This document provides information about fossil fuels, their formation, types, and environmental impacts. It discusses:
- Fossil fuels like coal, oil, and natural gas are formed from the remains of ancient organisms over millions of years.
- Coal forms from partially decayed remains of plants that fell into swamps hundreds of millions of years ago and were subjected to heat and pressure over time.
- There are various types of coal classified by their carbon content and other properties, including lignite, bituminous, and anthracite.
- Coal is a widely used fuel but mining and use have environmental impacts like acid mine drainage, subsidence, and greenhouse gas emissions.
All of the presentations that i have uploaded are made by me for school projects from 9-12 grade.For most of them you actually need to have learned something to recite and what you see on the presentations are just hints.
All of the presentations that i have uploaded are made by me for school projects from 9-12 grade.For most of them you actually need to have learned something to recite and what you see on the presentations are just hints.
this ppt was presented on fossil fuel by Mr.Amanullah Adeel and scholar student originally from Afghanistan at Shivaji University, Kolhapur Maharashtra India. This is focused on energy production and consumption in worldwide and fossil fuels impacts on environment.
THIS PRESENTATION COVERS THE TYPES OF FOSSIL FUELS ALONG WITH SOME INTERESTING FACTS AND DETAILED EXPLANATION ABOUT CALORIFIC VALUES IN FUELS
COVERS ANNA UNIVERSITY FOSSIL FUELS SYLLABUS
Thirteen and a half percent of the atoms in the Earth's crust are hydrogen (most of this hydrogen is in sea water), but because hydrogen is so light, it makes up only 0.75 percent of the Earth's crust by weight. The importance of hydrogen is highlighted in this module.
CHE 102 LECTURE 7 FOSSIL FUELSAn oil refinery or petrole.docxmccormicknadine86
CHE 102: LECTURE 7 FOSSIL FUELS
An oil refinery or petroleum refinery is an industrial plant where crude oil is transformed and refined into more useful products such as gasoline, diesel fuel, jet fuel, naptha, asphalt, heating oil, kerosene, liquefied petroleum gas, and fuel oils.
Oil, coal, natural gas and other fossil fuels are called "fossil" because these fuels are the preserved carbon-hydrogen remnants of ancient life. Coal is formed from plants that decomposed and accumulated in ancient swamps.
EXAMPLES: Fossil Fuels:
Coal: Coal is the primary fuel for the production of electricity and is responsible for about 40% of the electric power supply in the United States.
Oil: Oil is the primary source for the world's transportation.
Natural Gas: About 27% of U.S. energy is fueled by natural gas. Natural gas is the cleanest burning fossil fuel.
CHEMISTRY: fossil fuel combustion.
One molecule of methane, combined with two oxygen molecules, react to form a carbon dioxide molecule, and two water molecules (usually given off as steam or water vapor) releasing energy. See Lecture 3 and figure below.
COAL
Coal is a combustible black or brownish-black sedimentary rock usually occurring in rock strata in layers or veins called coal beds or coal seams. The harder forms, such as anthracite coal, can be regarded as metamorphic rock because of later exposure to elevated temperature and pressure.
NOTE: Geologists classify rocks into three main rock types. Rocks are either a single mineral or a combinations of minerals.
Sedimentary rocks are a type of rock that formed by the accumulation or deposition of small particles (minerals or organic matter) at the Earth’s surface, subsequently followed by their cementation on the floor of oceans or other bodies of water. Examples: sandstone, limestone (see below).
Limestone is a carbonate sedimentary rock that is often composed of the skeletal fragments of marine organisms such as coral, foraminifera, and molluscs. Its major materials are the minerals calcite (CaCO3).
and aragonite,
which are different crystal forms of calcium carbonate (CaCO3).
Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock is subjected to heat and pressure, causing profound physical or chemical changes. The precursor may be a sedimentary, igneous, or existing metamorphic rock. Examples: slate, marble.
