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Self Introduction. 
• Name: Muhammad Shozab Mehdi 
• Qualifications: 
– BSc. Chemical Engineering (2003), NFC Institute of Engineering 
and Technology (IET), Multan, Pakistan. 
– MS leading to PhD in Chemical Engineering (2013), Pakistan 
Institute of Engineering and Technology, Islamabad, Pakistan. 
– Research in Chemical Engineering Laboratory (LGC), Toulouse, 
France. 
• Research Interest: Hydrodynamics and Mass Transfer in 
Multiphase flows. 
• Office: FMSE-xxx, Ext: xxxx, Email: xxxxx@giki.edu.pk 
• Teaching Assistant: Mr. Jahanzaib Ahmad Ansari, Ext: 
xxxx, Email: xxxxxxxxxxxx@giki.edu.pk
CH 212: Fuel and Combustion 
Spring – 2014
Introduction 
Fuel: Anything which burn to 
give heat in presence of oxygen. 
Combustion: The process of 
burning fuel. 
• Burning is the intense 
chemical reaction with the 
emission of heat and other 
exhaust gases when fuel reacts 
with oxygen.
Introduction (contd.) 
• Where does the energy comes from the combustion reactions? 
• The energy stored in the chemical bonds that hold the carbon and 
hydrogen atoms together, releases when bonds are broken and 
atoms are rearranged. 
• How does this energy stored in fuel? 
• This energy stores in fuel by the process of photosynthesis which 
converts sunlight into chemical energy and storing it in the bond of 
sugar. Plants needs Carbon dioxide, Water and sunlight to make 
sugar. The overall reaction is: 
6CO2 + 6H2O + Sunlight -----> C6H12O6 + 6O2 
• These plants when became dead, buried under the soil, as more and 
more soil deposited over them for thousands of years, they became 
compressed and then under high temperature and pressure 
converted into fossil fuel.
Introduction (contd.)
Importance 
• Almost 70% of energy used in the world came 
from combustion sources.
Importance (contd.) 
• Heat for homes comes directly from combustion. 
• Electricity for homes generated by burning fossil fuel. 
• Our transportation system relies almost entirely on combustion. 
– Air craft are entirely powered by fuel burning. 
– Most trains are powered by diesel engine. 
– Most of the domestic vehicles use gasoline. 
• Industrial process rely heavily on combustion. 
– Iron, steel, aluminum and other metal refining industries employ 
furnaces for producing raw products. 
– Cement industry is the heavy user of heat energy delivered by 
combustion. 
– Other example of industrial combustion devices are boiler, refinery, 
glass melters and solid dryers etc.
Course Description 
• Various conventional and non-conventional fuels; their 
characterization and processing including refining, coal 
gasification and natural gas treatment. 
• Various aspect of combustion and related balances. 
• Fuel economy, burners classification and design. 
• Flame analysis and its various regimes and 
temperatures; Interface energy balances and heat 
distribution; oxygen diffusion and flame front; 
flammability limits and flame quenching. 
• Furnaces, boilers and engines (I.C & G.T). 
• Emission control (SOx & NOx).
Books (Text & Reference) 
• Flame and Combustion by J. F. Griffiths and J. 
A. Barnard, 3rd Ed. 1995 
• An Introduction to Combustion; Concept and 
Applications by Stephen R. Turns, 2nd Ed. 2000 
• Elements of Fuel, Furnaces and Refractories by 
O. P. Gupta 4th Ed. 1997
Before Mid 
Solid Fuel Liquid Fuel Gaseous Fuel 
•Introduction and 
•Origin and composition 
classification of fuels. 
of petroleum. 
•Fundamentals / 
•Classification of 
Definitions. 
petroleum and their 
•Solid fuel [Wood, 
characteristics. 
Charcoal, Peat]. 
•Constituents of 
•Origin of coal 
petroleum and their 
•Solid fuel [Lignite, 
uses. 
Bituminous coal, 
•Processing of crude oil 
Anthracite]. 
[Distillation, Cracking, 
•Constituents of coal. 
Reforming]. 
•Testing of coal. 
•Properties of 
•Carbonization of coal. 
petroleum products. 
•Methane from coal 
mines. 
•Wood gas. 
•Bio gas. 
•Gas from underground 
gasification of coal. 
•Natural gas. 
•Liquified petroleum 
gas. 
•Refinery gases. 
•Producer gas. 
•Water gas. 
•Blast furnace gas. 
•Coke oven gas. 
• Various aspect of combustion and related balances.
After Mid 
• Various aspect of combustion and related 
balances. 
• Fuel economy, burners classification and design. 
• Flame analysis and its various regimes and 
temperatures; Interface energy balances and heat 
distribution; oxygen diffusion and flame front; 
flammability limits and flame quenching. 
• Furnaces, boilers and engines (I.C & G.T). 
• Emission control (SOx & NOx).
Marks Distribution 
• Assignments (Nos?): ?% 
• Quizzes (Nos?): ?% 
• Midterm exam: ?% 
• Final Exam: ?% 
• Attendance: ?%
Classification of Fuels
General Classification of Fuels 
• Fossil fuels: 
Those which have been derived from fossil remains of plants and 
animal life and are found in crust of earth. For example coal, 
petroleum and natural gas etc. 
• By-product fuels: 
Those which are co-product of regular manufacturing process and 
of secondary in nature. For example coke oven gas from 
manufacturing of coke and blast furnace gas from making of iron. 
• Chemical fuels: 
Those which are of an toxic in nature and normally not used in 
conventional processes. For examples hydrazine, ammonium nitrate 
etc. 
• Nuclear fuels: 
Those which release heat by fission (uranium, plutonium etc.) or by 
fusion (deuterium, tritium etc.)
Classification based on Occurrence 
• Solid Fuels: 
Wood, charcoal, coal, coke etc. 
• Liquid Fuels: 
petroleum and its products (gasoline, 
kerosene, diesel, furnace oil, lubricating oil 
etc), Liquid fuel from coal liquefaction etc. 
• Gaseous Fuels: 
Natural gas, refinery gas, gas from coal 
gasification, wood gas, bio gas etc.
Classification based on Nature of Fuel 
• Primary Fuels: 
Those which occurred in nature i.e. wood, coal, natural gas and 
petroleum. 
• Secondary Fuels: 
Those which are derived from primary fuels e.g. fuel oil and 
kerosene derived from petroleum, coke oven gas derived from coal 
etc. 
Secondary fuels are further classified into: 
– Manufactured: 
Those which are manufactured for some specific purpose e.g. coke 
made for iron making, gasoline made for internal combustion engine, 
producer gas made for industrial heating etc. 
– By-Product: 
Those which are co-product of regular manufacturing process e.g. tar, 
refinery gas etc.
