The document discusses energy density, specific energy, CO2 emissions, and global warming. It provides definitions for energy density as the energy produced per unit volume and specific energy as the energy produced per unit mass. Renewable energy sources can be replenished faster than they are used, while non-renewables are used faster than they can be replaced. Strategies to reduce CO2 emissions include improving energy efficiency, reducing dependence on carbon fuels, and using renewable energy and carbon capture/storage technologies.
Equilibrium and types of equilibrium,Physical Equilibrium ,Chemical Equilibrium ,Law of Mass Action,The Equilibrium Constant (K),Relationship between Kc and Kp
I Hope You all like it very much. I wish it is beneficial for all of you and you can get enough knowledge from it. Clear and appropriate objectives, in terms of what the audience ought to feel, think, and do as a result of seeing the presentation. Objectives are realistic – and may be intermediate parts of a wider plan.
Equilibrium and types of equilibrium,Physical Equilibrium ,Chemical Equilibrium ,Law of Mass Action,The Equilibrium Constant (K),Relationship between Kc and Kp
I Hope You all like it very much. I wish it is beneficial for all of you and you can get enough knowledge from it. Clear and appropriate objectives, in terms of what the audience ought to feel, think, and do as a result of seeing the presentation. Objectives are realistic – and may be intermediate parts of a wider plan.
Co2 emission rate per MWh of energy generated from coal fired plantsDavid Palmer, EIT
It has been proven that carbon dioxide emissions (greenhouse gases GHGs) absorb energy, slowing or preventing the loss of heat to space. In this way, GHGs act like a blanket, making Earth warmer than it would otherwise be. This process is commonly known as the “greenhouse effect”. How much GHGs are actually emitted from Ontario plants.
Module 7 - Energy Balance chemical process calculationsbalaaguywithagang1
Chemical process calculations involve various computations and analyses to design, optimize, and understand chemical processes. Here are some descriptions highlighting different aspects of chemical process calculations:
Material Balances:
Material balances are the cornerstone of chemical process calculations, ensuring that the amounts of all components entering and leaving a system are properly accounted for.
These calculations involve tracking the flow rates and compositions of substances throughout a process, often using mass or mole balances.
Energy Balances:
Energy balances involve quantifying the energy inputs and outputs in a chemical process.
These calculations are crucial for understanding the heat transfer requirements, evaluating energy efficiency, and optimizing process conditions.
Reaction Kinetics:
Chemical reactions kinetics calculations focus on understanding the rates at which reactions occur and how they are influenced by various factors such as temperature, pressure, and catalysts.
These calculations help in determining the optimal reaction conditions and designing reactors for desired conversion rates.
Phase Equilibrium Calculations:
Phase equilibrium calculations deal with determining the distribution of components between different phases in a system, such as liquid-liquid or vapor-liquid equilibrium.
These calculations are essential for designing separation processes like distillation, extraction, and absorption.
Thermodynamic Calculations:
Thermodynamic calculations involve applying thermodynamic principles to predict the behavior of chemical systems.
These calculations include determining properties such as enthalpy, entropy, Gibbs free energy, and fugacity, which are crucial for process design and optimization.
Process Simulation:
Process simulation involves using computer software to model and simulate chemical processes.
These simulations allow engineers to predict process behavior under different operating conditions, optimize process parameters, and troubleshoot potential issues.
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In coal fired power plants coal is a main fuel for combustion purpose. Before use of coal different tests are to be carried out to analysis the constituent elements and some undesirable contamination in the coal. Discuss the analysis procedures of the coal.
The analysis of coal is as follows C=82%, H=6%,O2=4% and remaining is ash. Determine the amount of theoretical air required for complete combustion. If the actual air supplied is 40% in excess and 80% of given carbon is burnt to CO2 and remaining is CO. Conduct the volumetric analysis of dry products of combustion.
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Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
A Strategic Approach: GenAI in EducationPeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
Biological screening of herbal drugs: Introduction and Need for
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2. Energy density = energy produced per unit vol
consumedvolume
releasedenergy
densityEnergy
.
