Joseph Martin 01-Biomass Combustion OstwaldDiagram

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    BIOMASS COMBUSTION 1

    COMBUSTION OF BIOMASS FUELS

    1. HEATING VALUE,AIR DEMAND AND FLUE GAS PRODUCTION1.1.

    Heating Value

    Combustion may be defined as a fast spontaneous chemical reaction of the oxidation-

    reduction type with large energy release. Such a reaction mainly involves the carbon and

    hydrogen elements of any type of fuel as reducers and the atmospheric oxygen as oxidizer.

    The main practical objective of a combustion is to transform the chemical latent heat of the

    reactants, i.e. the so called Heating Value, into sensible heat. This last can be carried out by

    direct radiation to the walls of the combustion chamber and/or by convection using the

    reaction products as a heat carrier, or directly converted into mechanical work in a

    thermodynamic process.The Heating Value of a fuel is defined as the heat release in a constant pressure process

    involving the unit of quantity of the fuel. The Lower Heating Value LHV is defined as the

    heat to be removed from the reaction products to obtain a final temperature equal to the initial

    temperature of the reactants, assuming that the reaction products remain in gaseous phase, i.e.

    that the condensation heat of the water is not available.

    This definition corresponds therefore to the difference between the standard enthalpy of the

    reactants and the standard enthalpy of the products under normal conditions.

    The standard enthalpy of the single chemical species such as C(graphite),H2, O2, ... is zero.

    The non-zero standard enthalpy H273of the normal products of a combustion involves CO2

    andH2O:

    273 2

    273 2 vap

    H ( CO ) 393500 kJ / kmole

    H ( H O ) 241800 kJ / kmole

    =

    =

    The non-zero standard enthalpy of the reactants involves a lot of more or less complicated

    chemical species, such as CO, hydrocarbons, alcohols, pure cellulose, ... , which are well

    known. Therefore, the standard enthalpy of a fuel completely defined in percentage ofsuch well defined chemical species would be easily computed by linear combination of their

    components. The following values are especially useful :

    273 a

    273

    273 4

    H ( CH ) 10870 a kJ / kmole ( for char or coke : a 0.2 )

    H ( CO ) 111100 kJ / kmole

    H ( CH ) 74700 kJ / kmole

    =

    =

    =

    By difference between the standard enthalpy of the reactants and the standard enthalpy of the

    products, one obtains the following values of severalLHV:

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    BIOMASS COMBUSTION 2

    2

    4

    0.2

    LHV( C ) 393500 kJ / kmole

    LHV( H ) 241800 kJ / kmole

    LHV( CO ) 282400 kJ / kmole

    LHV( CH ) 802400 kJ / kmole

    LHV( CH ) 420120 kJ / kmole

    =

    =

    =

    =

    =

    Unfortunately, the actual fuels are often very variable combinations of such species, and their

    composition may only be defined as an elementary percentage of single species, without a

    thorough knowledge of their actual chemical structure.

    A lot of formulae have been proposed to approximate the LHVof several actual fuels, more

    especially solid fuels, on basis of their elementary composition. This last can be expressed in

    a very convenient form, as a stoechiometry formula written for one atom of carbon :

    y x z uCH O N S

    For pure and dry biomass fuels of the ligno-cellulosic type, nitrogen and sulphur are usually

    negligible and the above formula may be rewritten as follows for a pure (without minerals)

    and dry fuel :

    y xCH O with y 1.44 and x 0.66

    A very good approximation of the Heating Value of such a fuel can be derived from an

    equivalent distribution of the actual (unknown) chemical bonds between C,Hand O,based on

    pyrolysis data and using simple compounds involving C O= , O H and C H . Thetotality of the oxygen is considered to be distributed on the carbon and on the hydrogen to

    form COandH2Obalancing the species as follows :

    y x 2 y

    x x xCH O CO 0.5 y H O (1 ) CH

    1 0.5 y 1 0.5 y 1 0.5 y + +

    + + +.

