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Vegetalia 2010, Cremona 20/03/2010 1 Il contributo potenziale dei suoli Europei nel contrastare l’effetto serra Luca Montanarella Commissione Europea

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  • Vegetalia 2010, Cremona 20/03/2010 1

    Il contributo potenziale dei suoli Europei nel contrastare l’effetto serra

    Luca Montanarella

    Commissione Europea

  • Vegetalia 2010, Cremona 20/03/2010 2

    Role of soils in global climate change

    Carbon dioxide (CO 2)Soil Organic Carbon pools and their evolution in time under different

    management practices: Soils as sink or source of CO2Methane (CH 4)

    Emissions in anaerobic conditions, role of permafrost areas, role of wetlands and peat resources

    Nitrogen oxides (N 2O, NOx)Microbial processes of denitrification and nitrificationFertilizer and manure inputs

  • Vegetalia 2010, Cremona 20/03/2010 3

    Global Warming Potential, IPPC 1996

    G as/Tim e Span 20 years 100 years 500 years

    Carbon dioxide (CO 2) 1 1 1

    M ethane (CH 4) 56 21 6.5

    Nitrous Oxide (N 20) 280 310 170

  • Vegetalia 2010, Cremona 20/03/2010 4

    Effect of Nitrogen Fertilization on N2O Emissions

  • Vegetalia 2010, Cremona 20/03/2010 5

    without Nitrogen fertilization with Nitrogen fertilization: mineral and manure

    Effect of Nitrogen Fertilization on N2O Emissions

    Source: JRC-IES/CAPRI Project

  • Vegetalia 2010, Cremona 20/03/2010 6

    Drained peatlands

    EUEUEUEU----25:25:25:25:

    7% 7% 7% 7% peatpeatpeatpeat areaareaareaarea

    ~4% ~4% ~4% ~4% draineddraineddraineddrained peatpeatpeatpeat areaareaareaarea

    (>60% of (>60% of (>60% of (>60% of peatpeatpeatpeat areaareaareaarea))))

    MontanarellaMontanarellaMontanarellaMontanarella et al.et al.et al.et al.

    MiresMiresMiresMires & & & & PeatPeatPeatPeat 2006200620062006

  • Vegetalia 2010, Cremona 20/03/2010 7

    Greenhouse gases in peatlands

    COCOCOCO2222NNNN2222OOOOCHCHCHCH4444

    Relative gas Relative gas Relative gas Relative gas fluxesfluxesfluxesfluxes –––– different different different different scalesscalesscalesscales per gas!per gas!per gas!per gas!

    Water Water Water Water tabletabletabletable

    DrainedDrainedDrainedDrained

    peatlandpeatlandpeatlandpeatland

    SourceSourceSourceSource

    SinkSinkSinkSink

    Water Water Water Water tabletabletabletable

    NaturalNaturalNaturalNatural

    peatlandpeatlandpeatlandpeatland

  • Vegetalia 2010, Cremona 20/03/2010 8

    Jones, Stolbovoi, Tarnocai, Broll, Spaargaren & Montanarella (eds.) (2009): Soil Atlas of the Northern Circumpolar Region, European Commission 2009, 144 pp. Office for Official Publications of the European Communities, Luxembourg.

  • Vegetalia 2010, Cremona 20/03/2010 9

    Biota560 Gt

    Atmosphere780 Gt

    +3.3 Gt/yr

    Soils2,500 Gt

    (i) SOC - 1,550 Gt(ii) SIC - 950 Gt

    Ocean38,400 Gt + 2.3 Gt/yr

    (i) Surface layer: 670 Gt(ii) Deep layer: 36,730 Gt(iii) Total organic: 1,000 Gt

    Fossil Fuels4,130 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/yrFossil fuelcombustion

    90 Gt/yr

    0.6+0.2 Gt/yr(deposition)

    60 Gt/

    yr (so

    il resp

    iration

    )

    Acceler

    ated so

    il eros

    ion

    1.1+ 0

    .2 Gt/yr

    (erosio

    n)MRT = 5Yr

    MRT = 25Yr

    Mean Residence Time (MRT) = 400Yr

    1.6 + 0.8 Gt/yrDeforestation

    MRT = 6Yr

    92.3 Gt/yr

    Biofuel offset?

