GEOL 101 Study Notes
GEOL 101: Sedimentary Rocks and Coal Formation
Types of Sedimentary Rocks
Optimal Characteristics for Specific Rock Roles
Source Rock:
Best type: Organic-rich shales (often black shale).
Rationale: High organic content allows for potential hydrocarbon generation after undergoing fracturing to release organic material.
In rare cases, limestones can preserve sufficient organic material, qualifying as potential source rocks.
Reservoir Rock:
Best types: Rocks with high porosity and/or high permeability.
Porosity: Number of holes (pores) within the rock.
Permeability: Ease of fluid flow through the pores, often enhanced by fractures.
Specific examples:
Sandstones and conglomerates: High primary porosity.
Fractured shale: May exhibit significant permeability and secondary porosity (porosity gained post-formation).
Dissolved limestones: Possessing secondary porosity as well.
Seal Rock:
Best types: Impermeable rocks, such as shales and slates, along with non-fractured crystalline igneous rocks.
Overview of Hydrocarbon Reserves
Key Factors:
Porosity: Indicates storage capacity for hydrocarbons.
Permeability: Determines the ability for hydrocarbons to flow through reservoir rocks.
Seal, Source, and Reservoir Rocks: Essential components in the formation and retention of hydrocarbons.
Coal
Coal Formation and Types (Section 14.6)
Formation Process
Stages of Coal Formation:
Peat: Initial accumulation of plant material.
Lignite: Formed at temperatures of less than during burial.
Bituminous Coal: Formed at temperatures between and during burial.
Anthracite ('hard coal'): Formed at temperatures between and during burial.
Coal Rank
Coal rank categorization based on carbon content:
Low rank: 60-70% carbon.
Intermediate rank: 70-80% carbon.
High rank: Approximately 90% carbon.
Coal Mining Methods
Methods Overview
Coal can be mined using two primary techniques:
Strip Mining:
Involves removing the overburden (surface layer) to expose the coal seam.
Advantages include ease of access and cost-effectiveness.
Process includes:
Use of machinery like draglines (shown in figures) for efficient excavation.
The area is eventually reclaimed after coal extraction.
Underground Mining:
Coal is extracted deep underground without exposure to the surface air (as shown in figures).
Techniques involve tunneling and may utilize sophisticated ventilation systems.
Mineral Resources Overview
Overview and Learning Objectives
Main Focus:
Understand ore formation, particularly in relation to environmental concerns associated with mining practices.
Discuss the interrelationship between renewable energy, rare earth elements (REEs), and non-renewable resources.
Formation of Ore Minerals
Definition of Ores
Ores: Naturally occurring rocks, metals, or minerals that can be economically processed to extract valuable metals.
Formation Processes of Ores
Crystallization in a Melt (Magmatic Deposits):
As magma cools, sulfide minerals crystallize at higher temperatures and accumulate, forming magmatic deposits with concentrated sulfide minerals.
Hydrothermal Activity (Precipitation from Hot Water):
Circulation of hot aqueous solutions, often through magma or surrounding rocks, dissolves metal ions.
As conditions shift (temperature, pressure), metals precipitate out of solution, leading to hydrothermal deposits.
Accumulation in Sediment:
Banded iron formations (BIF):
Resulting from the precipitation of iron oxide minerals as atmospheric oxygen increased between 2.5 billion and 1.8 billion years ago.
Composed of alternate layers of gray iron oxides (magnetite or hematite) and chert (jasper).
Accumulation as Nodules:
In certain marine environments, manganese oxide minerals form lumpy deposits called manganese nodules on the ocean floor.
These nodules are estimated to contain a significant supply of copper and manganese, with ongoing exploration for mining technologies.
Interaction with Groundwater:
Groundwater can alter ore-bearing rocks, dissolving minerals and carrying ions to new locations, resulting in the precipitation of ore minerals in higher concentrations.
Environmental Concerns Related to Mining
Negative Effects of Mining on Environment
Acid Mine Runoff:
Mining can lead to heavy metal concentration in surface waters, resulting in acidification, harmful alterations in pH, affecting aquatic ecosystems.
Acid Rain:
Produced as a byproduct of smelting and refining processes, these gases can lead to environmental damage due to the leaching of soil nutrients and negative effects on water bodies.
Summary of Environmental Concerns
Key issues include:
Landscape degradation
Unequal mineral deposit distribution
Acid mine runoff
Acid rain impacts on soil and ecosystems.
Rare Earth Elements (REEs)
Characteristics and Importance
Nature of REEs:
Rare Earth Elements are not actually 'rare', but their extraction poses significant challenges.
Typically found in low concentrations and rarely exist in pure forms.
Applications of REEs
Common uses in technology and renewable energy:
LEDs, TVs, lasers, batteries, fuel cells, superconductors, magnets, wind turbines, hybrid vehicles, mobile phones, and more.
Overview of REE Production
World Distribution (2019):
Notable outputs by country:
Australia: 21,000 tonnes
China: 132,000 tonnes
United States: 26,000 tonnes
Other countries contribute smaller quantities, e.g., India (3,000), Russia (2,700).
REEs are crucial for renewable technologies yet are finite resources with geographic disparities in mining.
Summary of Mineral Resources Overview
REEs are vital for modern technologies, particularly in renewable energy applications. Despite their label, they are not 'rare', but their availability is limited, presenting challenges for sustainability and resource management.