GENERAL_ASPECTS_OF_ENERGY_MANAGEMENT_AND_ENERGY_AUDIT (CHAPTER 11:NEW AND RENEWABLE ENERGY SOURCES (NRES))

 

 GENERAL_ASPECTS_OF_ENERGY_MANAGEMENT_AND_ENERGY_AUDIT 

 (CHAPTER 11:NEW AND RENEWABLE ENERGY SOURCES (NRES))

Concept of New and Renewable Energy

Renewable energy is energy obtained from sources that are essentially inexhaustible such as sun and wind. Examples of renewable resources include wind power, solar power, geothermal energy, tidal power, bio- energy (bio-fuels grown sustainably) and hydropower. A renewable energy system  converts the energy found in sunlight, wind, falling-water, sea-waves, geothermal heat, or biomass into a form, we can use such as heat or electricity. Another important feature of renewable energy is that it can be used without the release of harmful pollutants. Renewable energy is also known as non-conventional energy. Renewable energy sources are essentially flows of energy unlike the fossil and nuclear fuels which are considered stocks of energy.

Fundamentals of Solar Energy

Solar radiation is radiant energy emitted by the sun comprising of ultra-violet, visible and infra-red radiation. The amount of solar radiation that reaches any given location is dependent on several factors including the geographic location, time of day, season, landscape, and local weather. Because the earth is round, the sun strikes the surface at different angles ranging from 0° (just above the horizon) to 90° (directly overhead). When the sun’s rays are vertical, the earth’s surface gets maximum energy possible. The more slanted the sun’s rays are, the longer they travel through the atmosphere, becoming more scattered and diffuse.

Solar Constant

Solar constant is the rate at which solar energy, at all wavelengths, is received per unit area at the top level of Earth’s atmosphere. The solar constant actually varies by about 0.3% over the 11-year solar cycle but averages about 1,368 W/m’. Each planet has its own planetary solar constant.

Solar Insolation

Solar Insolation is the amount of solar energy that strikes a square metre of the earth’s surface in a single day. Insolation is greatest when the surface is normal to the Sun. As the angle increases beyond a direction normal to the surface and the sunlight, the insolation is reduced in proportion to the cosine of the angle. The average incoming radiation is known as solar insolation and is one-fourth the solar constant, or 342 W/2.

By knowing the insolation levels of a particular area, required size of solar collector and energy output can be calculated. An area with poor insolation levels will need a larger collector than an area with high insolation levels. The values are generally expressed in kWh/m/7/day. India receives solar energy in the region of 5 to 7 kWh/m? for 300 to 330 days in a year. This energy is sufficient to set up 20 MW solar power plant per square kilometre land area.
Solar energy can be used through two different routes, namely, Solar Thermal Energy and Solar  electric (Solar Photovoltaic) Energy. Solar thermal systems uses the sun’s heat and convert it into heat energy while solar photovoltaic systems uses sun’s heat to produce electricity.

Solar Thermal Energy
Solar collectors are the main component of most of solar energy systems. The collector absorbs the sun’s energy and converts it into heat energy. This energy is then transferred to a fluid or air which is used to heat water, generate electricity, dry materials, distill water or cook food. When used for heating purpose, solar thermal system can partially or fully replace the conventional fuels such as coal, oil and electricity.
Various applications of solar thermal energy discussed are
¢ Solar Water Heating System (Flat-plate collector & Evacuated tube collector)
¢ Solar Thermal Power Systems (Power tower,parabolic trough collector)

Solar Water Heating System
A solar water heating system (Figure 11.1) consists of a flat plate or evacuated tube solar collector, a storage tank and connecting pipes. The system is generally installed on the roof or on open ground, with the collector facing the sun and connected to a continuous water supply. The collectors are generally mounted on a north-facing roof (in southern hemisphere). Water stored in the tank remains hot overnight . as the storage tank is insulated and heat losses are small.
Figure 11.1 Solar Water Heating System
Solar Flat Plate Collector
The most common collector is called a flat-plate collector. Flat-plate collectors heat the circulating fluid to a temperature of about 40-60°C. Flat plate collector is highly dependent upon ambient temperatures. It has good efficiency if ambient temperature is high. Consequently, heat output is higher during summer months than winter months in a flat plate collector.
The flat plate collector (Figure 11.2) usually comprises of copper tubes welded to copper sheets (both coated with a highly absorbing black coatings) with toughened glass sheet on top for cover and insulating material at the bottom. The entire assembly is placed in a flat box.

Evacuated Tube Collector
For higher temperatures, evacuated tube collectors are used. Evacuated tube collector is less dependent upon ambient temperature unlike flat plate collector and its efficiency does not drop with ambient temperature. In this type of solar collector, evacuated glass tubes are used instead of copper in which case a separate cover sheet and insulating box are not required. Water flows through the tubes, absorbs solar heat and is stored in a tank. This type of solar collector can reach high temperatures upto 150°C.
Evacuated tube collector is shown in Figure 11.3.
Evacuated tube collector comprises of two concentric glass tubes fused in the ends as shown in Figure 11.4. The air is evacuated from the gap between the tubes.
The evacuated double-walled glass tube provides thermal insulation similar to that of thermally insulated “Thermos” bottle. The outer glass tube is clear, and the surface of the inner glass tube is coated with a special heat material that absorbs the sun’s energy.
Sun rays penetrate the outer clear glass and heat energy is absorbed by the inner coated glass. The vacuum permits the heat radiation to enter the outer tube. The absorbent coating on the inner tube converts short wave radiation to long wave radiation thus preventing re-radiation to atmosphere. Since conduction cannot take place in vacuum, heat loss due to conduction back to atmosphere is also prevented. Because of this principle, more heat is trapped compared to a flat plate collector. The heat
loss in Evacuated tube collector is less than 10% compared with 40% for a flat plate collector. Water
flows in through a third, innermost concentric feeder tube and hot water flows out in the annulus outside the feeder tube in contact with the absorber tube surface.

Solar Electrical Energy

There are broadly two ways of generating electrical energy from solar power; the thermal route and direct conversion route through photovoltaic. There are two basic types of solar thermal power stations: power tower and parabolic trough collector.

Power Towers

A typical power tower (see Figure 11.5) operation is described as follows:

1. Sunlight is concentrated and directed from a large field of heliostats (mirrors) to a receiver on a tall tower.
2. Molten salt (for example liquid sodium) from the cold salt tank is pumped through the central receiver where it is heated to 566°C).
3. The heated salt from the receiver is stored in the hot salt thermal storage tank.
4. Molten salt is pumped from the hot salt tank through a steam generator that creates steam,
which drives a steam turbine, generating electricity.
5. Cold salt at 288°C flows back to the cold salt thermal storage tank and is re-used.
Parabolic Trough Collector
Parabolic Trough Collector is currently the most proven solar thermal electric technology. This system uses a Series of specially designed parabolic curved, trough shaped reflectors that focus the sun’s energy onto a receiver tube running at the focus of the reflector as shown in Figure 11.6. Because of their parabolic shape, troughs can focus the sun at 30-60 times its normal intensity on the receiver pipe. Heat transfer fluid (such as water) in the receiver is heated to a temperature of about 400°C. Large arrays of these collectors are coupled to provide high temperature water for driving a steam turbine. The collectors are aligned on an east-west axis and the troughs are rotated to follow the sun to
maximize the sun’s energy input to the receiver tube. Such power stations can produce many megawatts (MW) of electricity, but are confined to areas where there is sufficient solar insolation.


Solar Photovoltaic Technology

Direct conversion of solar energy to electricity takes place through photoelectric effect. The photoelectric or photovoltaic effect is the process in which the two dissimilar materials in close contact produce an electrical voltage when struck by light or radiant energy. Discrete packets of light energy known as photons, strike the Photovoltaic (PV) cell, knocking the electrons in the silicon material out of their normal energy state, putting them in a position to be conducted as electricity (Refer Figure 11.7).

The photoelectric effect only occurs when a photon which has the correct amount of energy strikes an atom in the solar cell. The amount of energy needed is dependent on the material the solar cellismadefrom.This means that the solar cell is not able to convert all the different wavelengths of light which are hitting it. Because of this,solar cells are “tuned” during their manufacturing to absorb the spectrum of sunlight that is most intense. This phenomenon is exploited to form the individual solar cells on wafers of silicon.Since Silicon is naturally reflective in nature, each photovoltaic cell is typically covered with an anti-reflective coating to minimize any loss from reflection.

PV panels comprise of PV cells. Solar cells are connected in series and parallel combinations to form modules that provide the required power. PV cells have been made with silicon (Si), gallium arsenide (GaAs), copper indium diselenide (CIS), cadmium telluride (CdTe), and a few other materials.

A Photovoltaic (PV) module comprise of PV panels (also known as solar panels), battery system, charge controller, inverter as shown in Figure 11.8.

