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Lecture 20
Assessment of
Biomass
Advantages
Large
potential energy source
Part of
natural C-cycle ΰ no addition to greenhouse problem
Disadvantages:
Low
efficiency
Competition
with food production
Large installations
needed for combustion; hydrogenation; pyrolysis ΰ transport of low energy material needed
ΰ Viable as alternative if waste can be used,
not very promising if energy crops are needed
Hydropower
Extraction
of power from flowing water
Energy
equation: E = mgh
m mass;
g gravitational attraction; h height
Three
types of approaches
Impoundment
(Reservoir)
Run-of-river
Diversion
River
dams
Pumped
Storage
Systematics of a
power plant (Fig. 1)
Example:
Large Power stations
in the World (Fig. 3)
Issues with
Hydropower
Advantages
Continuous
low cost power
Low
maintenance costs
No
consumption of exhaustible fuels
Little
air pollution
Reservoir
lakes ΰ recreation
Flood
protection regulation of downstream flow
Groundwater
recharge
High
efficiency 80 ΰ 90 %
Disadvantages:
High
initial cost
Strong
variations in water levels affect recreation
Conflict
between flood protection and power production
Loss of
land for agriculture
Stream
valley inundated
Evaporation
losses
Seismic
instability
Fish
migration
Change
in
Windpower
Extraction
of energy from moving air
Energy
equation
Ekin = ½
mv2
M = rAv
Ekin = ½
rAv3
r density of air (1.25
kg/m3); A area swept out by rotor; v wind velocity
Efficiency
(Fig. 4):
Theoretical:
63 %
Practical:
40 %
Wind potential in
the
Installed wind
capacity (Fig. 6)
Issues with wind
energy
Advantages:
Low
maintenance cost
No
exhaustible fuel needs
No green
house gas release
Many
areas are suitable for wind energy
Compatible
with other land use
Disadvantages:
Relatively
small energy output ΰ many structures needed
Unreliable
energy production
Problems
with birds
Interference
with radiosignals (?)
Best
places along coast or off shore
Ocean Thermal
Energy Conversion
Production
of Electricity using temperature difference in ocean waters
Origin
of T differences: Variation of solar flux with latitude (Fig. 7)
Deep
water is cold due to thermohaline convection (Fig.
8)
Efficiency:
Carnot Cycle
h = (Tin Tout)/Tout (in deg K)
An
Collection
of energy from solar heat
Energy
production based on Carnot cycle
Small temperature
differences ΰ low efficiency ΰ large systems needed
Small
environmental impact in open system
Closed
system: Use of fluids with low evaporation T ΰ some problematic fluids under consideration
Not in
current use
Future:
Open ocean systems ΰ problem of energy transfer ΰ combination of electricity and aluminum production
Other solar
schemes
Waves
Ocean
currents
Solar
Tower (Fig. 10)