Ppt_biowaste Treatment and Soil Protection

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    Bio-waste Treatment and

    Soil Protection

    Luca Montanarella

    European Commission

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    EU Thematic Strategy for Soil Protection

    adopted by the European Commission on

    the 22nd of September 2006

    COMMUNICATION COM(2006) 231 on the Thematic Strategy

    for Soil ProtectionDIRECTIVE COM(2006) 232 establishing a framework for the

    protection of soil and amending Directive 2004/35/EC

    IMPACT ASSESSMENT SEC(2006) 620 of the Thematic

    Strategy for Soil Protection

    http://ec.europa.eu/environment/soil/index.htm

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    Recognizing soil multi-functionality

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    ACTIONS AND MEANS of the Soil Thematic

    Strategy

    Still to be implemented:Framework legislation with protection and sustainable use

    of soil as its principal aim;

    Already in the implementation phase:Integration of soil protection in the formulation and

    implementation of national and Community policies;

    Research supported by Community and national research

    programmes;Public awareness of the need to protect soil.

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    Integration of soil protection in EU policies

    Common Agricultural Policy (CAP)Climate Change Policy

    Water Protection Policy

    Biodiversity Protection PolicyForest Protection Policy

    Regional Policies

    Food Safety (EFSA)

    Energy Policy

    Development PolicyWaste Policy

    ..etc

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    Bio-waste as a major source of soil organic carbon

    OriginTurnover

    Complexity

    Decomposing fresh OM(Particulate organic matter)

    Microorganisms

    Colloidal OMPolysaccharides and biomolecules

    Humic substances

    soluble OM

    -OH

    CO2Corg

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    Biota

    560 Gt

    Atmosphere

    780 Gt+3.3 Gt/yr

    Soils

    2,500 Gt(i) SOC - 1,550 Gt

    (ii) SIC - 950 Gt

    Ocean

    38,400 Gt + 2.3 Gt/yr(i) Surface layer: 670 Gt

    (ii) Deep layer: 36,730 Gt

    (iii) Total organic: 1,000 Gt

    Fossil Fuels

    4,130 Gt

    (i) Coal: 3,510 Gt

    (ii) Oil: 230 Gt(iii) Gas: 140 Gt

    (iv) Other: 250 Gt

    120 + 2.0 Gt/yr (photosynthesis)

    Plant respiration60 + 1.6 Gt/yr

    60 Gt/yr

    7.5 Gt/yr

    Fossil fuelcombustion

    90 Gt/yr

    0.6+0.2 Gt/yr(deposition)

    60Gt/yr

    (soilr

    espira

    tion)

    Accel

    eratedsoil

    erosio

    n

    1.1+0

    .2Gt/yr

    (erosio

    n)MRT = 5Yr

    MRT = 25Yr

    1.6 + 0.8 Gt/yr

    Deforestation

    MRT = 6Yr

    92.3 Gt/yr

    Biomass (food, fiber, fuel, etc)

    Bio-waste returning to the soil organic carbon pool?

    Global Carbon Pools and Dynamics

    Human activities

    (adapted from R. Lal, 2008)

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    Organic Carbon (%)No Data0 - 11 - 22 - 55 - 1010 - 2525 - 35> 35

    Organic carbon content (%) in

    the surface horizon (0-30 cm) ofsoils: total 71 GtC in EU

    Organic CarbonGt

    0.02.55.07.510.012.5

    15.0

    0.5 3.5

    5.0

    1.67.1

    0.30.8 5.8

    0.7

    2.0

    0.6

    5.6

    5.7

    13.8 12.5

    1.5

    1.8

    1.1

    1.1 0.6

    1.2 1.00.2

    0.5 0.5 1.0

    2.3

    1.0

    0.20.6

    0.2

    0.2

    National Soil Organic Carbon

    stocks (0-30cm) in Gt.