One silicon cell generally produces 0.5 Volts. 36 such cells connected together are called a PV module and it has enough voltage to charge 12 V battery and run pump and motor. Modules can be connected together to form an array and generate more power.

The wattage output of a PV module is rated in terms of peak Watt (Wp). The peak Watt output power from a module is defined as the maximum power output that the module could deliver under standard test conditions. Single PV module can be manufactured with capacity ranging from 5 Wp to 120 Wp.

Stand-alone SPV Power Plant: These systems are used where conventional grid supply is not available, or is irregular. In an SPV power plant, electricity is centrally generated and made available to users through a local grid in a ‘stand-alone mode’. The most common use for such plants is the electrification of remote villages, power for hospitals, hotels, communication equipment, railway stations, border outposts etc.

Grid connected Solar System: Grid connected solar system (Figure 11.9) use an inverter that synchronizes with the utility power. These systems do not generally require batteries, although batteries can be used to provide backup power if the utility power goes out. Grid connected solar is easier to install and maintain than stand-alone system.

Building-integrated PV Systems: In building-integrated photovoltaic (BIPV) system, PV panels are integrated into the roof or facade of a building as shown in Figure 11.10. BIPV provides photovoltaic power as well as weather proofing and glazing of buildings. SPV panels generate electricity during the daytime, which is used to meet a part of the electrical energy needs of the building. Since PV cells are integrated into the buildings, no separate costly mountings are required.
Wind Energy
The use of wind energy is not new and has been used for thousand of years for applications such as water pumping, milling grains, mechanical power, sailing etc. However, it is the use of wind energy for electricity generation that is receiving most attention today. Modern windmills are normally called as wind turbines as their functions are similar to gas and steam turbines. They are also called as wind energy conversion systems (WECS), and those used to generate electricity are described as wind generators.

How Wind is Created?
As the earth orbits the sun daily, it receives light and heat. The majority of the heat from the sun is received North Pole at the equator and it gradually reduces towards both Gold Cold poles. Across the earth these heat differences help create wind. In warmer regions of the earth the air is hot and is therefore at a high pressure, compared to colder regions, where the air is at a low pressure. Wind is the
movement of air from area’s of high pressure to low pressure. Ideally, wind should flow from equator to the direction of either pole if earth is not rotating.
However, rotation of earth creates a force known as Coriolis force. The Coriolis force is swirling action on the winds because of earth rotation. This causes series of wind circulations in both northern and southern latitude as shown in Figure 11.11.
The local winds are largely affected by earth terrain. The earth has large flat plains (desert regions), areas covered with plant life (rainforests), very uneven regions (mountain ranges) and very smooth regions (seas and oceans), all of which affect the wind near the surface of the earth to varying levels. Sea breeze is set up when hot air rises from land, which is heated faster than sea, rises into the sky where it cools off. High in the sky, the cooled air now moves towards the sea and sinks pressing cold air from sea towards land.
Variability in Wind Speed and its Effect
Wind speed and direction are continuously fluctuating. The wind will vary over few hours with weather system. Generally, tropics have steady moderate winds all year, temperate latitudes have much more variation in wind speed and in particular more high wind speed occurrences. Sites with more wind speed will generate more power. The Table 11.1 gives a guideline of different wind speeds and their potential in producing electricity.
Description of Wind Energy Technology
The most common type is horizontal-axis machines. Horizontal-axis wind turbines have the main rotor shaft and electrical generator at the top of a tower, and must be pointed into the wind.Blades on rotor of horizontal-axis machines can be in the front (upwind) or behind (downwind) of the tower.

Components of wind turbine system
The various components of a wind turbine system are shown in the Figure 11.12 and detailed  description is given as follows:

Rotor: The shape of rotor blade and angle in relation to the relative wind direction affect the aerodynamic performance of the blades. Rotors can be single bladed, twobladed or three-bladed. Multi-bladed rotors are also available. Two- and three-bladed rotors are commonly used for power generation. The three-bladed rotors operate more smoothly and generally more quietly than two-bladed rotors. Multi-bladed rotors have large starting torque in light winds and are used for water pumping and low frequency mechanical power.
Nacelle Assembly: Nacelle is the part of wind turbine at top of tower housing containing gear box, generator assemblies and any control component. The main components of Nacelle assembly are shown in Figure 11.13.
Low-speed shaft: The low-speed shaft, which is the main shaft, is connected directly to the rotor hub.
The rotor turns the low-speed shaft at about 30 to 60 rotations per minute.
High-speed shaft: The high-speed shaft is connected to the low-speed shaft by the gear box and drives
the generator. The high-speed shaft will turn at between 1,000 and 1,800 rpm.
Gear box: Gears connect the low-speed shaft to the high-speed shaft and increase the rotational speeds
from about 30 to 60 rotations per minute (rpm) to about 1,000 to 1,800 rpm, which is the rotational
speed required by most generators to produce electricity.
Generator: The generator converts the turning motion of wind turbines blades into electricity. For
commercial applications, the most common type of generator is an induction generator that produces
50-cycle AC electricity.
Disc Brake: The disc brake is located on main shaft before the gear box or on high speed shaft after
the gear box. The basic purpose is to slow down the rotor.
Yaw Control: It is necessary for rotor axis to be aligned with wind direction in order to extract as much of wind kinetic energy as possible. Large wind turbines with upwind rotors require yaw control to align the rotor with the wind. To enable this, any change in wind direction, sensors activate the yaw
control motor, which rotates the nacelle and rotor assembly until turbine 1s properly aligned.

Operating Characteristics of Wind Turbine
A few of the important operating characteristics of a wind turbine include the cut-in speed, rated speed,
cut-out speeds, power output and capacity factor. Refer Figure 11.14.

Cut-in Speed: There is a minimum speed at which a wind turbine can reliably produce useable power.
This is known as the cut-in speed which is generally around 5 m/s.
Rated Speed: Most wind turbines are designed to generate maximum power at a fixed wind speed. This is known as rated power and the minimum wind speed at which it is achieved is the rated wind speed. The rated wind speed is chosen to fit the local site and wind regime and 1s often 1.5 times the site mean wind speed.
Cut-out Speed (Furling Speed): Above a certain speed beyond the rated speed, the wind turbine will need to shut down and stop operation to prevent damage to the unit. Cut-out speeds vary by manufacturer from about 20 to 30 m/s. The wind speed at which shut down occurs is called the cut-out speed. Cutout speed is also known as furling speed.
Betz Limit: It is impossible for the blades of a wind turbine to be 100% efficient since some of the wind energy must pass through the blades to make the turbine turn. Air flowing over the blades and through the rotor area makes a wind turbine function. The wind turbine extracts energy by slowing down the wind. The theoretical maximum amount of energy in the wind that can be collected by a wind turbines rotor is approximately 59%. This value is known as the Betz limit. Considering the Betz limit and the efficiency losses through the generator, gearbox, etc, will result in only about 15-25% of
the wind energy being converted into useful power.

Rotor Efficiency: The ability of a turbine rotor to extract the wind’s power depends upon its “efficiency”.
Thus to express the power output of the turbine, a non-dimensional coefficient of performance of the
blades (Cp) is included. The coefficient of performance of blades (Cp) varies with speed and generally varies between 0.33 -0.59.
Power Available from the wind turbine: Power extracted by wind turbine is proportional to the cross
sectional area of the wind intercepted by wind turbine and cube of the wind speed.
The power generated by a wind turbine can be found using the following formula:

Power generated is highly dependent upon wind speed. Doubling the wind speed increases the power
by eight times, but doubling the turbine area only doubles the power. Thus optimizing the siting of
wind turbines in the highest wind speed areas has significant benefit and critical for the best economic
performance.
For example, consider a wind turbine with 6 m diameter rotor, a coefficient of performance of 0.30,
generator efficiency of 0.8, a gearbox efficiency of 0.90, and a wind speed of 11 m/s.
What is the expected power output in watts?
P=0.5 * 1.2 * 3.14/4 * 6? * 0.30 * 0.8 * 0.9 * 11^3
P = 4875 watts, or 4.875 kW

Capacity Factor: The capacity factor of a wind turbine is the actual energy output of a wind turbine
during a given time period, usually one year, compared to its theoretical maximum energy output.
The capacity factor (CF) is,
CF = kWh produced / (8760 * Nameplate rating of the wind turbine, kW)
Typical capacity factors are 20-40% with values at the upper end of the range in particularly favorable
sites.
A 2.5 MW wind turbine could produce theoretical maximum of 21,900,000 kWh’s per year
(2.5 * 1,000 *8760).
However, due to the variability of the wind the unit has actually produced 5,000,000 kWh per year.
In this example, the capacity factor is,
CF = 5,000,000 / (2.5 * 1,000 *8760)
CF = 22.8%

