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    973 2

    RELEASE OF FUEL BOUND NITROGEN IN BIOMASS DURING HIGH

    TEMPERATURE PYROLYSIS AND GASIFICATION

    Jiachun Zhou

    Mechanical Engineering Department

    Universityof Hawaii at Manoa

    2540 Dole Street

    Honolulu, Hawa ii 96822

    Phone: (808)956-2342; Fax: (808)956-2335

    Stephen M. Mas utanil, Darren M. ishimura,

    Scott

    Q.

    Turn, Charles M. Kinoshita

    Haw aii Natural Energy Institute

    University of Hawaii at Manoa

    2540 Dole Street

    Honolulu, Hawaii 96822

    ABSTRACT

    Pyrolysis and gasification of two biomass feedstocks with

    significantly different fuel-bound nitrogen (FBN) content were

    investigated to determine the effect of operating conditions on

    the partitioning of FB N among gas species. Experiments w ere

    performed in a bench-scale, indirectly-heated, fluidized bed

    reactor. Data were obtained over a range of temperatures and

    equivalence ratios representative of commercial biomass gasi-

    fication processes. An assay of all major nitrogenous comp o-

    nents of the gasification products was performed for the first

    time, providing a clear accounting of the evolution of FBN.

    Results indicate that: (1)

    NH3

    is the dom inant nitrogenous gas

    species produced during pyrolysis of biomass; 2) the majority

    of FBN is converted to NH3 or N2 during gasification; relative

    levels of NH3 and N2 are determined by thermochemical reac-

    tions which are affected strongly by temperature; (3) N2

    appears to be produced from NH 3 in the gas phase.

    INTRODUCTION

    During pyrolysis and gasi f ica t ion of b iomass fue ls ,

    nitrogenous com pound s, such as ammonia (NH3), hydrogen

    cyanid e (HCN), and oxides of nitrogen (NO NO2 or NO,;

    N 20 ) may evolve from fuel-bound nitrogen

    (FBN).

    These gas-

    phase pollutants pass through end-use systems with the

    synthesis gas, where they can poison catalysts or may undergo

    further oxidization and be emitted as NO,, which is the primary

    contributor to photo chem ical smog. Although research on

    biomass gasification has been pursued for many years, to date

    only a few studies have been conducted on the formation,

    deposi t ion , and aba tement of n i t rogenous pol lu tants .

    Additional effort in this area is warranted given the current

    Gasification Combined Cycle) power systems and liquid fuel

    syn the s i s .

    interest in utilizing biomass gas for

    IGCC

    (Integrated

    'author

    to

    whom correspondence should be

    addressed

    Although fuel nitrogen chemistry in coal combustion and

    gasification systems has been extensively investigated, it is

    unclear whether these results can be applied to biomass, since

    nitrogen is bound in different forms in these two solid fuels.

    Earlier work suggests that fuel structure significantly

    influences FBN evolution.

    The format ion of n i t rogen-conta in ing spec ies dur ing

    biomass gasification ha:: been investigated by several

    researchers ( Ish imura e al. 1994; Furman et

    al.

    1992;

    Leppalahti, 1993; Evans

    ef

    al. 1988). Thes e studies identified

    NH3, HCN, and N2 as the major nitrogenous components of the

    synthesis gas and documented effects of varying gasification

    conditions on their concenlrations . In all of these studies, N2

    levels were inferred from a nitrogen balance rather than

    measured d i rec t ly . Hence , som e uncer ta in ty remains

    concerning the partitioning of FBN.

    Reaction pathways that have been proposed for biomass

    FBN evolution are largely based on models developed for coal

    combustion and gasification. The extent to which these

    models apply is unclear due to the aforementioned differences

    in fuel structure.

    In order to clarify the mechanisms by which biomass FBN is

    released and converted during gasification and pyrolysis, an

    investigation was initiated comprising experimental and

    mode l ing compone n t s . Th i s pa pe r summ a r i z e s t he

    experiments. Results of the modeling study are provided in

    Zhou

    t

    al. (1997).