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite (see above) or dolomite. In Geology, the term marble refers to metamorphosed limestone. The Taj Mahal in the Indian city of Agra is entirely clad in marble.I was amazed to find that the limestone in the Taj Mahal structure is so transparent, the interior of this architectural masterpiece is “illuminated.”
Igneous rock is formed through the cooling and solidification of lava (or magma) from vo ...
CHE 102 LECTURE 7 FOSSIL FUELSAn oil refinery or petrole.docxbissacr
CHE 102: LECTURE 7 FOSSIL FUELS
An oil refinery or petroleum refinery is an industrial plant where crude oil is transformed and refined into more useful products such as gasoline, diesel fuel, jet fuel, naptha, asphalt, heating oil, kerosene, liquefied petroleum gas, and fuel oils.
Oil, coal, natural gas and other fossil fuels are called "fossil" because these fuels are the preserved carbon-hydrogen remnants of ancient life. Coal is formed from plants that decomposed and accumulated in ancient swamps.
EXAMPLES: Fossil Fuels:
Coal: Coal is the primary fuel for the production of electricity and is responsible for about 40% of the electric power supply in the United States.
Oil: Oil is the primary source for the world's transportation.
Natural Gas: About 27% of U.S. energy is fueled by natural gas. Natural gas is the cleanest burning fossil fuel.
CHEMISTRY: fossil fuel combustion.
One molecule of methane, combined with two oxygen molecules, react to form a carbon dioxide molecule, and two water molecules (usually given off as steam or water vapor) releasing energy. See Lecture 3 and figure below.
COAL
Coal is a combustible black or brownish-black sedimentary rock usually occurring in rock strata in layers or veins called coal beds or coal seams. The harder forms, such as anthracite coal, can be regarded as metamorphic rock because of later exposure to elevated temperature and pressure.
NOTE: Geologists classify rocks into three main rock types. Rocks are either a single mineral or a combinations of minerals.
Sedimentary rocks are a type of rock that formed by the accumulation or deposition of small particles (minerals or organic matter) at the Earth’s surface, subsequently followed by their cementation on the floor of oceans or other bodies of water. Examples: sandstone, limestone (see below).
Limestone is a carbonate sedimentary rock that is often composed of the skeletal fragments of marine organisms such as coral, foraminifera, and molluscs. Its major materials are the minerals calcite (CaCO3).
and aragonite,
which are different crystal forms of calcium carbonate (CaCO3).
Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock is subjected to heat and pressure, causing profound physical or chemical changes. The precursor may be a sedimentary, igneous, or existing metamorphic rock. Examples: slate, marble.
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite (see above) or dolomite. In Geology, the term marble refers to metamorphosed limestone. The Taj Mahal in the Indian city of Agra is entirely clad in marble.I was amazed to find that the limestone in the Taj Mahal structure is so transparent, the interior of this architectural masterpiece is “illuminated.”
Igneous rock is formed through the cooling and solidification of lava (or magma) from vo.
this ppt was presented on fossil fuel by Mr.Amanullah Adeel and scholar student originally from Afghanistan at Shivaji University, Kolhapur Maharashtra India. This is focused on energy production and consumption in worldwide and fossil fuels impacts on environment.
THIS PRESENTATION COVERS THE TYPES OF FOSSIL FUELS ALONG WITH SOME INTERESTING FACTS AND DETAILED EXPLANATION ABOUT CALORIFIC VALUES IN FUELS
COVERS ANNA UNIVERSITY FOSSIL FUELS SYLLABUS
Thirteen and a half percent of the atoms in the Earth's crust are hydrogen (most of this hydrogen is in sea water), but because hydrogen is so light, it makes up only 0.75 percent of the Earth's crust by weight. The importance of hydrogen is highlighted in this module.
CHE 102 LECTURE 7 FOSSIL FUELSAn oil refinery or petrole.docxmccormicknadine86
CHE 102: LECTURE 7 FOSSIL FUELS
An oil refinery or petroleum refinery is an industrial plant where crude oil is transformed and refined into more useful products such as gasoline, diesel fuel, jet fuel, naptha, asphalt, heating oil, kerosene, liquefied petroleum gas, and fuel oils.