Biomass Energy
Biomass is basically organic matter such as wood, straw, crops, algae, sewage sludge, animal waste and/or other biological waste. Bioenergy is the energy derived from biomass. In energy terms, biomass can be viewed as a form of stored solar energy. The sun’s energy is captured and stored (via photosynthesis) in the biomass material. The carbon dioxide released during the burning of biomass when used as fuel is largely balanced by the absorption/ capture of carbon dioxide during its growth. Hence it is considered ‘carbon neutral’ The different methods used to generate energy from biomass are:

Direct Combustion of Biomass
Biomass energy used to generate heat and electricity through direct combustion in modern devices, ranging from very small scale domestic boiler to multi megawatt size power plant electricity. Direct combustion is the combustion of biomass in a grate, stoker or fluidized bed with excess air followed by capturing the release of energy, which can then be used to provide steam or hot water for process heating and/or for providing electricity. Solid biomasses include coconut shells, rice husks, bagasse, wood waste, oil seed cakes such as de-oiled bran (DOB) etc. Biomasses of low bulk density are processed into pellets or briquettes. A typical pelleted fuel is shown in Figure 11.15

Gasification of Biomass
Biomass contains carbon, hydrogen and oxygen molecules. Complete combustion would produce carbon dioxide (CO,) and water vapour (H,O) whereas combustion under controlled conditions 1.¢e. partial combustion produces carbon monoxide (CO) and hydrogen (H,), which are combustible gases. The biogas produced through gasification is called as producer gas. The producer
gas has relatively low calorific value, ranging from 1000 to 1200 kcal / Nm>. The conversion efficiency
of the gasification process is the range of 60-70%. It can be used for combustion in a reciprocating
engine. When gas is used in dual fuel DG set, it can result in 65-85% diesel savings.
Gasification is a partial combustion of biomass and takes place at temperature of about 1000°C. Partial
combustion is facilitated by supplying air less than stoichiometric requirements. The products of
combustion are combustible gases like Carbon monoxide (CO), Hydrogen (H,) and traces of Methane
(CH,) and non useful products like tar and dust. The production of these gases is by reaction of water
vapor and carbon dioxide through a glowing layer of charcoal. Thus, the key to gasifier design is to
create conditions such that (a) biomass is reduced to charcoal and, (b) charcoal is converted at suitable
temperature to produce CO and H.,.
1. gasification system consists of four main stages:
2. Feeding of feedstock
3.Gasifier reactions where gasification takes place
4. Cleaning of resultant gas Drying Zone
5. Utilization of cleaned gas.
Biomass gasifier (Figure 11.16) is a thermo chemical converter / reactor where various physical and chemical reactions take place. Biomass is passed through various zones — Drying/ Distillation Zone,Pyrolysis Zone, Combustion Zone & Reduction Zone. When the biomass is passed through all the above zones, it gets converted into a high quality combustible gas called Producer Gas.




Spark ignition engines running on producer gas on an average produces 0.55-0.75 kWh of energy from
1 kg of biomass. Compression ignition (diesel) engines cannot run completely on producer gas. Thus
to produce 1 kWh of energy they consume  kg of biomass and 0.07 litres of diesel. Consequently
they effect 80-85% diesel saving.

Biomethanation of Biomass (Anaerobic Process)
Biomass can also be converted into bio-methane gas which is composed mainly of methane and carbon
dioxide. The process is based on biological digestion / anaerobic digestion (biomethanation) of biomass.
This is the only process giving additional advantage of high grade manure as the by-product. The raw materials for biomethanation process include manure, sewage sludge, municipal solid waste, fruit and vegetable waste, food waste, distillery wastes and other biodegradable wastes. Bio-methane can completely replace natural gas for applications using natural gas such as boilers, furnaces, IC engines etc.
Biomass offers higher energy efficiency through form of biogas than by direct burning (refer chart). Biogas produced through anaerobic process (in the absence of air) using cow dung as input material is generally called as Gobar gas. The gobar gas is a gas mixture typically comprising of around 60% methane and 40% carbon dioxide that is formed when organic matter such as dung, industrial organic wastes,vegetable wastes etc. are broken down by specific bacteria in the absence of air, at slightly elevated
temperatures (most optimum between 35 - 40°C). The biogas process is also known as anaerobic digestion or fermentation, and provides a clean fuel that can be produced on a scale varying from a small household system to a large commercial plant of several thousand cubic metres. Biogas can be used for electricity generation or purified to be used as a vehicle fuel.
Anaerobic digestion is a four-stage process as specific bacteria feed on certain organic materials. In the first stage, acidic bacteria dismantle the complex organic molecules into smaller molecules and in the second stage, these molecules further breakdown into organic acids, carbon dioxide and ammonia. A second type of bacteria (methanogenic bacteria) starts to convert these molecules into acetates and hydrogen in the third stage, which then converts to methane in the fourth stage. These methane producing bacteria are particularly influenced by the ambient conditions, which can slow or halt the process completely if conditions are not favourable.
A typical biogas plant using floating drum biogas prevalent in India is described in Figure 11.17. This design consists of a tank or a well with a partition wall to prevent mixing of influent fresh dung slurry with the outgoing spent slurry. The gas produced is trapped under a plastic or a metallic drum. With the continuous production more gas is trapped under this bell and the drum rises. This acts as a gas storage unit and when the tap above is released, the gas is discharged at more or less constant pressure. A non-return valve in the outlet is a valuable investment to prevent air being drawn into the digester, which would destroy the activity of the bacteria and provide a potentially explosive mixture inside the drum.

Biofuels from Biomass
Biomass can be converted into liquid fuels such as Ethanol and Biodiesel to partially replace the conventional petroleum fuels.
Ethanol is commonly produced by the fermentation of molasses, a by-product in sugar manufacture. It is also produced by fermenting any biomass feedstock rich in carbohydrates (starch, sugar or cellulose). e.g.: Sugar beet, Sweet corn and Ligno-cellulosic materials (straw and wood waste), which
are much cheaper than molasses, are now being considered for manufacturing ethanol. Ethanol is used
as a fuel additive to cut down vehicle’s carbon monoxide and other smog causing emissions. Flexible
fuel vehicles, which run on mixture of gasoline, use up to 85% ethanol.
Biodiesel is a good alternative for diesel. The most economical way of producing biodiesel is by transesterification of extracted oil (e.g. Jatropha seeds oil) with alcohol such as methanol. Jatropha is anon edible tree-borne oilseed which grows in dry and arid land. Biodiesel can be used as an additive
to reduce vehicle emissions (typically 20%) or in its pure form as a renewable alternative fuel for diesel engines. All oils extracted from plant origin, waste cooking oil and animal fat can be used as raw materials for biodiesel production. The biodiesel cycle is shown in Figure 11.18.
Hydro Power
Water power can be harnessed in many ways; the most common way is to use a turbine which is turned
by water moving in a controlled manner. Large dams hold water which can be used to provide energy for industry and grid electrification systems. Smaller systems can provide energy to remote regions without the need to build dams. Classification of hydro by size is given in the Table 11.2.

Micro-hydro power is the small-scale harnessing of energy from falling water; for example, harnessing enough water from a local river to power a small factory or village. The Figure 11.19 shows the main components and layout of a run-of-the-river micro-hydro scheme. This type of scheme requires no water storage but instead diverts some of the water from the river which is channelled along the side of a valley before being ‘dropped’ into the turbine via a penstock.

Water into Watts
To determine the power potential of the water flowing in a river or stream it is necessary to determine
both the flow rate of the water and the head through which the water can be made to fall. The potential
power can be calculated as follows:
Small water turbines rarely have efficiencies better than 80%. Power will also be lost in the pipe carrying the water to the turbine, due to frictional losses. A rough guide used for small systems of a few kW rating is to take the overall efficiency as approximately 50%. Thus, the theoretical power must
be multiplied by 0.50 for a more realistic figure.
Example: A turbine generator set operating at a head of 10 metres with flow of 0.3 cubic metres per second will deliver approximately, (9.81 x 0.5 x 0.3 x 10 =) 14.715 kiloWatts of electricity.

Fuel Cell
Input to a Fuel Cell is hydrogen. Hydrogen combines with oxygen to produce electricity through an electrochemical process with water and heat as by-products. Since conversion of the fuel to energy takes place using an electrochemical process (not combustion process), fuel cell is a clean, quiet and highly efficient process. Although there are many types of fuel cells, the principle of operation is similar.

Operation of Fuel Cell
A Fuel Cell (Figure 11.20) consists of two catalyst coated electrodes surrounding an electrolyte. One electrode is an anode and the other is a cathode. The process begins when hydrogen molecules enter the anode. The catalyst coating separates hydrogen’s negatively charged electrons from the positively charged protons. The electrolyte allows the protons to pass through to the cathode, but not the electrons.
Instead the electrons are directed through an external circuit which creates electrical current. While the electrons pass through the external circuit, oxygen molecules pass through the cathode. The oxygen and the protons combine with the electrons after they have passed through the external circuit producing water and heat.