    The remaining hydrogen is then distributed on the carbon to form CH4and a residual coke

    CH0.2 as follows :

    y 0.2 4

    x x 4 y y 0.2

    (1 )CH (1 )( CH CH )1 0.5y 1 0.5 y 3.8 3.8

    ++ + .

    One obtains therefore the global equivalence :

    y x 2

    4 0.2

    x xCH O CO 0.5 y H O

    1 0.5 y 1 0.5 y

    x y 0.2 x 4 y(1 ) CH (1 ) CH

    1 0.5 y 3.8 1 0.5 y 3.8

    ++ +

    + +

    + +

    and the following expressions of theLHVof a pure and dry biomass fuel :

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    BIOMASS COMBUSTION 3

    y xCH O

    xLHV 400000 100600 y (117600 100600 y ) ( kJ / kmole )

    1 0.5 y

    x400000 100600 y (117600 100600 y )

    1 0.5 y( kJ / kg ) .

    12 y 16 x

    + ++

    + ++

    + +

    Withy = 1.44andx = 0.66, the valueLHV" is therefore 18500 kJ/kg.

    Biomass fuels are often (unfortunately) neither pure neither dry. The mineral matter content

    (Mm)may generally be considered as a dilutant of the active species. The moisture content

    (Hu) plays not only a role of dilutant, but also a role of active species with a negative LHV,

    corresponding to its heat of vaporisation 2500 kJ/kg, consumed during the combustion

    process. Assuming that (Mm") and ( Hu" )are expressed as weight ratios to the pure and dry

    fuel, the actualLHVof the raw fuel can be easily derived from the valueLHV"of the pure and

    dry fuel, as follows :

    LHV 2500( Hu )LHV kJ / kg

    1 ( Mm ) ( Hu )

    =

    + +.

    An equivalent formula may be written using the weight ratios (As)and (Hu)to the raw fuel :

    LHV [1 ( Mm ) ( Hu )] LHV 2500 ( Hu ) kJ / kg= .

    Table 1 illustrates the strong decrease of the Heating Value with the moisture content, more

    especially for high mineral content fuels.

    0 0.10 0.20 0.30 0.40

    0 18500 16400 14300 12200 10100

    0.05 17575 15475 13375 11275 9175

    0.10 16650 14550 12450 10350 8250

    0.15 15725 13625 11525 9425 7325

    0.20 14800 12700 10600 8500 6400

    Table 1.

    Lower Heating Value (kJ/kg) of a biomass fuel versus the moisture and the mineral contents

    It is obvious that an efficient biomass combustion system must include a pre-drying device

    using any available low potential heat, e.g. heat recovered from the exhaust gases, in order to

    maximize the actual availableLHVof the fuel.

    (Hu)

    (Mm)

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    BIOMASS COMBUSTION 4

    Considering now that only the active matter is an "expensive" consumable, a convenient

    "reference" Heating ValueLHVre may be expressed as the heat release corresponding to the

    quantity of the pure and dry matter in the raw fuel, i.e. out of the negative LHV of themoisture :

    refLHV [1 ( Mm ) ( Hu )] LHV=

    The "availability" of this reference Heating Value for any fuel may be expressed as the ratio

    between the actual Heating Value LHV of the fuel and its "reference" LHVre . This"availability factor" is a fundamental quality factor of the energy content for a biomass fuel :

    LHV

    2500( Hu ) 1

    [1 ( Mm ) ( Hu )] LHV

    With the above value 18500 kJ/kg for LHV", one obtains the following values of this

    availability factor as a function of the moisture content and of the mineral content :

    0 0.10 0.20 0.30 0.40

    0 1 0.985 0.966 0.942 0.910

    0.05 1 0.984 0.964 0.938 0.902

    0.10 1 0.983 0.961 0.932 0.892

    0.15 1 0.982 0.958 0.926 0.880

    0.20 1 0.981 0.955 0.919 0.865

    Table 2.

    LHVrefavailability factor of a biomass fuel versus the moisture and the mineral contents

    These values of theLHV availability factorare more significant at an energy viewpoint than

    those of the LHV itself, which are combining the energy loss due to the moisture and the

    dilution effect of the non fuel content. However, it appears obvious again that an efficient

    energy use of a biomass fuel needs an external pre-drying , in order to avoid the in situ

    consumption of energy during the combustion itself.