Oil, coal, natural gas and other fossil fuels are called "fossil" because these fuels are the preserved carbon-hydrogen remnants of ancient life. Coal is formed from plants that decomposed and accumulated in ancient swamps.
EXAMPLES: Fossil Fuels:
Coal: Coal is the primary fuel for the production of electricity and is responsible for about 40% of the electric power supply in the United States.
Oil: Oil is the primary source for the world's transportation.
Natural Gas: About 27% of U.S. energy is fueled by natural gas. Natural gas is the cleanest burning fossil fuel.
CHEMISTRY: fossil fuel combustion.
One molecule of methane, combined with two oxygen molecules, react to form a carbon dioxide molecule, and two water molecules (usually given off as steam or water vapor) releasing energy. See Lecture 3 and figure below.
COAL
Coal is a combustible black or brownish-black sedimentary rock usually occurring in rock strata in layers or veins called coal beds or coal seams. The harder forms, such as anthracite coal, can be regarded as metamorphic rock because of later exposure to elevated temperature and pressure.
NOTE: Geologists classify rocks into three main rock types. Rocks are either a single mineral or a combinations of minerals.
Sedimentary rocks are a type of rock that formed by the accumulation or deposition of small particles (minerals or organic matter) at the Earth’s surface, subsequently followed by their cementation on the floor of oceans or other bodies of water. Examples: sandstone, limestone (see below).
Limestone is a carbonate sedimentary rock that is often composed of the skeletal fragments of marine organisms such as coral, foraminifera, and molluscs. Its major materials are the minerals calcite (CaCO3).
and aragonite,
which are different crystal forms of calcium carbonate (CaCO3).
Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock is subjected to heat and pressure, causing profound physical or chemical changes. The precursor may be a sedimentary, igneous, or existing metamorphic rock. Examples: slate, marble.
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite (see above) or dolomite. In Geology, the term marble refers to metamorphosed limestone. The Taj Mahal in the Indian city of Agra is entirely clad in marble.I was amazed to find that the limestone in the Taj Mahal structure is so transparent, the interior of this architectural masterpiece is “illuminated.”
Igneous rock is formed through the cooling and solidification of lava (or magma) from vo ...
CHE 102 LECTURE 7 FOSSIL FUELSAn oil refinery or petrole.docxbissacr
CHE 102: LECTURE 7 FOSSIL FUELS
An oil refinery or petroleum refinery is an industrial plant where crude oil is transformed and refined into more useful products such as gasoline, diesel fuel, jet fuel, naptha, asphalt, heating oil, kerosene, liquefied petroleum gas, and fuel oils.
Oil, coal, natural gas and other fossil fuels are called "fossil" because these fuels are the preserved carbon-hydrogen remnants of ancient life. Coal is formed from plants that decomposed and accumulated in ancient swamps.
EXAMPLES: Fossil Fuels:
Coal: Coal is the primary fuel for the production of electricity and is responsible for about 40% of the electric power supply in the United States.
Oil: Oil is the primary source for the world's transportation.
Natural Gas: About 27% of U.S. energy is fueled by natural gas. Natural gas is the cleanest burning fossil fuel.
CHEMISTRY: fossil fuel combustion.
One molecule of methane, combined with two oxygen molecules, react to form a carbon dioxide molecule, and two water molecules (usually given off as steam or water vapor) releasing energy. See Lecture 3 and figure below.
COAL
Coal is a combustible black or brownish-black sedimentary rock usually occurring in rock strata in layers or veins called coal beds or coal seams. The harder forms, such as anthracite coal, can be regarded as metamorphic rock because of later exposure to elevated temperature and pressure.
NOTE: Geologists classify rocks into three main rock types. Rocks are either a single mineral or a combinations of minerals.
Sedimentary rocks are a type of rock that formed by the accumulation or deposition of small particles (minerals or organic matter) at the Earth’s surface, subsequently followed by their cementation on the floor of oceans or other bodies of water. Examples: sandstone, limestone (see below).