Fundamentals / Definitions
• Rank of Coal: It denote the maturity of coal. So peat the most 
immature coal has a lowest rank while the anthracite the most 
mature coal has highest rank. 
• Metamorphism of coal: The process of conversion of lignite to 
anthracite is called metamorphism of coal or coalification. 
• Carbonization of coal: Heating of coal in absence of air at high 
temperature to produce coke, tar and gases is called carbonization 
of coal. 
• Gasification of coal: Heating of coal in insufficiently less amount of 
air plus steam to produce a gas rich in CO and H2 is called 
gasification of coal. 
• Proximate analysis of coal: Finding out the weight percent of 
moisture, volatile matter, fixed carbon and ash content in coal. The 
analysis is useful in deciding the utilization for a particular purpose. 
• Ultimate analysis: Finding out the weight percent of carbon, 
hydrogen, nitrogen, oxygen and sulphur of pure coal free from 
moisture and inorganic constituents. The analysis is useful in 
designing of coal burning equipments.
• Calorific value: The quantity of heat liberated by combustion of unit 
quantity of fuel is called its calorific value. 
– Gross calorific value: Where the heat obtained from condensation of 
water vapours in the flue gases is also include. 
– Net calorific value: Where the heat obtained from condensation of 
water vapours in the flue gases is not include. 
• Flue gas: The gaseous product of combustion of a fuel. 
• Heat capacity: Amount of heat required to raise the unit weight of 
substance by one degree. 
• Specific heat: It is the ratio of heat capacity of a substance to the 
heat capacity of water (Cp > Cv). 
• Ignition temperature: It is the minimum temperature at which the 
fuel ignites. 
• Flash point: It is the minimum temperature at which the fuel give 
enough vapours which produces a momentary flash when exposes 
to flame. 
• Pour point: It is the minimum temperature at which fuel keeps its 
flowing nature when cooled under specific conditions.
Solid Fuel
Wood 
Domestic fuel used in tropical countries 
where forest are abundant and other 
fuels are not easily and cheaply 
available.
• Main combustible components: cellulose and 
lignin (compounds of carbon, hydrogen and 
oxygen) 
• Minor combustible components: resin and 
waxes. 
• Non combustible components: Water (25-50% in 
freshly cut and 10-15% in air dried) 
• Ash content: very low (<1%) but because oxygen 
content is very high (upto 45%) therefore its 
calorific value is very low. 
• Calorific value: 4000-5000 kcal/kg. 
• Density: 650 kg/m3.
Composition of Air-dried Wood 
Proximate Analysis 
• Cellulose: 50% 
• Lignin: 30% 
• Moisture: 15% 
• Water soluble: 2.5% 
• Resin & Wax: 2% 
• Ash: 0.5% 
Ultimate Analysis 
• Carbon: 50% 
• Hydrogen: 6% 
• Oxygen: 44%
Properties of wood 
• It is clean, readily ignites, burn with long clean 
flame in excess air and leaves only small 
amount of ash. 
• Wood is a solid fuel as dense as coal but to 
obtain same amount of heat as any given 
weight of coal can produce, you have to burnt 
wood, four times the weight of coal. 
• It is used to produce charcoal.
Charcoal 
Carbonization of wood at 600oC
Stages Involved in Carbonization of 
Wood 
Stage 1: At 100-120oC ---> moisture expelled results in 
moisture free wood. 
Stage 2: At 275oC ---> initial decomposition takes place 
results in formation of little distillate gas containing 
acetic acid and water. 
Stage 3: At 350oC ---> active distillation of wood takes 
place results in emission of liquid (acetic acid, methyl 
alcohol, tar etc) and gases (CO, CO2, N2, H2, CnHn). 
Stage 4: At 350-600oC ---> slow evolution of residual 
volatile matters from the wood charcoal left in 3rd 
stage.
Products of Carbonization of Wood 
• Charcoal: Solid product left after the 
carbonization of coal. 
• Hot gases: Cooled to separate 
– Wood gas 
– Liquid in two layer 
• Upper layer is Pyrolignious acid (mixture of acetic acid, 
acetone and water). 
• Lower layer is wood tar (fractionated to separate many 
chemicals).
Uses and Composition of Charcoal 
• Used for removal of obnoxious and coloring 
material from solution, gases, vapors and 
petroleum products by adsorption on its surface. 
• Used as a feed stock for gasification to make 
producer gas which is used as a fuel for domestic 
and industrial use. 
• Used as raw material for production of carbon 
sulfide. 
• Charcoal contains 80% carbon, 15% oxygen and 
nitrogen, 2% hydrogen and 3% ash.
Merits and Demerits 
• Because of porous in nature it has high 
specific surface area as compared to coal. 
• Ash content is very low. 
• Calorific value is high as compared to wood. 
• Mechanical strength is very poor.
Peat 
First stage in formation of coal from 
wood (cellulose) 
The most immatured coal
Formation of Peat 
• Peat is the first stage in the formation of coal 
from wood (cellulose). 
• It is not strictly a coal or else can be termed as 
the most immatured coal. 
• It is formed by gradual decaying (action of 
bacteria under high pressure and 
temperature) of remains of plants in moist 
places.
Properties of Peat 
• Peat is light brown in color. 
• Highly fibrous in nature. 
• With increase in depth the color becomes darker and 
fibrous structure disappeared. 
• Composition of peat varies from nature of plants, 
depth in deposit and age. 
• Freshly mined peat contains about 90% water and 10% 
solid. Therefore cannot be used unless air dried. 
• Calorific value is 650 kcal/kg for freshly mined peat and 
5000 kcal/kg for air dried peat.
Composition of Peat 
Proximate Analysis 
• Moisture: 20% 
• Volatile matter: 50% 
• Fixed carbon: 25% 
• Ash: 5% 
Ultimate Analysis 
• Carbon: 55% 
• Hydrogen: 6% 
• Oxygen: 33% 
• Nitrogen: 3% 
• Sulfur: 1%
Gasification of Peat 
• Peat is gasified in presence of steam and air to produce 
producer gas. 
• Steam requirement is very low because peat itself contain 
sufficient moisture. 
• Typical composition of gas is: 
• CO2 – 13% 
• CO – 18% 
• H2 – 11% 
• CH4 – 2.5% 
• N2 – 55.5% 
• Caloric value is 1000 kcal/kg 
• Gas yield is 2500 Nm3/ton of peat
Other non Fossil Domestic Fuel
Origin of coal 
• Coal is a complex mixture of plant substances altered in varying degree by 
physical and chemical processes. 
• These processes which changed plant substances into coal has taken 
million of years and has been accomplished by bacteria, heat and pressure 
inside the earth’s crust. 
