Renewable and Non-Renewable Energy Sources: Comparison and Analysis, Study notes of Physics

A comprehensive overview of various primary, secondary, renewable, and non-renewable energy sources. It delves into the specific energy and energy density of different fuels, including uranium, hydrogen, natural gas, gasoline, kerosene, diesel, and coal. The document also discusses the production of electricity, nuclear power, and the advantages and disadvantages of different energy sources. It concludes with a discussion on solar, hydroelectric, wind, and thermal energy transfer.

Typology: Study notes

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TOPIC 8
ENERGY PRODUCTION
ENERGY SOURCES
PRIMARY SOURCES: all types of unprocessed energy sources that can be found in
nature
SECONDARY SOURCES: processes / exploited to mechanical work / electrical forms
EG: electricity
RENEWABLE SOURCES: readily replenished - a fuel that is creased faster / equally fast
as it is consumed
EG: solar energy / wind energy
NON-RENEWABLE SOURCES: a fuel that is consumed faster than it is created - will be
depleted
EG: fossil fuels / nuclear fuel
RENEWABLE ENERGY SOURCES
NON-RENEWABLE ENERGY SOURCES
solar power
wind power
hydroelectric power
tidal power
geothermal
biomass
coal
oil
natural gas
nuclear power
SPECIFIC ENERGY (Es): amount of energy that can be extracted from a unit mass of
fuel
energy / mass
ENERGY DENSITY (Ed): amount of energy that can be extracted from a unit volume of
fuel mass
energy / volume
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TOPIC 8

ENERGY PRODUCTION

ENERGY SOURCES

PRIMARY SOURCES: all types of unprocessed energy sources that can be found in

nature

SECONDARY SOURCES: processes / exploited to mechanical work / electrical forms

EG: electricity

RENEWABLE SOURCES: readily replenished - a fuel that is creased faster / equally fast

as it is consumed EG: solar energy / wind energy

NON-RENEWABLE SOURCES: a fuel that is consumed faster than it is created - will be

depleted EG: fossil fuels / nuclear fuel

RENEWABLE ENERGY SOURCES NON-RENEWABLE ENERGY SOURCES

● solar power ● wind power ● hydroelectric power ● tidal power ● geothermal ● biomass ● coal ● oil ● natural gas ● nuclear power

SPECIFIC ENERGY (Es): amount of energy that can be extracted from a unit mass of

fuel ⇒ energy / mass

ENERGY DENSITY (Ed): amount of energy that can be extracted from a unit volume of

fuel mass ⇒ energy / volume

FUEL SPECIFIC ENERGY (Es)

J kg¯¹

ENERGY DENSITY (Ed)

J m¯³ uranium - 235 7.0 x 10¹³ 1.3 x 10¹⁸ hydrogen 1.4 x 10⁸ 1.0 x 10⁷ natural gas 5.4 x 10⁷ 3.6 x 10⁷ gasoline 4.6 x 10⁷ 3.4 x 10¹⁰ kerosene 4.3 x 10⁷ 3.3 x 10¹⁰ diesel 4.6 x 10⁷ 3.7 x 10¹⁰ coal 3.2 x 10⁷ 7.2 x 10¹⁰

SANKEY DIAGRAMS: show the energy transfer & loss

⇒ width of each arrow is proportional to the amount of energy transfer

ENERGY DEGRADATION

● while energy may be completely converted into work in a single process, a CYCLICAL PROCESS is required to convert thermal energy to work continuously ● in accordance with the 2ND LAW OF THERMODYNAMICS , some energy will be lost to the surroundings & cannot be used to perform useful work

DEGRADED ENERGY: unavailable energy

FOSSIL FUELS: produced by the decomposition of buried animals & plant material due

to pressure & bacteria EG: oil / coal / natural gas

NUCLEAR REACTOR

NUCLEAR FUEL: the fuel is held in rods so that the neutrons released will fly out & cause

nuclear fission in other rods

GRAPHITE CORE: slows the neutrons down so that they are more likely to be absorbed

into a nearby fuel rod

CONTROL RODS: raised / lowered to stop neutrons from travelling between fuel rods &

therefore, change the speed of the chain reaction ⇒ absorb any excess neutrons

MODERATOR: slows down the fast moving neutrons so they can be absorbed by fuel rods

⇒ collide with H₂O molecules & transfer KE so slow down ordinary / heavy H₂O

COOLANT: heated by the energy released from the fission reactions & is used to boil H₂O

to drive turbines in the power station

CONCRETE SHIELD: the daughter products of the fission reaction are radioactive & can

be hazardous ⇒ many of the features of the reactor are designed to control the speed of the reaction & the T°C inside the shielding ⇒ an uncontrolled fission reaction can cause an explosion

RISKS WITH NUCLEAR POWER

● fission of U-238 ending up in Plutonium- ADVANTAGE: non-fissionable U-238 can be used to produce energy RISK: Pu-239 can be used as a NUCLEAR WEAPON ● NUCLEAR WASTE is ↑ radioactive with long half-life ○ currently, buried deep underground in containers avoiding leakage

ADVANTAGES DISADVANTAGES

  • ↑ power output ⇒ ↑ energy density
  • large reserves of nuclear fuels
  • nuclear power stations do not produce ghgs
  • radioactive waste products are difficult to dispose of
  • major public health hazard should ‘something go wrong’
  • problems associated with uranium mining
  • possibility of producing materials for nuclear weapons