    1.2. Air demand and flue gas productionThe here-above symbolic formula of the chemical composition of a ligno-cellulosic fuel is

    very convenient to compute the stoechiometric air demand in terms of volumea1

    V or in terms

    (Hu)

    (Mm)

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    BIOMASS COMBUSTION 5

    of massa1

    m . The stoechiometric reaction of such a fuel with dry air may be expressed as

    follows :

    y x 2 2 2 2 2

    y 2x y y 2xCH O (1 ) ( O 3.76 N ) CO H O 3.76 (1 ) N

    4 2 4

    + + + + + + (1)

    where the atmospheric air has been considered to be a dry O2/N2mixture. Taking in account

    the normal molecular volume 3N

    22.710m / kmole and the involved molecular weights, one

    may write :

    3

    a1 N

    a1

    y 2x(1 )

    4V 108.1 m air / kg fuel 12 y 16 x

    y 2x(1 )

    4m 137.9 kg air / kg fuel 12 y 16 x

    +

    =+ +

    +

    = + +

    Similarly, the stoechiometric volume and the stoechiometric mass of the flue gases is easily

    computed :

    3

    f 1 N

    y x108.1 130.8 85.4

    4 2V m flue gas / kg fuel 12 y 16 x

    + =

    + +

    f 1 a1

    y 2x1

    4m 1 m 1 137.9 kg flue gas / kg fuel 12 y 16 x

    +

    = + = ++ +

    Taking in account the moisture (Hu)and the mineral matter (As), the hereunder expressions

    are to be written for the raw fuel :

    a1 a1 a1 a1

    f 1 f 1 f 1 a1

    V [1 ( As ) ( Hu )] V , m [1 ( As ) ( Hu )] m ,

    V [1 ( As ) ( Hu )] V 1.262 ( Hu ) , m 1 [1 ( As ) ( Hu )] m .

    = =

    = + = +

    For any actual combustion process, an air-excess factor is needed to ensure complete

    combustion. Therefore, the actual air demand and the flue gas production are to be written :

    a a1 a a1 f f 1 a1V V , m m , V V ( 1)V= = = + .

    The practical values to be derived from the here-above formulae for typical ligno-cellulosic

    materials, withy = 1.44andx = 0.66 are :

    3 3 3

    a1 N N a1 N

    3 3 3

    f 1 N N f 1 N

    V 4.61 m dry air / m dry fuel , m 5.92 kg dry air / m dry fuel

    V 5.29 m flue gases / m dry fuel , m 6.92 kg flue gases / m dry fuel

    = =

    = =

    considering the fuel as being dry and without mineral matter.

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    BIOMASS COMBUSTION 6

    2. COMBUSTION STEPS AND COMBUSTION CONTROL2.1. Some fundamentals about biomass fuels combustionThe combustion process for an actual biomass fuel / oxidizer system is of course more

    complicated than the behaviour of the "pure gaseous system" or of the "simple

    carbon/oxygen" system. For an homogeneous gaseous phase fuel/oxidizer system, such as the

    H2/ O2or the CH4/ O2system, the combustion process essentially involves chain reactions

    carried by radicals such as OH, H, O, ... . For the heterogeneous solid/gaseous phase C /O2

    system, the main combustion process essentially involves CO formation by adsorption-

    desorption phenomena on active carbon sites, followed by homogeneous gaseous phase

    oxidation. For solid fuels, devolatilisation and thermal decomposition always lead to an

    heterogeneous solid-gas fuel system, in which the importance of the gaseous phase depends

    on the balance between the so called "volatile matter" content and the "fixed carbon" of thefuel.

    The ligno-cellulosic biomass fuels have a relatively high (80 %) volatile content and a

    significant (20 %) fixed carbon content. During the combustion, both oxidation processes

    (homogeneous and heterogeneous) may be in competition as illustrated fig. 1.

