energy system modelling summer semester 2018, lecture 1...dec 01 dec 03 dec 05 dec 07 dec 09 dec 11...
TRANSCRIPT
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Energy System Modelling
Summer Semester 2018, Lecture 1
Dr. Tom Brown, [email protected], https://nworbmot.org/
Karlsruhe Institute of Technology (KIT), Institute for Automation and Applied Informatics (IAI)
11th July 2018
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Table of Contents
1. Administration
2. Course outline
3. Introduction: Balancing Variable Renewable Energy
4. Electricity Consumption
5. Electricity Generation
6. Variable Renewable Energy (VRE)
7. Balancing a single country
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Administration
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Contact Details
Dr. Tom Brown
Young Investigator Group Leader
Energy System Modelling Research Group
Institute for Automation and Applied Informatics (IAI)
KIT, North Campus
https://nworbmot.org/
I am a physicist who has specialised in the optimisation of energy systems and the interactions
of complex networks. I now work at the intersection of informatics, economics, engineering,
mathematics, meteorology and physics.
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Lectures and Exercise Classes
The course will take place over five days: 11.7, 13.7, 16.7, 17.7 and 18.7.
Each day will consist of 3 lectures and one exercise class:
09:45-11:15 Lecture 1
11:30-13:00 Lecture 2
14:00-15:30 Exercise Class
15:45-17:15 Lecture 3
Some of the exercises will require you to program in Python, so please bring a laptop. We will
help you to install Python and the requisite libraries.
The course has 4 ECTS points.
Location: 50.41 Raum 145/146
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Course Website
You can find the course website here:
https://nworbmot.org/courses/esm-2018/
by following the links from:
https://nworbmot.org/
Course notes, exercise sheets and other links can be found there.
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Registration for Oral Exam
To get an evaluation at the end of the course, you need to register online for the oral
examination.
The oral examinations will take place some time in August on a single date. The date will be
decided during the final lecture, based on when we are all available.
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MA Thesis: Industrial Demand in a Fossil-Free European Energy System
We have some exciting opportunities in the Energy System Modelling group at IAI to look at
the integration of industrial demand and emissions in our European energy system model.
See the advert:
https://nworbmot.org/courses/esm-2018/esm-ma-bio-industry.pdf
Objectives:
• Collect sustainable biomass potentials for each European country by fuel type (forest
residues, agricultural residues, municipal waste, etc.) based on existing sources.
• Collect energy use and emissions per country per industry from standard statistical sources.
• Build the different energy pathways into an existing model of the European energy system.
• Simulate the optimal mix of energy sources and technologies to eliminate CO2 emissions
from the industrial sector.
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Literature
There is no book which covers all aspects of this course. In particular there is no good source
for the combination of data analysis, complex network theory, optimisation and energy systems.
But there are lots of online lecture notes. The world of renewables also changes fast...
The following are concise:
• Volker Quashning, “Regenerative Energiesysteme”, Carl Hanser Verlag Munchen, 2015
• Leon Freris, David Infield, “Renewable Energy in Power Systems”, Wiley, 2006
• Goran Andersson Skript, “Elektrische Energiesysteme: Vorlesungsteil
Energieubertragung,” online
• D.R. Biggar, M.R. Hesamzadeh, “The Economics of Electricity Markets,” Wiley, 2014
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Course outline
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Course outline
This course will cover the following topics:
• General properties of renewable power, time series analysis
• Backup generation, curtailment
• Network modelling in power systems
• Storage modelling
• Optimization theory
• Energy system economics
• Dynamics of renewable energy networks (synchronization, etc.)
• Complex network techniques for renewable energy networks (flow tracing, etc.)