    PROCEDURES

    A series of biomass gasification and pyrolysis experiments

    were performed. In the p:yrolysis tests, no oxidizing gas was

    supplied to the reactor; however, oxidation reactions occurred

    due to fuel-bound oxygen and moisture contained in the

    biomass.

    Experiments were performed in a bench-scale fluidized bed

    reactor. Th e reactor consists of an 89 mm i.d. stainless steel

    pipe enclosed within a stack of electric heaters that allow

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    uniform temperatures to be maintained in the fluidized bed.

    0.21-0.42 mm diameter Alum ina beads comprise the bed

    which has a static height of about 700 mm. Biomass is fed

    into the reactor from a sealed hopper with an auger-type screw

    feeder. Gases pass through a high temperatur e char filter

    before entering the sampling system . Details of the facility

    are given in Zhou (1994) and Ishimura (1994).

    The m ajor nitr ogen ous species, NH,, N2, HCN , and NO,,

    were quantified either on-line or by off-line analysis of

    extracted gas samples. A gas chromatograph (GC), ion-

    specific electrodes (ISE), and a chemiluminescence analyzer

    (CLA) comprised the principal instrumentation employed in

    this study.

    A nitrogen species gas sampling system was installed

    downstream of the sintered metal char filter. NH3 and HCN

    were collected by absorption into liquid solutions and

    measured with ISEs. The NH3/HCN samp ling train consisted of

    four bubblers arranged in series. Th e first two bubblers were

    filled with 15 0 ml of 0.1-M su lfuric acid (H2S0 4) used to trap

    NH,. Th e remaining bubblers were filled with a mixture of 145

    ml of 0.1-M sodium hydroxide (NaOH) and 5 ml of 0.117-M

    lead acetate trihyd rate (Pb Ace03 H20) which reacts with and

    absorbs HCN.

    Downstream

    of

    the bubblers, a small slipstream of the

    biomass synthesis gas was directed into a CLA to detect and

    quantify NO,. The CLA was calibrated before each experiment

    with two certified EPA Protocol gas mixtures containing 9 and

    90

    ppm NO in N2. The CLA was recalibrated after each test run

    to assess instrument drift . Since the accuracy of CLA

    measurements of NO may be affected by other species present

    in the synthesis gas mixture, (e.g., H2 and CO) a correction

    recommended by Matthews

    et al.

    (1977) was applied to the raw

    data.

    A second sampling train in parallel with the NH,/HCN

    bubblers was used to collect synthesis gas samples and

    nitrogenous tars. Gases were analyzed with a Perkin-Elm er

    Auto System GC equipped with a thermal conductivity detector

    (TCD). A stainless steel packed column (12.2 m x 3.2 mm)

    from Alltech Associates, Inc. was em ployed to separate the

    adjacent Ar, 0 2 , and N2 chromato gram peaks. Analyses were

    conducted at low chamber temperatures and carrier gas flow

    rates. A PE Nelson Model 1020 Personal Integrator interfaced

    with the GC was used to determine gas concentrations from the

    chrom atogram s (manual integration w as sometime s used to

    infer 0 2 concentrations). The GC was calibrated with two gas

    mixture standards that had compositions similar to the

    biomass gas.

    Difficulty in quantifying N2 to date has prevented a

    comprehensive inventory of FBN products. In the present

    system, contamination of samp les by ambient air posed the

    greatest problem (the tests used an O;?/Ar mixture, ra ther than

    air, to gasify the biomass). Since the gasifier was operated at

    positive internal pressures and the fuel hopper was sealed, the

    possibility

    of

    tramp air leaking into the gasifier is negligible.

    Any contamination therefore arose from air leaks into the

    collection bulbs and vials, or the

    G

    during sampling and

    analysis. Fortunately,

    air

    contamination

    of

    this type can be

    identified via its O2 content.

    Since gasification occurs with a deficiency of oxidizer, both

    experiments and simulations indicate that residual O2 levels in

    the products are negligibly low. 0 detected by the GC

    analysis may then be attributed to air contam ination. The

    known N2 /0 2 ratio in the air can be applied to quantify the

    'contaminant' Nz from the 0 2 measurements. This amount may

    then be subtracted from the total N2 detected with the GC to

    estimate N2 from FBN.

