Petroleum and natural gas are complex, naturally occurring mixtures of hydrocarbons formed over millions of years through the anaerobic decomposition of marine organisms.
The Marine Genesis Process
Unlike coal, which originates primarily from terrestrial vegetation, petroleum and natural gas are derived from the remains of ancient microscopic marine plankton, algae, and bacteria.
- Deposition: Dead marine organic matter settles on the ocean floor and becomes intermixed with inorganic mud and silts, forming organic-rich sedimentary layers.
- Lithification: Successive layers of sediment accumulate above, trapping the organic material in an oxygen-depleted (anaerobic) environment.
- Catagenesis: Under sustained thermal conditions (60°C to 120°C) and lithostatic pressure at depths of 2 to 4 kilometers, the organic matter converts first into kerogen, and then into liquid hydrocarbons (petroleum). This specific temperature range is geologically termed the Oil Window.
- Thermal Cracking: If temperatures exceed 120°C due to deeper burial, the liquid hydrocarbons undergo further thermal cracking, breaking down into lighter gaseous hydrocarbons (natural gas).
Geological Traps and Reservoirs
Hydrocarbons migrate upward from their fine-grained source rocks through porous and permeable carrier beds (such as sandstone or limestone) due to buoyancy. Their migration is halted when they encounter an impermeable rock layer (cap rock, such as shale or salt domes), creating a geological trap. Within these reservoirs, the fluids naturally segregate by density: natural gas occupies the uppermost layer, floating directly above the liquid petroleum, while saline water settles at the base.
Chemical Composition of Petroleum and Natural Gas
Elemental Profile of Crude Petroleum
Crude petroleum is not a single chemical compound but a dark, viscous liquid mixture. Its elemental composition generally falls within narrow parameters:
- Carbon: 83% to 87%
- Hydrogen: 10% to 14%
- Sulfur: 0.05% to 6% (High sulfur defines “sour crude”; low sulfur defines “sweet crude”)
- Nitrogen and Oxygen: 0.1% to 2%
Hydrocarbon Classes in Petroleum
The chemical properties of crude oil are determined by its constituent hydrocarbon families.
- Alkanes (Paraffins): Saturated straight or branched-chain hydrocarbons with the general formula CnH2n+2. They range from gaseous methane (C1) to solid waxes (>C20).
- Cycloalkanes (Naphthenes): Saturated cyclic hydrocarbons with the general formula CnH2n. They constitute a major fraction of mid-boiling petroleum distillates.
- Aromatics: Unsaturated cyclic hydrocarbons containing one or more benzene rings (CnH2n-6). They possess high octane values but are subject to strict environmental regulations due to toxicity.
Compositional Profile of Natural Gas
Natural gas is predominantly a mixture of light gaseous alkanes.
- Methane (CH4): Constitutes 70% to 90% of the total volume.
- Ethane (C2H6), Propane (C3H8), and Butane (C4H10): Constituting 5% to 15%.
- Impurities: Carbon Dioxide (CO2), Hydrogen Sulfide (H2S), Nitrogen (N2), and Helium (He).
Industrial Refining and Fractional Distillation
Crude petroleum must be separated into usable commercial fractions based on the different boiling points of its constituent hydrocarbons. This is achieved through fractional distillation in a fractionating column.
Main Distillation Fractions
| Commercial Fraction | Boiling Point Range (°C) | Carbon Chain Length | Primary Applications |
| Refinery Gases | < 20 | C1 to C4 | Liquefied to form LPG; petrochemical feedstock. |
| Gasoline (Petrol) | 40 – 170 | C5 to C10 | Spark-ignition internal combustion engines. |
| Kerosene (Paraffin Oil) | 170 – 250 | C10 to C16 | Jet turbine fuel; domestic heating and lighting. |
| Diesel Oil (Gas Oil) | 250 – 350 | C15 to C18 | Compression-ignition heavy transport engines. |
| Lubricating Oil & Wax | 350 – 450 | C17 to C20 | Mechanical friction reduction; paraffin wax products. |
| Residual Bitumen | > 450 | > C30 | Road construction; waterproofing industrial coatings. |
Secondary Refining Processes
To match market demand with distillation yields, heavy fractions undergo secondary chemical processing.
- Thermal and Catalytic Cracking: The chemical breaking of long-chain, high-molecular-weight hydrocarbons into smaller, highly demanded light fragments (e.g., converting heavy gas oil into gasoline).
- Catalytic Reforming: The rearrangement of straight-chain alkanes into branched-chain alkanes or aromatic rings using a platinum catalyst. This process elevates the octane rating of the fuel without altering its molecular weight.
Commercial Varieties of Natural Gas
Compressed Natural Gas (CNG)
- Specification: Natural gas compressed to a pressure of 200–250 bars.
- Environmental Status: Used as a clean transport fuel alternative. It emits significantly fewer particulate matter (PM), volatile organic compounds (VOCs), and carbon monoxide emissions than diesel or petrol.
Liquefied Natural Gas (LNG)
- Specification: Natural gas purified and cryogenically cooled to -162°C (-260°F).
- Physical Alteration: Liquefaction reduces the volume by approximately 600 times, rendering long-distance transoceanic transport viable via specialized cryogenic tankers when pipelines are impractical.
Liquefied Petroleum Gas (LPG)
- Specification: A byproduct of petroleum refining and natural gas processing, rather than natural gas itself. It consists of Propane (C3H8) and Butane (C4H10) liquefied under moderate pressure.
- Safety Odorant: Naturally odorless, it is intentionally spiked with Ethyl Mercaptan (C2H5SH) to ensure immediate olfactory detection in the event of a leak.
Key Fact-Sheet for UPSC Prelims
- Strategic Petroleum Reserves (SPR): Underground rock caverns used by nations to store crude oil to mitigate supply disruptions. In India, SPR facilities are managed by the Indian Strategic Petroleum Reserves Limited (ISPRL) at Visakhapatnam, Mangaluru, and Padur.
- Associated vs. Non-Associated Gas: Natural gas found directly dissolved in or capping a crude oil reservoir is termed “associated gas.” If it occurs independently in isolated geological strata without liquid petroleum, it is classified as “non-associated gas.”
- Gas Hydrates (Clathrates): Crystalline solids wherein physical cages of water molecules trap individual methane molecules under conditions of low temperature and high pressure. They are found beneath permafrost regimes and deep ocean sediments.
- Shale Gas: An unconventional natural gas resource locked within fine-grained, low-permeability sedimentary shale formations. Extraction requires advanced hydro-fracturing (“fracking”) and directional horizontal drilling technologies.
