The main differences in formation conditions between oil and gas are related to temperature, pressure, and the organic material.
1. Oil Formation:
Oil is typically formed in conditions where moderate temperatures and pressures are present. This occurs about 2,000 to 15,000 feet (600 to 4,500 meters) below the Earth's surface.
The temperature in the oil formation window is generally between 60 and 120 degrees Celsius (140 to 248 degrees Fahrenheit).
At these temperatures, organic material undergoes a process called catagenesis, transforming it into liquid hydrocarbons, which make up crude oil.
2. Gas Formation:
On the other hand, natural gas forms under higher temperatures and pressures than oil.
The gas formation window is typically found at greater depths, around 15,000 to 20,000 feet (4,500 to 6,000 meters).
The temperature in the gas formation window is higher than 120 degrees Celsius (248 degrees Fahrenheit).
Organic material undergoes a more extensive process called pyrolysis, leading to the formation of gaseous hydrocarbons such as methane.
Kerogen Types I-IV: Kerogen refers to the organic matter in sedimentary rocks that can be converted into hydrocarbons. The kerogen type in a source rock influences the hydrocarbons (oil or gas) generated. Kerogen is classified into four types:
Type I Kerogen: This kerogen is rich in algal and lacustrine (lake-derived) organic material. It has a high hydrogen-to-carbon ratio and is more likely to generate oil.
Type II Kerogen: This type is derived from marine plankton and is considered the most prolific source of oil. It has a balanced hydrogen-to-carbon ratio.
Type III Kerogen: This kerogen is derived from terrestrial plants and can generate oil and gas, depending on the thermal conditions during maturation.
Type IV Kerogen: This type is almost inert and does not contribute significantly to the generation of hydrocarbons. It is often found in rocks that have not undergone sufficient thermal maturation.
The main difference between gas and oil formation in the source rock is related to the type of organic matter input. All hydrocarbons (e.g., oil or gas) require similar conditions for transforming organic matter into hydrocarbon. The Kerogen Type I produces oil, Type II produces both oil and gas, and Type III produces only gas. The gases are mainly generated at higher maturities from kerogen Type II than oil.