    Two types of biomass, leucaena and sawdust, containing

    significantly different amounts of FBN, were gasified and

    pyrolized in these experim ents. Leucae na, a fast-grow ing

    nitrogen-fixing plant, is being considered as a potential

    dedicated energy crop (Hubbard

    &

    Kinoshita, 1993). Th e low-

    FBN sawdust which was used consisted of a mixture of several

    hardwood species (e.g., fir, poplar, oak ash). Proxim ate and

    ultimate analyses of these feedstocks are provided inTable 1.

    TABLE

    1

    ANALYSES OF FEEDSTOCKS

    Leucaena

    Proximate A nalysis,

    Mo i s tu re 10 .4

    Volatile Matter 74 .28

    Fixed Carbon 18 .54

    A sh 7 .18

    Ultimate Analysis, (dry basis)

    [C]: Carbon 48. 43

    [HI: Hydrogen 5. 64

    [O]: Oxygen 36.02

    [SI: Sulfur 0.22

    [N]: Nitrogen 2.5 1

    A sh 7 .18

    Sawdust

    7 . 6 8

    7 7 . 7 0

    1 4 . 2 8

    0 . 3 4

    4 8 . 4 5

    5 . 1 1

    4 6 . 0 1

    0 . 0 3

    < 0.1

    0 . 3 7

    The leucaena, which consisted of leaves and small branches,

    was harvested and exposed to air for several day s to reduce its

    moisture content. Both sawdust and leucaena feedstocks were

    milled to yield particles less than 3 mm in size.

    Parametric tests were performed to investigate the effects of

    operating parameters on FBN evolution in pyrolysis and gasi-

    fication. Parameters that were varied included bed temperature

    and equivalence ratio (ER). ER is defined as the actual oxidizer-

    to-fuel ratio (mass basis) divided by the stoichiometric

    oxidizer-to-fuel ratio.

    ER

    ranged from 0.18 to 0.40 in the

    gasification tests. Bed temperatures between 700" to 950"C,

    which are representative of commercial gasifiers (Wang,

    1991), were investigated. No steam was injected during any of

    the tests although the biomass feedstocks contained small

    amounts of moisture. Biomass feed rate was about 3 kg/h.

    In the pyrolysis tests, the bed was fluidized by injection of

    pure argon. Low biomass feed rates (0.73 to 0.87 kg/h) and

    high argon flow rates were employed to limit reactions

    between char and gas species and minimize their effect on the

    gas species concentration data.

    EXPERIMENTAL RE SULTS AND DISCUSSION

    P v r o l v s i s

    Tests

    Te s t s w e re pe r fo rme d to de t e rmine the r e l a t i ve

    concentrations of gas-phase nitrogen species produced by

    pyrolysis of biomass, and to investigate the influence of

    temperature on this process. Species concentrations, on an

    inert-free basis, are plotted against temperature in Figure 1 .

    These results are for leucana feedstock.

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    TABLE 2 FUEL NITROGEN PARTITIONING DURING

    PYROLYSIS

    OF

    LEUCAENA

    u .

    700

    750 800 850

    9

    TP-3

    (a) NH3 concentration vs. temperature.

    2oOT

    7 75 800 850 900

    (b) NO and HCN concentration vs. temperature.

    T C)

    FIGURE

    1

    NITROGENOUS SPECIES CONCENTRATIONS

    IN PYROLYSIS GAS (LEUCAENA)

    As pyrolysis temperature increases from 700C to 900"C,

    NH3 levels are observed to decline by a factor of six from about

    48,000 ppmV to 8,000 ppmV. HCN and NO concentrations

    also fall (from around 20 ppmV to less than 10 ppmV for HCN

    and from 1 70 ppmV to around 40 ppmV for NO), albeit less

    drastically. NH3 was detected at much higher concentrations

    than the other two nitrogen species.

    These results indicate

    that NH3 is the dominant nitrogenous pyrolysis product and

    that levels of the three nitrogen pollutants decrease with

    pyrolysis temperature.