• Two theories namely “in-situ” theory and “drift theory” have been 
suggested by geologists regarding mechanism of formation of coal from 
plant substances. 
• In situ theory: According to this theory, coal seam occupies the same site 
where the original plants grew and where their remains accumulated 
several million years ago to produce coal under the action of heat, 
pressure and bacteria. 
• Drift theory: According to this theory plants, tree etc were uprooted and 
drifted by rivers to lakes and deposited there to form coal during the 
course of time after they got buried underground. 
• Stages information of coal: plants/trees  peat  lignite  sub-bituminous 
coal  bituminous coal  anthracite coal  graphite.
• Points in favor of “in-situ” theory: 
– In the existing peat deposits; the decayed plant substances had 
accumulated at the place of origin. 
– Large quantity of fossil fuel have been found under the coal seam. 
– Composition of coal seam is generally constant over a wide area. If the 
original decaying plants and tree had been drifted from their original 
place then they would have a great variation in composition of coal. 
• Points in favor of “drift” theory: 
– In coal seam, the percentage of inclined trunks of fossil is much more 
than the vertical position. It the coal had been formed at the same 
place where the plants substances decayed then fossil trunks would 
have been vertical. 
– To form one meter thick coal seam, ten meter thick seam of peat is 
required, So for the formation of ten meter thick coal seam should 
have resulted from hundred meter thick seam of peat, which occur no 
where. 
– Seams of coal are made up of different layers separated by layers of 
clay or sandstone which vary in thickness from merely a film to several 
meters. As the plants accumulated under water some slits also settled 
along with them. Thus at later stage some mineral mater got mixed 
with coal as it formed.
• Stages for transformation of wood to coal: 
• The initial transformation of wood to coal is due to the action of 
bacteria (aerobic or anaerobic) causing degradation of organic 
matters (e.g. cellulose, lignin etc. present in wood) and removal 
of oxygen. 
• The bacterial action produced acidity which if accumulated 
prevented further action and coal formation could not proceed. 
• In some cases the soil was alkaline which neutralized the acidity 
and bacterial action continued to take place further degradation 
of organic matter. This explain why coal is found along with 
certain types of rocks. 
• Bacterial action takes place in initial stage breaks up organic 
matters into simpler molecules. 
• The degraded organic matters, as time passed, gave rise to peat. 
• Beyond this stage heat, pressure and time became the chief 
factors for further conversion of peat into different rank of coal.
Lignite 
• It is the second stage product in the formation of coal from wood. 
• It is friable and occurs in thick seams (up to 30 meter thick) near the 
surface of earth. 
• It moisture content is up to 60 % and calorific value is around 5000 
kcal/kg. 
• On exposes to air the brown color darkens and moisture content reduces 
to equilibrium value of 10 – 20 %. 
• On drying lignite shrinks and break up in irregular manner. 
• It is likely to ignite spontaneously as it adsorbs oxygen readily and must 
not be stored in open without care. 
• Composition and property of lignite varies widely. The carbon content is 
70 – 75 % and oxygen content is 20 – 25 %. 
• In large number of cases the ratio of volatile matter to fixed carbon is 1:1. 
• Raw Lignite is inferior fuel due to high moisture content, low calorific 
value, small size and bad weathering properties. 
• Lignite is of economic importance where it is readily available and other 
fuels do not occur in abundance.
Composition of Lignite 
Proximate Analysis 
• Moisture: 10 – 30 % 
• Volatile matter: 40 – 45 % 
• Fixed carbon: 30 – 35 % 
• Ash: 3.5 – 7.5 % 
Ultimate Analysis 
• Carbon: 70 – 73 % 
• Hydrogen: 4.6 – 5.5 % 
• Oxygen: 22 – 26 % 
• Nitrogen: 0.6 – 1.0 % 
• Sulfur: 0.6 – 1.5 %
Bituminous Coal 
• It is the most common variety of coal. 
• It is black and brittle which burns and ignites readily with 
yellow smoky flame. 
• It has low moisture content i.e. less than 10 % and carbon 
content varies from 75 – 90 % where as volatile matter 
content is 20 – 45 %. 
• Depending upon the volatile matter content, it is termed as 
low volatile, medium volatile and high volatile coal. 
• Its calorific value based on dry mineral free basis goes up to 
9000 kcal/kg. 
• It is used for power generation, coke making, gasification 
and domestic use.
Composition of Bituminous coal 
Proximate Analysis 
• Moisture: 3.5 – 8 % 
• Volatile matter: 16 – 36 % 
• Fixed carbon: 49 – 72 % 
• Ash: 7 – 8.5 % 
Ultimate Analysis 
• Carbon: 68.5 – 79.5 % 
• Hydrogen: 4.5 – 5.5 % 
• Oxygen: 4.5 – 16.5 % 
• Nitrogen: 1 – 1.4 % 
• Sulfur: 0.5 – 1 %
Anthracite coal 
• It is most matured coal hence of highest rank. 
• It is hard and burns without smoke with a short non-luminous 
flame. 
• It has high carbon content i.e. 85 – 95 % and low volatile matter 
content i.e. less than 10 %. 
• It ignite with difficulty due to low volatile matter content. 
• Its calorific value may be up to 8000 to 8500 kcal/kg which is less 
than bituminous coal de to its lower hydrogen and volatile matter 
content. 
• It has sub-metallic lustre and sometime even a graphitic 
appearance. 
• The chief use of anthracites are in boilers and metallurgical 
furnaces. 
• On calcining it gives thermo-anthracite which is a raw material for 
the production of carbon electrode.
Composition of Anthracite coal 
Proximate Analysis 
• Moisture: 2.5 – 3 % 
• Volatile matter: 3 – 8.5 % 
• Fixed carbon: 79 – 87.5 % 
• Ash: 7 – 9.5 % 
Ultimate Analysis 
• Carbon: 80 – 86.5 % 
• Hydrogen: 2.5 – 3.5 % 
• Oxygen: 3 – 4.5 % 
• Nitrogen: 0.5 – 1.5 % 
• Sulfur: 0.5 %
Significance of constituents of coal 
Proximate analysis 
• Moisture 
• Volatile matter 
• Fixed carbon 
• Ash 
Ultimate analysis 
• Carbon 
• Hydrogen 
• Nitrogen 
• Sulphur 
• Oxygen
Moisture 
• In general high moisture content in coal is undesirable because: 
– it reduces the caloric value of fuel 
– it increases the consumption of coal for heating purpose 
– it lengthens the time of heating 
– it increases the cost for purchase and transportation. 
• Owing to its nature, origin and occurrence, coal is always associated 
with moisture. 
• When coal is exposed to atmosphere its external moisture (free 
moisture) evaporates but apparently dry coal still contain some 
moisture (inherent moisture). 