Individual fuel cells can then be placed in a series to form a fuel cell stack. The stack can be used in
a system to power a vehicle or to provide stationary power to a building.
In general all fuel cells have the same basic configuration - an electrolyte and two electrodes. Whatever be the type of fuel cell, all require hydrogen as fuel. Hydrogen is a secondary energy resource, meaning it must be made from another fuel. Hydrogen can be produced in a variety of ways such as steam reforming of natural gas, electrolysis of water, gasification of biomass, etc. The biggest hurdle to large scale commercial exploitation of fuel cell is the cost of production of hydrogen which is now very  high.



Applications of Fuel Cells
The type of fuel cells used is decided by the application in which it is used. Since fuel cells are capable
of producing power anywhere in the | Watt to 10 Megawatt range, they can be applied to almost any application that requires power.
The low power range fuel cells can be used as source of power for personal electronics applications such as charging of cell phones, personal computers etc. The high power fuel cells (1 kW — 100 kW range) fuel cell can be used to power vehicles. The megawatt range fuel cells can be used to convert energy for distributed power uses. Application of fuel cells in the transportation sector has significant advantages like reduced complexity of design.

Energy from Wastes
Energy can be recovered from wastes (trash) via combustion of waste in incinerators and generating power. A typical Waste-to-Energy power plant using direct combustion is explained in Figure 11.21. Power generation from landfill gas Biogas produced from landfill is known as Landfill gas (Figure 11.22). This process is also an anaerobic digestion process as bacteria decompose organic matter naturally in absence of oxygen over time.
Landfill gas is composed mainly of methane and carbon dioxide. The methane gas produced in landfill
sites normally escapes into the atmosphere and contributes to greenhouse gas emissions. However, if
perforated pipes are inserted into the landfill, the landfill gas will travel through the pipes under natural
pressure to be used as energy source.
Wave Energy
Sea waves are the result of the concentration of energy from various natural sources like sun, wind, tides, ocean currents, moon, and earth rotation. Waves originate from wind and storms far out to sea and can travel long distances without significant energy loss, and hence power production is much steadier and more predictable. Unlike the wind and solar, power from sea waves continues to be produced round the clock.
Wave energy contains roughly 1000 times the kinetic energy of wind. Hence it allows smaller devices to produce power. Wave energy varies as the square of wave height whereas wind power varies with the cube of air speed. Water being 850 times as dense as air results in much higher power produced from wave averaged over time. Theoretically it is possible to extract 40 MW of power per km of coast where there are gentle waves (say | m height) and 1000 MW per km of coast where the wave height is
5m.
Kinetic energy from waves can be used to power a turbine. As shown in the Figure 11.23, the wave rises into a chamber. The rising water forces the air out of the chamber. The moving air spins a turbine which can turn a generator. When the wave goes down, air flows through the turbine and back into the chamber through doors that are normally closed thus generating power even when wave is receding.

Tidal Energy
How tide is caused?
Tidal energy is another form of ocean energy. Tides are generated by the combination of the moon and sun’s gravitational forces. Greatest effects of tides are in spring when sun and moon combine forces. Bays and inlets amplify the tide. Cycles of low and high tides occur twice a day. When tides come into
the shore, they can be trapped in reservoirs behind dams. Then when the tide drops, the water behind the dam can be let out just like in a regular hydroelectric power plant. In order for the tidal energy to be practicable for energy production, the height difference needs to be atleast 5 m is needed. The principle of working of tidal energy is shown in Figure 11.24.

Geothermal Energy
The top most part of the earth is the crust. Below the crust of the earth is a layer called mantle. The top layer of the mantle is a hot liquid rock called magma (see Figure 11.25). The crust of the earth floats on this liquid magma mantle. When magma breaks through the surface of the earth in a volcano, it is called lava.

For every 100 meters you go below ground, the temperature of the rock increases about 3°C. So, at a depth of about 3000 metres below ground, the temperature of the rock would be hot enough to boil water. Deep under the surface, water sometimes makes its way close to the hot rock and turns into boiling hot water or into steam. The hot water can reach temperatures of more than 148°C. When this hot water comes up through a crack in the earth, it is known as hot spring.
Some of the areas have so much steam and hot water that it can be used to generate electricity. Holes are drilled into the ground and pipes lowered into the hot water. The hot steam or water comes up through these pipes from below ground. A geothermal power plant is like in a regular power plant except that no fuel is burned to heat water into steam. Different types of geothermal power plants are described as follows:

Dry Steam Power Plants
A dry steam power plant (Figure 11.26) draws steam from a hydrothermal production well and sends it to a turbine/generator. The steam turns the turbine to generate electricity and is then condensed and returned to the geothermal reservoir via an injection well.
Flash Steam Power Plants
Flash Steam Power (Figure 11.27) draws hot water from a hydrothermal production well to a flash tank where a drop In pressure “‘flashes”’ the hot water (182°C) to steam. The steam turns a turbine/generator that generates electricity. The steam is then condensed and along with the remaining hot water not flashed into steam is returned to the geothermal reservoir via an injection well.

Binary Cycle Power Plant
Binary Cycle Power Plants (Figure 11.28) operateon the lower-temperature waters, 107° to 182°C).  These systems use two closed loops. Binary cycle pumps hot water from well to a heat exchanger where hot water is used to heat a working fluid, usually organic compound with low boiling point.
This working fluid is then vaporized in a heat exchanger and used to turn a turbine. The geothermal water and the working fluid are confined to separate closed loops. So there are no emissions into the air.




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GENERAL_ASPECTS_OF_ENERGY_MANAGEMENT_AND_ENERGY_AUDIT (CHAPTER 10:ENERGY EFFICIENCY AND CLIMATE CHANGE)

 

 GENERAL_ASPECTS_OF_ENERGY_MANAGEMENT_AND_ENERGY_AUDIT

  (CHAPTER 10:ENERGY EFFICIENCY AND CLIMATE CHANGE)

Energy and Environment

The combustion of hydrocarbon based fuels in industrial activity generates by-product materials, many of which are considered to be air pollutants (Figure 10.1). The principal emissions which impact on the air environment are carbon dioxide, particulate matter (dust), sulphur oxides, nitrogen oxides, hydrocarbons, and carbon monoxide. Particulate matter is predominantly generated during the combustion of solid fuels such as coal, lignite, biomass etc mostly from ash content in the fuel. Sulphur oxide (SOx) emissions mainly occur from combustion of oil and coal due to sulphur content in the fuel. Nitrogen oxides (NOx) emissions are also associated with fuel combustion, both from fuel as well as combustion air. Both SOx and NOx emissions have been identified as major air pollutants globally as they lead to acid rain which is a trans-boundary environmental issue. The main sources of carbon monoxide emissions are due to incomplete combustion of fuels.

Carbon dioxide resulting from the oxidation of carbon in fuels during combustion dominates the total emissions. Although, carbon dioxide is not considered as a pollutant, it is considered as a major contributor to global warming and climatic change.

Global Environmental Issues
One of the most important characteristics of global environmental issues is that it affects all mankind on a global scale without regard to any particular country or region. These environmental issues have global significance and need to be addressed through international efforts. The whole world is a stakeholder and this raises issues on who should do what to combat environmental problems.
Some of the key environmental issues of global significance are
1. Acid rain
2. Ozone layer depletion
3. Global warming and climatic change
4. Loss of biodiversity

Acid Rain

Acid rain is caused by release of sulphur oxides and nitrogen oxides from combustion of fossil fuels, which then mix with water vapour in atmosphere to form sulphuric acids and nitric acids respectively (Refer Figure 10.2).

The effects of acid rain are as follows:

1.Acidification of lakes, streams, and soils

2. Direct and indirect effects (release of metals, for example: Aluminum which washes away plant nutrients)

3. Killing of wildlife (trees, crops, aquatic plants, and animals)

4. Decay of building materials and paints, statues, and sculptures

5. Health problems (respiratory, burning- skin and eyes)


Ozone Layer Depletion

Ozone layer is a thin layer of ozone (O,) present in stratosphere which extends from 10-50 km from the earth (Figure 10.3). The ozone layer is highly beneficial to life on earth as it blocks the sun’s Ultraviolet radiations (UV-B) from reaching the earth. Any disturbance or depletion of ozone layer would result in an increase of harmful radiation reaching the earth’s surface leading to dangerous consequences.

Ozone, which is highly unstable, is produced and destroyed naturally in the stratosphere and until recently, this resulted in a well-balanced equilibrium (see Figure 10.4). Ozone is formed when oxygen molecules absorb ultraviolet radiation with wavelengths less than 240 nanometres and is destroyed when it absorbs ultraviolet radiation with wavelengths greater than 290 nanometres.



Ozone Depletion Process

In recent years, scientists have measured a seasonal thinning of the ozone layer primarily at the South Pole. This phenomenon is being called the ozone layer depletion. It was found that ozone is easily broken down by man-made chlorine and bromine compounds. These compounds are found to be responsible for most of the ozone layer depletion. The main chemical responsible for the problem is identified as Chloro fluro carbons (CFCs) which were used in refrigerator and air conditioners.