    The measured partitioning of FBN is given in Table 2.

    Pyrolysis reactions convert less than 1% of the fuel nitrogen

    into HCN and N O at the conditions examined.

    As

    temperature

    increases from 700C to 9OO"C, the fraction of FBN remaining

    in the char decreases from about

    50

    to 41%.

    Most of the fuel

    n i t rogen appa ren t ly evo lves a s NH3 and N2, with

    decomposition of

    NH3

    being a probable source of the

    N2

    (Ishimura, 1994).

    T C 7 0 0 '750 8 0 0 8 5 0 9 0 0

    N(NOx)/Nf% 0.19

    0 . 1 9

    0 . 1 4 0 . 1 0

    0 . 0 8

    N(NH3)/Nf,%

    5 4 . 1 3 4 8 . 7 4

    2 5 . 8 1 1 3 . 4 9

    1 0 . 4 8

    N(HCN)/Nf% 0.02

    0.03 0.01

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    35 T

    NH3 N2

    75

    800 850

    900

    950

    TW

    FIGURE

    3

    VARIATION OF NH3 N2 CONCENTRATIONS

    WITH TEMPERATURE (LEUCAENA; ER=0.25)

    Measured NH3 and N2 concentrations in the gasified leucaena

    are plotted against temperature in Figure 3. NH3 decreases

    sharply from approximately 31,000 ppmV at 750C to 6,000

    ppmV at 900C. A slight increase in NH3 is observed at

    950C. Over the same temperature range, molecular nitrogen

    (N2 ) generally increases with temperature (9,500 ppmV to

    17,000 ppmV); however, the data suggest that a small decrease

    in Nz may occur between 900C and 950C. Th e high levels of

    NH3 in the product gas are consistent with the results of the

    pyrolysis tests. Since NH3 and z exhibit opposite trends in

    response to changes in temperature, there may be a basis to

    propose that conversion of NH3 to N2 is the critical thermo-

    chemical path in the evolution

    of

    FBN during gasification of

    b ioma ss .

    Concentrations of NO and HCN are plotted against gasifier

    bed temperature in Figure 4. NO decreases from 30 ppmV at

    750C to 5 ppmV at 95OOC; HCN concentration falls from

    55

    ppmV at 750C to 30 ppmV at 950C. The measurements

    indicate that these two species exist in the synthesis gas at

    levels two to three orders of magnitude smaller than NH3.

    A HCN NO

    O 40

    2

    8

    3

    2

    I I

    I

    750

    800

    85

    900 95

    T

    ( C)

    FIGURE

    4

    VARIATION OF NO HCN CONCENTRATIONS

    WITH TEMPERATURE (LEUCAENA; ER=0.25)

    The distribution of leucaena FBN among the nitrogenous

    species NH,, N2, NO, and HCN for

    ER

    = 0.25 (7 50 T to 950C)

    is presented in Table 3. Mo st of this nitrogen forms NH3 and

    N2; less than 1 of the FBN is detected as HCN and NO, The

    strong influence of temperature is apparent from the data:

    between 750C and 950"C, the fraction of FBN present as NH3

    in the synthesis gas decreases from approximately 60% to

    10%.

    Over this same temperature range, fu el nitrogen existing

    as

    N

    increases from

    40

    to about 85%. It also is interesting

    to note that the slight increase in NH3 me asured between

    900C and 950C exactly compensates for the corresponding

    decrease in N2.

    TABLE3 FUEL NITROGEN PARTITIONING AS A

    FUNCTIONOFTEMPERATURE (LEUCAENA; ER=0.25)

    T C 7 5 0 8 0 0 8 5 0 9 0 0 9 5 0

    N(NOx)/Nf,% 0.06

    0.04

    0 . 0 2 0.02

    0.01

    N(NH3)/Nf,%

    6 3 . 5 48.74

    2 5 . 8 1 1 3 . 4 9 1 0 . 4 8

    N(HCN)/Nf,% 0.11

    0.09

    0 . 0 8 0 . 0 7 0.07

    N(char)/Nf,%

    7.7

    5 . 2 2 . 0 2 . 0 1.2

    N(N2)/Nf,% 38.6

    6 9 . 9 8 0 . 3 8 8 . 7

    8 5 . 7

    Concentration data from the sawdust gasification tests are

    plotted in Figure

    5.

