Chapter 6a Petroleum Origin, Chemistry & Generation Flashcards
1
Q
What are the different theories of the origin of Petroleum?
A
- Inorganic origin
- Organic origin
2
Q
Explain the Inorganic Origin of petroleum.
A
- H and C came together under great P and T and formed O&G where chemical reactions occured
- The O&G then seeped through porous rocks to deposit in various natural underground traps
- It has also excluded the hypothesis that petroleum is a finite substance
- There are some theories that describe the inorganic origin of petroleum:
- Metal Carbide Theory
- Volcanic Theory
- Earthquake Theory
- Serpentinization Theory
- Overwhelming evidences : - geographical location & stability with depth
3
Q
Explain what is the Organic Origin of Petroleum
A
- The O&G are formed from remains of plants and animals.
Remains of plants=coal
Remains of animals=O&G - These remains will settled into the sea and accumulated and buried at the ocean floor.
- The accumulation of the remains will be compressed for million of years.
- The increase in P & T with the absence of Oxygen will change the sediments/mud/sand/silt into rock and organic matter into kerogen
- Kerogen will be transformed into petroleum and natural gas via cracking
- Evidences for Organic Origin of petroleum:
- presence of brine with petroleum
- petroleum is found in association with sedimentary rock
- molecules of HC similar to organic matter
4
Q
What are the 4 Hydrocarbon series? (Refer to notebook for better memorization)
A
- Paraffin
- occur as chain-like structures
- general formula: CnH2n+2
- the carbon number ‘n’ ranges from methane (n=1) to over 40
- C1-C5 = gaseous, C5 above = normally liquid
- high molecular weight paraffins become viscous, waxy solids
- Dry gas = natural gas composed of nearly pure methane
- Wet gas = natural gas that contains other heavier paraffin gasses along with methane - Naphthenes
- Form a closed ring structure
- General formula: CnH2n
- Compound of naphthenes series have chemical & physical properties similar to equivalent paraffins with the same carbon number
- form the major components of most crude oils together with paraffins - Aromatics
- General formula: CnH2n-6
- Have a structure based on a hexagonal ring of carbons with alternate single and double bonds
- Basic unit name is Benzene ring
- Responsible for the strong odor and fluorescence in oils and extract - Resins & Asphaltenes
- composed of fused benzene ring networks but they contain other atoms and are not true HCs
- these impurities include the high molecular weight NSO compounds
- the heaviest components of crude oil and the major components in many natural tars and asphalts
5
Q
Saturated HC vs Unsaturated HC
A
- Saturated HC
-contain only c-c single bonds
-ethane - Unsaturated HC
-contain two or more covalent bonds
-ethene
6
Q
What is the method of classifying crude oil that was proposed by Tissot and Welte (1978) that represents 6 crude oil classes?
A
- Draw triangle by plotting paraffin, napthenes and combination of aromatic HC & NSO compounds
7
Q
What are the 3 main crude oil classes?
A
Most normal crude oils fall within 3 main classes:
- Be rich in paraffins (paraffinic oils)
- Have nearly equal amounts of paraffin and naphthenes - which together make up more than 50% of the crude (parafinitic-naphthenic oil)
- Have subequal amounts of paraffins and naphthenes - which total less than 50% where the composition is dominated by aromatics & the resins and asphaltenes
8
Q
What is Kerogen?
A
- composed of a variety or organic materials, including algae, pollen, wood, vitrinite and structureless material
-the types of kerogen present in a rock largely control the type of HCs generated in that rock
- the H content of kerogen is the controlling factor for oil vs gas yields
9
Q
What are the 4 fundamentally different classes of kerogens?
A
- Type I - Algal
- derived mostly from the remains of algae
- when it matures, it yields mainly crude oil
- capable of generating the most petroleum of all the kerogen types - Type II - Mixed
- consists mostly of amorphous material, derived from the bacterial & mechanical breakdown of a mixture of marine, one celled plants & animals
- this kerogen is oil-prone but yields more natural gas than Type I
- Type I and Type II kerogens are referred to as Sapropelic Kerogens - Type III - Coaly
- derived from the higher land plants, is sometimes known as coaly kerogen
-The humic material in Type III kerogen has a low capacity to form oil and yields mostly natural gas
- Type III kerogen has a low capacity to form oil and yields mostly natural gas - Type IV - Inert
- consists mostly of inert particles that have been highly oxidized before burial, like charcoal.
- It is the rarest kerogen type and has practically no ability to generate either oil or gas.