.
. = consumedmass
releasedenergy
energySpecific
.
.
. =%100
.
.
×=
inputtotal
outputuseful
Efficiency
Specific energy = energy produced per unit mass
Renewable
↓
Replenished at rate faster than it is used
Energy
Energy efficiency
Non renewable
↓
Used faster than they can be replaced
Renewable Non renewable
solar
hydro
geothermal
biomass
wind
nuclear
coal
gasoline
gas
Carbon footprint.
Strategies to reduce CO2 emission
Increase energy
efficiency/conservation
Reduce dependency on carbon based
Alternate source of energy (renewable)
Capture and storage from fossil fuel
CO2 sequestration, reduce deforestration
Total amt greenhouse gas
produced during human activity
Expressed in CO2 equivalent.
3. Find specific energy/energy density of hexane.
(density hexane = 0.6548g cm-1
)
∆H combustion hexane , ∆Hc = - 4163kJ mol-1
Formula C6H14 Mr = 86.2 g mol -1
86.2 g release - 4163 kJ
1 g release – 4163/86.2 = 48.3 kJ
3
6.131
6548.0
2.86
cm
Density
Mass
Vol
Vol
Mass
Density
===
=
consumedmass
releasedenergy
energySpecific
.
.
. =
consumedvolume
releasedenergy
densityEnergy
.
.
. =
Energy density
↓
Specific Energy x Density
48.3 x 0.6548 = 31.6 kJcm-1
131.6 cm3
release - 4163 kJ
1 cm3
release – 4163/131.6
= 31.6 kJ cm-3
Power station generate power, 550 x 106
Js-1
.
Overall efficiency of 36% for conversion of heat to electricity
Find energy generated (output) in 1 year
Find energy needed (input) for energy generation
Find mass coal used, assuming coal has ∆H of graphite
Total energy output
550 x 106
x 60 x60x 24 x 365 = 1.73 x 1016
J
1 year
kJinputTotal
inputtotal
inputtotal
outputuseful
Efficiency
13
16
1082.4.
%100
.
1073.1
%36
%100
.
.
×=
×
×
=
×= ∆H comb graphite, ∆Hc = - 394kJ mol-1
M carbon Mr = 12 g mol -1
394 kJ released by – 1 mol C
4.82 x 1013
kJ released by – 1.22 x 1011
mol C
1 mol C – 12 g
1.22 x 1011
mol C – 1.47 x 1012
g of C
4. % mass carbon in coal – Highest
CO2 emission highest when combusted
kJinputTotal
inputtotal
inputtotal
outputuseful
Efficiency
7
7
1071.4.
%100
.
1000.4
%85
%100
.
.
×=
×
×
=
×=
4.00 x 107
kJ energy required to heat a home.
Methane combustion for heat is 85% efficient
∆H comb methane, ∆Hc = - 891 kJ mol-1
Formula CH4 Mr = 16 g mol -1
0.0221 x 106
cm3
release - 891 kJ
1 cm3
release – 891/0.0221 x 106
= 40126 kJ cm-3
Find mass methane required.
Find specific energy and energy density for CH4
∆H comb CH4 ∆Hc = - 891 kJ mol-1
Mr CH4 Mr = 16 g mol -1
(density CH4 = 723 x 10-6
g cm-1
)
consumedmass
releasedenergy
energySpecific
.
.
. = consumedvolume
releasedenergy
densityEnergy
.
.
. =
16 g release - 891 kJ
1 g release – 891/16 = 55.5 kJ
Energy density
↓
Specific Energy x Density
55.5 x 723 x 10-6
= 40126 kJcm-1 36
6
100221.0
10723
16
cmVol
Density
Mass
Vol
Vol
Mass
Density
×=
×
==
=
−
Find % mass carbon in coal (CH), gasoline (C8H18), gas (CH4)
Suggest why coal is a poor choice for fuel
% mass carbon in coal (CH)
%92%100
13
12
%100
.
.