    NH3 is observed to decrease from 950

    ppmV at 700C to about

    400

    ppmV at 900C. NO and HCN are

    again detected at much lower levels than NH3. Wh ile the

    general trends agree with the leucaena results, differences in

    the FBN content of the two feedstocks once again are

    manifested in the large difference in absolute values of

    concentrations of nitrogenous species. The exception

    to

    this

    is NO, which was detected at higher levels in the gasified

    sawdust. This behavior is not presently understood and

    warrants additional study.

    1000

    8 800

    8

    6

    8

    400

    3

    NH3

    A HCN

    NO

    7 750

    800

    850 900

    T PC

    FIGURE 5 NITROGENOUS SPECIES CONCENTRATIONS

    VERSUS TEMPERATURE (SAWDUST, ER=0.25)

    As mentioned previously, this study is the first to report a

    comprehensive inventory of FBN for biomass gasification.

    The present m easurem ents of N2 confirm that this species

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    accounts for the large quantities of fuel nitrogen denoted as

    " miss ing" i n p rev ious i nve s t iga t ions . A l though the

    possibili ty of contamination of samples with ambient air

    introduces a level of uncertainty into the data, relatively good

    closure was attained in the nitrogen balance which ranged from

    about 98%

    to

    120% for the leucaena experiments. On the other

    hand, the carbon balance for the same tests fell between 94%

    and 98%. Th is suggests that further refinement of the nitrogen

    spe c i e s me a su re me n t sy s t e ms a nd p ro toc o l s ma y be

    worthwhile pursuing.

    Theoretical calculations have determined that the optimum

    range of equivalence ratios for biomass gasification is 0.2 to

    0.4 (Wa ng, 1991). Tests were performed at three values of ER

    within this range to examine the effect of this parameter on

    Fl3N chemis try. It was discovered that, unlike temperature, ER

    does not significantly impact concentrations of nitrogenous

    species in the synthesis gas. Figures 6 and 7 summarize the

    influence of both ER and temperature on the amounts of NH3

    and N2 produced when leucaena is gasified.

    30000

    a

    25000L\^ ^ ^ ^

    A ER=0.18

    ER=0.25

    ERd.32

    750 800 850 900 950

    TW)

    FIGURE6 NH3 CONCENTRATION AS A FUNCTION OF

    TEMPERATURE AND ER (LEUCAENA)

    20000

    15000

    e

    5

    10000

    0

    ER=O.18

    ER=0.25

    5000]

    ~

    ,

    R=O.32

    750

    800 850 900 950

    T

    C)

    FIGURE7 N2 CONCENTRATION AS A FUNCTION OF

    TEMPERATURE AND ER (LEUCAENA)

    At temperatures in excesfs of 800C , NH3 conce ntrations

    measured at three values of ER are comparable. Th e Nz results,

    presented in Figure

    7,

    appear to be more sensitive to ER . This

    may, however, simply reflect the greater uncertainty in these

    data.

    Figure 8plots the variation of NO and H C N with ER at

    800C. Higher ER appears to favor lower concentrations of

    both of these species. These changes in NO and HCN levels,

    however, do not significantly impact the partitioning of FBN

    since NO and HCN account for a very small fraction of the fuel

    nitrogen

    (4 ).

    0.1

    0.2

    0.3

    0.4

    ER

    FIGURE8 VARIATION OF NO AND HCN WITH ER

    AT 8 C (LEUCAENA)

    The modest inf lu ence of ER o n concentra tions of

    nitrogenous species is supported by the results of the sawdust

    gasification experiments. A:< seen in Figure 9 , a change in ER

    from 0.25 to

    0.37

    only induces NH3 concentrations to increase

    from 310 ppmV to 350 ppmV. Th e single data point at ER

    =

    0.18 suggests that NH3 may be affected strongly by this

    parameter below ER

    =

    0.25. No experiments were performed at

    ER