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Introduction: Balancing Variable Re-
newable Energy
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The Global Carbon Dioxide Challenge: Budgets from 2016
600 Gt budget gives 33% chance of 1.5◦C (Paris: ‘pursue efforts to limit [warming] to 1.5◦C’)
800 Gt budget gives 66% chance of 2◦C (Paris: hold ‘the increase...to well below 2◦C’)
13Source: ‘Three years to safeguard our climate,’ Nature, 2017
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Research questions
1. What infrastructure (wind, solar, hydro generators, heating/cooling units, storage and
networks) does a highly renewable energy system require and where should it go?
2. Given a desired CO2 emissions reduction (e.g. 95% compared to 1990), what is the
cost-optimal combination of infrastructure?
3. How do we deal with the variablility of wind and solar: balancing in space with networks
or in time with storage?
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Daily variations: challenges and solutions
00:0030-Apr
03:0006:0009:0012:0015:0018:0021:000.0
0.2
0.4
0.6
Germ
an so
lar g
ener
atio
n [p
er u
nit]
Germany solar
00:0025-Apr
03:0006:0009:0012:0015:0018:0021:00
0.2
0.4
0.6
0.8
1.0
Germ
an ro
ad tr
ansp
ort [
per u
nit]
Germany road transport
Daily variations in supply
and demand can be
balanced by
• short-term storage
(e.g. batteries,
pumped-hydro, small
thermal storage)
• demand-side
management (e.g.
battery electric
vehicles, industry)
• east-west grids over
multiple time zones
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Synoptic variations: challenges and solutions
Jan2011
3103 10 17 240.0
0.2
0.4
0.6
0.8
Germ
an w
ind
gene
ratio
n [p
er u
nit]
Germany onshore windSynoptic variations in
supply and demand can be
balanced by
• medium-term
storage (e.g.
chemically with
hydrogen or methane
storage, thermal
energy storage, hydro
reservoirs)
• continent-wide grids
Transmission lines
Country nodes
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Seasonal variations: challenges and solutions
Jan2011
FebMar AprMay Jun Jul AugSep OctNovDec0.0
0.1
0.2
0.3
0.4
0.5
0.6
Mon
thly
yie
ld [p
er u
nit c
apac
ity]
Germany onshore windGermany solar
Jan2011
FebMar AprMay Jun Jul AugSepOct NovDec0
50
100
150
200
250
Germ
an h
eat d
eman
d [G
W] Germany heat demand
Seasonal variations in
supply and demand can be
balanced by
• long-term storage
(e.g. chemically with
hydrogen or methane
storage, long-term
thermal energy
storage, hydro
reservoirs)
• north-south grids
over multiple
latitudes
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Variability: Single wind site in Berlin
Looking at the wind output of a single wind plant over two weeks, it is highly variable,
frequently dropping close to zero and fluctuating strongly.
Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0
0.2
0.4
0.6
0.8
1.0
Pro
file
norm
alis
ed b
y m
ax (
per
unit
)
Berlin wind
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Electricity consumption is much more regular
Electrical demand is much more regular over time - dealing with the mismatch between
locally-produced wind and the demand would require a lot of storage...
Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0
0.2
0.4
0.6
0.8
1.0
Pro
file
norm
alis
ed b
y m
ax (
per
unit
)
Germany load
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Variability: Different wind conditions over Germany
But the wind does not blow the same at every site at every time: at a given time there are a
variety of wind conditions across Germany. These differences balance out over time and
space.
20Source: https://earth.nullschool.net/
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Variability: Single country: Germany
For a whole country like Germany this results in valleys and peaks that are somewhat
smoother, but the profile still frequently drops close to zero.
Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0
0.2
0.4
0.6
0.8
1.0
Pro
file
norm
alis
ed b
y m
ax (
per
unit
)
Berlin wind
Germany onshore wind
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Variability: Different wind conditions over Europe
The scale of the weather systems are bigger than countries, so to leverage the full smoothing
effects, you need to integrate wind at the continental scale.
22Source: https://earth.nullschool.net/
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Variability: A continent: Europe
If we can integrate the feed-in of wind turbines across the European continent, the feed-in is
considerably smoother: we’ve eliminated most valleys and peaks.
Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0
0.2
0.4
0.6
0.8
1.0
Pro
file
norm
alis
ed b
y m
ax (
per
unit
)
Berlin wind
Germany onshore wind
Europe all wind
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Variability: A continent: Wind plus Hydro
Flexible, renewable hydroelectricity from storage dams in Scandinavia and the Alps can fill
many of the valleys; excess energy can either be curtailed (spilled) or stored.
Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0
0.2
0.4
0.6
0.8
1.0
Pro
file
norm
alis
ed b
y m
ax (
per
unit
)
Wind
Hydro
Storing/Curtailment
Electrical Demand
24
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Costs: No interconnecting transmission allowed
Technology by energy:offshore
wind
10%
onshorewind
35%
solar
37%
run of river
4%
gas
5%
hydro
9%
Average cost e86/MWh:
0
20
40
60
80
100
Avera
ge s
yst
em
cost
[EU
R/M
Wh]
offshore wind
onshore wind
solar
gashydrogen storage
battery storage
Transmission lines (= 10 GW)
Yearly energy (= 50 TWh/a)
Countries must be self-sufficient at all times; lots of storage
and some gas to deal with fluctuations of wind and solar. 25
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Dispatch with no interconnecting transmission
For Great Britain with no interconnecting transmission, excess wind is either stored as
hydrogen or curtailed:
Jul 01 Jul 03 Jul 05 Jul 07 Jul 09 Jul 11 Jul 13
20
0
20
40
60
Pow
er
[GW
]
Demand
GB onshore wind
GB offshore wind
GB gas
GB hydrogen storage
GB onwind available
GB offwind available
26
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Costs: Cost-optimal expansion of interconnecting transmission
Technology by energy:offshore
wind
8%
onshorewind
56%solar17%
run of river5%
gas
5%
hydro
10%
Average cost e64/MWh:
no lines optimal0
20
40
60
80
100
Avera
ge s
yst
em
cost
[EU
R/M
Wh]
transmission linesoffshore wind
onshore wind
solargashydrogen storagebattery storage
Transmission lines (= 10 GW)
Yearly energy (= 50 TWh/a)
Large transmission expansion; onshore wind dominates. This
optimal solution may run into public acceptance problems. 27
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Dispatch with cost-optimal interconnecting transmission
Almost all excess wind can be now be exported:
Jul 01 Jul 03 Jul 05 Jul 07 Jul 09 Jul 11 Jul 1340
20
0
20
40
60
80
100
120
140
Pow
er
[GW
]
Demand
GB onshore wind
GB offshore wind
GB gas
GB hydrogen storage
GB onwind available
GB offwind available
Exports
28
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Electricity Only Costs Comparison
0 50 100 150 200 250
Allowed interconnecting transmission lines [TWkm]
0
50
100
150
200
250
300
Syst
em
cost
[EU
R b
illio
n p
er
year]
today'sgrid
battery storage
hydrogen storage
gas
solar
onshore wind
offshore wind
transmission lines
• Average total system costs
can be as low as e 64/MWh
• Energy is dominated by wind
(64% for the cost-optimal
system), followed by hydro
(15%) and solar (17%)
• Restricting transmission
results in more storage to
deal with variability, driving
up the costs by up to 34%
• Many benefits already locked
in at a few multiples of
today’s grid29
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Different flexibility options have difference temporal scales
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0
0.2
0.4
0.6
0.8
1.0
1.2
Energy level of storage (norm
ed)
hydrogen storagereservoir hydro
• Hydro
reservoirs are
seasonal
• Hydrogen
storage is
synoptic
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Different flexibility options have difference temporal scales
Aug2011
08 15 22 290.0
0.2
0.4
0.6
0.8
1.0
1.2
Energy level of storage (norm
ed)
battery storagePHS
hydrogen storagereservoir hydro
• Pumped hydro
and battery
storage are
daily
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Features of this example
This example has several features which will accompany us through this lecture:
1. We have to account for the variations of wind and solar in time and space.
2. These variations take place at different scales (daily, synoptic, seasonal).
3. We often have a choice between balancing in time (with storage) or in space (with
networks).
