solar cooker data
DESCRIPTION
Solar Cooker Data. TimePlain Insulated ( o C)( o C) 02322 22930 43236 63340 83443 103545 123546 143547 163547. TimePlain Insulated ( o C)( o C) 183547 203547 223547 243547 263547. Energy Resources. - PowerPoint PPT PresentationTRANSCRIPT
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Solar Cooker Data
Time Plain Insulated (oC) (oC)
0 23 222 29 304 32 366 33 408 34 4310 35 4512 35 4614 35 4716 35 47
Time Plain Insulated (oC) (oC)
18 35 4720 35 4722 35 4724 35 4726 35 47
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Energy Resources
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Energy is the capacity to do work.
Energy is measured in Joules
1 Joule of energy can raise 1 N of weight exactly 1 meter
1 J=1N•m
(PS: your diet offers ~5-10 million J/day)
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First Law of Thermodynamics
Energy can neither be created nor destroyed. It can be converted to another form.
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Energy is the capacity to do work.
Forms include:
•
•
•
•
•
•
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Energy is the capacity to do work.
Forms include:
• Kinetic energy
• Potential energy
• Chemical energy
• Heat
• Elastic potential energy
• Electrical energy
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Energy is the capacity to do work.
Forms include:
• Kinetic energy
• Potential energy
• Chemical energy
• Heat
• Elastic potential energy
• Electrical energy
Together, these are called “mechanical energy”
Friction converts kinetic energy to heat
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Conversion of energy
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Conversion of energyElectrical energy lifts cars
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Conversion of energyHighest potential energy
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Conversion of energyHighest kinetic energy
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Conversion of energypotential kinetic
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Conversion of energykinetic potential
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Heat: Rule 1
• All matter is composed of particles in constant motion
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Heat: Rule 2
• Temperature is a measure of the kinetic energy of the particles.
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Heat: Rule 2 (a and b)
• Temperature is a measure of the kinetic energy of the particles.
a) When you heat a sample, the particles speed up
b) When you cool a sample the particles slow down
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Heat: Rule 2 (a and b)
• Temperature is a measure of the kinetic energy of the particles.
a) When you heat a sample, the particles speed up
b) When you cool a sample the particles slow down
Absolute zero is the temperature at which the particles stop (-273oC)
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Particles in motion:
• Solid Liquid Gas
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Heat transfer
• Hot things cool and cold things warm up.
• Duh.
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Heat transfer
• Hot things cool and cold things warm up.
Three ways:
1)
2)
3)
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Heat transfer
• Hot things cool and cold things warm up.
Three ways:
1) Convection
2) Conduction
3) Radiation
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Convection
Heat is carried up by the hotter mantle material which is less dense.
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Conduction
Cold Hot
Objects in contact
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Conduction
Cold Hot Not so
cold
Not so hot
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Conduction
Cold Hot Not so
cold
Not so hot
Hot (fast) particles collide with cool (slow) particles. The fast ones slow down while the
slow ones speed up
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Conduction
Cold Hot Not so
cold
Not so hot
Fast (hot) particles collide with slow (cool) particles. The hot ones cool down while the
cool ones warm up
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Radiation
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• Heat is transferred by electromagnetic radiation—visible and not-so-visible light.
Radiation
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The electromagnetic spectrum
Warm objects “glow” in infrared light
Hot objects glow in visible light
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Review—How can this hot object
lose heat?
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Review—How can this hot object
lose heat?
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Energy, Work, and Power
• Energy .
• Work
.
• Power
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
Work = Force x distance
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
Work = Force x distance
Energy = the amount of work done
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
Work = Force x distance
Energy = the amount of work done
Power = work / time
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
Measured in Joules
Measured in Joules
Measured in Watts
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Energy, Work, and Power
• Energy—the capacity to do work
• Work—exerting a force over a distance
• Power—the rate of work being done
Measured in J, kJ, cal, kcal, ft-lb, BTU, Q, kWh
Measured in W, hp, ft-lb/s
Measured in J, kJ, cal, kcal, ft-lb, BTU, Q, kWh
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U&A Question 5
• 300 hp=300 x (550 ft-lb/s) =165000 ft-lb/s!