=×=
×=
masstotal
carbonmass
% mass carbon gasoline (C8H18)
%84%100
114
96
%100
.
.
=×=
×=
masstotal
carbonmass
% mass carbon methane (CH4)
%75%100
16
12
%100
.
.
=×=
×=
masstotal
carbonmass
5. Coal burned to produce 500 x 103
kJ , has specific energy of 33 kJ g-1
Find mass coal burned, if efficiency is 38%.
MF for coal is CH. Find mass CO2 produced
kJinputTotal
inputtotal
inputtotal
outputuseful
Efficiency
6
3
1031.1.
%100
.
10500
%38
%100
.
.
×=
×
×
=
×=
33 kJ released by – 1 g coal
1.31 x 106
kJ released by – 39900 g coal
↓
Mol coal – 39 900/14 = 3062 mol
CH + 1.25O2 CO→ 2 + 0.5H2O
1 mol CH – 1 mol CO2
3062 mol CH – 3062 mol CO2
Mass CO2 – mol x RMM
Mass CO2 – 3062 x 44 = 135000g CO2
Fuel Specific
energy/kJ g-1
Carbon content
by mass/%
Coal 32 94
Oil 42 83
hydrogen 142 0
Find CO2 produced for each 1000kJ energy from each source
Identify best and worse fuel used.
32 kJ released by – 1 g coal
1000 kJ released by – 31.3 g coal
↓
% C by mass = 0.94 x 31.3 = 29.4 g C
C + O2 → CO2
1 mol C – 1 mol CO2
12 g C – 44g CO2
29.4 g C – (44 x 29.4)/12 = 108g CO2
42 kJ released by – 1 g oil
1000 kJ released by – 23.8 g oil
↓
% C by mass = 0.83 x 23.8 = 19.7 g C
C + O2 → CO2
1 mol C – 1 mol CO2
12 g C – 44g CO2
19.7 g C – (44 x 19.7)/12 = 72g CO2
142 kJ released by – 1 g H2
1000 kJ released by – 7 g H2
↓
% C by mass = 0
ZERO Emission CO2
Click here Carbon calculator
6. Energy density
↓
Specific Energy x Density
Fuel Formula ∆H
combustion/kJ/mol-1
Ethanol C2H5OH -1367
Coal C - 394
C2H5OH + 3O2 → 2CO2 + 3H2O
1 mol ethanol – 2 mol CO2
2.2 mol ethanol – 4.4 mol CO2
Which release more CO2 ?
Ethanol fuel
Mass CO2 – mol x RMM
Mass CO2 – 4.4 x 44 = 193g CO2
Coal fuel
C + O2 → CO2
1 mol C - 1 mol CO2
8.3 mol C – 8.3 mol CO2
Mass CO2 – mol x RMM
Mass CO2 – 8.3 x 44 = 366 g CO2
Find specific energy/energy density of ethanol and pure coal.
(density ethanol/coal = 0.789 gcm-1
/ 2267kg m-3
)
Find carbon footprint in mass CO2 produced when 100g ethanol/coal burn
consumedmass
releasedenergy
energySpecific
.
.
. =
46 g release - 1367 kJ
1 g release – 1367/46 = 29.7 kJ
Energy density
↓
Specific Energy x Density
29.7 x 0.789 = 23.4 kJcm-1
consumedmass
releasedenergy
energySpecific
.
.
. =
12 g release - 394 kJ
1 g release – 394/12 = 32.8 kJ
32.8 x 2267 = 74.3 kJcm-1
Mass ethanol, 100g – 100/46
= 2.2 mol
Mass coal, 100g – 100/12
= 8.3 mol
7. 1.33 x 106
kJ energy (output) required to heat a home.
Find % mass carbon in two fuels
Find carbon footprint in terms of mass CO2 produced
Fuel Formula Specific
energy/kJ g-1
Efficiency /
%
Coal CH 31 65
Oil C5H9O4 22 70
% mass of carbon in Coal (CH)
%2.92%100
112
12
%.
.
.
%.