4. Optimisation is important to increase cost-effectiveness, but we should also look at
near-optimal solutions.
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It’s not just about electricity demand...
EU28 CO2 emissions in 2015 (total 3.2 Gt CO2, 8% of global):
public electricity and heat
33.3%residential heating
11.8%services heating 4.9%rail transport 0.2%
road transport
26.8%
navigation
4.7%
aviation
4.9% industry (non-electric)13.0%
other0.4%
33Source: Brown, data from EEA
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...but electification of other sectors is critical for decarbonisation
Wind and solar dominate the expandable potentials for low-carbon energy provision, so
electrification is essential to decarbonise sectors such as transport and heating.
Fortunately, these sectors can also offer crucial flexibility back to the electricity system.
34Source: Tesla; heat pump: Kristoferb at English Wikipedia
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Efficiency of renewables and sector coupling
exceed 50 %.
Fuel
Fossil-fuel condensing power station
Losses
Electricity
Renewableelectricity
Tom
orro
wTo
day
Electricity Heat Transport
Wind/solar energy
Electricity Renewableelectricity
Electric mobility
Renewableelectricity
Ambient heat
Heat pumps
Losses
Heat
Fuel
Gas heating
Losses
Heat Fuel
Internal-combustion engine
Losses
Propulsion
Propulsion
Losses
35Source: BMWi White Paper 2015
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Low cost of renewable energy 2017 (NB: ignores variability)
36Source: Lazard’s LCOE Analysis V11
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Energy Transition: Several changes happening simultaneously
Energiewende: The Energy Transition, consists of several parts:
• Transition to an energy system with low greenhouse gas emissions
• Renewables replace fossil-fuelled generation (and nuclear in some countries)
• Increasing integration of international electricity markets
• Better integration of transmission constraints in electricity markets
• Sector coupling: heating, transport and industry electrify
• More decentralised location and ownership in the power sector
37
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What can informatics contribute?
In all these questions we are limited by computational complexity.
Informatics can contribute on the data side:
• Processing and analysing enormous weather datasets
• Geographical potential analysis with GIS tools
• Visualisation of results
and on the algorithmic side:
• Data reduction: clustering and PCA examples to follow later
• New optimisation routines for speed and accuracy
• Information theory to trace interdependencies
Build on informatics’ interdisciplinary links to engineering, economics, meteorology,
mathematics and physics.38
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Electricity Consumption
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Why is electricity useful?
Electricity is a versatile form of energy carried by electrical charge which can be consumed in a
wide variety of ways (with selected examples):
• Lighting (lightbulbs, halogen lamps, televisions)
• Mechanical work (hoovers, washing machines, electric vehicles)
• Heating (cooking, resistive room heating, heat pumps)
• Cooling (refrigerators, air conditioning)
• Electronics (computation, data storage, control systems)
• Industry (electrochemical processes)
Compare the convenience and versatility of electricity with another energy carrier: the chemical
energy stored in natural gas (methane), which can only be accessed by burning it.
40
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Power: Flow of energy
Power is the rate of consumption of energy.
It is measured in Watts:
1 Watt = 1 Joule per second
The symbol for Watt is W, 1 W = 1 J/s.
1 kilo-Watt = 1 kW = 1,000 W
1 mega-Watt = 1 MW = 1,000,000 W
1 giga-Watt = 1 GW = 1,000,000,000 W
1 tera-Watt = 1 TW = 1,000,000,000,000 W
41
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Power: Examples of consumption
At full power, the following items consume:
Item Power
New efficient lightbulb 10 W
Old-fashioned lightbulb 70 W
Single room air-conditioning 1.5 kW
Kettle 2 kW
Factory ∼1-500 MW
CERN 200 MW
Germany total demand 35-80 GW
42
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Energy
In the electricity sector, energy is usually measured in ‘Watt-hours’, Wh.
