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    copyright reserved 2005, Sasol Technology, 31 January 2005

    SULPHUR BEHAVIOUR IN THESASOL-LURGI FIXED BED DRYBOTTOM GASIFICATION

    PROCESS15-17 May 2007

    M.P Skhonde, RH Matjie, TJ van der Walt, JR Bunt

    2007 Topsoe Catalysis Forum: Sulphur Management

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    Background

    Sasol-Lurgi Fixed Bed Dry Bottom gasification process asdeployed at the Sasol in Secunda, South Africa consumes morethan 30million tons of coal per annum

    Production of more than 150000 barrels/day of fuels andchemicals

    Coal is an abundant resource with a promising future in energy

    and petrochemicals productionCoal is also a potential source of pollution, with increasedutilisation leading to even more environmental footprints

    Coals used in the Secunda operation gasification plant have low

    sulphur content (1-2%) compared to other coals.

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    Sulphur formation in coal

    Sulphur in coal originates from the original plant materials and fromthe ambient fluids in the coal-forming environment

    Sea water interaction with the peat during coal formation will resultin elevated levels of sulphur in coal

    Low sulphur coal seams were deposited in an alluvial environmentand the peat was not influenced by seawater and is derived from

    the parent plant materialHigh sulphur coals are associated with marine strata e.g. HerrinCoal in the Illinois Basin that is overlain by the marine Anna Shale

    and Brereton Limestone

    Organic sulphur is formed by reaction of reduced sulphur specieswith the premaceral humic substances formed by bacterialdecomposition of the peat

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    SO4-2 in sea water

    Bacterial reduction

    Dissolved H2S

    Precipitation of pyrite

    Reaction with Fe

    Sulphur formation in coalSulphur formation in coal

    PyriteFramboids

    CellInfillings

    Reaction withPre-maceral humic substance

    Organically bound

    sulphur

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    Sulphur in coal

    Forms of sulphurin coal

    Organicallybound

    sulphurSulphideminerals

    Sulphate

    minerals

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    Gasification process

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    The fate of sulphur in the Secunda plant

    Sulphur incoals from

    mines

    Coalpreparation

    plant

    Steam plant

    gasification

    SOx

    S in ash

    Gas cooling

    S in gas liquortar/oil/naphtha

    H2S inraw gas

    S recovery unit

    Elementalsulphurproduct

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    H2S emissions reduction options

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    Coal destoning

    Coals from themines

    Coalscreening

    Physicalseparation

    gasification

    Raw gas to gas

    purification

    Fine coal tosteam plant Discard coal

    Cleancoal

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    Sulpholin process

    Upstream gasproduction units Sulpholin units

    Off-gasGranulation unit

    Bagged andunbagged sulphur

    granulesSodium sulphate

    unit

    Sodium sulphatecrystals

    Off-gas stacks toatmosphere

    Untreatedoff-gas Treated

    off-gas

    Moltensulphur

    Sulphur

    granulesSulpholinsolution

    Sodiumsulphatecrystals

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    Sulphur production by chemical absorption

    Upstream gasproduction

    unitsabsorber regenerator

    Clausereactor

    Sulphurproduct

    Aminesolvent

    Off-gas stack toatmosphere

    Treated off-gases

    Selectedoff-gasstreams

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    Sulphuric acid production

    Upstream gas

    productionunits Incineration

    SO2 converter and

    acid plant

    Sulphuric acidproduct

    air

    Offgas stacks toatmosphere

    Selectedoff-gasstreams

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    Sulphur fate in a gasification process

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    Methodology

    SampleNumber

    E32 Top of Gasifier

    Bosman skirt

    D24

    Pyrolysis zone

    C16

    Gasification zoneB8

    Ash bedA1

    Bottom of Gasifier

    Gas

    Ash

    Steam,oxygenor air

    coal

    zone

    drying

    pyrolysis

    gasification

    combustion

    Ash bed

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    Analysis done

    Sulphur content

    Total sulphur (ASTM D4239)Mineral sulphur(ISO157)Sulphate sulphur(ISO157)Organic sulphur(ISO157)

    XRDQuantification on Siroquant

    Computer Controlled Scanning Electron Microscopy(CCSEM)

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    Gasifier temperature profile (Bunt, 2005)

    0

    5

    10

    15

    20

    25

    30

    35

    0200 400 600 800 1000 1200 1400 1600

    Temperature (oC)

    Sample number

    Average temperature Surface temperature Peak temperature

    Drying zone

    Reduction

    zone

    Pyrolysis

    zone

    Slow pyrolysis

    with gasification

    Fast pyrolysis

    Gasification

    Oxidation

    Start of combustion zone

    and ash bed

    E32

    D24

    C16

    B8

    A1

    Gasifier height

    top

    bottom

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    Sulphur content across the gasifier