=×
+
=
=
carbon
masstotal
carbonmass
carbon
% mass of carbon in oil (C5H9O4)
%45%100
)64()9()60(
125
%.
.
.
%.
=×
++
×
=
=
carbon
masstotal
carbonmass
carbon
31 kJ released by – 1 g coal
2.05 x 106
kJ released by – 66000 g coal
↓
% C by mass = 0.922 x 66000 = 60 800g C
kJInput
inputtotal
input
output
Efficiency
6
6
1005.2
%100
.
1033.1
%65
%100
×=
×
×
=
×=
C + O2 → CO2
1 mol C – 1 mol CO2
12 g C – 44g CO2
60 800 g C – (44 x 60 800)/12 = 223000 g CO2
kJInput
inputtotal
input
output
Efficiency
6
6
109.1
%100
.
1033.1
%70
%100
×=
×
×
=
×=
22 kJ released by – 1 g oil
1.9 x 106
kJ released by – 86 400 g oil
↓
% C by mass = 0.45 x 86 400 = 38 900g C
C + O2 → CO2
1 mol C – 1 mol CO2
12 g C – 44g CO2
38 900 g C – (44 x 38 900)/12 = 142000 g CO2
Which release more CO2 ?
8. 10 000 kJ energy (output) required to heat a home.
Find carbon footprint in terms of mass CO2 produced
Fuel Formula ∆H
combustion/kJ/mol-1
Ethanol C2H5OH -1367
Methylbenzene C7H8 -3910
1367 kJ released by – 1 mol ethanol
10 000 kJ released by – 7.31 mol ethanol
C2H5OH + 3O2 → 2CO2 + 3H2O
1 mol ethanol – 2 mol CO2
7.31 mol ethanol – 14.6 mol CO2
Which release more CO2 ?
Ethanol fuel
Mass CO2 – mol x RMM
Mass CO2 – 14.6 x 44 = 643 g CO2
Methylbenzene fuel
3910 kJ released by – 1 mol C7H8
10 000 kJ released by – 2.56 mol C7H8
C7H8 + 9O2 → 7CO2 + 4H2O
1 mol C7H8 - 7 mol CO2
2.56 mol C7H8 – 17.9 mol CO2
Mass CO2 – mol x RMM
Mass CO2 – 17.9 x 44 = 789 g CO2
9. GHG allow short wavelength radiation to pass through
but absorb longer wavelength, IR radiation from earth.
Some radiation is re radiated back to earth
Greenhouse Effect
Re radiated
long wavelength Re radiated
long wavelength
Greenhouse Gases (GHG)
Gas Greenhouse
factor/GWP
Relative
abundance/%
Overall
contribution
Carbon dioxide CO2 1 0.036 50
Water (H2O) 0.1 0.1 -
Methane(CH4) 30 0.0017 18
Dinitrogen oxide (N2O) 280 0.0003 6
Hydrofluorocarbon (HFC) 400-10000 - -
CFC 11000 - -
Perfluorocarbon (PFC) 9000 - -
Sulphur hexafluoride (SF6) 16000 - -
Global Warming Potential
Global Warming Potential (GWP)
Compare ability of gas to absorb IR radiation
to CO2 absorbing ability (as a std)
Water – main/abundant greenhouse gas
– produced naturally
– Contribution not significant
10. Molecule CO2 absorb IR
• Vibration within molecule cause a net change in dipole moment
• Freq of radiation matches vibrational natural freq of molecule
radiation will be absorbed, causing a change in amplitude of molecular vibration.
• Permanent dipole not necessary, only a change in dipole moment
• Not all bond absorb IR . Bond must have an electric dipole (bond polarity)
that changes as it vibrates.
