A report on Petroleum and Fossil fuel

Fractional distillation apparatus.
Since oil fields are located only at certain places on earth, only some countries are oil-independent; the other countries depend on the oil-production capacities of these countries
Oil derrick in Okemah, Oklahoma, 1922.
A petrochemical refinery in Grangemouth, Scotland, UK
Shale bings near Broxburn, 3 of a total of 19 in West Lothian.
An oil well in the Gulf of Mexico
This wartime propaganda poster promoted carpooling as a way to ration vital gasoline during World War II.
The Global Carbon Project shows how additions to since 1880 have been caused by different sources ramping up one after another.
Unconventional resources are much larger than conventional ones.
Global surface temperature reconstruction over the last 2000 years using proxy data from tree rings, corals, and ice cores in blue. Directly observational data is in red, with all data showing a 5 year moving average.
Octane, a hydrocarbon found in petroleum. Lines represent single bonds; black spheres represent carbon; white spheres represent hydrogen.
In 2020, renewables overtook fossil fuels as the European Union's main source of electricity for the first time.
Structure of a vanadium porphyrin compound (left) extracted from petroleum by Alfred E. Treibs, father of organic geochemistry. Treibs noted the close structural similarity of this molecule and chlorophyll a (right).
A hydrocarbon trap consists of a reservoir rock (yellow) where oil (red) can accumulate, and a caprock (green) that prevents it from egressing.
Some marker crudes with their sulfur content (horizontal) and API gravity (vertical) and relative production quantity.
Nominal and inflation-adjusted US dollar price of crude oil, 1861–2015.
Oil consumption per capita (darker colors represent more consumption, gray represents no data) (source: see file description).
Diesel fuel spill on a road.
Seawater acidification.
Global fossil carbon emissions, an indicator of consumption, from 1800. {{legend|black|Total}}{{legend|blue|Oil}}
Rate of world energy usage per year from 1970.<ref name="BP-Report-2012">BP: Statistical Review of World Energy {{webarchive|url=https://web.archive.org/web/20130516003736/http://www.bp.com/sectiongenericarticle800.do?categoryId=9037130&contentId=7068669 |date=May 16, 2013 }}, Workbook (xlsx), London, 2012</ref>
Daily oil consumption from 1980 to 2006.
Oil consumption by percentage of total per region from 1980 to 2006: {{legend|red|US}}{{legend|blue|Europe}}{{legend|#D1D117|Asia and Oceania}}.
Oil consumption 1980 to 2007 by region.

The main fossil fuels are coal, crude oil and natural gas.

- Fossil fuel

A fossil fuel, petroleum is formed when large quantities of dead organisms, mostly zooplankton and algae, are buried underneath sedimentary rock and subjected to both prolonged heat and pressure.

- Petroleum
Fractional distillation apparatus.

10 related topics with Alpha

Overall

Crystal structure of dry ice

Carbon dioxide

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Chemical compound made up of molecules that each have one carbon atom covalently double bonded to two oxygen atoms.

Chemical compound made up of molecules that each have one carbon atom covalently double bonded to two oxygen atoms.

Crystal structure of dry ice
Stretching and bending oscillations of the CO2 carbon dioxide molecule. Upper left: symmetric stretching. Upper right: antisymmetric stretching. Lower line: degenerate pair of bending modes.
Pellets of "dry ice", a common form of solid carbon dioxide
Pressure–temperature phase diagram of carbon dioxide. Note that it is a log-lin chart.
Carbon dioxide bubbles in a soft drink
Dry ice used to preserve grapes after harvest
Use of a CO2 fire extinguisher
Comparison of the pressure–temperature phase diagrams of carbon dioxide (red) and water (blue) as a log-lin chart with phase transitions points at 1 atmosphere
A carbon-dioxide laser
Keeling curve of the atmospheric CO2 concentration
Atmospheric CO2 annual growth rose 300% since the 1960s.
Annual flows from anthropogenic sources (left) into Earth's atmosphere, land, and ocean sinks (right) since the 1960s. Units in equivalent gigatonnes carbon per year.
Pterapod shell dissolved in seawater adjusted to an ocean chemistry projected for the year 2100.
Overview of the Calvin cycle and carbon fixation
Overview of photosynthesis and respiration. Carbon dioxide (at right), together with water, form oxygen and organic compounds (at left) by photosynthesis, which can be respired  to water and (CO2).
Symptoms of carbon dioxide toxicity, by increasing volume percent in air.
Rising levels of CO2 threatened the Apollo 13 astronauts who had to adapt cartridges from the command module to supply the carbon dioxide scrubber in the Lunar Module, which they used as a lifeboat.
CO2 concentration meter using a nondispersive infrared sensor

Burning fossil fuels is the primary cause of these increased CO2 concentrations and also the primary cause of global warming and climate change.

