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3/28/2019
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Renewable Energy Resources
The big picture: Energy (power) reaching the Earth’s surface
Solar: Radiated energy at land surface
84,000 TW (TW = Terawatt = 1012 W)
Tides: Gravitational interaction
of Earth, Moon, and Sun
3 TW
Geothermal: Heat from radioactive decay
of long-lived isotopes within the Earth
44 TW
~99.95%
~0.05%
~0.003%
This power is ~ half that at the ‘top’ of the atmosphere
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Energy fluxes (Power per unit area)
Energy flux = Energy / (Area*Time)
Space- and time-averaged
Solar: 160 W/m2
Geothermal: 0.09 W/m2
Tide: 0.006 W/m2
We use these fluxes directly when
developing alternative / renewable
energy resources
Your text makes use of fluxes
The big picture: Energy use
2008 Global energy use ~ 500 exajoules
(5001018 J)
Equivalent to 15 TW power consumption
The breakdown:
13 TW Fossil fuels (85+%)
1 TW Nuclear
1 TW Renewable / Alternative
Mostly hydroelectric
Wee bits everything else
Po
we
r co
nsu
mp
tio
n (
TW
)
EIA 2008 data
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Review Problem: What was the per capita power consumption in 2008?
Given: Total power consumption of 15 TW in 2008
Global population ~ 7 billion
Globally, how many 100 W light bulbs are ‘you’ using at all times?
?
Time out
In kicking our ‘fossil sunshine’ habit, what
are the major challenges we face?
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46 coal-fired plants in Minnesota:
XCEL Energy (MSP):
30 plants @ 8961 MW total
ALLETE (DLH):
9 plants @ 1441 MW total
Great River Energy (Maple Grove):
3 plants @ 1400 MW total
Excelsior (Minnetonka):
4 plants @ 1035 MW total
Average MN fossil plant ~ 300 MW output
Typical fossil plant output ~ 200 – 500 MW
Typical nuclear plant output ~ 500 MW – 2 GW
Always keep in mind the ‘economies of scale’
Gut check: A useful measuring stick, perhaps?
Outline
• Geothermal
• Tides
• Solar
• Hydroelectric
• Wind
• Waves
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Sources of energy (heat) on Earth:
Solar input from above (~160 W / m2)
Geothermal heat from below (~90 mW / m2)
Wide range depending on geology / tectonics
~ 20 mW / m2 in subduction zones
~ 200 mW / m2 in volcanic provinces
Source for geothermal is radioactive decay of elements
(Uranium, Thorium, Potassium in crust and mantle)
Geothermal Energy
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Location, location, location…
Large-scale exploitation of
geothermal energy feasible in
regions of intense heat flow
In practice, this means volcanic
regions inboard of subduction zones
Example: “The Ring of Fire”
Geothermal Energy: Basics
General idea: ‘Mine’ heat from below
Note: In volcanic regions, geothermal
gradient can reach 80+ ºC/km
Approach:
• Drill series of deep wells
• Inject cold water from surface
• Recover hot water
• Run hot water through ‘heat
exchanger’ to concentrate heat
• Produce steam
• Steam turbine produces electricity
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Two basic approaches: Depends on geology
Vapor-dominated (“direct / dry steam”) Liquid-dominated (“flash / wet steam”)
Pressure at depth low enough
to allow vapor phase (steam)
High pressure maintains liquid
(water) phase at depth
CountryCapacity (MW)
2007
Capacity (MW)
2010
% national
production
USA 2687 3086 0.3%
Philippines 1970 1904 27%
Indonesia 992 1197 3.7%
Mexico 953 958 3%
Italy 811 843
New Zealand 472 628 10%
Iceland 421 575 30%
Japan 535 536 0.1%
El Salvador 204 204 14%
Kenya 129 167 11.2%
Costa Rica 162 166 14%
Top ten countries in terms of installed geothermal electricity capacity
Data: Bertani, R. (2007), "World Geothermal Generation in 2007", Geo-Heat Centre Quarterly Bulletin, 28 (3): 8–19
Holm, A. (2010), Geothermal Energy:International Market Update, Geothermal Energy Association
Recall: Average MN fossil plant output is 300 MW
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Wairakei Geothermal Field
Geothermal Case Study: New Zealand (North Island)
Situated on Pacific ‘ring of fire’; intense volcanic activity
Water-saturated geothermal reservoirs (“flash / wet steam” approach)
Output ~ 180 MW (How does this compare to a MN fossil plant?)
Produces ~7% of country’s energy needs; future goal is 20% (~2020)
Geothermal Energy for the home:
Residential Geothermal
• Same basic idea: Mine heat from
below surface
• ‘Produce’ heat for house /
business—not electricity
• Depths are shallow, i.e. a few
meters in your back yard
• Temperature difference is small
(~10 – 20 ºC)
• Requires efficient heat pump
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Geothermal Energy for the home: Residential Geothermal
Heat pumps: The basics
Requires special ‘refrigerant’
Captures latent heat of vaporization
in evaporator
Energy input compresses vapor,
thereby elevating its temperature
Releases heat of vaporization in
condenser
Liquid drops pressure and cools
Heat pump is part of overall system
On the ‘cool’ side, circulating fluid ‘mines’
heat from Earth (geothermal heat)
On the ‘hot’ side, circulating fluid moves
heat throughout structure
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latent heat of
vaporization
IN
latent heat of
vaporization
OUT
IN
External input
Geothermal Energy: Municipal applications
Is this feasible for Duluth?
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OTEC: Ocean Thermal Energy Conversion
a.k.a. the world’s largest heat pump…
Basic idea is simple: Can we somehow
exploit the temperature gradient in the
world’s oceans?
‘Evaporator’ uses warm surface water to
vaporize NH3
Vapor drives turbine = electricity
Deep cold water used in ‘condenser’
Theoretical efficiency ~ 6%
Modern systems ~2-3% efficient
However, oceans are HUGE heat reservoirs
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