• Molecules absorb IR – cause changes in modes of vibration (stretch/bend)
IR Absorption and Molecular Vibration
Molecular Vibration
Stretching Mode Bending Mode
Symmetric Stretching
• change in bond length
• bond become shorter/longer
• IR ACTIVE (change in dipole)
• IR INACTIVE (No change in dipole)
Asymmetric Stretching
• change in bond length
• bond become shorter/longer
• IR ACTIVE (change in dipole)
• IR INACTIVE (No change in dipole)
Symmetric Bending
• change in bond angle
• bond angle bigger/smaller
• IR ACTIVE (change in dipole)
• IR INACTIVE (No change in dipole)
Asymmetric Bending
• change in bond angle
• bond angle bigger/smaller
• IR ACTIVE (change in dipole)
• IR INACTIVE (No change in dipole)
wagging twisting rocking scissoring
Greenhouse Effect
GHG allow short wavelength radiation to pass through
but absorb IR longer wavelength radiation
11. Stretching Mode Bending Mode
Symmetric Stretching
- Bond polarity cancel out
- NO change dipole moment
- IR (inactive)
Asymmetric Stretching
- change in bond length
- change dipole moment
- Absorb IR (active)
Symmetric Bending
- change in bond angle
- change dipole moment
- Absorb IR (active)
Molecular Vibration for CO2
IR spectrum for CO2
Click here Spectra database (Ohio State) Click here Spectra database (NIST)
Molecular Vibration
Click here CO2 level (NASA)
Click here CO2 level (NOAA)
CO2 level over time
Click here CO2 level (CDIAC)
12. Click here CO2 level (NASA)
Click here CO2 level (NOAA)
CO2 level over time
Click here CO2 level (CDIAC)
Ocean acidification
Effect of ocean acidification
-Decrease in pH level
- Disturb marine /coral reef development/ecosystem
- CaCO3 needed for skeleton/shell for marine organisms
- Reduce ability of reef building coral to produce skeleton
Equilibrium bet CO2 (atmosphere) with aq CO2 (ocean)
Effect of increased CO2 level
Equilibrium bet CO2 (atmosphere) with aq CO2 (ocean)
CO2 (g) CO↔ 2 (aq)
↓
CO2 (aq) + H2O H↔ 2CO3 (aq)
↓
H2CO3 (aq) H↔ +
(aq) + HCO3
-
(aq)
↓
HCO3
-
(aq) H↔ +
(aq) + CO3
2-
(aq)
H+
ion (acidic)
13. Carbon Capture Storage/Sequestration (CCS)
i. Explain high solubility CO2
ii. Predict sign ∆H sol for CO2 in water, deduce how its solubility increase with temp
iii. High level CO2 lead to positive feedback whereby increase global temp are amplified. Exp its mechanism
iv. Ocean acidification is due to a drop in pH from 8.2 to 8.1. Find the % increase in acidity.
Capture and storage from fossil fuel
i. CO2 – polar bond, form H2 bonding with water.
ii. ∆H solution –ve, due to strong H2 bonding with water (favourable)
Increase in Temp- shift equi to left (endo) to reduce temp again
High Temp – decrease CO2 solubility
iii. High Temp – amplify the process as less CO2 dissolve – more CO2 in atmosphere – higher temp
CO2 (aq) + H2O H↔ 2CO3 (aq) ∆H = -ve polar bond polar
92.8
10
10
103.610][
][log2.8
][log
−−+
+
+
×==
−=
−=
H
H
HpH
91.8
10
10
109.710][
][log1.8
][log
−−+
+
+
×==
−=
−=
H
H
HpH
%25%100
)103.6(
)109.7()103.6(
%. 9
99
=×
×
×−×
= −
−−
increase
H2 bonding
14. Acknowledgements
Thanks to source of pictures and video used in this presentation
Thanks to Creative Commons for excellent contribution on licenses
http://creativecommons.org/licenses/
http://spmchemistry.onlinetuition.com.my/2013/10/electrolytic-cell.html
http://www.chemguide.co.uk/physical/redoxeqia/introduction.html
http://educationia.tk/reduction-potential-table
http://2012books.lardbucket.org/books/principles-of-general-chemistry-v1.0/s23-
electrochemistry.html
Prepared by Lawrence Kok
Check out more video tutorials from my site and hope you enjoy this tutorial
http://lawrencekok.blogspot.com