Limestone is a carbonate sedimentary rock that is often composed of the skeletal fragments of marine organisms such as coral, foraminifera, and molluscs. Its major materials are the minerals calcite (CaCO3).
and aragonite,
which are different crystal forms of calcium carbonate (CaCO3).
Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock is subjected to heat and pressure, causing profound physical or chemical changes. The precursor may be a sedimentary, igneous, or existing metamorphic rock. Examples: slate, marble.
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite (see above) or dolomite. In Geology, the term marble refers to metamorphosed limestone. The Taj Mahal in the Indian city of Agra is entirely clad in marble.I was amazed to find that the limestone in the Taj Mahal structure is so transparent, the interior of this architectural masterpiece is “illuminated.”
Igneous rock is formed through the cooling and solidification of lava (or magma) from vo.
All of us want an affordable and reliable energy source which we can only get by using coal energy. Although using coal energy is very significant for us and living without it would become impossible, we should always open our minds to the damage the continuous use of coal energy will eventually bring to us and to our environment.
Energy Efficiency in Thermal Utilities
Fuels and Combustion: Introduction to fuels, properties of fuel oil, coal
and gas, storage, handling and preparation of fuels, principles of
combustion, proximate and ultimate analysis, calorific values,
gasification, composition of coal.
Steam System: Properties of steam, assessment of steam distribution
losses, steam leakages, steam trapping, condensate and flash steam
recovery system, identifying opportunities for energy savings.
Insulation and Refractories: Insulation-types and application, economic
thickness of insulation, heat savings and application criteria, Refractory types, selection and application of refractories, heat loss.
Waste Heat Recovery: Classification, advantages and applications,
commercially viable waste heat recovery devices, saving potential.
The various sources of energy can be listed as follows:
1. Fossil Fuels
2. Stored or flowing water (Hydel Energy)
3. Nuclear Fuels (Nuclear Energy)
4. Sun (Solar Energy)
5. Wind (Wind Energy)
6. Rise and fall of tides (Tidal Energy)
7. Geothermal Energy
8. Biomass and bio-fuels
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Earliest Galaxies in the JADES Origins Field: Luminosity Function and Cosmic ...Sérgio Sacani
We characterize the earliest galaxy population in the JADES Origins Field (JOF), the deepest
imaging field observed with JWST. We make use of the ancillary Hubble optical images (5 filters
spanning 0.4−0.9µm) and novel JWST images with 14 filters spanning 0.8−5µm, including 7 mediumband filters, and reaching total exposure times of up to 46 hours per filter. We combine all our data
at > 2.3µm to construct an ultradeep image, reaching as deep as ≈ 31.4 AB mag in the stack and
30.3-31.0 AB mag (5σ, r = 0.1” circular aperture) in individual filters. We measure photometric
redshifts and use robust selection criteria to identify a sample of eight galaxy candidates at redshifts
z = 11.5 − 15. These objects show compact half-light radii of R1/2 ∼ 50 − 200pc, stellar masses of
M⋆ ∼ 107−108M⊙, and star-formation rates of SFR ∼ 0.1−1 M⊙ yr−1
. Our search finds no candidates
at 15 < z < 20, placing upper limits at these redshifts. We develop a forward modeling approach to
infer the properties of the evolving luminosity function without binning in redshift or luminosity that
marginalizes over the photometric redshift uncertainty of our candidate galaxies and incorporates the
impact of non-detections. We find a z = 12 luminosity function in good agreement with prior results,
and that the luminosity function normalization and UV luminosity density decline by a factor of ∼ 2.5
from z = 12 to z = 14. We discuss the possible implications of our results in the context of theoretical
models for evolution of the dark matter halo mass function.
Professional air quality monitoring systems provide immediate, on-site data for analysis, compliance, and decision-making.
Monitor common gases, weather parameters, particulates.
Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Slide 1: Title Slide
Extrachromosomal Inheritance
Slide 2: Introduction to Extrachromosomal Inheritance
Definition: Extrachromosomal inheritance refers to the transmission of genetic material that is not found within the nucleus.
Key Components: Involves genes located in mitochondria, chloroplasts, and plasmids.
Slide 3: Mitochondrial Inheritance
Mitochondria: Organelles responsible for energy production.
Mitochondrial DNA (mtDNA): Circular DNA molecule found in mitochondria.
Inheritance Pattern: Maternally inherited, meaning it is passed from mothers to all their offspring.
Diseases: Examples include Leber’s hereditary optic neuropathy (LHON) and mitochondrial myopathy.
Slide 4: Chloroplast Inheritance
Chloroplasts: Organelles responsible for photosynthesis in plants.
Chloroplast DNA (cpDNA): Circular DNA molecule found in chloroplasts.
Inheritance Pattern: Often maternally inherited in most plants, but can vary in some species.
Examples: Variegation in plants, where leaf color patterns are determined by chloroplast DNA.
Slide 5: Plasmid Inheritance
Plasmids: Small, circular DNA molecules found in bacteria and some eukaryotes.
Features: Can carry antibiotic resistance genes and can be transferred between cells through processes like conjugation.
Significance: Important in biotechnology for gene cloning and genetic engineering.
Slide 6: Mechanisms of Extrachromosomal Inheritance
Non-Mendelian Patterns: Do not follow Mendel’s laws of inheritance.
Cytoplasmic Segregation: During cell division, organelles like mitochondria and chloroplasts are randomly distributed to daughter cells.
Heteroplasmy: Presence of more than one type of organellar genome within a cell, leading to variation in expression.
Slide 7: Examples of Extrachromosomal Inheritance
Four O’clock Plant (Mirabilis jalapa): Shows variegated leaves due to different cpDNA in leaf cells.
Petite Mutants in Yeast: Result from mutations in mitochondrial DNA affecting respiration.
Slide 8: Importance of Extrachromosomal Inheritance
Evolution: Provides insight into the evolution of eukaryotic cells.
Medicine: Understanding mitochondrial inheritance helps in diagnosing and treating mitochondrial diseases.
Agriculture: Chloroplast inheritance can be used in plant breeding and genetic modification.
Slide 9: Recent Research and Advances
Gene Editing: Techniques like CRISPR-Cas9 are being used to edit mitochondrial and chloroplast DNA.
Therapies: Development of mitochondrial replacement therapy (MRT) for preventing mitochondrial diseases.
Slide 10: Conclusion
Summary: Extrachromosomal inheritance involves the transmission of genetic material outside the nucleus and plays a crucial role in genetics, medicine, and biotechnology.
Future Directions: Continued research and technological advancements hold promise for new treatments and applications.
Slide 11: Questions and Discussion
Invite Audience: Open the floor for any questions or further discussion on the topic.
The increased availability of biomedical data, particularly in the public domain, offers the opportunity to better understand human health and to develop effective therapeutics for a wide range of unmet medical needs. However, data scientists remain stymied by the fact that data remain hard to find and to productively reuse because data and their metadata i) are wholly inaccessible, ii) are in non-standard or incompatible representations, iii) do not conform to community standards, and iv) have unclear or highly restricted terms and conditions that preclude legitimate reuse. These limitations require a rethink on data can be made machine and AI-ready - the key motivation behind the FAIR Guiding Principles. Concurrently, while recent efforts have explored the use of deep learning to fuse disparate data into predictive models for a wide range of biomedical applications, these models often fail even when the correct answer is already known, and fail to explain individual predictions in terms that data scientists can appreciate. These limitations suggest that new methods to produce practical artificial intelligence are still needed.
In this talk, I will discuss our work in (1) building an integrative knowledge infrastructure to prepare FAIR and "AI-ready" data and services along with (2) neurosymbolic AI methods to improve the quality of predictions and to generate plausible explanations. Attention is given to standards, platforms, and methods to wrangle knowledge into simple, but effective semantic and latent representations, and to make these available into standards-compliant and discoverable interfaces that can be used in model building, validation, and explanation. Our work, and those of others in the field, creates a baseline for building trustworthy and easy to deploy AI models in biomedicine.