• Air-dried moisture content of coal is determined by observing loss 
in weight of coal sample on heating at 105 degree centigrade. 
• Air-dried moisture of coal decreases with increasing rank from a 
value of 25% for lignite to a minimum value of 0.5% for low volatile 
bituminous coal.
Volatile matter 
• Certain gases like CO, CO2, CH4, H2, N2, O2, CXHY etc, are present in 
coal which comes out during its heating in absence of air. 
• These gases are called volatile matter of coal. 
• Coal with high volatile matter content: 
– Ignites easily i.e. it has low ignition temperature 
– Burns with long smoky yellow flame 
– Give more quantity of coke oven gas when it is heated in absence of 
air. 
• Volatile matter does not include moisture of coal but it contain 
moisture that is formed from oxygen and hydrogen of coal during 
the decomposition. 
• Volatile matter expressed as per cent on dry mineral matter free 
basis. 
• Higher the volatile matter, lower the fixed carbon.
Ash content 
• Ash is the combustion product of mineral matters presents in the 
coal. 
• It is comprises mainly of silica, alumina and ferric oxide with varying 
amount of other oxide such as calcium and magnesium. 
• High ash content in coal is undesirable in general. 
• A coal with high ash content is harder and stronger and has lower 
calorific value. 
• Ash content of coal is reduced by its washing. 
• Coal contains inorganic mineral substance which are converted into 
ash by chemical reaction during combustion. Ash and coal are 
therefore not the same. 
• The bulk of mineral matter of coal is due to clay or shale consisting 
of alumino-silicates of different composition. Other major 
constituents may be calcite and pyrites. 
• When coal burns these mineral matter decomposed resulting loss 
in weight hence the ash of coal is always less than the mineral 
matter content.
Fixed carbon 
• It is the pure carbon present in coal. 
• Higher the fixed carbon, higher will be the 
calorific value. 
• In anthracite where the value of volatile 
matter is very small, fixed carbon and total 
carbon are almost same. 
• In other coals, fixed carbon is always less then 
total carbon.
Total Carbon 
• Its mean fixed carbon plus the carbon present 
in the volatile matters. 
• Total carbon is always more than fixed carbon 
in any coal. 
• High total carbon coal will have high calorific 
value.
Hydrogen 
• It increases the calorific value of coal. It is 
associated with volatile matter of coal. 
• The content of coal from peat to bituminous 
varies between 4.5 and 6.5 and is not related 
to the rank of coal. 
• Beyond the bituminous stage the hydrogen 
content sharply decreases to a value of 1 – 2% 
in anthracite.
Nitrogen 
• Nitrogen in coal is present up to 1 – 3% and 
comes from the protein matter presents in plant. 
• Presence of inert nitrogen decreases the calorific 
value of coal. 
• However when coal is carbonized, its hydrogen 
and nitrogen combined thereby producing NH3 
which is recovered as (NH4)2SO4 (by reacting it 
with H2SO4) which is a valuable fertilizer. 
• Nitrogen content does not have any relation with 
rank of coal. 
• In most coal it is between 1 – 2%.
Sulphur 
• Though its presence increases the calorific value 
of coal but has several undesirable effects. 
• The oxidation product of sulphur i.e. SO2 in 
presence of moisture cause corrosion of the 
equipment and cause atmospheric pollution. 
• Sulphur is highly undesirable in metallurgical coal 
used for iron and steel making as it badly effect 
the properties of iron and steel. 
• The sulphur content of coal has no relation to its 
rank or composition.
Oxygen 
• Less the oxygen content better the coal as it 
reduces its calorific value. 
• It decreases from lignite to anthracite. 
• As the oxygen content of coal increases it 
moisture holding property increases. 
Phosphorus & Chlorine
Washing of coal 
• Most of the coal when mined contain impurities associated with it 
which must be removed before the coal is used. 
• These impurities are removed from coal by washing. 
• Coal contain two types of impurities. 
– Fixed or inherent impurities which are derived from coal forming 
plants and cannot be removed by washing. 
– Free impurities which are adhering to the surface of coal and 
comprise mainly of dirt and rock particles which can be removed by 
washing. 
• Washing of coal: 
– Reduces its ash content 
– Reduces its sulphur content 
– Increase its heating value 
– Improves its coking property
Principle of washing of coal 
• Specific gravity of pure coal varies from 1.2 to 1.7 
and that of free impurities from 1.7 to 4.9. 
• The coal can be separated by its impurities by 
utilizing difference in specific gravity. 
• If the average specific gravity of pure coal is 1.3 
and it is suspended in liquid of specific gravity 1.5 
then the impurities being heavier will sink in it 
whereas the pure coal will float. 
• Washing medium used in industrial coal washing 
is a slurry of sand and water or that of water and 
iron ore.
Properties and testing of coal 
• Determination of moisture content: A known amount of finely 
powdered coal sample is kept in a silica crucible and heated in a 
muffle furnace at 105 – 110 degree centigrade for one hour. The 
process of heating, cooling and weighing is repeated for number of 
times until the constant weight of anhydrous coal is achieved. 
• Determination of volatile matter: It is the loss in weight of 
moisture free powdered coal when heated in crucible fitted with 
cover in a muffle furnace at 950 degree centigrade for 7 minutes. 
• Determination of ash content: It is the weight of residue obtained 
after burning a weighed quantity of coal in an open crucible at 750 
degree centigrade in a muffle furnace until a constant weight is 
achieved. 
• Determination of fixed carbon: It is determined indirectly by 
deducting the sum total of moisture, volatile matter and ash 
percentage from 100
• Determination of carbon and hydrogen: 
– A known amount of coal is burnt in a current of dry oxygen 
thereby converting Carbon and hydrogen of coal into 
Carbon dioxide and water respectively. 
– The product of combustion are then passed over weighed 
tubes of anhydrous calcium chloride and potassium 
hydroxide, which absorb water and carbon dioxide 
respectively. 
– The increase in weight of calcium chloride tube represent 
the weight of water formed while increase in weight of 
potassium hydroxide tube represent the weight of carbon 
dioxide formed. 
– The percentage of carbon and hydrogen then can easily be 
calculated. 
• Determination of Nitrogen in coal: 
• Determination of Sulphur in coal:
• Determination of Calorific Value by bomb calorimeter: 
• Strong stainless 
steel vessel (25 – 30 
atm). 
• Provided with 
electrode, crucible, 
and oxygen inlet 
valve. 
• Bomb placed in 
copper calorimeter. 
• Calorimeter is 
surrounded by 
water and air jacket 
provided with 
electrical stirrer.
Carbonization of Coal 
Low temperature carbonization 
(LTC) 
• It carried out at 700 degree C. 
• It produces semi coke which is used as 
smokeless domestic fuel. 