• This motor could lift 165000 lbs at a rate of 1 ft/s
(or)
• 16500 lbs (a freight elevator) at 100 ft/s
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How do you get energy to do work?
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To generate electricity…
How would you like to heat your
water?
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Second Law of Thermodynamics
When energy converted to another form, some of the energy is lost as unusable heat.
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Second Law of Thermodynamics
When energy converted to another form, some of the energy is lost as unusable heat.
(or)
Energy conversion is never 100% efficient.
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Electricity
• A generator generates electricity.
• Work done on the generator is converted to electrical energy
• You do work on the generator by turning the crank.
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What turns your crank?
• A turbine converts kinetic energy of a fluid into rotation.
• Most electricity is made by steam driving a turbine
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To generate electricity…
How would you like to heat your
water?
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Options for turning a turbine
Heatsteam
•
•
•
•
•
•
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Options for turning a turbine
Heatsteam
• Coal
• Natural gas
• Nuclear fission
• Biomass
• Solar
• Ocean thermal
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Options for turning a turbine
Heatsteam Direct
• Coal 1)
• Natural gas 2)
• Nuclear fission 3)
• Biomass
• Solar
• Ocean thermal
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Options for turning a turbine
Heatsteam Direct
• Coal 1) Hydroelectric
• Natural gas 2) Wind
• Nuclear fission 3) Tidal
• Biomass
• Solar
• Ocean thermal
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Options for turning a turbine
Heatsteam Direct
• Coal 1) Hydroelectric
• Natural gas 2) Wind
• Nuclear fission 3) Tidal
• Biomass
• Solar
• Ocean thermal
Someday, nuclear fusion?
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Photovoltaic cells
• Photovoltaic (PV) cells convert light directly to electrical energy (no generator).
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Electrical generation
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Energy coming in
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Energy lost
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Energy provided as electricity
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First Law of Thermodynamics
• Energy is never created nor destroyed
(See Slide 1)
• Matter is never created nor destroyed
• They can be converted into each other.
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Global Carbon Cycle
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Carbon Cycle
• Where is the carbon?
1)
2)
3)
4)
Carbon moves from one form to another.
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Carbon Cycle
• Where is the carbon?
1) In fossil fuels and minerals
2) Living systems
3) Oceans
4) Atmosphere
Carbon moves from one form to another.
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Who cares?
• Natural systems maintain the balances.
• Anthropogenic (man-made) carbon flow comes from living systems and fossil fuels to the atmosphere
• Greenhouse gasses (CO2 and methane in the atmosphere) contribute to global warming.
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Acid Rain
• Burning fossil fuels contributes to acid rain
• Acid rain affects fish, amphibians, plants & surface water.
• Limestone neutralizes some of the acidity.
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pH• pH measures
acidity
• pH<7 is acidic
• pH>7 is basic
• pH=7 is neutral
• (see p R48)
• (Acid rain has pH 5.1-4.3 or less)
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Oil
Petroleum: from petro- “rock” & –oleum “oil”
Crude oil—(from the well) is distilled into:
• Natural gas
• Gasoline
• Kerosene
• Diesel
• Fuel oil
• Asphalt
From lowest to highest
boiling point
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Oil Use
Oil became:
--the fastest growing energy resource in 1920
--the greatest used energy resource in 1950
The US:
• --uses about 20,000,000 barrels of oil per day (about 1/5 of the world total)
• --produces about 5,000,000 barrels of oil/day (about 1/17 of world total)
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An oil reservoir
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An oil reservoir
Drill here.
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Solar and Wind Power
• See “Digging Deeper” in activity 8