CO2 is eventually sequestered (stored for the long term) in rocks and organic deposits like coal, petroleum and natural gas.

Average surface air temperatures from 2011 to 2021 compared to the 1956–1976 average

Climate change

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Contemporary climate change includes both global warming and its impacts on Earth's weather patterns.

Contemporary climate change includes both global warming and its impacts on Earth's weather patterns.

Average surface air temperatures from 2011 to 2021 compared to the 1956–1976 average
Change in average surface air temperature since the industrial revolution, plus drivers for that change. Human activity has caused increased temperatures, with natural forces adding some variability.
Global surface temperature reconstruction over the last 2000 years using proxy data from tree rings, corals, and ice cores in blue. Directly observed data is in red.
Drivers of climate change from 1850–1900 to 2010–2019. There was no significant contribution from internal variability or solar and volcanic drivers.
concentrations over the last 800,000 years as measured from ice cores (blue/green) and directly (black)
The Global Carbon Project shows how additions to since 1880 have been caused by different sources ramping up one after another.
The rate of global tree cover loss has approximately doubled since 2001, to an annual loss approaching an area the size of Italy.
Sea ice reflects 50% to 70% of incoming solar radiation while the dark ocean surface only reflects 6%, so melting sea ice is a self-reinforcing feedback.
Projected global surface temperature changes relative to 1850–1900, based on CMIP6 multi-model mean changes.
The sixth IPCC Assessment Report projects changes in average soil moisture that can disrupt agriculture and ecosystems. A reduction in soil moisture by one standard deviation means that average soil moisture will approximately match the ninth driest year between 1850 and 1900 at that location.
Historical sea level reconstruction and projections up to 2100 published in 2017 by the U.S. Global Change Research Program
The IPCC Sixth Assessment Report (2021) projects that extreme weather will be progressively more common as the Earth warms.
Scenarios of global greenhouse gas emissions. If all countries achieve their current Paris Agreement pledges, average warming by 2100 would still significantly exceed the maximum 2 °C target set by the Agreement.
Coal, oil, and natural gas remain the primary global energy sources even as renewables have begun rapidly increasing.
Economic sectors with more greenhouse gas contributions have a greater stake in climate change policies.
Most emissions have been absorbed by carbon sinks, including plant growth, soil uptake, and ocean uptake (2020 Global Carbon Budget).
Since 2000, rising emissions in China and the rest of world have surpassed the output of the United States and Europe.
Per person, the United States generates at a far faster rate than other primary regions.
Academic studies of scientific consensus reflect that the level of consensus correlates with expertise in climate science.
Data has been cherry picked from short periods to falsely assert that global temperatures are not rising. Blue trendlines show short periods that mask longer-term warming trends (red trendlines). Blue dots show the so-called global warming hiatus.
The 2017 People's Climate March took place in hundreds of locations. Shown: the Washington, D.C. march, protesting policies of then-U.S. President Trump.
Tyndall's ratio spectrophotometer (drawing from 1861) measured how much infrared radiation was absorbed and emitted by various gases filling its central tube.
alt=Underwater photograph of branching coral that is bleached white|Ecological collapse. Bleaching has damaged the Great Barrier Reef and threatens reefs worldwide.<ref>{{Cite web|url=https://sos.noaa.gov/datasets/coral-reef-risk-outlook/|title=Coral Reef Risk Outlook|access-date=4 April 2020|publisher=National Oceanic and Atmospheric Administration|quote=At present, local human activities, coupled with past thermal stress, threaten an estimated 75 percent of the world's reefs. By 2030, estimates predict more than 90% of the world's reefs will be threatened by local human activities, warming, and acidification, with nearly 60% facing high, very high, or critical threat levels.}}</ref>
alt=Photograph of evening in a valley settlement. The skyline in the hills beyond is lit up red from the fires.|Extreme weather. Drought and high temperatures worsened the 2020 bushfires in Australia.<ref>{{harvnb|Carbon Brief, 7 January|2020}}.</ref>
alt=The green landscape is interrupted by a huge muddy scar where the ground has subsided.|Arctic warming. Permafrost thaws undermine infrastructure and release methane, a greenhouse gas.
alt=An emaciated polar bear stands atop the remains of a melting ice floe.|Habitat destruction. Many arctic animals rely on sea ice, which has been disappearing in a warming Arctic.<ref>{{harvnb|IPCC AR5 WG2 Ch28|2014|p=1596|ps=: "Within 50 to 70 years, loss of hunting habitats may lead to elimination of polar bears from seasonally ice-covered areas, where two-thirds of their world population currently live."}}</ref>
alt=Photograph of a large area of forest. The green trees are interspersed with large patches of damaged or dead trees turning purple-brown and light red.|Pest propagation. Mild winters allow more pine beetles to survive to kill large swaths of forest.<ref>{{Cite web|url=https://www.nps.gov/romo/learn/nature/climatechange.htm|title=What a changing climate means for Rocky Mountain National Park|publisher=National Park Service|access-date=9 April 2020}}</ref>
Environmental migration. Sparser rainfall leads to desertification that harms agriculture and can displace populations. Shown: Telly, Mali (2008).<ref>{{harvnb|Serdeczny|Adams|Baarsch|Coumou|2016}}.</ref>
Agricultural changes. Droughts, rising temperatures, and extreme weather negatively impact agriculture. Shown: Texas, US (2013).<ref>{{harvnb|IPCC SRCCL Ch5|2019|pp=439, 464}}.</ref>
Tidal flooding. Sea-level rise increases flooding in low-lying coastal regions. Shown: Venice, Italy (2004).<ref name="NOAAnuisance">{{cite web|url=http://oceanservice.noaa.gov/facts/nuisance-flooding.html |title=What is nuisance flooding? |author=National Oceanic and Atmospheric Administration |access-date=April 8, 2020}}</ref>
Storm intensification. Bangladesh after Cyclone Sidr (2007) is an example of catastrophic flooding from increased rainfall.<ref>{{harvnb|Kabir|Khan|Ball|Caldwell|2016}}.</ref>
Heat wave intensification. Events like the June 2019 European heat wave are becoming more common.<ref>{{harvnb|Van Oldenborgh|Philip|Kew|Vautard|2019}}.</ref>

