New Zealand Biochar Reseach Center Workshop 2010

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    Marta Camps

    BIOCHAR RESEARCH AT THE NZBRC.

    THE SOIL SCIENCE STREAM

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    RESEARCH ON BIOCHAR AND SOILS

    C sequestration- C recovery

    - C stability

    - how to account for

    the stable fraction?

    - decomposition

    rates

    - priming effect on

    NOM

    Added value

    Feedstock/

    productionCharacterisation

    - available nutrients

    - liming equivalence- activation surface

    charge

    - determining CEC

    and other surfaceproperties

    Behaviour in

    soils

    - nutrient fertility

    - water retentioncapacity

    LIFE CYCLE ANALYSIS+ LOGISTICS + ECONOMICS

    POLICY MAKERS/STAKEHOLDERS

    - nutrient fertility

    - water retentioncapacity

    - C recovery

    - C stability

    - available nutrients

    - liming equivalence- activation surface

    charge

    - how to account for

    the stable fraction?

    - determining CEC

    and other surfaceproperties

    - decomposition

    rates

    - priming effect on

    NOM

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    BIOCHAR AND CARBON SEQUESTRATION

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    CARBON RECOVERY AND STABILITY

    C recovery (%)

    Corn stover HC 57Corn stover BC 350 55

    Corn stover BC 400 48

    Corn stover BC 550 45

    Biochar

    Biochar Hydrochar

    Hydrochar

    PYROLYZER

    PRESSURE

    VESSEL

    Biochar

    Biochar Hydrochar

    Hydrochar

    PYROLYZER

    PRESSURE

    VESSEL

    C=100 C=100

    C~50

    C~50

    C~60

    C~40

    Chemical

    Products

    Water

    Volatile

    Compounds

    (Bioenergy)

    BiomassAgricultural and forestry

    residues, grasses, etc

    Hydrochar ProcessBiochar Process

    A.B. Fuertes (persona communication)

    Pressure reactor used for thehydrothermal carbonization of biomass

    Rotatory drum kiln

    PRODUCTION PROCESS

    Fu

    ertes et al. (unpublished)

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    CARBON RECOVERY AND STABILITY

    2

    1

    3

    9

    7

    6

    5

    4

    8

    10

    1

    0

    2

    0.0 1.00.2 0.4 0.6 0.8

    (O/C) atomic ratio

    0.5

    1.5

    (H/C)atomicratio

    Decarboxylation

    Dehydration

    Demethanation

    Reaction Lines

    CS

    HC

    BC

    1 Wood

    2 Cellulose

    3 Lignin

    4 Peat

    5 Lignite

    6, 7, 8, 9 Bitum. coals

    10 Anthracite

    350

    400

    550 oC

    400 oC

    350 oC

    HC% volatiles Cdicro (%)

    CORN STOVER 350 45 33.1

    CORN STOVER 400 31 21.9

    CORN STOVER 550 19 14.6Modified from Fuertes et al. (submitted to Aust. J. Soil Res.)

    aromaticpeak

    O-subst.

    aromatic C

    methoxyl C

    Alkyl C

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    CARBON RECOVERY AND STABILITY

    (c)

    (d)

    (e)

    (f)

    (a)

    (b)

    Fuertes et al. (submitted to Aust. J. Soil Res.)

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    tc

    BCS (0)

    BCS (100)

    100time (years)0

    HOW TO ACCOUNT FOR THE STABLE C?

    Frac tion o f the initia l amo unt of b ioc har-C

    tha t is stab le over 100 yea rs

    In the c ontext of b ioc har-C a s a GHG mitiga tion a c tivity, any amount o f Cstored awa y from the a tmosphere for a t lea st 100 yea rs c an be c omputed as

    a GHG mitiga tion benefit

    Ca rbon Gold p rop osed me thod ology: (volatile C/ fixed C) < 0.5 b ioc har assumed inert

    Pigneri et al. (2009)

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    AVAILABLE C?

    Pine

    400 oC 1 m2 g-1

    550 oC 368 m2 g-1

    Poplar

    400 oC 3 m2 g-1

    550 oC 55 m2 g-1

    Willow

    400 oC 3 m2 g-1

    550 oC 149 m2 g-1

    Calvelo-Pereira et al. (NZBRC worshop-2010)

    N2-BET

    400 oC-biochar 550 oC-biochar

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    AVAILABLE C?

    Calvelo-Pereira et al. (NZBRC worshop-2010)

    pH

    5.7

    7.27.5

    5.2

    8.8

    8.6

    We c annot justify the sequestra tion o f ca rbon on thebasis of the C c ontent and stab ility in the b ioc har,indep end ently of the evo lution of the b ioc har in soils

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    PRIMING EFFECT ON NOM DECOMPOSITION?

    Te Anau soils (Molloy, 1993)

    Waiareka soils (Molloy, 1993)

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    THE ADDED VALUE OF BIOCHAR

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    Hydroponics.co.nz

    Woodville

    BIOCHAR AND NZ SOILS

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    SURFACE CHARGE

    282 284 286 288 290 292 294

    Binding energy (eV)

    Intensity

    (a.u.)

    (c)

    (b)

    (a)

    C 1s core level spectra(Yao et al., submitted to Chemosphere)

    BS biochar

    BS biochar

    + water

    BS biochar +

    water +HA

    Simulating a rain of 1000 mm during 80 years

    in the lab...CHx, C-C/C=C

    -C-OR

    >C=O

    >COOR

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    + alkaline tannery waste

    + pyrolysis

    C 1s core level spectra(Hina et al., submitted to Aust. J. Soil Res.)

    Activating in the lab...

    SURFACE CHARGE

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    EU-control EU-diluted EU-concentrated

    PI-control PI-diluted PI-concentrated

    SURFACE CHARGE

    (Hina et al., submitted to Aust. J. Soil Res.)

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    R = 0.94

    0.0

    0.2

    0.4

    0.6

    0.8

    1.0

    1.2

    1.4

    1.6

    1.8

    0 20 40 60 80 100

    TotalHClextractablebases(keqt-1)

    Lime equivalence (kg CaCO3 t-1)

    LIMING EQUIVALENCE

    (Aitkenhead et al., in preparation)

    Umbrisol

    Podzol

    pH: 5.7 7.2 7.5 5.2 8.8 8.6

    Ash %: 2.6 4.0 5.7 3.1 6.5 5.2

    (Calvelo-Pereira et al., NZBRC workshop-2010)

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    0

    1

    2

    3

    4

    5

    6

    7

    8

    0 5 10 15 20

    Biomass(gdryweig

    ht)

    Rate of application (t/ha)

    BS (0 mg N)

    BG (0 mg N)

    BS (200 mg N)

    BG (200 mg N)

    NUTRIENT FERTILITY

    (Wisnubroto et al., NZBRC workshop-2010)

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    NUTRIENT FERTILITY

    0

    1

    2

    3

    4

    5

    6

    7

    8

    0 5 10 15 20

    Biomass(gdryweight)

    Rate ofapplication (t/ha)

    BS (0 mgN)

    BG(0 mgN)

    BS (200 mgN)

    BG(200 mgN)

    (Wisnubroto et al., NZBRC workshop-2010)

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    THANK YOU!!!

    www.biochar.co.nz