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    SCHOOL OF

    COMPUTING&

    ELECTRICAL

    ENGINEERING

    1

    BAHIR DAR UNIVERSITY(IOT)

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    Group Members2

    Addisu Feyissa.079/2001

    Alem Hailu...117/2001

    Andinet Fikadu.168/2001Birhanu Girma..315/2001

    Biruk Teshome..326/2001Delelegn Zeleke377/2001

    Desalegn Gibtsu395/2001

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    Contents3

    Introduction

    Formation of Fossil Fuels

    Types of Fossil FuelsFossil Fuels in Ethiopia

    Use of Fossil fuels

    Problems in using Fossil FuelsConclussion

    i l

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    Energy Conversion & RuralElectrification

    4

    Project 1

    Servay of National

    Fossil Fuels

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    1. Introduction5

    Our World has so many energy sourses. e.g energyfrom the sun,wind and falling water.

    We can also get energy from materials which arefound under ground that contain stored energy.

    These stored energy sourses are known as FossilFuels (it took million of years for fossil fuels tocome to be).

    Becouse of so long time to be formed again, most

    geologists feel that little or no new fossil fuel isbeing produced.

    For this reason, we call fossil fuels "are

    nonrenewable" energy sources.

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    Contd6

    By digging out the deposited energy sources andburn them, we can get useful energy.

    Electric power generation has to be applied on Fossil

    Fuels before any use. Fossil fuels are the dominant sources of primary

    energy in the world economy.

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    2. Formation of Fossil Fuels7 Fossil fuels are found deposited in rock formations.

    They were formed between 350 million and 650million years ago.

    The processes by which they formed are not totallyunderstood.

    Decayed remains of ancient plants and/or animalswere buried by sediments.

    Through the action of heat and pressure over millionsof centuries, they were chemically changed.

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    Contd8

    These sediments exerted pressure one on the otherfor thousands of years:-results heat.

    Through the action of heat and pressure over

    millions of centuries, they were chemically changed:-chemical reaction takes place.

    Decayed remains of ancient plants or animals wereburied (covered) by sediments and form layers as

    they sank under the water of swamps.

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    3.Types of Fossil fuels9

    Because of they have been formed from theorganic remains of prehistoric plants and

    animals, this implies that fossil fuels areindirect form of chemically stored energy.

    The main constituents of fossil fuels are

    1. Crude Oil2. Natural gas

    3. Coal

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    Crude Oil10

    Oil is found in beds of sedimentary rocks.

    It is account for the largest share in theworlds primary energy.

    There are so many consumers of oil.

    Among them the transport sector will beincreasingly important as a consumer of

    oil. The share of final energy consumption of

    oil is rising from 47% in 2002 to 54% by2030 according to world energy out look.

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    contd11

    In the developing economies, the demand for oil will risenot only because of transport, but also the following needs.

    consumption in the industrial

    residential

    services sectors The growth of oil supply is 77 million barrels per day in

    2000 to 121.3 million barrels per day in 2030 (IEA 2004).

    Volatility in oil prices can be occasioned by the impact ofsevere weather conditions on offshore supplies, industrialstrife impacting on short-term supplies, the threat ofterrorist strikes against oil infrastructure, and politicaluncertainties in producing regions like the Middle East,Russia, Central Asia, Venezuela and Africa

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    Natural gas12

    Natural gas is composed primarily of methane (CH4). Itdoes contain other chemical species, such as butaneand propane.

    It has much to offer as an energy source that makes itpreferable to other forms of fossil fuels.

    It burns much cleaner than coal or oil, and it producesless carbon dioxide for each unit of energy.

    Initially, it was used for lighting in homes andbuildings.

    The increased production of electricity to day led to adecline in this usage, although there became a growingdemand for its use to heat homes, water and cook.

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    Contd13

    Its simple chemical nature makes it a much bettersource to use in high efficiency fuel cells thaneither coal or gas

    As a usable energy source, natural gas really has

    only one stumbling block, but it is a major one.

    it is hard to transport and store.

    If the transport or storage system is not completely

    sealed, natural gas will leak. These problems have kept natural gas from

    widespread usage throughout history, even thoughits existence has been known about for a long time.

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    Coal14

    Coal resources are vast and widely distributedaround the world.