1 kWh = power consumption of 1 kW for one hour
E.g. a 10 W lightbulb left on for two hours will consume
10 W * 2 h = 20 Wh
It is easy to convert this back to the SI unit for energy, Joules:
1 kWh = (1000 W) * (1 h) = (1000 J/s)*(3600 s) = 3.6 MJ
43
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Electricity spot market: trading of energy
Energy is traded in MWh; current price around 30-40 e/MWh, but sinking thanks to
renewables and the merit order effect:
44Source: Agora Energiewende
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Consumption metering
• Look for your
electricity meter at
home
• Mine here shows
42470.3 kWh
• Check what the value
is a week later
45
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Electricity bill
My bill for 2014-5: 1900 kWh for a year, at a cost of e570, which corresponds to 0.3 e/kWh
or 300 e/MWh. But the spot market price is 30 e/MWh, so what’s going on??
46
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Household price breakdown
Although the wholesale price is going down, other taxes, grid charges and renewables subsidy
(EEG surcharge) have kept the price high.
HOWEVER the EEG is only high because it is paying for solar panels bought at a time when
they were still comparatively expensive; but through the German subsidy, production volumes
were high and the learning curve has brought the costs down exponentially.47Source: Agora Energiewende
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Yearly energy to power
Germany consumes around 600 TWh per year, written 600 TWh/a.
What is the average power consumption?
600 TWh/a =(600 TW) ∗ (1 h)
(365 ∗ 24 h)
=600
8760TW
= 68.5 GW
48
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Discrete Consumers Aggregation
The discrete actions of individual consumers smooth out statistically if we aggregate over many
consumers.
49
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Load curve properties
The Germany load curve (around 500 TWh/a) shows daily, weekly and seasonal patterns;
religious festivals are also visible.
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0
10
20
30
40
50
60
70
80
DE load [
GW
]
DE load
50
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Load duration curve
For some analysis it is useful to construct a duration curve by stacking the hourly values from
highest to lowest.
0 20 40 60 80
Percentage of time during year
0
10
20
30
40
50
60
70
80
DE load [
GW
]
DE load
51
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Load density function
Similarly we can also build the probability density function:
0 20 40 60 80 100
DE load [GW]
0.000
0.005
0.010
0.015
0.020
0.025
0.030
0.035
0.040
Pro
babili
ty d
ensi
ty
DE load
52
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Load spectrum
If we Fourier transform, the seasonal, weekly and daily frequencies are clearly visible.
0 50 100 150 200 250 300 350 400
frequency [a−1]
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
1.8
Spect
ral densi
ty
1e9
DE load
53
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Electricity Generation
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How is electricity generated?
Conservation of Energy: Energy cannot be created or destroyed: it can only be converted
from one form to another.
There are several ‘primary’ sources of energy which are converted into electrical energy in
modern power systems:
• Chemical energy, accessed by combustion (coal, gas, oil, biomass)
• Nuclear energy, accessed by fission reactions, perhaps one day by fusion too
• Hydroelectric energy, allowing water to flow downhill (gravitational potential energy)
• Wind energy (kinetic energy of air)
• Solar energy (accessed with photovoltaic (PV) panels or concentrating solar thermal power
(CSP))
• Geothermal energy
NB: The definition of ‘primary’ is somewhat arbitrary.55
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Power: Examples of generation
At full power, the following items generate:
Item Power
Solar panel on house roof 15 kW
Wind turbine 3 MW
Coal power station 1 GW
56
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Generators
With the exception of solar photovoltaic panels (and electrochemical energy and a few other
minor exceptions), all generators convert to electrical energy via rotational kinetic energy and
electromagnetic induction in an alternating current generator.