    Figure 1

    CHyOx

    Pyrolysis CHs

    CO2 H2O

    CnHm CO H2

    Oxidation

    O2 O2

    Oxidation

    CHsReduction

    CO H2

    O2OxidationO2

    CO2 H2O

    CnHm CO H2

    CHs CO H2

    CHs

    CHs

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    BIOMASS COMBUSTION 7

    This first global approach shows the main interlaced steps of the combustion process.

    At a temperature of about 200 C (for the most complex and thus the least stable

    compounds) to about 500 C (for the simplest and consequently the most stable

    compounds), a thermal cracking or pyrolysis initially decomposes the fuel, forming

    radicals. The so formed radicals can lead to gaseous (possibly condensable) recombinationproducts of and/or solids products.

    The gaseous products consist of hydrocarbon chains (CnHm,)still being able to include

    radicals ; for biomass fuels which contain oxygen, the gaseous products comprise a

    fraction of partial oxidation (CO, H2)and of complete oxidation (CO2, H2O)species.

    The solid products, only formed by complex fuels, consist of a coke or char, which is

    carbon-rich compound (CHs); this coke appears as a porous skeleton image of the

    original structure of the fuel ; for pulverized fuels, spongy particles or cenospheres, are

    formed, whereas embers result from big pieces of fuels.

    The reaction of the pyrolysis products with oxygen then gives place to a first phase of

    oxidation. At this level the so called "primary" oxygen is reacting as follows.

    The oxidation of the gas compounds involves chain reactions whose active elements

    are radicals which are chain carriers responsible of a flame combustion if the

    flammability limits are locally met. The flame structure depends on the formation on

    the mixture between the fuel gas fraction and the locally available oxygen.

    The oxidation of the char needs the adsorption of O2by the active sites of the porous

    char surface, forming adsorbed C(O) from which CO is desorbed to burn then in

    gaseous phase.

    If these oxidation processes are incomplete, one may obtains the following products.

    Residual pyrolysis gases or partial oxidation products resulting from the lack of

    reactivity or "quenching" at low temperature.

    Solid long chain of carbon and hydrogen (in a ratio close to CH0.2) forming soot,

    synthesized from the ultimate gaseous residues of the fuel at high temperature without

    oxygen.

    The carbon of the solid products resulting from oxygen lacking can react with the

    surrounding oxidation products CO2andH2O, in a reduction step forming COandH2. If

    the temperature is sufficient, the solid phase can thus completely disappear. The so

    obtained gas phase includes thus a still combustible fraction .

    If necessary, in particular when the combustion process leads to the primary formation of

    a still combustible gas, a second oxidation step is needed, using additional or secondary

    oxygen, to obtain finally complete oxidation products and therefore to transform into heat

    the whole heating value of the fuel.

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    BIOMASS COMBUSTION 8

    From these considerations, it can be said that a successful combustion of a solid fuel such as a

    ligno-cellulosic fuel requires at least the following conditions

    The gaseous pyrolysis products must form a flammable mixture with air, and this mixture

    must be heated (locally or globally) up to the ignition (critical) temperature. Moreover, if

    this gaseous mixture is flammable but lacking in air, secondary air must be added withoutfreezing the system, to completely oxidize the gaseous phase emerging from the fuel.

    The solid particles of char must form a bed or a suspension able to completely react with

    oxygen. This can be achieved efficiently only if the pyrolysis gaseous phase leave the

    solid phase free for landing of oxidizing species on the active carbon surface. The locally

    formed COmust be burned in a subsequent combustion step, using secondary air.

    The above considerations may be illustrated fig. 2, showing the combustion arrangement of a

    45 MWthsuperheated steam generator burning wood and bark chips on a moving grate.

    Figure 2

    The primary air supply is distributed under the grate, to ensure the flame pyrolysis and rich

    combustion of the pyrolysis gases (upper part of the grate) and to completely burn the char

    (lower part of the grate). the secondary air is distributed at the throat of the combustion

    chamber, to completely oxidize the partial oxidation products emerging from the primary

    zone. A flue gas recirculation is installed at intermediate zones is for NOx emissions

    abatement.

