains substantial amounts of sulfur.
The geographic location is important because it affects transportation costs to the refinery. Light crude oil is more desirable than heavy oil since it produces a higher yield of gasoline, while sweet oil commands a higher price than sour oil because it has fewer environmental problems and requires less refining to meet sulfur standards imposed on fuels in consuming countries. Each crude oil has unique molecular characteristics which are understood by the use of crude oil assay analysis in petroleum laboratories.
Extraction of petroleum
The most common method of obtaining petroleum is extracting it from oil wells found in oil fields. With improved technologies and higher demand for hydrocarbons various methods are applied in petroleum exploration and development to optimize the recovery of oil and gas (Enhanced Oil Recovery, EOR). Primary recovery methods are used to extract oil that is brought to the surface by underground pressure, and can generally recover about 20% of the oil present.
The natural pressure can come from several different sources; where it is provided by an underlying water layer it is called a water drive reservoir and where it is from the gas cap above it is called gas drive. After the reservoir pressure has depleted to the point that the oil is no longer brought to the surface, secondary recovery methods draw another 5 to 10% of the oil in the well to the surface.
In a water drive oil field, water can be injected into the water layer below the oil, and in a gas drive field it can be injected into the gas cap above to repressurize the reservoir. Finally, when secondary oil recovery methods are no longer viable, tertiary recovery methods reduce the viscosity of the oil in order to bring more to the surface. These may involve the injection of heat, vapor, surfactants, solvents, or miscible gases as in carbon dioxide flooding.
It is also possible to chemically transform methane or coal into the various hydrocarbons found in oil. The best-known such method is the Fischer-Tropsch process. It was a concept pioneered during the 1920s in Germany to extract oil from coal and became central to Nazi Germany's war efforts when imports of petroleum were restricted due to war. It was known as Ersatz (English:"substitute") oil, and accounted for nearly half the total oil used in WWII by Germany. However, the process was used only as a last resort as naturally occurring oil was much cheaper. As crude oil prices increase, the cost of coal to oil conversion becomes comparatively cheaper. The method involves converting high ash coal into synthetic oil in a multi-stage process.
During the oil price increases since 2003, alternatives methods of producing oil gained importance. The most widely known alternatives involve extracting oil from sources such as oil shale or tar sands. These resources exist in large quantities; however, extracting the oil at low cost without excessively harming the environment remains a challenge.
Bunker fuel is technically any type of fuel oil used aboard ships. It gets its name from the containers (known as Bunker Tanks) on ships and in ports that it is stored in, called bunkers. The Australian Customs and the Australian Tax Office defines a bunker fuel as the fuel that powers the engine of a ship or aircraft. Bunker A is No. 2 fuel oil, bunker B is No. 4 or No. 5 and bunker C is No. 6. Since No. 6 is the most common, "bunker fuel" is often used as a synonym for No. 6. No. 5 fuel oil is also called navy special fuel oil or just navy special, No. 6 or 5 are also called furnace fuel oil (FFO); the high viscosity requires heating, usually by a reticulated low pressure steam system, before the oil can be pumped from a bunker tank. In the context of shipping, the labelling of bunkers as previously described is rarely used in modern practice.
