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This section covers fossil fuels, combustion and fuel calculations, the different forms of energy including the renewable versus non-renewable and conventional versus non-conventional distinctions, electrochemical cells and water splitting, small hydro power, hydrogen energy and fuel cells, solar thermal and photovoltaic applications, wind, geothermal, biofuels, nuclear energy, and waste to energy including sanitary landfill and gasification.
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Classification of Energy Sources • Non-renewable sources exist in a fixed stock and are consumed far faster than they form: coal, petroleum, natural gas and nuclear fuels.
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Renewable sources are replenished on a human timescale: solar, wind, hydro, biomass, geothermal and tidal. • Conventional means long established and commercially dominant — coal, oil, gas, large hydro and nuclear; non-conventional means the newer alternatives — solar, wind, biogas, tidal, geothermal and fuel cells.
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The two classifications are not the same, which is a favourite trap: large hydro is renewable but conventional, while nuclear is non-renewable yet is often grouped with conventional sources. • Primary energy is taken directly from nature; secondary energy such as electricity or hydrogen must be manufactured from a primary source.
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Hydrogen and electricity are energy carriers, not energy sources — an important and frequently examined distinction.
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Fossil Fuels and Their Analysis • Coal ranks in order of increasing carbon content and calorific value: peat → lignite → sub-bituminous → bituminous → anthracite.
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Anthracite has the highest carbon and calorific value and the lowest moisture and volatile matter; peat the reverse. • Proximate analysis reports moisture, volatile matter, ash and fixed carbon, and is the routine commercial test.
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Ultimate analysis reports the elemental composition — C, H, O, N, S and ash — and is what combustion calculations require.
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Distinguishing the two is a standard question. • Calorific value: the gross or higher calorific value (GCV/HCV) assumes the water formed is condensed and its latent heat recovered; the net or lower calorific value (NCV/LCV) assumes it leaves as vapour.
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GCV is therefore always greater than NCV, and the difference is largest for hydrogen-rich fuels.
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A bomb calorimeter measures GCV at constant volume. • Typical values worth carrying: natural gas about 50 MJ/kg, fuel oil about 44, bituminous coal 25-33, dry wood 15-18, and hydrogen about 142 MJ/kg on a gross basis — the highest of any chemical fuel by mass, though very low by volume unless compressed or liquefied.
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Combustion and Fuel Calculations • Stoichiometric (theoretical) air is the exact quantity needed for complete combustion.
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In practice excess air is supplied to ensure complete burning: typically 5-20 per cent for gaseous fuels, 15-30 for liquid and 20-50 for solid fuels. • Too little air leaves carbon monoxide and unburnt carbon; too much air carries heat out with the flue gas and lowers efficiency — the optimum is a balance between the two losses, found in practice by monitoring flue-gas oxygen. • Key stoichiometry to memorise:
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C + O₂ → CO₂ requires 32/12 = 2.67 kg O₂ per kg C;
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2H₂ + O₂ → 2H₂O requires 8 kg O₂ per kg H₂;
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S + O₂ → SO₂ requires 1 kg O₂ per kg S. • The standard formula for theoretical oxygen, allowing for oxygen already present in the fuel, is O₂ required = 2.67C + 8(H − O/8) + S kg per kg of fuel, and since air is 23.2 per cent oxygen by mass (21 per cent by volume), the theoretical air = O₂ required / 0.232. • Flue gas analysis by Orsat apparatus gives CO₂, O₂ and CO on a dry volume basis, absorbed successively in potassium hydroxide, alkaline pyrogallol and ammoniacal cuprous chloride — in that order.
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The reported analysis is dry, because water vapour condenses in the sampling line. • Flame temperature: the adiabatic flame temperature is the maximum attainable, with no heat loss and complete combustion; it falls as excess air increases, because the extra nitrogen must be heated too.