Bio
Dr. Michel Dumontier is the Distinguished Professor of Data Science at Maastricht University, founder and executive director of the Institute of Data Science, and co-founder of the FAIR (Findable, Accessible, Interoperable and Reusable) data principles. His research explores socio-technological approaches for responsible discovery science, which includes collaborative multi-modal knowledge graphs, privacy-preserving distributed data mining, and AI methods for drug discovery and personalized medicine. His work is supported through the Dutch National Research Agenda, the Netherlands Organisation for Scientific Research, Horizon Europe, the European Open Science Cloud, the US National Institutes of Health, and a Marie-Curie Innovative Training Network. He is the editor-in-chief for the journal Data Science and is internationally recognized for his contributions in bioinformatics, biomedical informatics, and semantic technologies including ontologies and linked data.
A brief information about the SCOP protein database used in bioinformatics.
The Structural Classification of Proteins (SCOP) database is a comprehensive and authoritative resource for the structural and evolutionary relationships of proteins. It provides a detailed and curated classification of protein structures, grouping them into families, superfamilies, and folds based on their structural and sequence similarities.
3. Fossil fuels are fuels formed by natural processes
such as anaerobic decomposition of buried dead
organisms, containing energy originating in
ancient photosynthesis.
The age of the organisms and their resulting fossil
fuels is typically millions of years, and sometimes
exceeds 650 million years.
Fossil fuels contain high percentages of carbon and
include petroleum, coal, and natural gas.
3
4. Kerosene, also known as
paraffin, lamp oil and
coal oil (an obsolete
term), is a combustible
hydrocarbon liquid,
derived from petroleum,
widely used as a fuel in
industry and households.
4
5. 5
Partially decayed remains of plants,
animals and microorganisms
300 million years ago
• much of earth’s climate was mild and
warm
– plants grew year round in vast
swamps
• as swamp plants and aquatic
microorganisms died
What are Fossil Fuels
6. 6
fell into or sunk in water,
decomposed very little due to
lack of oxygen
heat and pressure that
accompanied burial of organic
material by sediments
converted decomposed
organic material into carbon-rich
materials we now call fossil fuels
What are Fossil Fuels Contd….
7. 7
Industrial societies need a lot of
energy and, at the moment, rely
on fossil fuels as the main source
of this energy.
Coal, oil and natural gas are
fossil fuels. They are carbon-
based materials that formed over
millions of years from the
remains of ancient plants and
animals.
What are Fossil Fuels Contd….
8. 8
Fossil fuels are so useful because
they contain stored chemical
energy, which is converted into
large amounts of useful heat
energy when the fuels are
burned.
the total amount of fossil fuels
available is limited and so
they are classed as non-
renewable energy resources
Fossil Fuels
9. 9
Formation Fossil Fuels
High Organic Production
Burial of organic material
Reducing conditions – little or no
free oxygen
Reducing conditions preserve
organic matter
Common conditions
13. 13
Coal
Solid fossil fuel formed in several
stages
Land plants that lived 300-400 million
years ago
Subjected to intense heat and pressure
over many millions of years
Mostly carbon, small amounts of sulfur
14. 14
Coal – what do we use it for?
Stages of coal formation
• 300 million year old forests
• peat > lignite > bituminous > anthracite
• Primarily strip-mined
Used mostly for generating electricity
• 62% of the world’s electricity
• 52% of the U.S. electricity
Enough coal for about 200-1000 years
• U.S. has 25% of world’s reserves
High environmental impact
15. 15
How coal was formed
About 350 million years ago,
trees and other plants
photosynthesized and stored
the Sun’s energy.
Dead plants fell into swampy
water and the mud prevented
them from rotting away.
Over the years, the mud piled up and squashed the
plant remains.
After millions of years under this pressure, the mud
became rock and the dead plants became coal.