    FeS2 + H2 Fe(1-x)S + H2S

    Fe(1-x)S + H2 + 2O2

    FeO/Fe2O3 + H2S

    Sulfur behaviour

    0.00

    0.50

    1.00

    1.50

    2.00

    2.50

    S0 01 S0 08 S0 16 S0 24 S0 32

    sample

    sulfur

    content%

    total sulfur

    mineral sulfur

    sulfate sulfur

    organic sulfu

    Bottom gasifier height top

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    Total sulphur to mineral sulphur correlation

    R2 = 0.9679

    0.00

    0.20

    0.40

    0.60

    0.80

    1.00

    1.20

    1.40

    1.60

    1.80

    0.00 0.50 1.00 1.50 2.00 2.50

    Total sulphur

    mineralsulphur

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    Sulphur bearing molecular composition-XRD

    FeS2 + H2 Fe(1-x)S + H2S

    Fe(1-x)S + H2 + 2O2 FeO/Fe2O3 + H2S

    Bottom gasifier height top

    Sulphur species in the crysta lline phase in ash (bas ed o n XR D )

    0.0

    1.0

    2.0

    3.0

    4.0

    5.0

    6.0

    7.0

    8.0

    9.0

    10.0

    1 8 16 24 32

    pyrite

    pyr r hoti teanhydri te

    Hemati te

    Magnetite

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    Sulphur association in ash

    Sulfur bearing mineral association in a gasifier

    0

    1

    2

    3

    4

    5

    6

    1 8 16 24 32

    Gasification samples

    %com

    position

    pyrite cleats

    Kaolinite (pyrite)

    Kaolinite(carbonate,

    pyrite)

    Quartz(carbonate,pyrite)

    Pyrrhotite/Fe-S-O/Fe-Oxide

    Fe-Ca-Al2Si2O5 interactionforming from Pyrite,carbonates & kaolinite

    Some of the FeOparticipate inslagging

    Fe-Al2Si2O5 interactionforming from pyrite &kaolinite

    Pyrite cleatstransformation

    Bottom gasifier height topFe-Ca-SiO2interaction formingfrom pyritecarbonates & quartz

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    Concluding remarks

    Most of the sulphur is released as H2S with small amounts ending up in the ashMost of the H2S comes from the reduction of pyrite to pyrhottite which takesplace in the pyrolysis zoneSome of the pyrhottite is further converted to various oxides of iron leading to

    formation of H2S in the gasification zoneVery small amount end up in the ash as anhydrite as well as part of interstitialand matrix glass compounds such as Fe-Ca-Al2Si2O5, Fe-Al2Si2O5, Fe-Ca-SiO2, and pyrrhotite/Fe-S-O/Fe-OSulphur in ash is retained mainly in:

    Sulphur oxide that reacted with high temperature transformation product (CaO) ofcalcite or dolomite to form anhydrite (CaSO4)As sulphur that reacted with the glassOrganically bound sulphur in unburnt carbon

    Understanding of the mode of occurrence and behaviour of sulphur important

    for development of sulphur capture methodsUnderstanding the behaviour of sulphur in a Sasol-Lurgi Fixed Bed Dry BottomGasification process and applying proven gas conditioning techniques,solutions to an emissions-free gas island are in reach

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    Thank you for your attention!!!

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    Minerals transformation at elevated temperatures

    Understanding of minerals transformation necessary for understanding ofpollutants emissions during coal processing

    During Combustion pyrite transforms to iron oxides, and

    In presence of C, Fe is produced and can react with other inorganic elements to

    form spinnel, srebrodolskite (Ca2Fe2O5), magnesioferrite (MgFe2O4), andbrownmillerite (Ca4Al2Fe2O10)

    Kaolinite (Al4Si4O10(OH)8) forms mullite(3Al2O3.2SiO2), alumina (Al2O3) andcristoballite (SiO2).

    Illite (K1.5Al4(Si6.5Al1.5)O(OH)4) forms spinnel and mulliteQuartz (SiO2) is non reactive but transforms to other forms -quartz, -quartz(573-870C), 2-tridymite (870-1470C), and 2 cristobalite (1470- hightemperatures) to form a liquid.Excluded carbonate minerals calcite (CaCO3), dolomite (CaMg(CO3)2), siderite(FeCO

    3), ankerite ((Fe, Ca, Mg, (CO

    3)3) are found in most bituminous coals.

    Calcite fragments at high temps(1000C) to form qui cklime (CaO).CaO react with water and sulphur oxides to form portlandite (Ca(OH)2) andanhydrite (CaSO4)At high temperatures (>1000C) CaO interacts with m ore reactive aluminium

    silicate such metakaolinite to form gehlenite (Ca2Al2SiO7) andanorthite (CaAl2Si2O8)