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PETROLEUM FORMATION
GROUP NO 03
1
 Introduction
 World’s most productive sedimentary basins
 Uses of petroleum
 Origin of petroleum
 Biogenesis
 Transformation of organic matter to hydrocarbon
 Petroleum system
2
OUTLINE
 Petroleum is defined as natural occurring hydrocarbons with some
quantity of S, O, N of containing compound and some metals that
can be recovered from a drill pipe.
 Petroleum or ‘Rock oil,' is a general term for crude oil and natural gas.
 High Sulphur (Poor Quality) – Mostly in Middle East countries
 Less Sulphur (High Quality) – USA, Japan, Europe countries
3
INTRODUCTION
 The term petroleum includes both oil , hydrocarbon gas and oil sand.
 The density of liquid petroleum oil is commonly less than that of water and the oil is
naturally buoyant.
4
Cont’d
 Saudi Arabia
 Kuwait
 Alaska – north slope
 Texas – Louisiana Gulf Coast
 Iraq and Iran
 Mexico
 Venezuela
5
WORLD’S MOST PRODUCTIVE
SEDIMENTARY BASINS
S 01 Constituent of oil uses
1 Petroleum gas in liquid form
(LPG)
Fuel for home and industry
2 Petrol Motor fuel, aviation fuel, solvent for dry
cleaning
3 Kerosene Fuel for stoves, lamps and for jet air crafts
4 Diesel Fuel for heavy motor vehicles, electric
generators
5 Lubricating oil Lubrication
6 Paraffin wax Candles, Vaseline etc.
7 Bitumen Paints, road surfacing
6
USES OF PETROLEUM
Table no 1: various constituents of petroleum and their uses
7
ORIGIN OF PETROLEUM
Cont’d
8
Two theoretical hypothesis on origin and formation of petroleum.
Abiogenesis
Biogenesis
 Abiogenesis
 Oldest theory
 Suggest that petroleum comes from the underneath part of mental very long time
ago before the existence of life on earth.
 Biogenesis
 Currently most acceptable theory
 Suggest that petroleum is formed from biological maters which subjected high
temperature under the absences of oxygen.
9
Cont'd
 Biogenetic origin of petroleum (Hydrocarbons)
 Suggests that petroleum come from a long time decaying of died organisms such as planktons,
zooplankton and other form of biological species
 Under a subjection of high temperature.
 According to that hypothesis, very long time ago, the organisms (marine living things,
terrestrial) died and buried and covered by silt in a sedimentary basin where they undergo a
very slow and very long lasting physical and chemical transformation which involves processes
such as diagenesis and kerogen formation.
10
BIOGENESIS
 These transformations occur in organic matter while buried in the ground, usually as part of
an organic-rich mud rock or marl. The organic-rich rocks are commonly referred to as
"source rocks".
 The three stages represent combinations of temperature, pressure, and time that yield
different types of hydrocarbons;
Diagenesis
Metagenesis
Catagenesis
11
TRANSFORMATION OF ORGANIC MATTER
TO HYDROCARBON
 Diagenesis is a process of compaction under mild conditions of temperature
and pressure.
 When organic aquatic sediments (proteins, lipids, carbohydrates) are
deposited, they are very saturated with water and rich in minerals.
 Through chemical reaction, compaction, and microbial action during burial,
water is forced out and proteins and carbohydrates break down to form new
structures that comprise a waxy material known as “kerogen” and a black
tar like substance called “bitumen”.
 All of this occurs within the first several hundred meters of burial.
12
Step 1: DIAGENESIS FORMS KEROGEN
TYPES OF KEROGEN
13
 Kerogen type I:
Algal (Oil prone) sapropelic
 Kerogen type II:
 Mixed
 Kerogen type III:
 Woody (gas prone) humic
Algae = Hydrogen rich = oil prone
Wood = Hydrogen poor = gas prone
 As temperatures and pressures increase (deeper burial) the process of catagenesis
begins, which is the thermal degradation of kerogen to form hydrocarbon chains.
 The process of catagenesis is catalyzed by the minerals that are deposited and
persist through marine diagenesis.
 The conditions of catagenesis determine the product, such that higher temperature
and pressure lead to more complete “cracking” of the kerogen and progressively
lighter and smaller hydrocarbons.
14
Step 2: CATAGENESIS (OR “CRACKING”) TURNS
KEROGEN INTO PETROLEUM AND NATURAL
GAS
 Petroleum formation, then, requires a specific window of conditions; too hot and the
product will favor natural gas (small hydrocarbons), but too cold and the plankton
will remain trapped as kerogen.