Burning fossil fuels for energy production creates most of these emissions.

Human activity since the Industrial Revolution, mainly extracting and burning fossil fuels (coal, oil, and natural gas), has increased the amount of greenhouse gases in the atmosphere, resulting in a radiative imbalance.

Wood was one of the first fuels used by humans.

Fuel

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Any material that can be made to react with other substances so that it releases energy as thermal energy or to be used for work.

Any material that can be made to react with other substances so that it releases energy as thermal energy or to be used for work.

Wood was one of the first fuels used by humans.
Wood as fuel for combustion
Coal is a solid fuel
A gasoline station
Fuel gauge for gasoline on a 50 ccm scooter, with the typical pictogram of a gas pump
A 20-pound (9.1 kg) propane cylinder
Extraction of petroleum
Two CANDU ("CANada Deuterium Uranium") fuel bundles, each about 50cm long and 10cm in diameter
Nuclear fuel pellets are used to release nuclear energy.

Crude oil was distilled by Persian chemists, with clear descriptions given in Arabic handbooks such as those of Muhammad ibn Zakarīya Rāzi.

Most liquid fuels in widespread use are derived from the fossilized remains of dead plants and animals by exposure to heat and pressure inside the Earth's crust.

Diagram describing the ideal combustion cycle by Carnot

Internal combustion engine

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Overhead cam 4-stroke gasoline engine: C – crankshaft