The ozone depletion process begins when Chloro fluro carbons (CFCs) and other ozone-depleting substances (ODS) emitted into the atmosphere reach stratosphere by diffusion. Strong UV radiations break apart the ODS molecules. CFCs, HCFCs, carbon tetrachloride, methyl chloroform release chlorine atoms, and halons and methyl bromide release bromine atoms. It is the chlorine and bromine atom that actually destroys ozone, not the intact ODS molecule. It is estimated that one chlorine atom can destroy from 10,000 to 100,000 ozone molecules before it is finally removed from the stratosphere.

Chemistry of Ozone Depletion

When ultraviolet light waves strike CFC (CFCI,) molecules in the upper atmosphere, a carbonchlorine bond breaks, producing a chlorine (Cl) atom. The chlorine atom then reacts with an ozone (O3) molecule breaking it apart and so destroying the ozone. This forms an ordinary oxygen molecule (O2) and a chlorine monoxide (ClO) molecule. Then a free oxygen atom breaks up the chlorine monoxide, releasing chlorine. The released chlorine is free to repeat the process of destroying more ozone molecules. A single CFC molecule can destroy 100,000 ozone molecules. The chemistry of ozone depletion process is shown in Figure 10.5. 

Effects of Ozone Layer Depletion
Effects on Human and Animal Health: Increased penetration of solar UV-B radiation is likely to have high impact on human health with potential risks of eye diseases, skin cancer and infectious diseases. Effects on Terrestrial Plants: Increased radiation is likely to change species composition in forest and grassland thus altering the bio-diversity in different ecosystems. It could also affect the plant community indirectly resulting in changes in plant form, secondary metabolism, etc.

Effects on Aquatic Ecosystems: High levels of radiation exposure in tropics and subtropics may affect the distribution of phytoplanktons, which form the foundation of aquatic food webs. It can also cause damage to early development stages of fish, shrimp, crab, amphibians and other animals, the most severe effects being decreased reproductive capacity and impaired larval development.

Effects on Bio-geo-chemical Cycles: Increased solar UV radiation could affect terrestrial and aquatic bio-geo-chemical cycles thus altering both sources and sinks of greenhouse and important trace gases, e.g. carbon dioxide (CO,), carbon monoxide (CO), carbonyl sulfide (COS), etc. These changes would contribute to biosphere-atmosphere feedbacks responsible for the atmosphere build-up of these greenhouse gases.

Effects on Air Quality: Reduction of stratospheric ozone and increased penetration of UV-B radiation result in higher photo dissociation rates of key trace gases that control the chemical reactivity of the troposphere. This can increase both production and destruction of ozone and related oxidants such as hydrogen peroxide, which are known to have adverse effects on human health, terrestrial plants and outdoor materials.

Ozone Depletion Counter Measures
International cooperation and agreement was signed at Montreal Protocol in 1974 to phase out ozone
depleting chemicals. The ozone depletion counter measures include,
¢ Tax imposed on use of ozone depleting substances
¢ Use of ozone friendly substitutes- HCFC and HFC (less ozone depleting potential and shorter life)
¢ Recycle of CFCs and Halons

Global Warming and Climatic Change
The atmosphere is a thin layer of gas which surrounds the Earth. The two most important layers in the atmosphere are known as the troposphere and the stratosphere. The air layer gets thinner and thinner with altitude. 90% of all the molecules in the atmosphere are in the troposphere. The atmosphere is composed mainly of 21% Oxygen, 78% Nitrogen, 0.04% carbon dioxide, and Argon 0.04% by volume. In addition, water vapour and several gases are present in very small amounts.

The Greenhouse Effect
The earth is surrounded by a blanket of gases including greenhouse gases. The greenhouse gases are those gases in the atmosphere which by absorbing thermal radiation emitted by the earth’s surface have a blanketing effect over the surface keeping it warmer than it would otherwise be. This results in build up of energy, and the overall warming of the atmosphere. This blanket traps energy in the atmosphere, much the same way as glass traps heat inside a greenhouse. Without naturally occurring greenhouse gases such as water vapour, carbon dioxide, methane and nitrous oxide, the earth’s average surface temperature would be a cold -18°C rather than the tolerable 15°C. This warming of the earth called the greenhouse effect (Figure 10.6) is a natural process which made life on Earth possible.
The Earth’s atmosphere allows short-wave solar radiation from sun to pass relatively unimpeded. The long-wave infrared radiation emitted from the warm earth’s surface is partially trapped and re-emitted downwards by greenhouse gases such as water vapour, carbon dioxide, methane, Nitrous oxide, in the upper atmosphere. In this way an energy balance is set up, which ensures that the Earth is warmer than it would be without it.
Enhanced Greenhouse Effect
The natural greenhouse effect is enhanced (Figure 10.6) by the increase of greenhouse gases in the atmosphere especially carbon dioxide from burning of fossil fuels, coal, oil and gas, together with wide deforestation over the past 200 years and more substantially over the past 50 years.
Although, water vapour is also considered as greenhouse gas, its amount in the atmosphere is not changing directly because of human activities. The other important greenhouse gases that are directly influenced by human activities leading to enhanced greenhouse effect are carbon dioxide, methane, nitrous oxide, the chlorofluorocarbons (CFCs) and ozone. There is now overwhelming evidence that
enhanced greenhouse effect from human activities is changing the global climate. It is estimated that the earth’s average temperature has risen by 0.75°C since 1880 because of emissions of greenhouse gases from human activity. The relation between CO, and global temperature variations is shown in Figure 10.7.
Greenhouse Gases
Carbon Dioxide: Carbon dioxide is the most important of the greenhouse gases because of its abundance in the atmosphere. The increase in carbon dioxide has contributed to about 60% of the enhanced greenhouse effect as its concentration of 397 ppm (Mauna Loa Observatory: November, 2014 data) is much higher than other greenhouse gases. It is also persistent with atmospheric lifetime of over 100 years.

Man-made Carbon Dioxide Emissions: The major source of CO, is fossil-fuel combustion (coal, petroleum, and natural gas). For the same amount of heat released, natural gas emits the least CO2. Coal-based power plants are the major CO, sources in many countries in the world. Among the industrial processes, cement is a major contributor of CO, as emissions occur from both fuel combustion and calcination of limestone.
Petroleum-burning motor vehicles are another major contributor of CO, emissions. Deforestation contributes too because when felled trees are burned, their stored carbon is released as CO2. At the same time, deforestation leaves fewer trees to take up atmospheric CO2.

Carbon Sequestration: It is the term given to the process of removing CO2 from large point sources
such as power plant, oil refineries, industrial process etc. The CO2 is then stored in geologic formations such as depleted oil and gas reservoirs, deep coal seams or saline reservoirs. Oceans are a major CO2 sink, containing about 50 times more carbon than the atmosphere. Terrestrial biomass including trees and grasses store about three times more Co2 than the atmosphere. Together, ocean and terrestrial ecosystems absorb about half the excess CO2 generated by human activities.

Methane: The main natural source of methane is from wetlands. Methane is also created when organic matter such as food and vegetables decompose without presence of oxygen- a process called anaerobic decomposition.

Anthropogenic sources include leakage during coal mining, leakage from natural gas pipelines and from petroleum wells, rice cultivation, belching from cattle and other livestock, decay of municipal solid wastes dumped in landfill sites and from wood burning.

Methane is a naturally occurring inflammable gas. Methane is produced by geological coal formations and by the decomposition of organic matter. Leading anthropogenic sources of methane are landfills, livestock digestive processes and wastes, especially ruminants (cud-chewing animals) and wetland rice cultivation.

Nitrous Oxide: The emissions to the atmosphere that are associated with human activities are from use of nitrogen fertilizer, manure, biomass combustion, fossil fuel combustion in power plant and the chemical industry (for example. nylon production). Also, N,O is contained in soil by bacteria. When farmers plow the soil and disturb the surface layer, N,O is released into the atmosphere. It is also released from catalytic converters in cars. It has an atmospheric lifetime of about 120 years.

Ozone: Ground-level ozone is a greenhouse gas. It can absorb infrared radiation and contribute to warming. Ground-level ozone forms from Volatile Organic Compounds (VOCs) and nitrogen oxides in the presence of heat and the sun’s ultraviolet radiation.

Chlorofluorocarbons (CFCs): The CFCs are man-made chemicals which vaporise just below room temperature and are non-toxic and non-flammable. CFC contains chlorine atoms and has been used in industry as refrigerants, cleaning solvents, manufacturing of insulation and propellants in spray cans.

They are so chemically unreactive and once released into the atmosphere, they remain for a long time of about 100 or 200 years before being destroyed.

As an outcome of Montreal Protocol, CFCs are phased out, being replaced by other halocarbonshydrochlorofluorocarbons (HCFCs) and hydrofluorocarbons (HFCs). While HCFC and HFC are less destructive to ozone than the CFCs, they are still considered as greenhouse gases.

