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Renewable Energy II
Hydroelectric power systems
high initial investment, low operating cost, long life expectancyno emissions; high capacity, reliabilityreservoirs provide water storage for navigation, irrigation, water supplyflood control, controlled discharge for recreation, fishing
reservoirs flood valuable land; displacement of towns; cultural historyreservoirs may increase evaporation and salinity of waterwater quality may decline due to impoundmentnatural fluctuations in stream flow are reduced – flooding reduced, but...temperature regimes are disrupted – cold water releasedsediment starvation of downstream system
Colorado River – Lake Powell, Lake Mead
Yangtze River – Three Gorges Dam
Nile River – Aswan High Dam
http://www.quarryscapes.no/images/Egypt_sites/aswan_loc.jpg
Aswan High Dam
Completed in 1970
Significant flood controland irrigation advantages
Floodplains downstreamstarved of new sedimentinput.
Delta subsidenceand erosion
Salinity
Destruction anddamage tocultural sites
http://www.cnsm.csulb.edu/departments/geology/people/bperry/geology303/_derived/geol303text.html_txt_NileDeltaEgypt.A2000060.0855.NASA.gif
http://blogs.nationalgeographic.com/blogs/news/chiefeditor/Three-Gorges-Dam-Map.jpg
Three Gorges Dam
Yangtze River
Hydropower to offsetnew coal-fired plants, flood control
Ecosystem impacts,water quality concernssocial displacement
Earthquakes?
Tidal and Wave Power
Tidal systems generally require a control dam (‘barrage’) to directflow through turbines.Some tidal systems have sufficient velocity to drive turbines without impoundment
Wave systems - experimental; disappointing to date
Geothermal
Steam and hot waterHot dry rock – injection and recovery of steam or hot water has beenproblematic
Ground, groundwater and lake geothermal – heat pump systemDepend on low-temperature (66-39 F heat exchangeprovide air conditioningClosed loop systems preferred
http://2.bp.blogspot.com/_cwrSE63jF7Y/R_uFKPAwsbI/AAAAAAAAARM/Tt0rHa96yhQ/s400/la_rance_tidal_power_plant.jpg
http://cache.gizmodo.com/assets/images/gizmodo/2008/07/seagen.jpg
http://home.clara.net/darvill/altenerg/images/wave.jpg
http://www.jamstec.go.jp/jamstec/MTD/Whale/proto1.jpg
Wave power – experimentalsystems to date
“Hot’ geothermal systems currently in operation depend onnatural recharge of cool surface water which is heated byhot rock or magma in areas of volcanic activity.
http://www.quantecgeoscience.com/Q_images/HotDryRockDiagram.jpg
Hot dry rock systemsrequire injection of cool surface water andproduction of steam or hotwater from fractured rockat depth.
These systems have not beensuccessfully developed to date. Loss of water to dry rock, and possible triggeringof earthquakes are ongoingproblems.
http://www.acegeo.com/_wp_generated/pp26641064.jpg
Lake or pond geothermal. Water at bottom of lakedoes not cool below 4C (39F). Heat pump requiredfor residential heating.
Craine Lake - a 22 acre private lake about 5 miles south of Hamilton.
Geothermal potential for 36 residences around the lake??
Craine LakeBathymetric Map
Depth Contours in Meters
Catie Carr – 8/27/08
100 meters
North
UT
M N
ort
hin
g N
AD
83
UTM Easting NAD 83
22-25oC
10-22oC
<10oC
100 meters
North
Craine LakeSummer Temperatures
UT
M N
ort
hin
g N
AD
83
UTM Easting NAD 83
TemperatureAugust, 2008
10 meters
5 meters
Lake surface
summer bottom water<10oC
summer surface layer22-25oC
thermocline layer
Summer thermal structure
Temperature Range
Volume of water
Cooling Capacity
in BTU (based on 2oC degree
temp. difference)
22-25 oC 438,000 m3
118,000,000 gallons
Not calculated
10-22 oC 59,800 m3
15,000,000 gallons
3 x 108 BTU
500 cooling days at 6000 BTU/hr
<10 oC 12,200 m3
3,000,000
6 x 107 BTU
100 cooling days at 6000 BTU/hr
<3.5oC
3.5-4.0oC
100 meters
North
UT
M N
ort
hin
g N
AD
83
UTM Easting NAD 83
Temperature February, 2009
10 meters
5 meters
Lake surface
slightly warmer bottom water<3.5 – 4.0 C
cold surface layer less than 3.5oC
Winter thermal structure