16. 16
Formation of Coal
The formation of coal from dead plant matter
requires burial, pressure, heat and time
The process works best under anaerobic
conditions (no oxygen) since the reaction with
oxygen during decay destroys the organic
matter
It is the carbon content of the coal that
supplies most of its heating value
The greater the carbon to oxygen ratio the
harder the coal, the more reduced the state of
the carbons and the more potential energy it
contains
18. Formation of Coal
The Formation of Coal Involves Several Steps:
2) Formation of Lignite Coal.
Compaction of the peat due to burial drives
off volatile components like water and
methane, eventually producing a black-
colored, organic-rich coal called lignite .
Burial
1) Formation of Peat.
Swamps are areas where organic matter
from plants accumulate. As the plants die
and get buried they compact to become
peat. With time and more compaction,
almost all of the water is lost and three
different grades of coal result.
Peat
Compactio
n
Lignite Coal Seam
Burial
19. Soft coal which consist of about 85% carbon
and burns readily but produces a lot of
smoke.
Compaction
Bituminous
Formation of Coal
The Formation of Coal Involves Several Steps:
Anthracite coal produces the most energy
when burned.
3) Formation of Bituminous Coal.
Further compaction and heating results in a
more carbon- rich coal called bituminous
coal.
Burial
4) Formation of Anthracite Coal.
If the rock becomes metamorphosed, a high
grade coal called anthracite is produced.
Burial
Metamorphis
m
Hard dark coal which consist of 90% to 95%
carbon and burns very hot and clean. Forms
as a result of metamorphic conditions.
Anthracite
Coal Seam
21. 21
Classification of Coal
The products of coalification are divided into four
major categories based on the carbon content of the
material
Peat Lignite
Bituminous Anthracite
23. 23
Nature of coal formation
exposed during formation to
– higher heat and pressure
» drier (lower water content)
» more compact (harder)
» higher heating value (=higher energy
content)
– lower heat and pressure
» wetter (higher water content)
» less compact (softer)
» lower heating value (=lower energy
content)
25. Fuel Efficiency
As the coals becomes
harder, their carbon
content increases,
and so does the
amount of heat
released
Anthracite produces
twice the energy
(BTUs) of lignite
27. 27
Terminology- Resource and Reserve
Resource : is how much coal is actually in the ground
Reserve: This term refers to coal which is both “demonstrated” (meaning we
know it exists) and is deemed to be economically and technologically
mineable at any time
http://www.groundtruthtre
kking.org/Issues/Alaska
Coal/CoalTerminology.ht
ml
31. Coal Mine
Coal occur in seams or beds
Thickness from inches to more
than 100 ft
Two types of mining e.g.
Strip (60%) and sub-surface
Strip: removed overburden rock and placed aside
Disadvantage of strip mining: erosion, acid mine
drainage, hazardous to surrounding vegetation and
aquatic life
33. Acid Mine Drainage
Sulphur in the exposed coal
combine with oxygen and water
vapor to form sulfuric acid
(H2SO4)
This acidic water is harmful to
vegetation and aquatic life.
34. First Chemical Reaction:
Oxidization of Pyrite
+2
FeS2 + O2 + H2O –> Fe + H2SO4
or (pyrite + dissolved oxygen + water) ->
(ferrous iron + sulfuric acid)
35. Second Chemical Reaction:
Oxidization of Soluble Iron
+2 + +3
Fe + O2 + H –> Fe + H2O
or (ferrous iron + oxygen +hydronium) -> (ferric iron + water)
44. The fuel is burned and the heat
produced is used to boil water. This
creates high-pressure, superheated
steam, which is then used to turn a
turbine.
How do fossil fuels produce electricity?
The turbine turns a generator and
so generates electricity.
Power stations that are fuelled by coal and oil, operate on the
same basic principle.
The cooling towers cool the steam, which condenses as water
and can then be recycled in the power station.
directly to turn the turbine.
Natural-gas-fired power stations do not use steam. The
natural gas is burnt and the hot gases produced are used