Because of their shorter lifetime, and lower concentrations, their contribution to global warming for a given rate of emission, will be less than for the CFCs. However, since their rate of manufacture could increase substantially their potential contribution to global warming is being included alongside other greenhouse gases.

The main sources of Hydroflurocarbons are leakage from refrigeration equipment, release during end of life destruction of equipment, use of HFC containing aerosols, air conditioners etc. These are best contained by recycling the refrigerants.

Perflurocarbons: Perfluorcarbons is also considered as an important greenhouse gas as it has a long atmospheric life, more than several thousand years. All emissions of these gases accumulate in the atmosphere and will continue to influence climate for thousands of years.

Primary aluminum production and semiconductor manufacture are the largest known man-made sources of perfluorocarbons.

Sulphur Hexafluoride (SF): Sulfur hexafluoride is the most potent greenhouse gas. It is used in insulation, electric power transmission equipment, the magnesium industry, semiconductor manufacturing to create circuitry patterns on silicon wafers, and as a tracer gas for leak detection.

Global Warming Potential (GWP)

The different types of greenhouse gases all have different properties. For example, the amount of time they reside in the atmosphere and the amount of heat that they trap can vary widely. Many of the greenhouse gases are extremely potent—some greenhouse gases such as sulphur hexafluoride can continue to reside in the atmosphere for thousands of years after they have been emitted.

Some greenhouse gases are 140 to 23,900 times more potent than CO, in terms of their ability to trap and hold heat in the atmosphere over a 100-year period. Even though these gases represent a very small proportion of the atmosphere, their enormous heat-holding potential makes them significant and represents a serious addition to global warming.

In order to understand specific greenhouse gases’ potential impact, they are rated on the basis of their global warming potential (GWP). The GWP of a greenhouse gas is the ratio of global warming—or radiative forcing—from one unit mass of a greenhouse gas to that of one unit mass of CO, over a period of time, making the GWP a measure of the “potential for global warming per unit mass relative to carbon dioxide.” In other words, greenhouse gases are rated on how potent they are compared to CO2

GWPs take into account the absorption strength of a molecule and its atmospheric lifetime. Therefore, if methane has a GWP of 23 and carbon has a GWP of | (the standard), this means that methane is 23 times more powerful than CO, as a greenhouse gas. The higher the GWP value, the larger the infrared absorption and the longer the atmospheric lifetime. As shown in Table10.1, even small amounts of sulfur hexafluoride and HFC-23 can contribute a significant amount to global warming. The increasing concentration of greenhouse gases, GWP and lifetime is given in Table 10.1.

Global Greenhouse Gas Emissions
Since the Industrial Revolution, annual CO, emissions from fuel combustion dramatically increased from near zero to almost 36 Giga tonnes of CO, in 2013. Among the many human activities that  roduce greenhouse gases, the use of energy represents by far the largest source of emissions.
Smaller shares correspond to agriculture, producing mainly CH, and N,O from domestic livestock and rice cultivation, and to industrial processes not related to energy, producing mainly fluorinated gases and N,O. Within the energy sector, CO, resulting from the oxidation of carbon in fuels during combustion dominates the total GHG emissions. CO, from fossil fuels & cement contributes almost 70% of global GHG emissions (Figure 10.8).

India’s Greenhouse Gas Emissions
India contributed to almost 7% of global emissions and is now third largest contributor in terms of
CO, emissions behind China and USA. Although, India’ emitted about 2.5 Giga tonnes of carbon
dioxide in 2013, the per capita emissions is still low at 1.6 tonnes per annum. Coal-based power
production, accounted for almost 70% of all of India’s coal-related CO, emissions.

Global Warming and Climatic Change Impacts
There is strong evidence now that most of the observed warming over the last 50 years is caused by human activities. Climate models predict that the global temperature will rise by about 6 °C by the year 2100. The major impacts of global warming are as follows:
Increasing Ocean Temperature and Rising Sea Levels During the twentieth century, observations show that the average sea level increased by about 20 cm.
The largest contribution to this rise is from thermal expansion of ocean water as the oceans warm the water expands and the sea level rises. A further increase in average sea level of 10 to 20 cm by 2030 and up to 1 m by 2100 is predicted. The coastal flooding will increasingly occur with rising sea level. People, who are already poor and overcrowded, may be forced from homes in low-lying countries such as Bangladesh. Even developed countries such as the Netherlands may lose land. Since half of the world populations live near the coastal zones, their vulnerability to rising sea levels are very high.

Snow and Ice Melting

Ice is already melting worldwide, especially at the earth’s poles. This includes mountain glaciers, ice sheets covering West Antarctica and Greenland, and Arctic sea ice. Snow and ice melting would also lead to rising sea levels. Also melting ice caps will disturb the ocean ecosystem. Fresh water from melting ice caps would desalinate the oceans and eco systems will be put out of balance and ocean currents which regulate the temperatures will be disturbed. Also cooling property of white ice caps which reflect heat back into space is lost further warming the earth.

Over the past 150 years, the majority of mountain glaciers monitored have been shrinking. Many glaciers at lower latitudes are now disappearing, and scientists predict that the majority of glaciers will be gone by the year 2100. As glaciers continue to shrink, summer water flows will drop sharply, disrupting an important source of water for irrigation and power in many areas that rely on mountain watersheds. Monitoring of Himalayan glaciers indicates that recession of some glaciers has occurred in some regions though not consistently across entire mountain chain.

Altered Rainfall Patterns

Rainfall patterns would be altered, with some areas getting more rainfall and others suffering more droughts. On warmer days, more water evaporates from soil and trees into the air leading to more clouds and rainfall. But moisture can also evaporate from dry soils, depriving them of already limited moisture.

A trend of increasing rainfall has been found along the west coast, northern Andhra Pradesh while decreasing monsoon rainfall trend has been observed over north-eastern India and some parts of Gujarat and Kerala.

Extreme Weather Events

Already, cyclones, storm, hurricanes are occurring more frequently and floods and draughts are more intense than before. This increase in extreme weather events are not considered as random events. Computer models predict this trend towards more powerful storms and hotter, longer dry periods. States of West Bengal, Gujarat and Kerala have reported increasing extreme weather trends.

More Severe Heat Waves

Heat waves and periods of unusually warm weather are already happening and are expected to increase with global warming. Already many cities in India are experiencing increasing heat waves due to global warming.

Temperatures that people from a hotter climate consider normal can be termed a heat wave in a cooler area if they are outside the normal pattern for that area. Severe heat waves have caused catastrophic crop failures, thousands of deaths from heat stroke, and widespread power blackouts due to increased use of air conditioners.

Loss of Biodiversity

Ecosystems will change - some species will move farther north or become more successful; others would not be able to move and could become extinct. Most of the world’s endangered species (some 25 per cent of mammals and 12 per cent of birds) may become extinct over the next few decades as warmer conditions alter the forests, wetlands, and rangelands they depend on, and human development blocks them from migrating elsewhere. The oceans, which are source of great biodiversity, would also be affected. For example the coral reefs, which have limited tolerance for warm waters would be severely affected.

Increased Diseases

Diseases currently restricted to existing hot regions may move into the newly warming regions. Malaria is one such disease, spread by mosquito vectors, infecting and killing millions each year in warm climates. As temperature increases in currently temperate regions, mosquitoes and other insects are expected to move in, spreading diseases as they go. In addition, indigenous disease organisms previously killed by winter cold will be better able to survive milder winters.

Dwindling Freshwater Supply

A higher sea level also means salty water can infiltrate fresh groundwater in coastal areas reducing the supply and also making it undrinkable. This is a major concern, since billions of people on earth  already lack access to freshwater. Higher ocean levels already are contaminating underground water sources in many parts of the world. Climate change is projected to decrease water availability in many aridand semi-arid regions. One third of the world’s population is now subject to water scarcity

Food Shortages

Food production needs to double to meet the needs of an additional 3 billion people in the next 30 years. Water resources will be affected as precipitation and evaporation patterns change around the world. This will affect agricultural output. Climate change 1s projected to decrease potential crop yields in the tropics and sub-tropics for almost any amount of warming. Food security is likely to be threatened and some regions are likely to experience food shortages and hunger.

International Agreements: United Nations Framework Convention on Climate Change (UNFCCC)

The United Nations Framework Convention on Climate Change (UNFCCC) was signed by over 160 countries at the United Nations Conference on Environment and Development held at Rio de Janeiro in June 1992 came into force from 1994.

It has set the agenda for action to slow and stabilize climate change. The signatories to the Convention recognized the reality of global warming and agreed that action to mitigate the effects of climate change needs to be taken and that developed countries should take the lead in this action.

The Convention mentions a short-term and one far-reaching objective. The short term objective aim is that developed countries should take action to return greenhouse gas emissions, in particular, those of carbon dioxide to their 1990 levels by the year 2000.