    2.2. Checking the combustion by the flue gas analysisAssuming that the combustion of a ligno-cellulosic fuel leads only to gaseous products

    excluding residual quenching gases, i.e. assuming that flammability conditions of the

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    BIOMASS COMBUSTION 9

    pyrolysis gases is ensured and that no flying carbon is passing through the system, one may

    write the stoechiometry of the fuel combustion (moisture included) as follows :

    y x 2 2 2 0 2 1 2 2 1 2 2 2 2CH O z H O w(O 3.76N ) a O a CO a CO b H b H O 3.76wN + + + + + + + + . (2)

    The conservation equations of the species may be written :

    carbon conservation : 1 2a a 1+ = (3)

    hydrogen conservation : 1 2y

    b b z2

    + = + (4)

    oxygen conservation : 0 1 2 2z

    2 a a 2 a b 2 w x2

    + + + = + + (5)

    By combining the second and the third of these relations, one eliminates b2andz, what leads

    to the remaining system:

    1 2a a 1+ = (6)

    1 0 1 2

    yb 2 a a 2 a 2 w x

    2 + = (7)

    The stoechiometric coefficients a0, a1, a2, b1 and w are related as follows to the volumic

    fractions [ ]' of the dry gas obtained, by the relations :

    0 12 0 1 2 1

    a a[ O ] , [ CO ] , ... , with a a a b 3.76w

    = = = + + + + .

    Therefore, the here-above system may be rewritten as follows :

    2

    2 2 2 2

    1[ CO ] [ CO ]

    2 y 2x[ H ] [ CO ] 2[ CO ] 2[O ] [ N ]

    3.76 2

    + =

    + =

    Eliminatingand replacing [N2]'by the closure equation :

    2 2 2 2[ N ] 1 [ O ] [ CO ] [CO ] [ H ] = ,

    one obtains the following linear equation or compatibility equation between the volume

    fractions of the dry flue gases :

    2 2 2

    y 2x y 2x4.76[O ] ( 2.88 3.76 )[CO ] ( 4.76 3.76 )[ CO ] 0.88[ H ] 1

    4 4

    + + + + = .(8)

    Considering the gaseous species CO, H2 , CO2 and H2O only existing locally at high

    temperature without O2, the following chemical equilibrium must be taken into account :

    2 2 2CO H CO H O+ +

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    BIOMASS COMBUSTION 10

    and this equilibrium becomes "frozen" when the temperature is decreasing under ... 850 ... C

    at the value :

    2

    2 2

    [ CO ][ H O ]2

    [CO ][ H ] .

    Considering the coefficients a1and b1as normally small compared to a2and b2, one may take

    from (3) and (4) the approximations :

    2 2

    ya 1 and b z

    2 = + ,

    what leads to write for the frozen equilibrium :

    2 1 2 1

    2 2 2 1 1 2

    [ CO ][ H O ] a b ay y [CO ]( z ) ( z ) 2

    [ CO ][ H ] a b 2 b 2 [ H ]= + = +

    from which results the following ratio between2

    [ H ] and [CO] :

    2[ H ] y 2z

    ( )[CO ] 4

    +=

    .

    The compatibility equation may thus be considered as a linear relation between the three

    independent parameters2 2

    [ O ] ,[ CO ] and [ CO ] :

    2 2

    y 2x y 2 z y 2 x4.76[O ] ( 2.88 3.76( ) 0.88 )[CO] (4.76 3.76 )[CO ] 1

    4 4 4

    + + + + + = . (9)

    This linear relation describes the plan ( 2 space) of the possible compositions in the of the3

    space{[O2]' [CO]' [CO2]'}, as illustrated fig. 3.

    Figure 3

    [CO]

    [O2]

    [CO2]

    Q

    R

    P

    O

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    BIOMASS COMBUSTION 11

    The summit coordinates of this composition plan are the following :

    2 P

    2 Q

    R

    1[ CO ]

    y 2x4.76 3.76

    4

    1[ O ]4.76

    1[CO]

    y 2x y 2 z2.88 3.76 0.88

    4 4

    =

    +

    =

    = +

    +

    The use of the compatibility equation (9) makes it possible to determine any of these three

    volume fractions knowing the two others. It is thus possible to obtain a complete diagnosis of

    the combustion of a fuel of parameters yandxknown thanks to the measurement of two of

    the three fractions.