• Yield of coke oven gas is less due to less 
cracking of hydrocarbons. 
• Yield of tar is high i.e. about 10% of dry 
coal. 
• Ammonia yield is low. 
• Calorific value of coke oven gas is high 
(6000 – 6500 kcal/kg) due to higher 
percentage of methane and 
unsaturated hydrocarbon in it. 
• The tar produce is aliphatic in nature. 
• Coke produced is weaker, bigger in size 
and more reactive. 
• Volatile matter content in coke is more. 
• Hydrogen content in coke oven gas is 
less i.e. 35 – 40%. 
High temperature carbonization 
(HTC) 
• It carried out at 1000 degree C. 
• It produces metallurgical coke for use in 
blast furnace. 
• Yield of coke oven gas is more due to 
more cracking of hydrocarbon. 
• Yield of tar is less i.e. about 3% of dry 
coal. 
• Ammonia yield is more. 
• Calorific value of coke oven gas is less 
(4200 – 4400 kcal/kg) due to lesser 
percentage of hydrocarbon resulting 
from cracking. 
• The tar produce is aromatic in nature. 
• Coke produced is stronger, smaller is 
size and less reactive. 
• Volatile matter content in coke is less. 
• Hydrogen content in coke oven gas is 
more i.e. 55 – 60%).

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Fuels and Combustion Lectures (GIKI)

  • 1. Self Introduction. • Name: Muhammad Shozab Mehdi • Qualifications: – BSc. Chemical Engineering (2003), NFC Institute of Engineering and Technology (IET), Multan, Pakistan. – MS leading to PhD in Chemical Engineering (2013), Pakistan Institute of Engineering and Technology, Islamabad, Pakistan. – Research in Chemical Engineering Laboratory (LGC), Toulouse, France. • Research Interest: Hydrodynamics and Mass Transfer in Multiphase flows. • Office: FMSE-xxx, Ext: xxxx, Email: xxxxx@giki.edu.pk • Teaching Assistant: Mr. Jahanzaib Ahmad Ansari, Ext: xxxx, Email: xxxxxxxxxxxx@giki.edu.pk
  • 2. CH 212: Fuel and Combustion Spring – 2014
  • 3. Introduction Fuel: Anything which burn to give heat in presence of oxygen. Combustion: The process of burning fuel. • Burning is the intense chemical reaction with the emission of heat and other exhaust gases when fuel reacts with oxygen.
  • 4. Introduction (contd.) • Where does the energy comes from the combustion reactions? • The energy stored in the chemical bonds that hold the carbon and hydrogen atoms together, releases when bonds are broken and atoms are rearranged. • How does this energy stored in fuel? • This energy stores in fuel by the process of photosynthesis which converts sunlight into chemical energy and storing it in the bond of sugar. Plants needs Carbon dioxide, Water and sunlight to make sugar. The overall reaction is: 6CO2 + 6H2O + Sunlight -----> C6H12O6 + 6O2 • These plants when became dead, buried under the soil, as more and more soil deposited over them for thousands of years, they became compressed and then under high temperature and pressure converted into fossil fuel.
  • 6. Importance • Almost 70% of energy used in the world came from combustion sources.
  • 7. Importance (contd.) • Heat for homes comes directly from combustion. • Electricity for homes generated by burning fossil fuel. • Our transportation system relies almost entirely on combustion. – Air craft are entirely powered by fuel burning. – Most trains are powered by diesel engine. – Most of the domestic vehicles use gasoline. • Industrial process rely heavily on combustion. – Iron, steel, aluminum and other metal refining industries employ furnaces for producing raw products. – Cement industry is the heavy user of heat energy delivered by combustion. – Other example of industrial combustion devices are boiler, refinery, glass melters and solid dryers etc.
  • 8. Course Description • Various conventional and non-conventional fuels; their characterization and processing including refining, coal gasification and natural gas treatment. • Various aspect of combustion and related balances. • Fuel economy, burners classification and design. • Flame analysis and its various regimes and temperatures; Interface energy balances and heat distribution; oxygen diffusion and flame front; flammability limits and flame quenching. • Furnaces, boilers and engines (I.C & G.T). • Emission control (SOx & NOx).
  • 9. Books (Text & Reference) • Flame and Combustion by J. F. Griffiths and J. A. Barnard, 3rd Ed. 1995 • An Introduction to Combustion; Concept and Applications by Stephen R. Turns, 2nd Ed. 2000 • Elements of Fuel, Furnaces and Refractories by O. P. Gupta 4th Ed. 1997
  • 10. Before Mid Solid Fuel Liquid Fuel Gaseous Fuel •Introduction and •Origin and composition classification of fuels. of petroleum. •Fundamentals / •Classification of Definitions. petroleum and their •Solid fuel [Wood, characteristics. Charcoal, Peat]. •Constituents of •Origin of coal petroleum and their •Solid fuel [Lignite, uses. Bituminous coal, •Processing of crude oil Anthracite]. [Distillation, Cracking, •Constituents of coal. Reforming]. •Testing of coal. •Properties of •Carbonization of coal. petroleum products. •Methane from coal mines. •Wood gas. •Bio gas. •Gas from underground gasification of coal. •Natural gas. •Liquified petroleum gas. •Refinery gases. •Producer gas. •Water gas. •Blast furnace gas. •Coke oven gas. • Various aspect of combustion and related balances.
  • 11. After Mid • Various aspect of combustion and related balances. • Fuel economy, burners classification and design. • Flame analysis and its various regimes and temperatures; Interface energy balances and heat distribution; oxygen diffusion and flame front; flammability limits and flame quenching. • Furnaces, boilers and engines (I.C & G.T). • Emission control (SOx & NOx).
  • 12. Marks Distribution • Assignments (Nos?): ?% • Quizzes (Nos?): ?% • Midterm exam: ?% • Final Exam: ?% • Attendance: ?%
  • 14. General Classification of Fuels • Fossil fuels: Those which have been derived from fossil remains of plants and animal life and are found in crust of earth. For example coal, petroleum and natural gas etc. • By-product fuels: Those which are co-product of regular manufacturing process and of secondary in nature. For example coke oven gas from manufacturing of coke and blast furnace gas from making of iron. • Chemical fuels: Those which are of an toxic in nature and normally not used in conventional processes. For examples hydrazine, ammonium nitrate etc. • Nuclear fuels: Those which release heat by fission (uranium, plutonium etc.) or by fusion (deuterium, tritium etc.)
  • 15. Classification based on Occurrence • Solid Fuels: Wood, charcoal, coal, coke etc. • Liquid Fuels: petroleum and its products (gasoline, kerosene, diesel, furnace oil, lubricating oil etc), Liquid fuel from coal liquefaction etc. • Gaseous Fuels: Natural gas, refinery gas, gas from coal gasification, wood gas, bio gas etc.