57Source: Wikipedia
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Example of electricity generation across major EU countries in 2013
NO ES GB DE FR0
100
200
300
400
500
600
700
800
900
Ele
ctri
city
Genera
tion in 2
013 [
TW
h/a
]
Solar
Wind
Biomass
Hydro
Oil
Gas
Hard Coal
Lignite
Nuclear
58
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Electricity generation in Germany per year
In 15 years Germany has gone from a system dominated by nuclear and fossil fuels, to one with
33% renewables in electricity consumption.
2002 2004 2006 2008 2010 2012 2014
year
0
100
200
300
400
500
600
Yearl
y e
lect
rici
ty g
enera
tion in G
erm
any [
TW
h/a
]
Nuclear
Brown Coal
Hard Coal
Gas
Hydro
Biomass
Wind
Solar
Exports
59Source: Author’s own representation based on
https://www.energy-charts.de/energy_en.htm
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Efficiency
When fuel is consumed, much/most of the energy of the fuel is lost as waste heat rather than
being converted to electricity.
The thermal energy, or calorific value, of the fuel is given in terms of MWhth, to distinguish it
from the electrical energy MWhel.
The ratio of input thermal energy to output electrical energy is the efficiency.
Fuel Calorific energy Per unit efficiency Electrical energy
MWhth/tonne MWhel/MWhth MWhel/tonne
Lignite 2.5 0.4 1.0
Hard Coal 6.7 0.45 2.7
Gas 15.4 0.4 6.16
Uranium 150000 0.33 50000
60
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Fuel costs to marginal costs
The cost of a fuel is often given in e/kg or e/MWhth.
Using the efficiency, we can convert this to e/MWhel.
Fuel Per unit efficiency Cost per thermal Cost per elec.
MWhel/MWhth e/MWhth e/MWhel
Lignite 0.4 4.5 11
Hard Coal 0.45 10 22
Gas 0.4 23 58
Uranium 0.33 3.3 10
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CO2 emissions per MWh
The CO2 emissions of the fuel.
Fuel tCO2/t tC02/MWhth tCO2/MWhel
Lignite 0.9 0.36 0.9
Hard Coal 2.4 0.36 0.8
Gas 3.1 0.2 0.5
Uranium 0 0 0
Current CO2 price in EU Emissions Trading Scheme (ETS) is around e16/tCO2
62
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CO2 emissions from electricity sector
Despite the increase in renewables in the electricity sector, CO2 emission have not been
reduced substantially in Germany. This is partly because German exports have also increased.
63Source: Agora Energiewende
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Variable Renewable Energy (VRE)
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Wind time series
Unlike the load, the wind is much more variable, regularly dropping close to zero and rarely
reaching full output (when aggregated over all of Germany).
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0
0.2
0.4
0.6
0.8
1.0
DE o
nw
ind [
per
unit
]
DE onwind
65
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Wind time series: weekly
If we take a weekly average we see higher wind in the winter and some periodic patterns over
2-3 weeks (synoptic scale).
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan2012
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
DE o
nwin
d [p
er u
nit]
DE onwind
66
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Wind duration curve
0 20 40 60 80
Percentage of time during year
0.0
0.2
0.4
0.6
0.8
1.0D
E o
nw
ind [
per
unit
]
DE onwind
67
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Wind density function
0.0 0.2 0.4 0.6 0.8 1.0
DE onwind [per unit]
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5Pro
babili
ty d
ensi
ty
DE onwind
68
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Wind spectrum
If we Fourier transform, the seasonal, synoptic and daily patterns become visible.
0 50 100 150 200 250 300 350 400
frequency [a−1]
0
20000
40000
60000
80000
100000
120000
Spect
ral densi
ty
DE onwind
69
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Solar time series
Solar is variable, but more predictable than wind.