    In the past, it was made use for combustion diagnosis of simple chemical apparatus based on

    selective absorbers, or of more expensive instruments based on physical properties to measure

    [O2]'and [CO2]or [CO]'and [CO2]' . The electronic miniaturization made it possible today

    to develop simple and non expensive apparatus using electrochemical cells based on the

    Nernst cell to measure the values of [O2]'and [CO]'. Theses measurement systems includes a

    microchip which then makes it possible to display the calculated content [CO2]'in addition

    to the directly measured values of the contents [O2]'and [CO]'.

    It will be noted finally that if the value of two of the three volume fractions constitutes a

    satisfying information for industrial or for checking purposes, it may be desirable, in the case

    of reference measurement, to have the redundant measurement of the three volume fractions,

    which makes it possible to minimize the uncertainty of the diagnosis by making use of

    adequate mathematical methods such as the method of least squares.

    2.3. The partial oxidation coefficient and the air excess coefficientThe ratio of the air coefficient w of the actual stoechiometry of the combustion to the air

    coefficient

    y 2x

    (1 )4

    + of the theoretical stoechiometry of the combustion is the air excess

    coefficient :

    w

    y 2x(1 )

    4

    +

    . (10)

    Similarly, a partial oxidation coefficient kmay be defined as the ratio :

    1

    2 1 2

    a[CO]k

    [ CO ] [ CO ] a a

    =

    + + (11)

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    BIOMASS COMBUSTION 12

    Using these definitions and the conservation equations (6) and (7), one may rewrite the

    general equation (2) as follows :

    y x 2 2 2

    2 2

    2

    2 2

    y 2xCH O z H O (1 )( O 3.76 N )

    4

    y 2 zkCO (1 k )CO k( )H

    4

    y 2x k y 2z[( 1)( 1 ) (1 )]O

    4 2 4

    k y 2 z y 2x(1 )( )H O 3.76 (1 ) N

    2 2 4

    + + + +

    ++ +

    ++ + + +

    + + + +

    (12)

    form this last equation, one may write the following expression :

    2

    2

    [ O ] y 2 x k y 2 z ( 1)(1 ) (1 )

    [CO ] [ CO ] 4 2 4

    += + + +

    +

    ,

    which may be rewritten by use of the kcoefficient (11):

    2

    2

    1 y 2 z [ O ] (1 )[ CO ]

    2 4 1y 2x

    (1 )([ CO ] [CO ] )4

    + +

    =

    + +

    . (13)

    The accurate determination of the air excess coefficient by means of (13) postulates the

    measurement of at least two of the three volume fractions {[O2]' [CO]' [CO2]'} by

    independent ways, the third of these volume fractions being deduced from both others by the

    compatibility equation (9). A better accuracy may of course be obtained by the direct

    measurement of the three volume fractions. If one may only measure to two of the volume

    fractions, the {[O2]' [CO]'}pair is the most adequate since it provides the most significant

    calculation of the third volume fractions by means of the compatibility equation (9).

    3. THE OSWALD DIAGRAM AND THE AIR EXCESS OPTIMISATION3.1. The Oswald diagramThe OSWALD diagram of a combustion (fig.2) illustrates in the { [CO2]' [O2]'}coordinates

    some of the particular lines related to the flue gases composition. The relations (11) and (13),

    can be rewritten in the following forms, linear in {[O2]' [CO]' [CO2]'}:

    2

    k[ CO ] [ CO ]

    1 k =

    (14)

    2 2

    y 2x y 2x 1 y 2z( 1)(1 )[CO ] [( 1)(1 ) (1 )][CO] [O ] 0

    4 4 2 4

    + + + + + + = . (15)

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    BIOMASS COMBUSTION 13

    These relations are the equations of the plans k = Cstand = Cst in the {[O2]' [CO]' [CO2]'}3

    space. Projecting in the {[CO2]' [O2]'}plan the intersections of the (14) and (15) plans

    with the composition plan (9), one obtains straight lines constituting the required remarkable

    lines, as illustrated fig. 4 .