The long-term objective of the Convention is that the concentrations of greenhouse gases in the atmosphere should be stabilized ‘at a level which would prevent dangerous anthropogenic interference with the climate system’, the stabilisation to be achieved within a time-frame sufficient to allow ecosystems to adapt naturally to climate change to ensure that food production is not threatened and to enable economic development to proceed in a sustainable manner.

The Intergovernmental Panel on Climate Change (IPCC)
The IPCC, the Intergovernmental Panel on Climate Change, was formed in 1988 by the World Meteorological Organization and the United Nations to review climatic data and periodically report on their findings.
Scientists with the Intergovernmental Panel on Climate Change (IPCC) concluded in a 1995 report that the observed increase in global average temperature over the last century “is unlikely to be entirely natural in origin” and that the balance of evidence suggests that there is a “discernible human influence on global climate.” Several of their conclusions are summarized below:
¢ Atmospheric greenhouse gases continue to increase as a result of human activities.
¢ The fraction of warming due to carbon dioxide exceeds 50%.
¢ Decreases of about 10% in snow cover have occurred since the late 1960s.
¢ Reductions in the year’s duration of lake and river ice cover occurred in the twentieth century.
¢ Increases in the heat contained in the world’s oceans have occurred since the late 1950s
¢ Between 0.1 and 0.2 m rise in global average sea levels occurred in the twentieth century.
The panel projects that, if current trends continue, increases in atmospheric greenhouse gases in the
twenty-first century will result in an average global temperature increase between 1.4 and 5.8°C. About 75% of the warming is expected to be due specifically to carbon dioxide. They also project sea-level rises of another 0.1 to 0.9 m.
The 1995 IPCC report greatly altered the world’s view of climate change, and led to the 1997 Kyoto
Protocol, an international agreement among industrialized nations to modestly reduce emissions of greenhouse gases.

Conference of Parties (COP)
The COP is the “supreme body” of the Convention. The Parties to the United Nations Framework Convention on Climate Change (UNFCCC) meet annually in form of COP. The primary task is to promote and review the implementation of the Convention and any related legal instruments (such as the Kyoto Protocol, etc.). Countries that have joined the UNFCCC are referred to as “Parties to the Convention”. The meetings held between each COP are known as Intersessional meetings.

The landmark COP is COP 3 which resulted in Kyoto Protocol in 1997. The Kyoto Protocol includes legally binding emission targets for developed countries (Annex I Parties) for the six major greenhouse gases, which are to be reached by the period 2008-2012.

The Kyoto Protocol
The Kyoto Protocol is an international agreement linked to the United Nations Framework Convention on Climate Change.The major feature of the Kyoto Protocol is that it sets binding targets for 37 industrialized countries and the European community for reducing greenhouse gas (GHG) emissions. This amounts to an average of five per cent against 1990 levels over the five-year period 2008-2012.
Recognizing that developed countries are principally responsible for the current high levels of GHG
emissions in the atmosphere as a result of more than 150 years of industrial activity, the Protocol places a heavier responsibility on developed nations under the principle of “common but differentiated
responsibilities.”
The Kyoto Protocol entered into force on 2005 when Russia signed the protocol. All the participating countries have ratified the protocol other than United States. USA which contributes to almost 25% of global greenhouse gases has not yet ratified the protocol citing reasons that protocol has failed to include binding targets and timetables for developing countries such as China and India and that US economy would be seriously harmed.

Kyoto Protocol Reductions
Parties to the Kyoto Protocol wanted flexibility in how they could pursue reductions in greenhouse
gas emissions. They spent great amounts of time discussing flexibility mechanisms, ways by which a nation could take credit for reducing emissions. Flexibility mechanisms are intended to supplement not replace direct actions by a country or company such as conserving fossil fuel.

Targets
The targets cover emissions of the six main greenhouse gases, namely:
1.Carbon dioxide (CO2)
2.Methane (CH4)
3. Nitrous oxide (N2O)
4.Hydrofluorocarbons (HFCs)
5. Perfluorocarbons (PFCs)
6. Sulphur hexafluoride (SF6)
The maximum amount of emissions (measured as the equivalent in carbon dioxide, CO,e) that a Party
may emit over the commitment period in order to comply with its emissions target is known as a Party’s assigned amount. The individual targets for Annex I Parties as per Kyoto Protocol are listed in Table 10.2.

* The 15 States who were EU members in 1990 will redistribute their targets among themselves, taking advantage of a scheme under the Protocol known as a “bubble’’, whereby countries have different individual targets, but which combined make an overall target for that group of countries. The EU has already reached agreement on how its targets will be redistributed.
** Some EITs (Economies In Transition) have a baseline other than 1990.
*** The US has indicated its intention not to ratify the Kyoto Protocol.
The Kyoto Protocol Mechanisms
Parties with commitments under the Kyoto Protocol have accepted targets for limiting or reducing greenhouse gas emissions. These targets are expressed as levels of allowed emissions, or “‘assigned amounts,” over the 2008-2012 commitment periods.
Under the Treaty, countries must meet their targets mainly through national measures. The Kyoto Protocol also offers them an additional means of meeting their targets by way of three market-based mechanisms. The Kyoto mechanisms are:
¢ Emissions trading — also known as “the carbon trading”
¢ Clean development mechanism (CDM)
¢ Joint implementation (JI).
The mechanisms help stimulate green investment as well as help Parties meet their emission targets
economically.

Emission Trading

Emissions trading allow countries that have emission units to spare - emissions permitted to them but not “used” - to sell this excess capacity to countries that are over their targets. Emission trading is also known as carbon trading since carbon dioxide 1s the principal greenhouse gas. Carbon 1s now tracked and traded like any other commodity. This is known as the “carbon market.”

Clean Development Mechanism (CDM)

The Clean Development Mechanism (CDM) allows a country with an emission-reduction under the Kyoto Protocol to implement an emission-reduction project in developing countries. Such projects can earn saleable certified emission reduction (CER) credits, each equivalent to one tonne of CO2 which can be counted towards meeting Kyoto Protocol targets. The mechanism results in sustainable development and emission reductions, while giving industrialized countries some flexibility in how they meet their emission reduction or limitation targets. The major CDM projects have been from renewable energy followed by waste handling and disposals.

Joint Implementation (JI)

The mechanism known as “joint implementation,” allows a country with an emission reduction under the Kyoto Protocol to earn emission reduction units (ERUs) from an emission-reduction or emission removal project in another Annex I country, each equivalent to one tonne of CO2, which can be counted towards meeting its Kyoto target. A JI project must provide a reduction in emissions by sources, or an enhancement of removals by sinks, that is additional to what would otherwise have occurred. Joint implementation offers Parties a flexible and economic means of fulfilling a part of their Kyoto commitments, while the host Party benefits from foreign investment and technology transfer.

The difference between JI-projects and CDM-projects is that JI-projects are done between countries that both have commitments, while the CDM-projects is between one country that has commitments and another country that does not have commitments. Emissions reductions that have been done through CDM-projects during the period 2000 to 2007 can be used for fulfilling commitments in Annex I countries for the period 2008-2012.

CDM Methodology and Procedure

Project Cycle for CDM

The various stages of the project cycle for CDM are shown in Figure 10.9. Of these, last three stages are performed throughout the life cycle of the project. Project Preparation: The first step in the CDM project cycle is the identification and formulation of potential CDM Projects. This can be done by comparing potential projects against the list of already approved methodologies available with UNFCCC. This step establishes that the CDM project is real, measurable and additional.


Potential CDM projects include,

Zero emission renewables — grid-connected electricity generation for renewable sources.

Biomass — grid-connected electricity from biomass.

Waste — landfill gas project activities.

Animal waste — change of animal waste management activities.

Cement — increasing the blend in cement production.

Energy efficiency

Small scale CDM projects include type | (renewable energy), type II (energy efficiency

improvements), and type III (other projects)

The CDM project developer is advised to carry out a technical and economic feasibility study of the project. This is not a requirement for the CDM project application, but it helps to prove the additionality of the project and gives clear information of Return on Investment with and without CDM. Depending on what the feasibility study covers, it can also facilitate the preparation of the Project Idea Note and the Project Design Document.

Development of Project Idea Note (PIN): If the results of the pre-screen and feasibility study are positive, the developer and/or their advisors should develop a Project Idea Note, or PIN. Although a PIN is not required for CDM application, it helps to inform the Designated National Authority (DNA) of the host country about the project and obtain feedback about the country’s specific sustainability requirements. The PIN also can be used to get feedback from potential carbon credit buyers in the marketplace about their level of interest, prior to going through the entire CDM process. The PIN will subsequently be screened by the recipient entities against the CDM rules and their investment criteria.