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
DE s
ola
r [p
er
unit
]
DE solar
70
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Solar time series: weekly
If we take a weekly average we see higher solar in the summer.
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan2012
0.00
0.05
0.10
0.15
0.20
0.25
DE s
ola
r [p
er
unit
]
DE solar
71
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Solar duration curve
0 20 40 60 80
Percentage of time during year
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8D
E s
ola
r [p
er
unit
]
DE solar
72
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Solar density function
0.0 0.2 0.4 0.6 0.8 1.0
DE solar [per unit]
0
1
2
3
4
5
6
7
8
9Pro
babili
ty d
ensi
ty
DE solar
73
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Solar spectrum
If we Fourier transform, the seasonal and daily patterns become visible.
0 50 100 150 200 250 300 350 400
frequency [a−1]
0
100000
200000
300000
400000
500000
600000
700000
800000
Spect
ral densi
ty
DE solar
74
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Balancing a single country
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Power mismatch
Suppose we now try and cover the electrical demand with the generation from wind and solar.
How much wind do we need? We have three time series:
• {dt}, dt ∈ R the load (varying between 35 GW and 80 GW)
• {wt},wt ∈ [0, 1] the wind availability (how much a 1 MW wind turbine produces)
• {st}, st ∈ [0, 1] the solar availability (how much a 1 MW solar turbine produces)
We try W MW of wind and S MW of solar. Now the effective residual load or mismatch is
mt = dt −Wwt − Sst
We choose W and S such that on average we cover all the load
〈mt〉 = 0
and so that the 70% of the energy comes from wind and 30% from solar (W = 147 GW and
S = 135 GW).76
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Mismatch time series
Jan2011
Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec200
150
100
50
0
50
100D
E m
ism
atc
h [
GW
]
DE mismatch
77
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Mismatch duration curve
0 20 40 60 80
Percentage of time during year
200
150
100
50
0
50
100D
E m
ism
atc
h [
GW
]
DE mismatch
78
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Mismatch density function
150 100 50 0 50
DE mismatch [GW]
0.000
0.002
0.004
0.006
0.008
0.010
0.012
0.014Pro
babili
ty d
ensi
ty
DE mismatch
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Mismatch spectrum
If we Fourier transform, the synoptic (from wind) and daily patterns (from demand and solar)
become visible. Seasonal variations appear to cancel out.
0 50 100 150 200 250 300 350 400
frequency [a−1]
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
Spect
ral densi
ty
1e10
DE mismatch
80
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How to deal with the mismatch?
The problem is that
〈mt〉 = 0
is not good enough! We need to meet the demand in every single hour.
This means:
• If mt > 0, i.e. we have unmet demand, then we need backup generation from
dispatchable sources e.g. hydroelectricity reservoirs, fossil/biomass fuels.
• If mt < 0, i.e. we have over-supply, then we have to shed / spill / curtail the renewable
energy.
81
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Mismatch
Mar2011
07 14 21 280
50
100
150
200Pow
er
[GW
]
consumed
backup
curtailment
82
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Mismatch
Jul2011
04 11 18 250
20
40
60
80
100
120
140
160
180Pow
er
[GW
]
consumed
backup
curtailment
83
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Mismatch
Dec2011
05 12 19 260
50
100
150
200Pow
er
[GW
]
consumed
backup
curtailment
84
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Mismatch duration curve
0 20 40 60 80
Percentage of time during year
100
50
0
50
Mis
matc
h [
GW
]backup
curtailment
85
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What to do?
Backup energy costs money and may also cause CO2 emissions.
Curtailing renewable energy is also a waste.
We’ll look in the next lectures at 4 solutions:
1. Smoothing stochastic variations of renewable feed-in over larger areas, e.g. the whole of
Europe.
2. Using storage to shift energy from times of surplus to deficit.
3. Shifting demand to different times, when renewables are abundant.
4. Consuming the electricity in other sectors, e.g. transport or heating.
86