Course Name: Reservoir Rock Properties
Course Code: PTE 3310C
Instructor: Hiwa Sidiq
University: Komar University of Science and Technology
Year: 2009
Syllabus
Overview of energy resources
Geology of oil
Origin of oil, migration, accumulation
Techniques to locate oil
Rock and mineral types, rock cycle, reservoir properties
Composition of the Earth
Understand energy sources and the concept of fossil fuels
Familiarize with essential elements of petroleum reservoirs and geology
Learn about sedimentary basins
Explore theories regarding the origin of petroleum
Grasp the impact of environmental deposition on petroleum generation
Identify different hydrocarbon trap types
Examine reservoir rock properties and their characterization
Change between 2010-2050: Transition in resource usage including renewables, petroleum, natural gas, coal, and nuclear energy
Comparison between OECD and non-OECD countries regarding energy usage trends over time.
Projections for renewable electricity generation from 2010 to 2050 with variations in oil and gas supply and renewable costs.
A dynamic hydrocarbon system functioning in a confined geological space over time.
Involves mature source rocks and the process of hydrocarbon expulsion.
Approximately 70% of the world's oil originated during the Mesozoic era characterized by a tropical climate with reduced oxygen levels.
Vitrinite reflection values, important for assessing the maturity level of source rocks, are used in hydrocarbon studies.
Type I: Oil-prone (Abundant, Lacustrine environments)
Type II: Oil and gas-prone (Moderate, Marine environments)
Type III: Gas-prone (Terrestrial environments)
Type IV: Non-hydrocarbon producing (Inert material)
Petroleum formation is dependent on depth and temperature with specific zones identified for oil and gas formation.
Organic-rich shales from Late Cretaceous to Early Jurassic
Conditions for the 'oil window': 60-120°C with depths of 2000-4500m.
Understanding the spatial arrangement of source, reservoir, and seal rocks within a petroleum system.
Geological processes occur in a consistent manner over time.
Rock layers are deposited horizontally.
Older layers are situated below younger ones in sedimentary sequences.
Younger geological features cut across older ones.
Disconformity: Parallel beds above and below the gap
Angular Unconformity: Older beds are inclined relative to younger beds
Nonconformity: Younger sedimentary rocks overlie older metamorphic or igneous rocks.
Igneous: Formed from cooling magma
Sedimentary: Compaction of sediments
Metamorphic: Altered by heat, pressure.
Earth's Crust Composition:
Metamorphic: 27.4%
Igneous: 64.7%
Sedimentary: 7.9%
Key Factors Affecting Fluid Flow:
Porosity
Permeability
Capillary pressure
Compressibility
Fluid saturation
Porosity measures the void space in a material, calculated as a fraction of the void volume to total volume.
Grain size, shape, sorting, and cementation during deposition.
Primary Porosity: Original pore spaces present at formation
Secondary Porosity: Developed through geological processes after deposition.
The notes cover fundamental principles of petroleum geology focusing on reservoir rock properties, geological time, energy sources, and oil formation processes. Understanding these concepts is essential for effective exploration and management of petroleum resources.