15
Cont'd
16
Cont’d
17
18
Petroleum system
19

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Group 03

  • 2.  Introduction  World’s most productive sedimentary basins  Uses of petroleum  Origin of petroleum  Biogenesis  Transformation of organic matter to hydrocarbon  Petroleum system 2 OUTLINE
  • 3.  Petroleum is defined as natural occurring hydrocarbons with some quantity of S, O, N of containing compound and some metals that can be recovered from a drill pipe.  Petroleum or ‘Rock oil,' is a general term for crude oil and natural gas.  High Sulphur (Poor Quality) – Mostly in Middle East countries  Less Sulphur (High Quality) – USA, Japan, Europe countries 3 INTRODUCTION
  • 4.  The term petroleum includes both oil , hydrocarbon gas and oil sand.  The density of liquid petroleum oil is commonly less than that of water and the oil is naturally buoyant. 4 Cont’d
  • 5.  Saudi Arabia  Kuwait  Alaska – north slope  Texas – Louisiana Gulf Coast  Iraq and Iran  Mexico  Venezuela 5 WORLD’S MOST PRODUCTIVE SEDIMENTARY BASINS
  • 6. S 01 Constituent of oil uses 1 Petroleum gas in liquid form (LPG) Fuel for home and industry 2 Petrol Motor fuel, aviation fuel, solvent for dry cleaning 3 Kerosene Fuel for stoves, lamps and for jet air crafts 4 Diesel Fuel for heavy motor vehicles, electric generators 5 Lubricating oil Lubrication 6 Paraffin wax Candles, Vaseline etc. 7 Bitumen Paints, road surfacing 6 USES OF PETROLEUM Table no 1: various constituents of petroleum and their uses
  • 8. Cont’d 8 Two theoretical hypothesis on origin and formation of petroleum. Abiogenesis Biogenesis
  • 9.  Abiogenesis  Oldest theory  Suggest that petroleum comes from the underneath part of mental very long time ago before the existence of life on earth.  Biogenesis  Currently most acceptable theory  Suggest that petroleum is formed from biological maters which subjected high temperature under the absences of oxygen. 9 Cont'd
  • 10.  Biogenetic origin of petroleum (Hydrocarbons)  Suggests that petroleum come from a long time decaying of died organisms such as planktons, zooplankton and other form of biological species  Under a subjection of high temperature.  According to that hypothesis, very long time ago, the organisms (marine living things, terrestrial) died and buried and covered by silt in a sedimentary basin where they undergo a very slow and very long lasting physical and chemical transformation which involves processes such as diagenesis and kerogen formation. 10 BIOGENESIS
  • 11.  These transformations occur in organic matter while buried in the ground, usually as part of an organic-rich mud rock or marl. The organic-rich rocks are commonly referred to as "source rocks".  The three stages represent combinations of temperature, pressure, and time that yield different types of hydrocarbons; Diagenesis Metagenesis Catagenesis 11 TRANSFORMATION OF ORGANIC MATTER TO HYDROCARBON
  • 12.  Diagenesis is a process of compaction under mild conditions of temperature and pressure.  When organic aquatic sediments (proteins, lipids, carbohydrates) are deposited, they are very saturated with water and rich in minerals.  Through chemical reaction, compaction, and microbial action during burial, water is forced out and proteins and carbohydrates break down to form new structures that comprise a waxy material known as “kerogen” and a black tar like substance called “bitumen”.  All of this occurs within the first several hundred meters of burial. 12 Step 1: DIAGENESIS FORMS KEROGEN
  • 13. TYPES OF KEROGEN 13  Kerogen type I: Algal (Oil prone) sapropelic  Kerogen type II:  Mixed  Kerogen type III:  Woody (gas prone) humic Algae = Hydrogen rich = oil prone Wood = Hydrogen poor = gas prone
  • 14.  As temperatures and pressures increase (deeper burial) the process of catagenesis begins, which is the thermal degradation of kerogen to form hydrocarbon chains.  The process of catagenesis is catalyzed by the minerals that are deposited and persist through marine diagenesis.  The conditions of catagenesis determine the product, such that higher temperature and pressure lead to more complete “cracking” of the kerogen and progressively lighter and smaller hydrocarbons. 14 Step 2: CATAGENESIS (OR “CRACKING”) TURNS KEROGEN INTO PETROLEUM AND NATURAL GAS
  • 15.  Petroleum formation, then, requires a specific window of conditions; too hot and the product will favor natural gas (small hydrocarbons), but too cold and the plankton will remain trapped as kerogen. 15 Cont'd
  • 17. 17
  • 19. 19