SOLAR POWER

SOLAR PANELS: collect heat from the Sun which is used to heat the H₂O

in pipes underneath ● flat collecting surface ● coating: ↓ reflection ● black surface below collects sunlight which heats up the H₂O in the pipe underneath for use in the house ADVANTAGE: cheap DISADVANTAGE: bulky

PHOTOVOLTAIC CELLS: convert light directly into electricity

● sunlight incident on photovoltaic cell makes the e¯ excited ⇒ establish a potential difference

ADVANTAGES DISADVANTAGES

  • ‘free’
  • inexhaustible
  • clean
  • ↓ power output
  • works during the day only
  • affected by cloudy weather
  • ↓ power output
  • requires large area
  • initial $$ ↑

WIND POWER: power derived from moving masses of air

⇒ typically ∼30% of the power carried in wind is converted to energy

BIGGEST LOSS OF EFFICIENCY: wind cannot be stopped completely by the turbine

⇒ not all KE is transferred

ADVANTAGES DISADVANTAGES

  • ‘free’
  • inexhaustible
  • clean
  • dependent on local wind conditions
  • aesthetic problems - large infrastructures
  • noise problems 1. mass of air = ƿ AvΔT 2. KE of air = ½mv² = ½ ƿ AvΔtv² = ½ ƿ AΔtv³ 3. power = E/Δt = ½ ƿ Av³

THERMAL ENERGY TRANSFER

CONDUCTION: transfer of energy due to ↑ energy e¯ colliding with neighbouring

molecules

CONVECTION

EG: air over a hot radiator in a room is heated, expands & rises, transferring warm air to the rest of the room - cold air takes its place through convection currents & the process repeats

RADIATION: transfer of energy through electromagnetic induction

BLACK-BODY RADIATION

● all bodies with a finite (Kelvin) T°C radiate energy in the form of EM radiation (due to oscillating electric charges)

STEFAN-BOLTZMAN LAW

EMISSIVITY: measures how effectively a black-body radiates ⇒ 0 ≤ 𝜺 ≤ 1

BLACK BODY: perfect absorber & radiator ⇒ none of the incident radiation is reflected

(not shiny) ⇒ 𝜺 = 1 ● anything which has a black & dull surface is close to a black body EG: coal at ↓ T°C: radiates a little bit & looks dull at ↑ T°C: radiates a lot & looks bright

ABSORPTION VS RADIATION

SURFACE T°C OF A BLACK BODY: Tb SURROUNDING T°C: Ts POWER ABSORBED: Pabs = 𝜺𝝈ATs⁴ POWER RADIATED: Prad = 𝜺𝝈ATb⁴ THERMAL EQUILIBRIUM: Tb = Ts / Pabs = Prad ● EM radiation with different 𝝺 is emitted - a continuous distribution of 𝝺 ● most energy is radiated at a specific 𝝺max determined by the **WIEN’S DISPLACEMENT LAW *** a body with ↑T°C emits more at short 𝝺 INTENSITY: power of radiation received per unit area

SOLAR CONSTANT (S): amount of solar radiation at the mean distance from the Sun to

the Earth ***** assuming the Sun is a black body - calculate the power radiated by using the Stefan-Boltzman law P = 3.9 x 10²⁶ W

ENERGY BALANCE

● at EQUILIBRIUM , the energy input must be equal to the energy output ● the effects of the Earth's atmosphere on its mean surface T°C ⇒ GREENHOUSE EFFECT

TEMPERATURE AT EARTH’S SURFACE

1) the Earth radiates power from the entire surface area of its spherical shape, so the power radiates is: 2) assume the Earth is a black body ⇒ 𝜺 = 1 3) equating the incident & outgoing intensities, we get: 4) solving the equation, we get: 5) T = -17°C ***** actual average T°C of the Earth surface = 288K / 15°C

THE GREENHOUSE EFFECT

GREENHOUSE GASES: CO₂ / CH₄ / H₂O / N₂O ⇒ found in the Earth’s atmosphere

⇒ both natural & man-made origins ● by using WIEN’S DISPLACEMENT LAW with T=288K, we find that the peak 𝝺 that is

radiated by the Earth is in the INFRARED REGION

● infrared radiation is STRONGLY ABSORBED by greenhouse gases ○ e¯ transition between the MOLECULAR ENERGY LEVELS ○ the energy difference corresponds to energy of photons with infrared 𝝺 ● the absorbed radiation is eventually RE-RADIATED IN ALL DIRECTION ⇒ some of the re-radiated energy is absorbed by the Earth again causing the surface to be warmer GREENHOUSE GAS NATURAL SOURCES ANTHROPOGENIC SOURCES H₂O evaporation of H₂O from oceans / rivers / lakes irrigation O₂ forest fires / volcanic eruptions / evaporation of H₂O from oceans burning fossil fuels in power plants & cars / burning forests CH₄ wetlands / ocean / lakes & rivers / termites flooded rice fields / farm animals / processing of coal / natural gas & oil / burning biomass N₂O forests / oceans / soil & grasslands burning fossil fuels / manufacture of cement / fertilisers / deforestation (↓ of nitrogen fication in plants)