PIN consists of approximately five pages providing indicative information on:
¢ Type and size of the project;
¢ Location of the project;
¢ Anticipated total amount of GHG reduction compared to the “business-as-usual’ scenario (which will be explored further in the Project Design Document);
¢ Suggested crediting life time;
¢ Suggested CER price (in US$/tCO, equivalent reduced)
¢ Financial structuring (indicating which parties are expected to finance the project; and
¢ Project’s other socio-economic or environmental effects/ benefits.

Development of Project Design Document: The PDD is the key document in the CDM cycle. The PDD is mandatory and is submitted to a Designated Operational Entity (DOE) for validation, and subsequently to the CDM Executive Board for registration before CERs are issued.
The baseline methodology and the baseline scenario are essential elements of PDD as these are used to calculate the amount of CER’s that are generated by the project. The baseline methodology outlines how baseline emissions are determined and baseline scenario determines the actual emissions before project implementation. Project proponents can either use an existing methodology to calculate the baseline for this kind of projects or choose to develop a new methodology.
Another central issue in CDM projects is from when, and for how long, the project will generate CER (also known as the crediting period). For almost all CDM projects, carbon credits are counted from the date that the project starts, and resulting in GHG emission reduction. For some rare CDM projects where CDM project had already started and been registered only afterwards, carbon credits are counted only from the date of registration as a CDM project.
The second question is for how long the project will be considered to generate CER. In principle this is for as long as the project fulfills the CDM requirements (and most importantly among these, that there are no new and more attractive technologies or projects that could replace the project on commercial grounds and generate even less GHG). This could become a very complicated issue to prove, and to make things easier, projects can either be valid for one period of ten years only, or for up to three periods of seven years each, but with revalidation of the project every seventh year.
The completed PDD along with the required reports has to be submitted to the DNA in the host country for approval. Host country approval of CDM projects is essential to ensure that governments retain sovereignty over their natural resources and their ability to mitigate emissions. The DNA’s responsibility is to review and approve the proposed project under CDM and to confirm whether the project meets the host country’s sustainable development criteria.
Host Country Approval: The National CDM Authority in the non-Annex I nation evaluates and approves the project and serves as a point of contact. Together with the investor, the host country developer must prepare a Project Design Document (PDD). National CDM Authority in India is Ministry of Environment & Forest (MoE&F)

Validation / Registration of Project: The PDD and host country approval documents are submitted to
an accredited DOE for review and validation. The DOE initiates the validation process by making PDD publicly available for comments by parties, stakeholders and UNFCCC accredited observers for 30 days. After 30 days, DOE prepares a report with verbal and written comments explaining how the
comments have been responded. Subsequently, the DOE undertakes a validation process of the CDM
project.
¢ This involves evaluating the PDD and associated documents against the requirements for CDM to confirm that all the information and assumptions made are accurate and reasonable.
¢ Validation occurs at the outset of a project and is distinct from verification, which occurs during the operation of the project.
Finally, the DOE submits the PDD, host country approval, and validation report to the CDM-Executive
Board for registration of the project. It is recommended that the project developer requests the DOE for a copy or confirmation of the request for registration.
Registration of the project with the CDM Executive Board is the act of formal acceptance of the validated project. The registration of the project with the Executive Board will be final after a aximum
of eight weeks after submission, unless the CDM EB decides to request a review.
Once the project has been registered, it can be implemented. However, since CERs can also accrue from the point of validation, certain projects are implemented prior to registration.
Project Implementation and Monitoring: Carbon funds are available through
¢ International tenders for CDM projects
¢ Voluntary corporate initiatives
¢ Multilateral Funds
¢ EU commitments for carbon purchase
¢ Bilateral negotiations with the consortium of buyers
The public funding for CDM projects must not result in the diversion of funds for official development
assistance (ODA). The CERs generated by CDM projects will be subject to 2% levy, to help particularly
vulnerable developing countries adapt to the adverse effects of climate change. Once the project is operational, the project participants have to monitor the project’s performance according to the procedures laid out in the validated monitoring plan of the PDD. Monitoring report is prepared including an estimate of CERs generated.
Monitoring is not a one time activity. It is continued for the entire duration of crediting period (7 years x 3 or 10 years). At the very minimum, technical project performance has to be monitored, including project output and related GHG emissions, environmental impact and leakage. The leakages are  indirect emissions increases or decrease outside the defined the project boundaries such as changed consumer behaviour or reduced transport.

Verification: Verification is the periodic review and ex-post determination of the monitored GHG emission reductions that have occurred as a result of the CDM project.The DOE verifies that the datacollectedby the developer are accurate and complete and have been collected in accordance with the monitoring plan. Verified GHG emission reductions from the CDM project form the basis for CERs. CERs are based on actual reductions during the specific time period for which the monitoring results are provided,which is usually one year.
An operational entity will verify that the CERs have resulted according to the guidelines and conditions agreed upon during the initial validation of the project. Subsequently, verification is carried out on an annual basis through the selected DOE. Refer Figure 10.10.

Certification and Issuance of CER: The operational entity provides a certification report that gives written assurance that a project achieved the reduction as verified. Unless a project participant or three Executive Board members request a review within 15 days, the CERs are issued.
However, current demand for CERs is low. A number of Annex I countries are not participating in the Kyoto Protocol or its second commitment period. In addition, approximately two-thirds of the present quantitative limit set by the European Union Emissions Trading System for the use of emission reduction units (ERUs) and CERs has already been used. Therefore currently confirmed demand is not nearly sufficient to accommodate the current supply capacities of the mechanism.
Requests for issuance have also declined though less significantly, primarily because the marginal cost of requesting issuance is relatively low in comparison with the costs of developing, implementing, and registering a project. Nevertheless, rates of issuance requests are well below the peak levels of 2011 and 2012 and may be expected to remain low in light of the current demand levels.

European Union’s Efforts to Combat Climate Change
The 2020 Climate and Energy Package (EU)
The climate and energy package is a set of binding legislation which aims to ensure the European Union meets its ambitious climate and energy targets for 2020.
These targets, known as the “20-20-20” targets, set three key objectives for 2020:
¢ A 20% reduction in EU greenhouse gas emissions from 1990 levels;
¢ Raising the share of EU energy consumption produced from renewable resources to 20%;
¢ A 20% improvement in the EU’s energy efficiency.
The 20-20-20 targets represent an integrated approach to climate and energy policy that aims to  combat climate change, increase the EU’s energy security and strengthen its competitiveness. These targets were set by EU leaders in March 2007, when they committed Europe to become a highly energyefficient, low carbon economy, and were enacted through the climate and energy package in 2009.

The EU Emissions Trading System (EU ETS)
The EU emissions trading system (EU ETS) is a policy tool evolved by European Union to combat climatic change by reducing industrial greenhouse gas emissions cost-effectively. The EU ETS covers more than 11,000 power stations and industrial plants in 31 countries, as well as airlines.

A ‘Cap and Trade’ System
The EU ETS works on the ‘cap and trade’ principle. A ‘cap’, or limit, is set on the total amount of certain greenhouse gases that can be emitted by the factories, power plants and other installations in the system. The cap is reduced over time so that total emissions fall.
Within the cap, companies receive or buy emission allowances which they can trade with one another as needed. They can also buy limited amounts of international credits from emission-saving projects around the world. The limit on the total number of allowances available ensures that they have a value.
After each year a company must surrender enough allowances to cover all its emissions, otherwise heavy fines are imposed. If a company reduces its emissions, it can keep the spare allowances to cover its future needs or else sell them to another company that is short of allowances. The flexibility that trading brings ensures that emissions are cut where it costs least to do so.
In 2020, emissions from sectors covered by the EU ETS will be 21% lower than in 2005. By 2030,
the Commission proposes, they would be 43% lower.

Sustainable Development
According to the Bruntland Commission Report “Our Common Future” presented in 1987, sustainable development is ‘meeting the needs of the present without compromising the ability of future  enerations to meet their own needs’.
A more detailed definition:
“Sustainable development means living on the Earth’s income rather than eroding its capital’ and ‘keeping the consumption of renewable natural resources within the limits of their replenishment’ It recognizes the intrinsic value of the natural world explaining that sustainable development ‘means handing down to successive generations’ not only manmade wealth (such as buildings, roads and railways) but also natural wealth, such as clean and adequate water supplies, good arable land, a wealth of wildlife and ample forests’.
Sustainable development encompasses three basic and inter-related objectives:
¢ Economic security and prosperity
¢ Social development and advancement
¢ Environmental sustainability
Sustainable development demands that we seek ways of living, working and being that enable all people of the world to lead healthy, fulfilling, and economically secure lives without destroying the environment and without endangering the future welfare of people and the planet.
Sustainable development as applied to energy and environment should consider the following:
 ¢ Inputs - such as fuels and energy sources, land and raw materials - are non-renewable they should be used up only as far as they can be substituted in future
¢ Where they are renewable they should be used up at a rate within which they can be renewed,
¢ Outputs - in production and consumption - should not overstrain ecosystems or the assimilation capacity of the ecosphere.



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Chapter 11

Followers