  • 16. Classification based on Nature of Fuel • Primary Fuels: Those which occurred in nature i.e. wood, coal, natural gas and petroleum. • Secondary Fuels: Those which are derived from primary fuels e.g. fuel oil and kerosene derived from petroleum, coke oven gas derived from coal etc. Secondary fuels are further classified into: – Manufactured: Those which are manufactured for some specific purpose e.g. coke made for iron making, gasoline made for internal combustion engine, producer gas made for industrial heating etc. – By-Product: Those which are co-product of regular manufacturing process e.g. tar, refinery gas etc.
  • 18. • Rank of Coal: It denote the maturity of coal. So peat the most immature coal has a lowest rank while the anthracite the most mature coal has highest rank. • Metamorphism of coal: The process of conversion of lignite to anthracite is called metamorphism of coal or coalification. • Carbonization of coal: Heating of coal in absence of air at high temperature to produce coke, tar and gases is called carbonization of coal. • Gasification of coal: Heating of coal in insufficiently less amount of air plus steam to produce a gas rich in CO and H2 is called gasification of coal. • Proximate analysis of coal: Finding out the weight percent of moisture, volatile matter, fixed carbon and ash content in coal. The analysis is useful in deciding the utilization for a particular purpose. • Ultimate analysis: Finding out the weight percent of carbon, hydrogen, nitrogen, oxygen and sulphur of pure coal free from moisture and inorganic constituents. The analysis is useful in designing of coal burning equipments.
  • 19. • Calorific value: The quantity of heat liberated by combustion of unit quantity of fuel is called its calorific value. – Gross calorific value: Where the heat obtained from condensation of water vapours in the flue gases is also include. – Net calorific value: Where the heat obtained from condensation of water vapours in the flue gases is not include. • Flue gas: The gaseous product of combustion of a fuel. • Heat capacity: Amount of heat required to raise the unit weight of substance by one degree. • Specific heat: It is the ratio of heat capacity of a substance to the heat capacity of water (Cp > Cv). • Ignition temperature: It is the minimum temperature at which the fuel ignites. • Flash point: It is the minimum temperature at which the fuel give enough vapours which produces a momentary flash when exposes to flame. • Pour point: It is the minimum temperature at which fuel keeps its flowing nature when cooled under specific conditions.
  • 21. Wood Domestic fuel used in tropical countries where forest are abundant and other fuels are not easily and cheaply available.
  • 22. • Main combustible components: cellulose and lignin (compounds of carbon, hydrogen and oxygen) • Minor combustible components: resin and waxes. • Non combustible components: Water (25-50% in freshly cut and 10-15% in air dried) • Ash content: very low (<1%) but because oxygen content is very high (upto 45%) therefore its calorific value is very low. • Calorific value: 4000-5000 kcal/kg. • Density: 650 kg/m3.
  • 23. Composition of Air-dried Wood Proximate Analysis • Cellulose: 50% • Lignin: 30% • Moisture: 15% • Water soluble: 2.5% • Resin & Wax: 2% • Ash: 0.5% Ultimate Analysis • Carbon: 50% • Hydrogen: 6% • Oxygen: 44%
  • 24. Properties of wood • It is clean, readily ignites, burn with long clean flame in excess air and leaves only small amount of ash. • Wood is a solid fuel as dense as coal but to obtain same amount of heat as any given weight of coal can produce, you have to burnt wood, four times the weight of coal. • It is used to produce charcoal.
  • 25. Charcoal Carbonization of wood at 600oC
  • 26. Stages Involved in Carbonization of Wood Stage 1: At 100-120oC ---> moisture expelled results in moisture free wood. Stage 2: At 275oC ---> initial decomposition takes place results in formation of little distillate gas containing acetic acid and water. Stage 3: At 350oC ---> active distillation of wood takes place results in emission of liquid (acetic acid, methyl alcohol, tar etc) and gases (CO, CO2, N2, H2, CnHn). Stage 4: At 350-600oC ---> slow evolution of residual volatile matters from the wood charcoal left in 3rd stage.
  • 27. Products of Carbonization of Wood • Charcoal: Solid product left after the carbonization of coal. • Hot gases: Cooled to separate – Wood gas – Liquid in two layer • Upper layer is Pyrolignious acid (mixture of acetic acid, acetone and water). • Lower layer is wood tar (fractionated to separate many chemicals).
  • 28. Uses and Composition of Charcoal • Used for removal of obnoxious and coloring material from solution, gases, vapors and petroleum products by adsorption on its surface. • Used as a feed stock for gasification to make producer gas which is used as a fuel for domestic and industrial use. • Used as raw material for production of carbon sulfide. • Charcoal contains 80% carbon, 15% oxygen and nitrogen, 2% hydrogen and 3% ash.
  • 29. Merits and Demerits • Because of porous in nature it has high specific surface area as compared to coal. • Ash content is very low. • Calorific value is high as compared to wood. • Mechanical strength is very poor.
  • 30. Peat First stage in formation of coal from wood (cellulose) The most immatured coal
  • 31. Formation of Peat • Peat is the first stage in the formation of coal from wood (cellulose). • It is not strictly a coal or else can be termed as the most immatured coal. • It is formed by gradual decaying (action of bacteria under high pressure and temperature) of remains of plants in moist places.
  • 32. Properties of Peat • Peat is light brown in color. • Highly fibrous in nature. • With increase in depth the color becomes darker and fibrous structure disappeared. • Composition of peat varies from nature of plants, depth in deposit and age. • Freshly mined peat contains about 90% water and 10% solid. Therefore cannot be used unless air dried. • Calorific value is 650 kcal/kg for freshly mined peat and 5000 kcal/kg for air dried peat.
  • 33. Composition of Peat Proximate Analysis • Moisture: 20% • Volatile matter: 50% • Fixed carbon: 25% • Ash: 5% Ultimate Analysis • Carbon: 55% • Hydrogen: 6% • Oxygen: 33% • Nitrogen: 3% • Sulfur: 1%
  • 34. Gasification of Peat • Peat is gasified in presence of steam and air to produce producer gas. • Steam requirement is very low because peat itself contain sufficient moisture. • Typical composition of gas is: • CO2 – 13% • CO – 18% • H2 – 11% • CH4 – 2.5% • N2 – 55.5% • Caloric value is 1000 kcal/kg • Gas yield is 2500 Nm3/ton of peat
  • 35. Other non Fossil Domestic Fuel
  • 36. Origin of coal • Coal is a complex mixture of plant substances altered in varying degree by physical and chemical processes. • These processes which changed plant substances into coal has taken million of years and has been accomplished by bacteria, heat and pressure inside the earth’s crust. • Two theories namely “in-situ” theory and “drift theory” have been suggested by geologists regarding mechanism of formation of coal from plant substances. • In situ theory: According to this theory, coal seam occupies the same site where the original plants grew and where their remains accumulated several million years ago to produce coal under the action of heat, pressure and bacteria. • Drift theory: According to this theory plants, tree etc were uprooted and drifted by rivers to lakes and deposited there to form coal during the course of time after they got buried underground. • Stages information of coal: plants/trees  peat  lignite  sub-bituminous coal  bituminous coal  anthracite coal  graphite.