    Model output Aggregated results

    Soil Organic Carbon Stocks Assessment

    Source: JRC-IES

    S il O i C b D i d Gl b l

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    CELL(structuralpolysaccharides)

    HUM(humic

    and protected)

    STABLE

    mineralization

    microbial

    synthesis

    0.3 yr

    LIGNIN

    2.5 yr

    LABILE

    0,87 yr

    25 yr

    3300 yr

    numerical values forsoil/land use =- 20% clay- temperature 12C- water/porevolume >

    0,4- annual crops conv.tillage

    CO2

    CO2

    CO2

    Vegetation, organic input

    Primary production,quality

    Soil, Land

    Use,Climate

    Balesdent, 2000

    Model of soil carbon

    dynamics

    Soil Organic Carbon Dynamics and Global

    Climate Change

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    Fig. 3 A schematic of the soil C dynamics upon conversion from a natural to agriculturalecosystem, and subsequent adoption of recommended management practices(RMPs). In most cases, the maximum potential equals the magnitude of historic Closs. Only in some soil-specific situations, the adoption of RMPs can increase SOCpool above that of the natural system. An example of this is acid savanna soils ofSouth America (Llanos, Cerrados) where alleviation of soil-related constraints candrastically enhance the SOC pool.

    Time (Yrs)

    100

    80

    60

    40

    20

    0

    20 40 60 80 100 120 140 160

    RelativeMagnitudeofSOCPoo

    l

    land useconversion

    subsistencefarming,

    none or lowoff-farm

    input, soildegradation

    newequilibrium

    adoption ofRMPs

    soilCs

    in

    k

    capacity

    Accelerated erosion

    Attainablepotential

    Maximumpotential

    Innovativetechnology I

    Innovativetechnology II

    X

    YRate

    Soil C Dynamics

    Source: R. Lal, 2008

    Wh l i SOC i

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    Where can we lose or gain SOC in

    Europe?

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    Estimation based on Eurostat data on munic ipal waste (2008)

    ORBIT/ECN, 2008, Compost production and use in the EU, Final report of ORBIT e.V. / European Compost Network ECN to European

    Commission, Joint Research Centre

    (http://ipts.jrc.ec.europa.eu/activi ties/sustainable_development/susproc.cfm)

    Total biowaste and green waste arising in the European Union

    The total annual arising of bio-waste in the EU is estimated at 76.5-102 Mt food and garden waste

    included in mixed municipal solid waste plus 24 Mt non-household green waste and industrial waste,i.e. from the food industry.

    U b d R l E

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    Urban and Rural Europe

    AC EU15

    Group

    60.00 70.00 80.00 90.00

    % Urban population

    5.00

    10.00

    15.00

    20.00

    %B

    uilt-upare

    a

    BG

    CZ

    LVLT

    PL

    RO

    SK

    MT

    AT

    BE

    DK

    FI

    FR

    DE

    GR

    LU

    NL

    ES

    UK

    Transport of bio-waste from urban

    to rural areas in Europe?

    The need for a partnership between the

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    The need for a partnership between the

    Urban and the Rural communities

    Bio-waste

    Biomass

    Max. distance 50 km

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    Quality standards for Bio-waste are needed

    Acidification and heavy metals distribution in

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    Acidification and heavy metals distribution in

    European soils

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    Innovative technologies: BIOCHAR

    Source: N. de Wit, 2009

    BIOCHAR potential feed stocks, products

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    p , p

    and applications

    Source: N. de Wit, 2009

    C l i

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    Conclusions

    European soils are threatened by a constant loss of soilorganic carbon

    Bio-waste could provide a win-win solution to wastedisposal and soil organic carbon restoration

    Major effort is still needed in assuring sufficient qualityof the materials to be spread on soils

    There is a need to build up confidence by land owners

    that the organic materials are indeed beneficial to soilsand therefore to the quality of agricultural products

    Innovative technologies could provide new solutions tothe disposal of bio-waste in European soils

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    Thank you!

    http://eusoils.jrc.ec.europa.eu/ http://ies.jrc.ec.europa.eu

    http://eusoils.jrc.ec.europa.eu/http://eusoils.jrc.ec.europa.eu/