    Figure 4

    The line PQ is the line of complete combustion k = 0 with the following remarkable

    points :

    point P, characterized by [O2 ]' = 0 and [CO]' = 0, corresponds to a complete

    combustion (k = 0)without air in excess (= 1)and is located at the coordinates :

    2 P 2 P

    1[ CO ] , [ O ] 0

    y 2x4.76 3.76( )

    4

    = =

    +

    .

    point Q, characterized by [CO2]' = 0 and [CO]' = 0, corresponds to an infinite air

    excess and thus corresponds to any coefficient k of unburned products and in

    particular with that k = 0. Its coordinates are :

    2 Q 2 Q

    1[ CO ] 0 , [ O ] 4.76 = =

    The line PSof stoechiometry = 1, with following remarkable points:

    Point P corresponds to k = 0and = 1 , as already described here-above

    point S corresponds to k = 1 and = 1 and is located on the [O2]' axis, since its

    coordinates are :

    2 S 2 S

    1 y 2z (1 )

    2 4

    [ CO ] 0 , [ O ] 3 y 2z y 2x( 1 ) 3.76(1 )2 4 4

    ++

    = =+ + + +

    0 5 10 15 20

    15

    10

    5

    % CO2

    % O2

    QS

    P

    k = 0

    k = 1

    = 1

    LF

    M

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    BIOMASS COMBUSTION 14

    The line SQof partial oxidation k = 1, is a portion of the [O2]'axis.

    Any normal combustion must lead to a figurative point located in triangle PQS, as close as

    possible of point Pif one wishes to minimize the excess of air to obtain flue gases as hot as

    possible, while remaining on line PQof complete combustion.

    Therefore :

    point L, located on line PQ, meets the requirement of complete combustion, but it

    corresponds to a important air excess or lean burn combustion. Except for particular

    technological reasons (low temperature asked for the use of the flue gases, abatement of

    pollutants,), such a point will normally not be retained like standard adjustment.

    point M is obtained by decreasing the air excess coefficient compared to that

    corresponding to the point Land will be preferred for applications where the character of

    not diluted flue gases is desirable, that is to say for thermodynamic reasons(transformation of heat into driving work, transfer of heat,), or for energy reasons

    (minimization of flows carrying heat, heat losses at the chimney, minimization of the

    ventilation power,).

    point Fcorresponds to a rich combustion. Obtained by reducing the air excess near = 1,

    it does not meet the requirement of complete combustion and must be rejected. It

    corresponds indeed to the production of carbon monoxide CO which is at the same time a

    highly toxic compound and a fuel gas from which the LHV is lost.

    3.2. The optimization of the air excessThe thermal quality of a combustion decreases at high values of , since the dilution of the

    flue gases by the air excess reduces the available temperature. On the one hand, a low

    temperature has an unfavorable effect on the kinetics of the combustion itself, and a large air

    excess may paradoxally lead to an incomplete combustion characterized by solid or

    condensable emissions, by quenching effect. On the other hand, a low temperature of the flue

    gases before heat exchange, needs a large size of the heat exchanger and means a low

    efficiency of the energy use, by increasing the relative exhaust losses which may be assumed

    to be at a constant temperature at the chimney.

    The need for a global air excess as small as possible appears therefore as an evidence.

    However, using a statistical reasoning about the air distribution, one may conclude that the

    unburned fraction kdepends on the mean value and on the local deviations of , i.e. on the

    possible misdistribution of the air surrounding the fuel.

    This distribution may be characterized by means of a probability densityp( loc)of the locally

    defined air excess loc . One of the simplest laws for such a distribution is the rectangular

    function:

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    BIOMASS COMBUSTION 15

    loc loc

    1p( ) for (1 ) (1 )

    2 = < < + (16)

    Figure 5

    This distribution (fig. 5) has a mean valueand a standard deviation

    3.

    One may obtain from this distribution function the following results :

    if1

    1