  • 37. • Points in favor of “in-situ” theory: – In the existing peat deposits; the decayed plant substances had accumulated at the place of origin. – Large quantity of fossil fuel have been found under the coal seam. – Composition of coal seam is generally constant over a wide area. If the original decaying plants and tree had been drifted from their original place then they would have a great variation in composition of coal. • Points in favor of “drift” theory: – In coal seam, the percentage of inclined trunks of fossil is much more than the vertical position. It the coal had been formed at the same place where the plants substances decayed then fossil trunks would have been vertical. – To form one meter thick coal seam, ten meter thick seam of peat is required, So for the formation of ten meter thick coal seam should have resulted from hundred meter thick seam of peat, which occur no where. – Seams of coal are made up of different layers separated by layers of clay or sandstone which vary in thickness from merely a film to several meters. As the plants accumulated under water some slits also settled along with them. Thus at later stage some mineral mater got mixed with coal as it formed.
  • 38.
  • 39. • Stages for transformation of wood to coal: • The initial transformation of wood to coal is due to the action of bacteria (aerobic or anaerobic) causing degradation of organic matters (e.g. cellulose, lignin etc. present in wood) and removal of oxygen. • The bacterial action produced acidity which if accumulated prevented further action and coal formation could not proceed. • In some cases the soil was alkaline which neutralized the acidity and bacterial action continued to take place further degradation of organic matter. This explain why coal is found along with certain types of rocks. • Bacterial action takes place in initial stage breaks up organic matters into simpler molecules. • The degraded organic matters, as time passed, gave rise to peat. • Beyond this stage heat, pressure and time became the chief factors for further conversion of peat into different rank of coal.
  • 40. Lignite • It is the second stage product in the formation of coal from wood. • It is friable and occurs in thick seams (up to 30 meter thick) near the surface of earth. • It moisture content is up to 60 % and calorific value is around 5000 kcal/kg. • On exposes to air the brown color darkens and moisture content reduces to equilibrium value of 10 – 20 %. • On drying lignite shrinks and break up in irregular manner. • It is likely to ignite spontaneously as it adsorbs oxygen readily and must not be stored in open without care. • Composition and property of lignite varies widely. The carbon content is 70 – 75 % and oxygen content is 20 – 25 %. • In large number of cases the ratio of volatile matter to fixed carbon is 1:1. • Raw Lignite is inferior fuel due to high moisture content, low calorific value, small size and bad weathering properties. • Lignite is of economic importance where it is readily available and other fuels do not occur in abundance.
  • 41. Composition of Lignite Proximate Analysis • Moisture: 10 – 30 % • Volatile matter: 40 – 45 % • Fixed carbon: 30 – 35 % • Ash: 3.5 – 7.5 % Ultimate Analysis • Carbon: 70 – 73 % • Hydrogen: 4.6 – 5.5 % • Oxygen: 22 – 26 % • Nitrogen: 0.6 – 1.0 % • Sulfur: 0.6 – 1.5 %
  • 42. Bituminous Coal • It is the most common variety of coal. • It is black and brittle which burns and ignites readily with yellow smoky flame. • It has low moisture content i.e. less than 10 % and carbon content varies from 75 – 90 % where as volatile matter content is 20 – 45 %. • Depending upon the volatile matter content, it is termed as low volatile, medium volatile and high volatile coal. • Its calorific value based on dry mineral free basis goes up to 9000 kcal/kg. • It is used for power generation, coke making, gasification and domestic use.
  • 43. Composition of Bituminous coal Proximate Analysis • Moisture: 3.5 – 8 % • Volatile matter: 16 – 36 % • Fixed carbon: 49 – 72 % • Ash: 7 – 8.5 % Ultimate Analysis • Carbon: 68.5 – 79.5 % • Hydrogen: 4.5 – 5.5 % • Oxygen: 4.5 – 16.5 % • Nitrogen: 1 – 1.4 % • Sulfur: 0.5 – 1 %
  • 44. Anthracite coal • It is most matured coal hence of highest rank. • It is hard and burns without smoke with a short non-luminous flame. • It has high carbon content i.e. 85 – 95 % and low volatile matter content i.e. less than 10 %. • It ignite with difficulty due to low volatile matter content. • Its calorific value may be up to 8000 to 8500 kcal/kg which is less than bituminous coal de to its lower hydrogen and volatile matter content. • It has sub-metallic lustre and sometime even a graphitic appearance. • The chief use of anthracites are in boilers and metallurgical furnaces. • On calcining it gives thermo-anthracite which is a raw material for the production of carbon electrode.
  • 45. Composition of Anthracite coal Proximate Analysis • Moisture: 2.5 – 3 % • Volatile matter: 3 – 8.5 % • Fixed carbon: 79 – 87.5 % • Ash: 7 – 9.5 % Ultimate Analysis • Carbon: 80 – 86.5 % • Hydrogen: 2.5 – 3.5 % • Oxygen: 3 – 4.5 % • Nitrogen: 0.5 – 1.5 % • Sulfur: 0.5 %
  • 46. Significance of constituents of coal Proximate analysis • Moisture • Volatile matter • Fixed carbon • Ash Ultimate analysis • Carbon • Hydrogen • Nitrogen • Sulphur • Oxygen
  • 47. Moisture • In general high moisture content in coal is undesirable because: – it reduces the caloric value of fuel – it increases the consumption of coal for heating purpose – it lengthens the time of heating – it increases the cost for purchase and transportation. • Owing to its nature, origin and occurrence, coal is always associated with moisture. • When coal is exposed to atmosphere its external moisture (free moisture) evaporates but apparently dry coal still contain some moisture (inherent moisture). • Air-dried moisture content of coal is determined by observing loss in weight of coal sample on heating at 105 degree centigrade. • Air-dried moisture of coal decreases with increasing rank from a value of 25% for lignite to a minimum value of 0.5% for low volatile bituminous coal.