    . This gives coal a major advantage, from an energy-

    security perspective, over other fuels. . However, only some of these resources are

    economically recoverable using current technology.

    Nonetheless, using estimates of proven coal

    reserves (coal that is both technologically andeconomically recoverable), todays worldreserve base represents more than 200 yearsof current production.

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    Contd15 The outlook for coal production and supply costs is

    subject to less uncertainty than are those for oil andgas.

    Continued productivity gains should result in some

    further cost reductions. While coal plants have relatively high capital costs, fuel

    costs are low relative to natural gas and coal plants willremain highly cost-competitive in the most efficient

    coal producing regions of the advanced economies. The biggest uncertainty for the coal industry concerns

    demand, which in turn is heavily dependent on howcoal-combustion technologies develop in response to

    environmental worries.

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    3.Fossil Fuels in Ethiopia16

    Energy is needed as an input in industry, agriculture,mining, construction and service-givingorganization.

    Ethiopia is one of the countries that depend uponimported petroleum products.

    The yearly import of petroleum products isabsorbing more than one third of Ethiopias annual

    exporting products. The need of domestic fuel in the country is the major

    factor for deforestation and soil degradation.

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    Contd17 Inter-Trappean coal and oil shale deposits are distributed on

    the South-Western and Central Plateau of Ethiopia:-

    1. Delbi-Moye

    2. Yayu

    3. Lalo-Sapo4. Sola and Chida

    5. Chilga,

    6. Nejo,

    7. Mush Valley The intra-cratonic Ogaden Basin (Eastern Ethiopia) and Blue

    Nile Basin (Central Ethiopia) covers an area of 350,000 kmand 120,000 km2, respectively.

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    18

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    Delbi-Moye Basin19

    Delbi is found 390 km west of Addis Ababa, and 48km south of Jimma.

    The basin is located between 2060 and 2240 meters

    above sea level. A total of 25 boreholes were drilled in the Delbi-

    Moye Basin.

    It consists of the lower basalt, lower

    sedimentary formation, middle basalt, uppersedimentary formation, upper basalt andacidic to intermediate volcanics.

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    Yayu20

    Yayu is 564 km from Addis Ababa along Jimma-Bedle Gambella road or 500 km along Nekemte-Bedle-Gambella road.

    The basin is found between 1300 and 1700 m abovesea level.

    A total of 100 boreholes were drilled in the YayuBasin.

    A total of 200,000,000 tones of coal depositsestimated in the Yayu Basin.

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    Chilga Basin21

    Chilga is located 52 km southwest of Gonder.

    The basin is found between 1900 and 2100 m abovesea level.

    12 boreholes were drilled in the central part of thebasin.

    The Chilga coal reserve is estimated to be 19, 700,000 tones.

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    Nejo basin

    22

    Nejo is located 190 km west of the town of Nekemte.

    The basin is found between 1700 and 1950 m abovesea level.

    The area consists of Precambrian basement rocks,Tertiary sediments and Tertiary volcanics.

    The total reserves coal in the Nejo area is estimatedto be 3 million tones

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    Mush valley23

    Mush Valley is situated 159 km northeast of AddisAbaba along Addis Ababa-Dessie road.

    The area is found between 2600-2800 m above sea

    level. The Inter-Trappean coal-bearing lacustrine

    sediments predominantly composed of sandstones,siltstones, carbonaceous shales and coal seams.

    Two coal seams are interbedded at different levels inthe coal-bearing sediments.

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    Wuchale area24

    Wuchale is 62 km from Dessie along Addis Ababa-Mekele road.

    The area is found between 2067 and 3560 m abovesea level.

    The total reserve is estimated to be 3.3 milliontones.

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    How to generate electricity25

    The chemical energy stored in solid fuel is used togenerate steam.

    This steam then drives turbine that drives agenerator to produce electricity.

    This process takes stored chemical energy to kineticto electrical energy. This is similar to the way that

    power can be harnessed using hydro-electric andwind turbines.

    Types of fossil fuel electricity generation facilities

    commonly found

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    Contd26

    i. steam cycle facilities (commonly used for largebase load facilities);

    ii. open cycle gas turbines (commonly used formoderate sized peaking facilities);

    iii. cogeneration and combined cycle facility (thecombination of gas turbines or internal

    combustion engines with heat recoverysystems); and

    iv. internal combustion engines (commonly used

    for small remote sites or stand-by (emergency)eneration .