    Soils contain the biggest terrestrial carbon pool: ca. 2,500 Gt globally

  • Vegetalia 2010, Cremona 20/03/2010 10

    Global TotalsSoil (1m layer) 2.011 GtVegetation 466 Gt

    Temp

    erate

    regio

    n

    Sava

    nnah

    Gras

    sland

    s

    Dese

    rts &

    Sem

    i -de

    serts

    Tund

    ra

    Wetl

    ands

    Crop

    lands

    Bore

    al re

    gion

    Trop

    ical r

    egio

    n

    Global Carbon Stocks in Billion Tons

    0

    100

    200

    300

    400

    500

    500

    Source: IPCC 2000

  • Vegetalia 2010, Cremona 20/03/2010 11

    Soil Organic Carbon Stocks Assessment

    Source: JRC-IES

  • Vegetalia 2010, Cremona 20/03/2010 12

    CELL(structuralpolysaccharides)

    HUM(humic

    and protected)

    STABLE

    mineralization

    microbialsynthesis

    0.3 yr

    LIGNIN

    2.5 yr

    LABILE

    0,87 yr

    25 yr

    3300 yr

    numerical values forsoil/land use =- 20% clay- temperature 12°C- 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

    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

    Rela

    tive M

    ag

    nit

    ud

    e o

    f S

    OC

    Po

    ol

    land useconversion

    subsistencefarming,

    none or lowoff-farm

    input, soildegradation

    newequilibrium

    adoption ofRMPs

    soil C

    sin

    k

    cap

    aci

    ty

    Accelerated erosion

    Attainablepotential

    Maximumpotential

    Innovativetechnology I

    Innovativetechnology II

    ∆X

    ∆YRate

    Soil C Dynamics

    Source: R. Lal, 2008

  • Vegetalia 2010, Cremona 20/03/2010 13

    Good Agricultural Practices

  • Vegetalia 2010, Cremona 20/03/2010 14

    Mitigation potential

  • Vegetalia 2010, Cremona 20/03/2010 15

    Bio-waste

    OriginTurnover

    Complexity

    Decomposing fresh OM(Particulate organic matter)

    Microorganisms

    Colloidal OMPolysaccharides and biomolecules

    Humic substances

    soluble OM

    -OH

    CO2Corg

  • Vegetalia 2010, Cremona 20/03/2010 16

    1

    Organic Carbon (%) No Data 0 - 1 1 - 2 2 - 5 5 - 10 10 - 25 25 - 35 > 35

    Organic carbon content (%) in the surface horizon (0-30 cm) of

    soils: total 71 GtC in EU

    Organic Carbon Gt 0.0 2.5 5.0 7.5 10.0 12.5 15.0

    0.5 3.5

    5.0

    1.6 7.1

    0.3

    0.8 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 1.0 0.2 0.5 0.5 1.0

    2.3

    1.0

    0.2 0.6

    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

  • Vegetalia 2010, Cremona 20/03/2010 17

    Where can we lose or gain SOC in Europe?

  • Vegetalia 2010, Cremona 20/03/2010 18

    Innovative technologies: BIOCHAR

    Source: N. de Wit, 2009

  • Vegetalia 2010, Cremona 20/03/2010 19

    Estimation based on Eurostat data on municipal waste (2008)ORBIT/ECN, 2008, Compost production and use in the EU, Final report of ORBIT e.V. / European Compost N etwork ECN to European

    Commission, Joint Research Centre(http://ipts.jrc.ec.europa.eu/activities/sustainabl e_development/susproc.cfm)

    Total biowaste and green waste arising in the Europe an 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.

  • Vegetalia 2010, Cremona 20/03/2010 20

    The need for a partnership between the Urban and the Rural communities

    Bio-waste

    Biomass

  • Vegetalia 2010, Cremona 20/03/2010 21

    Grazie per l’attenzione!

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