JAMES E. VAN BLARICUM - optical indexJAMES E. VAN BLARICUM - VALVE POTSJAMES E. VAN BLARICUM - Exhaust valveJAMES E. VAN BLARICUM - parallel foldJAMES E. VAN BLARICUM - drilling platformJAMES E. VAN BLARICUM - rich gasJAMES E. VAN BLARICUM - permeabilityJAMES E. VAN BLARICUM - formationJAMES E. VAN BLARICUM - pozzolan-lime reactionJAMES E. VAN BLARICUM - kelly spinnerJAMES E. VAN BLARICUM - silicic acidJAMES E. VAN BLARICUM - hammer testJAMES E. VAN BLARICUM - gas condensateJAMES E. VAN BLARICUM - circulating pressureJAMES E. VAN BLARICUM - ARC WELDERJAMES E. VAN BLARICUM - SquJAMES E. VAN BLARICUM - Boyle's Law Single CellJAMES E. VAN BLARICUM - low-yield clayJAMES E. VAN BLARICUM - progressive cavity pumping systemJAMES E. VAN BLARICUM - gal minJAMES E. VAN BLARICUM - HEAT EXCHANGER, FINNED TUBEJAMES E. VAN BLARICUM - Weighting materialJAMES E. VAN BLARICUM - PH (pH)JAMES E. VAN BLARICUM - pit-level recorderPITCHJAMES E. VAN BLARICUM - DEAD WELLJAMES E. VAN BLARICUM - Secondary cementingJAMES E. VAN BLARICUM - acceleratorJAMES E. VAN BLARICUM - Garrett Gas TrainJAMES E. VAN BLARICUM - transgressiveJAMES E. VAN BLARICUM - moving-source methodJAMES E. VAN BLARICUM - transient-pressure testingJAMES E. VAN BLARICUM - nominal filterJAMES E. VAN BLARICUM - ExchangerJAMES E. VAN BLARICUM - BEAM WELLJAMES E. VAN BLARICUM - tail cementJAMES E. VAN BLARICUM - blowing the dripJAMES E. VAN BLARICUM - MBT testJAMES E. VAN BLARICUM - slime-forming bacteriaJAMES E. VAN BLARICUM - Stage separationJAMES E. VAN BLARICUM - observerJAMES E. VAN BLARICUM - LC50JAMES E. VAN BLARICUM - shakerJAMES E. VAN BLARICUM - ppmJAMES E. VAN BLARICUM - upstrokeJAMES E. VAN BLARICUM - workoverJAMES E. VAN BLARICUM - continuous phaseJAMES E. VAN BLARICUM - blank casingJAMES E. VAN BLARICUM - landing depthJAMES E. VAN BLARICUM - kriging weightsJAMES E. VAN BLARICUM - DOUBLESJAMES E. VAN BLARICUM - Side-door elevatorsJAMES E. VAN BLARICUM - Ram blowout preventerJAMES E. VAN BLARICUM - TECTONIC MAPTEGJAMES E. VAN BLARICUM - arrivalJAMES E. VAN BLARICUM - PODJAMES E. VAN BLARICUM - zinc basic carbonateJAMES E. VAN BLARICUM - RaspJAMES E. VAN BLARICUM - petrochemicalJAMES E. VAN BLARICUM - acoustic waveJAMES E. VAN BLARICUM - metric systemJAMES E. VAN BLARICUM - mass balanceJAMES E. VAN BLARICUM - grease-injection systemJAMES E. VAN BLARICUM - formateJAMES E. VAN BLARICUM - time after bitJAMES E. VAN BLARICUM - blooey lineJAMES E. VAN BLARICUM - aggradationJAMES E. VAN BLARICUM - BHAJAMES E. VAN BLARICUM - Rectifier bedJAMES E. VAN BLARICUM - PULLIROD LINEJAMES E. VAN BLARICUM - recordJAMES E. VAN BLARICUM - MILLIDARCYJAMES E. VAN BLARICUM - TMJAMES E. VAN BLARICUM - bridging materialJAMES E. VAN BLARICUM - prospectJAMES E. VAN BLARICUM - HIDE THE THREADSJAMES E. VAN BLARICUM - pneumatic controlJAMES E. VAN BLARICUM - DOODLE BUGJAMES E. VAN BLARICUM - base slurryJAMES E. VAN BLARICUM - casing-potential profileJAMES E. VAN BLARICUM - vertical resolutionJAMES E. VAN BLARICUM - angle-azimuth indicatorJAMES E. VAN BLARICUM - single-phase flowJAMES E. VAN BLARICUM - Production TreeJAMES E. VAN BLARICUM - PARCOMJAMES E. VAN BLARICUM - APIJAMES E. VAN BLARICUM - screenJAMES E. VAN BLARICUM - gone to waterJAMES E. VAN BLARICUM - hook loadJAMES E. VAN BLARICUM - remote sensingJAMES E. VAN BLARICUM - blockageJAMES E. VAN BLARICUM - fire wallJAMES E. VAN BLARICUM - wirelineJAMES E. VAN BLARICUM - MERCAPTANJAMES E. VAN BLARICUM - Wash pipeJAMES E. VAN BLARICUM - SaddleJAMES E. VAN BLARICUM - RiserJAMES E. VAN BLARICUM - appraisalJAMES E. VAN BLARICUM - rig upJAMES E. VAN BLARICUM - residual oilJAMES E. VAN BLARICUM - multiphase fluidJAMES E. VAN BLARICUM - reservoir communicationJAMES E. VAN BLARICUM - bound-fluid logJAMES E. VAN BLARICUM - directivityJAMES E. VAN BLARICUM - Gaussian collocated cosimulationJAMES E. VAN BLARICUM - unloading valveJAMES E. VAN BLARICUM - Section of landJAMES E. VAN BLARICUM - humic acidJAMES E. VAN BLARICUM - Natural gas plantJAMES E. VAN BLARICUM - casing valveJAMES E. VAN BLARICUM - granular LCMJAMES E. VAN BLARICUM - sourceJAMES E. VAN BLARICUM - CMCJAMES E. VAN BLARICUM - POLYMERIZATIONJAMES E. VAN BLARICUM - routine core analysisJAMES E. VAN BLARICUM - hydrocarbon kitchenJAMES E. VAN BLARICUM - AMINE UNITJAMES E. VAN BLARICUM - gridding algorithmJAMES E. VAN BLARICUM - pressure dropJAMES E. VAN BLARICUM - MONKEY BOARDJAMES E. VAN BLARICUM - effective shot densityJAMES E. VAN BLARICUM - pipe dollyJAMES E. VAN BLARICUM - DIEJAMES E. VAN BLARICUM - flagJAMES E. VAN BLARICUM - calcium sulfateJAMES E. VAN BLARICUM - flocculationJAMES E. VAN BLARICUM - high-specific-gravity solidsJAMES E. VAN BLARICUM - pipeline oilJAMES E. VAN BLARICUM - COME-ALOIJAMES E. VAN BLARICUM - positive-displacement meterJAMES E. VAN BLARICUM - bottom-hole choke
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