  • 48. Volatile matter • Certain gases like CO, CO2, CH4, H2, N2, O2, CXHY etc, are present in coal which comes out during its heating in absence of air. • These gases are called volatile matter of coal. • Coal with high volatile matter content: – Ignites easily i.e. it has low ignition temperature – Burns with long smoky yellow flame – Give more quantity of coke oven gas when it is heated in absence of air. • Volatile matter does not include moisture of coal but it contain moisture that is formed from oxygen and hydrogen of coal during the decomposition. • Volatile matter expressed as per cent on dry mineral matter free basis. • Higher the volatile matter, lower the fixed carbon.
  • 49. Ash content • Ash is the combustion product of mineral matters presents in the coal. • It is comprises mainly of silica, alumina and ferric oxide with varying amount of other oxide such as calcium and magnesium. • High ash content in coal is undesirable in general. • A coal with high ash content is harder and stronger and has lower calorific value. • Ash content of coal is reduced by its washing. • Coal contains inorganic mineral substance which are converted into ash by chemical reaction during combustion. Ash and coal are therefore not the same. • The bulk of mineral matter of coal is due to clay or shale consisting of alumino-silicates of different composition. Other major constituents may be calcite and pyrites. • When coal burns these mineral matter decomposed resulting loss in weight hence the ash of coal is always less than the mineral matter content.
  • 50. Fixed carbon • It is the pure carbon present in coal. • Higher the fixed carbon, higher will be the calorific value. • In anthracite where the value of volatile matter is very small, fixed carbon and total carbon are almost same. • In other coals, fixed carbon is always less then total carbon.
  • 51. Total Carbon • Its mean fixed carbon plus the carbon present in the volatile matters. • Total carbon is always more than fixed carbon in any coal. • High total carbon coal will have high calorific value.
  • 52. Hydrogen • It increases the calorific value of coal. It is associated with volatile matter of coal. • The content of coal from peat to bituminous varies between 4.5 and 6.5 and is not related to the rank of coal. • Beyond the bituminous stage the hydrogen content sharply decreases to a value of 1 – 2% in anthracite.
  • 53. Nitrogen • Nitrogen in coal is present up to 1 – 3% and comes from the protein matter presents in plant. • Presence of inert nitrogen decreases the calorific value of coal. • However when coal is carbonized, its hydrogen and nitrogen combined thereby producing NH3 which is recovered as (NH4)2SO4 (by reacting it with H2SO4) which is a valuable fertilizer. • Nitrogen content does not have any relation with rank of coal. • In most coal it is between 1 – 2%.
  • 54. Sulphur • Though its presence increases the calorific value of coal but has several undesirable effects. • The oxidation product of sulphur i.e. SO2 in presence of moisture cause corrosion of the equipment and cause atmospheric pollution. • Sulphur is highly undesirable in metallurgical coal used for iron and steel making as it badly effect the properties of iron and steel. • The sulphur content of coal has no relation to its rank or composition.
  • 55. Oxygen • Less the oxygen content better the coal as it reduces its calorific value. • It decreases from lignite to anthracite. • As the oxygen content of coal increases it moisture holding property increases. Phosphorus & Chlorine
  • 56. Washing of coal • Most of the coal when mined contain impurities associated with it which must be removed before the coal is used. • These impurities are removed from coal by washing. • Coal contain two types of impurities. – Fixed or inherent impurities which are derived from coal forming plants and cannot be removed by washing. – Free impurities which are adhering to the surface of coal and comprise mainly of dirt and rock particles which can be removed by washing. • Washing of coal: – Reduces its ash content – Reduces its sulphur content – Increase its heating value – Improves its coking property
  • 57. Principle of washing of coal • Specific gravity of pure coal varies from 1.2 to 1.7 and that of free impurities from 1.7 to 4.9. • The coal can be separated by its impurities by utilizing difference in specific gravity. • If the average specific gravity of pure coal is 1.3 and it is suspended in liquid of specific gravity 1.5 then the impurities being heavier will sink in it whereas the pure coal will float. • Washing medium used in industrial coal washing is a slurry of sand and water or that of water and iron ore.
  • 58. Properties and testing of coal • Determination of moisture content: A known amount of finely powdered coal sample is kept in a silica crucible and heated in a muffle furnace at 105 – 110 degree centigrade for one hour. The process of heating, cooling and weighing is repeated for number of times until the constant weight of anhydrous coal is achieved. • Determination of volatile matter: It is the loss in weight of moisture free powdered coal when heated in crucible fitted with cover in a muffle furnace at 950 degree centigrade for 7 minutes. • Determination of ash content: It is the weight of residue obtained after burning a weighed quantity of coal in an open crucible at 750 degree centigrade in a muffle furnace until a constant weight is achieved. • Determination of fixed carbon: It is determined indirectly by deducting the sum total of moisture, volatile matter and ash percentage from 100
  • 59. • Determination of carbon and hydrogen: – A known amount of coal is burnt in a current of dry oxygen thereby converting Carbon and hydrogen of coal into Carbon dioxide and water respectively. – The product of combustion are then passed over weighed tubes of anhydrous calcium chloride and potassium hydroxide, which absorb water and carbon dioxide respectively. – The increase in weight of calcium chloride tube represent the weight of water formed while increase in weight of potassium hydroxide tube represent the weight of carbon dioxide formed. – The percentage of carbon and hydrogen then can easily be calculated. • Determination of Nitrogen in coal: • Determination of Sulphur in coal:
  • 60. • Determination of Calorific Value by bomb calorimeter: • Strong stainless steel vessel (25 – 30 atm). • Provided with electrode, crucible, and oxygen inlet valve. • Bomb placed in copper calorimeter. • Calorimeter is surrounded by water and air jacket provided with electrical stirrer.
  • 61. Carbonization of Coal Low temperature carbonization (LTC) • It carried out at 700 degree C. • It produces semi coke which is used as smokeless domestic fuel. • Yield of coke oven gas is less due to less cracking of hydrocarbons. • Yield of tar is high i.e. about 10% of dry coal. • Ammonia yield is low. • Calorific value of coke oven gas is high (6000 – 6500 kcal/kg) due to higher percentage of methane and unsaturated hydrocarbon in it. • The tar produce is aliphatic in nature. • Coke produced is weaker, bigger in size and more reactive. • Volatile matter content in coke is more. • Hydrogen content in coke oven gas is less i.e. 35 – 40%. High temperature carbonization (HTC) • It carried out at 1000 degree C. • It produces metallurgical coke for use in blast furnace. • Yield of coke oven gas is more due to more cracking of hydrocarbon. • Yield of tar is less i.e. about 3% of dry coal. • Ammonia yield is more. • Calorific value of coke oven gas is less (4200 – 4400 kcal/kg) due to lesser percentage of hydrocarbon resulting from cracking. • The tar produce is aromatic in nature. • Coke produced is stronger, smaller is size and less reactive. • Volatile matter content in coke is less. • Hydrogen content in coke oven gas is more i.e. 55 – 60%).