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Renewable and Non-conventional Sources Source Principle Strengths Limitations Solar thermal Concentrating or flat-plate collectors convert radiation to heat Simple, good for water and process heat Intermittent; needs storage; area intensive Solar PV Photovoltaic effect in a semiconductor junction generates DC directly No moving parts, modular, falling cost Commercial module efficiency typically 15-22 per cent; intermittent Wind Aerodynamic lift turns a rotor driving a generator Low running cost; mature technology Site specific, variable;
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Betz limit caps efficiency at 59.3 per cent Hydro (including small and micro) Potential energy of falling water drives a turbine High efficiency (80-90 per cent), dispatchable, long life Site specific; seasonal flow variation; sediment handling Geothermal Heat extracted from hot rock or fluids underground Continuous base load, small footprint Limited to suitable geology; scaling and dissolved gases Biomass and biofuels Combustion, digestion or fermentation of organic matter Storable, carbon neutral in principle, uses wastes Land and water use, food competition, seasonal supply Nuclear fission Heat from splitting heavy nuclei raises steam Very high energy density, no combustion emissions Waste management, capital cost, safety and proliferation Waste to energy Incineration, gasification, digestion or landfill gas recovery Reduces waste volume and recovers energy Emission control, variable feed, public acceptance • Hydro turbine selection by head is a standard question:
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Pelton (impulse) for high head, Francis (reaction, mixed flow) for medium head, and Kaplan (reaction, axial flow) for low head and high flow.
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Small, mini and micro hydro are classified by capacity, and micro-hydro is of particular importance for rural electrification in mountainous terrain. • Biofuels are grouped as solid (wood, charcoal, briquettes), liquid (bioethanol from fermentation of sugars or starch, biodiesel from transesterification of oils with methanol) and gaseous (biogas from anaerobic digestion, roughly 50-70 per cent methane and the balance mainly carbon dioxide; producer gas and syngas from gasification). • Generations of biofuel: first from food crops, second from lignocellulosic residues, third from algae — the progression being driven by the food-versus-fuel objection. • Gasification converts a solid fuel with a controlled, sub-stoichiometric supply of air, oxygen or steam into a combustible gas, chiefly CO, H₂ and CH₄.
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It differs from combustion precisely in being oxygen starved, and from pyrolysis in that pyrolysis uses no oxygen at all. • Sanitary landfill places waste in lined, compacted cells with daily cover, leachate collection and treatment, and gas extraction.
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Landfill gas is roughly half methane and half carbon dioxide, and since methane is a far more potent greenhouse gas than carbon dioxide, capturing and burning it is beneficial even when the energy is not used.
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Electrochemical Cells, Water Splitting and Fuel Cells • A galvanic (voltaic) cell converts chemical energy to electrical energy spontaneously; an electrolytic cell does the reverse, consuming electrical energy to drive a non-spontaneous reaction.
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In both, oxidation occurs at the anode and reduction at the cathode — but the sign convention reverses: the anode is negative in a galvanic cell and positive in an electrolytic cell, which is a classic point of confusion. • Water splitting (electrolysis):
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2H₂O → 2H₂ + O₂, with hydrogen released at the cathode and oxygen at the anode in a 2:1 volume ratio.
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The theoretical decomposition voltage is 1.23 V, but practical cells need 1.8-2.0 V because of overpotentials and resistance.
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Routes include alkaline, PEM and solid-oxide electrolysis, and the colour convention — green hydrogen from renewable electricity, blue from natural gas with carbon capture, grey from natural gas without it — is worth knowing. • A fuel cell converts chemical energy directly to electricity without a combustion step, so it is not limited by Carnot efficiency — the single most examined fact about fuel cells.
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Practical efficiencies of 40-60 per cent electrical, and up to 85 per cent in combined heat and power, are achieved. • The hydrogen-oxygen fuel cell has the overall reaction 2H₂ + O₂ → 2H₂O, producing only water as a by-product.
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Principal types are the PEM (proton exchange membrane, low temperature, used in vehicles), alkaline (used in spacecraft), phosphoric acid, molten carbonate and solid oxide (high temperature, tolerant of carbon monoxide and suitable for stationary power).