Overhead cam 4-stroke gasoline engine: C – crankshaft

Diagram describing the ideal combustion cycle by Carnot
Reciprocating engine of a car
Diesel generator for backup power
Bare cylinder block of a V8 engine
Piston, piston ring, gudgeon pin and connecting rod
Valve train above a Diesel engine cylinder head. This engine uses rocker arms but no pushrods.
Engine block seen from below. The cylinders, oil spray nozzle and half of the main bearings are clearly visible.
Diagram showing the operation of a 4-stroke SI engine. Labels:
1 ‐ Induction
2 ‐ Compression
3 ‐ Power
4 ‐ Exhaust
Diagram of a crankcase scavenged 2-stroke engine in operation
Diagram of uniflow scavenging
Bosch magneto
Points and coil ignition
Diagram of an engine using pressurized lubrication
P-V diagram for the ideal Diesel cycle. The cycle follows the numbers 1–4 in clockwise direction.
Turbofan jet engine
Turbine power plant
Brayton cycle
The Wankel rotary cycle. The shaft turns three times for each rotation of the rotor around the lobe and once for each orbital revolution around the eccentric shaft.
One-cylinder gasoline engine, c. 1910
Electric starter as used in automobiles

ICEs are typically powered by fossil fuels like natural gas or petroleum products such as gasoline, diesel fuel or fuel oil.

The greenhouse effect of solar radiation on the Earth's surface caused by emission of greenhouse gases.

Greenhouse gas

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Gas that absorbs and emits radiant energy within the thermal infrared range, causing the greenhouse effect.

Gas that absorbs and emits radiant energy within the thermal infrared range, causing the greenhouse effect.

The greenhouse effect of solar radiation on the Earth's surface caused by emission of greenhouse gases.
Radiative forcing (warming influence) of different contributors to climate change through 2019, as reported in the Sixth IPCC assessment report.
Atmospheric absorption and scattering at different wavelengths of electromagnetic waves. The largest absorption band of carbon dioxide is not far from the maximum in the thermal emission from ground, and it partly closes the window of transparency of water; hence its major effect.
Concentrations of carbon monoxide in the Spring and Fall of 2000 in the lower atmosphere showing a range from about 390 parts per billion (dark brown pixels), to 220 parts per billion (red pixels), to 50 parts per billion (blue pixels).
Increasing water vapor in the stratosphere at Boulder, Colorado
Schmidt et al. (2010) analysed how individual components of the atmosphere contribute to the total greenhouse effect. They estimated that water vapor accounts for about 50% of Earth's greenhouse effect, with clouds contributing 25%, carbon dioxide 20%, and the minor greenhouse gases and aerosols accounting for the remaining 5%. In the study, the reference model atmosphere is for 1980 conditions. Image credit: NASA.
The radiative forcing (warming influence) of long-lived atmospheric greenhouse gases has accelerated, almost doubling in 40 years.
Top: Increasing atmospheric carbon dioxide levels as measured in the atmosphere and reflected in ice cores. Bottom: The amount of net carbon increase in the atmosphere, compared to carbon emissions from burning fossil fuel.
400,000 years of ice core data
Recent year-to-year increase of atmospheric.
Major greenhouse gas trends.
The US, China and Russia have cumulatively contributed the greatest amounts of since 1850.

The vast majority of anthropogenic carbon dioxide emissions come from combustion of fossil fuels, principally coal, petroleum (including oil) and natural gas, with additional contributions from cement manufacturing, fertilizer production, deforestation and other changes in land use.

The ring road around Amsterdam (shown in red). Ring roads mark the edge of city centers. At exits of ring roads such as this, distribution centers can be set up.

Stranded asset

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Stranded assets are "assets that have suffered from unanticipated or premature write-downs, devaluations or conversion to liabilities".

Stranded assets are "assets that have suffered from unanticipated or premature write-downs, devaluations or conversion to liabilities".

The ring road around Amsterdam (shown in red). Ring roads mark the edge of city centers. At exits of ring roads such as this, distribution centers can be set up.

Companies extracting fossil fuels (fossil oil, coal) face the threat that, due to their contribution towards global warming, consumers could switch to emissionless alternative fuels instead (i.e. hydrogen, biofuels, ...).

It should be mentioned here that oil companies produce not only fuel (i.e. gasoline, diesel, ...) from crude oil but also produce various fossil oil derivates which are used by the petrochemical industry.

Real development of global photovoltaics additions vs. predictions by the IEA, 2002-2016

International Energy Agency

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Paris-based autonomous intergovernmental organisation established in the framework of the Organisation for Economic Co-operation and Development (OECD) in 1974 in the wake of the 1973 oil crisis.

Paris-based autonomous intergovernmental organisation established in the framework of the Organisation for Economic Co-operation and Development (OECD) in 1974 in the wake of the 1973 oil crisis.