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    5.Use of Fossil fuels

    27

    Coal is crushed to a fine dust and burnt.

    Oil and gas can be burnt directly

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    Coal-Fired Steam Cycle28

    The characteristics and composition of coal varymore than those for other fuels commonly used inelectricity production).

    Ash is also extracted from the bottom of the boiler(bottom ash).

    Ash is transported to ash dams as a slurry, densephase (paste), or dry. Fly ash from some power

    stations can be used as a resource, such as blendingwith cement.

    Ash is composed of modified coal mineral matter,i.e. primarily compounds of silicon, aluminum,

    iron, calcium, manganese, potassium, sodium and

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    Contd29

    The major emissions to air include carbon monoxide(CO), oxides of nitrogen (NOx), sulfur dioxide (SO2),emissions of metals (usually reported as metal &compounds for the NPI),organic compounds, carbondioxide (CO2) and water vapour.

    Carbon dioxide and water vapour are not NPIsubstances and are not reported to the NPI.

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    Gas and Oil-Fired Steam Cycle30

    A major difference between coal-fired facilities andgas or oil-fired facilities, is that gas and oil facilities

    burn the fuel with minimal on-site processing beforecombustion.

    Generally, they do not have control equipment tocollect particulate matter, as emissions of particulatematter are low for gas and generally low for oil.

    Emissions to air include carbon dioxide (CO2), watervapour, oxides of nitrogen (NOx), carbon monoxide(CO), minor emissions of metals and metalcompounds and organics, and sulfur dioxide (SO2)

    for oil firing.

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    Contd31

    Fig. over all flow diagram for a steamcycle facility

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    6.Disadvantages of Fossil Fuels

    32 Carbon Monoxide. Carbon monoxide (CO) is a

    product of incomplete combustion of any fuel. It is

    both a highly poisonous gas and the principalconstituent of photochemical smog

    Sulfur Oxides. Sulfur oxides arise duringcombustion from oxidation of sulfur in sulfurcontaining

    fuels (some coals and some petroleum-basedproducts). The principal product is sulfur dioxide:

    S (in fuel) + O2 SO2

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    Contd33

    Nitrogen Oxides. Nitrogen oxides have twosources.Fuel NOxis produced when nitrogen atomschemically combined with the molecules of the fuelare oxidized during the combustion process to form

    nitric oxide: 2 N (in fuel) + O2 2 NO

    Unburned Hydrocarbons. Unburnedhydrocarbons represent another source of air

    pollution associated with the use of fossil fuels(especially gasoline), even though they are not aresult of combustion.

    Greenhouse Effect

    social and economic effect

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    7.How to solve the problem

    34

    reduce capacity or close down the plant;

    reduce emissions by installing scrubbers orswitching to low-sulfur fuel;

    purchase emissions allowances from companies(electric power plants, primarily) that exceed their

    emission reduction goals.

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    8.Conclusion35

    The Ethiopian coal and oil shale deposits occur betweentwo volcanic flows. The coal and oil shale-bearingsedimentary basins in Ethiopia are one of the strikingexamples of an Inter-Trappean continental

    sedimentation. Proximate and calorific value analysis results revealed

    that the Ethiopian coal deposits range from lignite-bituminous coal.

    The coal measures of Ethiopia belong to tertiary andminor amounts of Mesozoic age. Various geochemicalstudies were carried out to determine the physico-chemical characteristics of the Ethiopian coal deposits.

    Oil and gas deposits possibly plays major role in the

    future energy budget of Ethiopia.

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    Contd36

    The coal and oil shale deposits of Ethiopia can beused for

    as a substitution firewood.

    production of oil and gas.

    to relieve the pressure on using wood as fuel forsmall-scale industries.

    gasification of lignite to produce chemicalfertilizers.

    the low-medium volatile bituminous coals of Moyearea used to produce coking coals for smelting of

    iron.

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    Recommendations37

    Extracting of Fossil fuels is very expensive, so thegovernment should invest funds on the extracting ofthese sources and open access for foreign investors.

    There should be educated power in the field studyingabout fossil fuels and other natural resources.

    The government should give special attention fornational resources because, The yearly import of

    petroleum products is absorbing more than one thirdof Ethiopias

    annual exporting products.