Real development of global photovoltaics additions vs. predictions by the IEA, 2002-2016

The IEA was initially dedicated to responding to physical disruptions in the supply of oil, as well as serving as an information source on statistics about the international oil market and other energy sectors.

In the past, the IEA has been criticized by environmental groups for underplaying the role of renewable energy technologies in favor of nuclear and fossil fuels.

A tar-like substance can be produced from corn stalks by heating them in a microwave. This process is known as pyrolysis.

Tar

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Dark brown or black viscous liquid of hydrocarbons and free carbon, obtained from a wide variety of organic materials through destructive distillation.

Dark brown or black viscous liquid of hydrocarbons and free carbon, obtained from a wide variety of organic materials through destructive distillation.

A tar-like substance can be produced from corn stalks by heating them in a microwave. This process is known as pyrolysis.
Tar kiln at Trollskogen in Öland, Sweden.
Birch tar.
A boat transporting pine tar barrels on Oulu River in 1910.
A New Method of Macarony Making As Practiced at Boston. Date made: 1830 Maker: Pendleton's Lithography; Johnston, David Claypoole Place: Boston, Massachusetts Description: Black and white print; outdoor scene of three men standing in front of a gallows with a broken rope hanging from the gallows. One man is tarred and feathered from the neck down and has the other half of the broken rope around his neck.

Tar can be produced from coal, wood, petroleum, or peat.

Mineral products resembling tar can be produced from fossil hydrocarbons, such as petroleum.

Structure of a vanadium porphyrin compound (left) extracted from petroleum by Alfred E. Treibs, father of organic geochemistry. The close structural similarity of this molecule and chlorophyll a (right) helped establish that petroleum was derived from plants.

Kerogen

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Solid, insoluble organic matter in sedimentary rocks.

Solid, insoluble organic matter in sedimentary rocks.

Structure of a vanadium porphyrin compound (left) extracted from petroleum by Alfred E. Treibs, father of organic geochemistry. The close structural similarity of this molecule and chlorophyll a (right) helped establish that petroleum was derived from plants.

Petroleum and natural gas form from kerogen.

When heated to the right temperatures in the earth's crust, (oil window c. 50–150 °C, gas window c. 150–200 °C, both depending on how quickly the source rock is heated) some types of kerogen release crude oil or natural gas, collectively known as hydrocarbons (fossil fuels).

Anacortes Refinery (Marathon), on the north end of March Point southeast of Anacortes, Washington, United States

Oil refinery

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Anacortes Refinery (Marathon), on the north end of March Point southeast of Anacortes, Washington, United States
A petrochemical refinery in Grangemouth, Scotland
ExxonMobil oil refinery in Baton Rouge, Louisiana (the fourth-largest in the United States)
Refinery, Bayport Industrial Complex, Harris County, Texas
Neste Oil refinery in Porvoo, Finland
The oil refinery in Haifa, Israel, is capable of processing about 9 million tons (66 million barrels) of crude oil a year. Its two cooling towers are landmarks of the city's skyline.
Crude oil is separated into fractions by fractional distillation. The fractions at the top of the fractionating column have lower boiling points than the fractions at the bottom. The heavy bottom fractions are often cracked into lighter, more useful products. All of the fractions are processed further in other refining units.
A breakdown of the products made from a typical barrel of US oil
Storage tanks and towers at Shell Puget Sound Refinery (Shell Oil Company), Anacortes, Washington
Schematic flow diagram of a typical crude oil distillation unit as used in petroleum crude oil refineries
Fire-extinguishing operations after the Texas City Refinery explosion
Refinery of Slovnaft in Bratislava
Oil refinery in Iran
Sample of crude oil (petroleum)
Cylinders of liquified petroleum gas
Sample of gasoline
Sample of kerosene
Sample of diesel fuel
motor oil
Pile of asphalt-covered aggregate for formation into asphalt concrete
Sulphur

An oil refinery or petroleum refinery is an industrial process plant where petroleum (crude oil) is transformed and refined into useful products such as gasoline (petrol), diesel fuel, asphalt base, fuel oils, heating oil, kerosene, liquefied petroleum gas and petroleum naphtha.

Petroleum fossil fuels are burned in internal combustion engines to provide power for ships, automobiles, aircraft engines, lawn mowers, dirt bikes, and other machines.