presentation on land-use management

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  • 7/30/2019 Presentation on Land-use Management

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    Land-usemanagement

    Soe Moe Win

    Myanmar

    19.10.2012, Friday

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    Land Use

    Changing ever-evolving human needs Forest grown and cut for needs

    Grasslands-turned into crop fields

    Crops fields-cultivated and fallowed forsome reasons

    Fields-consumed by growing urbanization

    Demand for biofuel crops involves riskthat land-use intensification increase

    Lead to a decrease in soil biodiversity

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    F

    O

    R

    E

    S

    T

    S

    G

    RA

    S

    Slands

    C

    RO

    P

    lands

    U

    RB

    A

    NLands

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    Forest

    temperature extremes

    light availability

    wind speed

    Soils

    extensive root systemsand leaf litter layers

    habitat and foodto soil fauna

    Offera protectivemicroclimate

    Reduce

    moisture

    Increase

    Provide

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    Coniferous forest

    soilsmore acidic (mor)

    Deciduous forests

    soilsnon acidic (mull)

    Soils

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    Have a good aeration

    Allow ion exchanges

    Favor a high soil biodiversity

    Exhibit high C:N ratios (10:15)

    Deciduous forests soils

    non acidic (mull)

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    Can be characterized by

    Fungal-dominated food-web(fungal to

    bacterial biomass ratio 5:1 to 10:1) Fungi-eating protists

    Nematodes andHigh densities of microarthropods

    and anecic earthworms

    3 of 27 species of earthworms

    associated with forest environment

    Others at low densities.

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    Have lower biological activity

    Restrict microbial activity and thefunctional groups.

    More heavily fungal-dominated (fungalto bacterial biomass ratios 100:1 to1000:1).

    Ecosystem-engineer communities-dominated by epigeic earthworms andenchytraeids

    Coniferous forest soils

    more acidic (mor)

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    C:N ratioCarbon nitrogen present in SOM

    Low ratio

    carbon close to nitrogen

    High ratio higher mass of carbon for

    each gram of nitrogen in OMAlways more carbon than nitrogen inOM

    A measure of quality of SOMLeaves much lower than wood

    Influences rates of decomposition

    C:N

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    Decompositionoccur

    fungal-dominated decomposition

    Fungi BacteriaBased pathway

    prefer carbon-richfood (cellulose)

    prefer nitrogen-rich food (leaves)

    Higher C:N

    slower turnover rates

    lower nitrogen mineralisation

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    Grasslands

    Ground covered by grass-dominatedvegetation

    Have Little or no tree cover

    Soil present the richest soil biodiversity

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    - Extensive rootsystems

    - Limited amountsof leaf litter

    - Low level of leaflitter

    - Fungal dominatedfood web with

    microbial biomass

    lands

    Characterize

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    Europe

    Host most diverse

    and abundantearthwormcommunities

    Some -dominatedby endogeic

    speciesOthers by

    anecic species

    Temperate

    Most biomass -

    explained byearthworm familyLumbricidae

    Represent 70-80 % of total soil

    biomass in lowtillage system

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    Croplands

    Soil biodiversity - so much lessSoil contains few arbuscular mycorrhizal

    fungi and few earthworms

    Soil community adapted to regulardisturbance

    Food chains based on bacteria-basedpathways

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    Conventionally cropped soils result

    stressed and depleted soil food webs.

    Intensively cropped, arable soils-characterized low organic matter inputs

    Low soil fungal/bacterial ratios

    Depleted bacteria-dominated chemicalengineers communities

    Biological regulator communities-reduced

    Dominated by opportunistic bacterial-feedingfauna

    Reduce earthworm and mycorrhizal fungi

    communities

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    Successive cropping culture

    Soil-borne diseases not drop anymore Beet cyst nematode or potato cyst

    nematode

    Need 3 years of non-crop to reducenematode population

    Shorter rotation nematode not decline

    Necessary to use biocides for control Bad soil invertebrates, ground and

    surface water quality

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    Management practices vary Severely impact soil biota

    Soil biodiversity peaks at intermediatemanagement intensities

    Species diversity and abundance

    Increase low-intermediate disturbance

    Peak at moderate agri disturbance

    Decrease with strong agri disturbance

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    Reducing management intensity ofan intensive cropping with

    Some degree of organic inputs Continuous plant cover

    Limited tillage

    Lead to the good environment Can enhance soil biodiversity

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    Effects -depend on intensity & depth

    plowing ripping turning

    Impacts of tillage

    Deep tillage

    Softer tillageIntensity

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    Impacts of tillage

    Obvious effect negative correlation

    between organisms size - biomass

    Disrupts scales of action-biological

    regulators & ecosystem engineers

    Devastate key groups of organisms

    fungi & earthworms

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    damaged or killed byintensive

    Light higher diversityof large worms thanconventional

    Effects differ-species

    disrupted

    &myceliabroken

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    Population ofbeneficialorganisms high

    Soil water holdingcapacity improve

    Crop left-overspromote diseasetransmission

    Weeds - lesscontrollable

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    Organic farming practices

    Provide a lower level of stress & higherorganic inputs for food web

    Increase potential niches for soil fauna

    Change relative abundance among soilorganisms group

    Promote some specific taxa-earthworms

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    Organic manure

    Promote soil

    microbial

    biomass

    Slow down

    microbial activity

    Farmyard manure

    Promote abundance of

    biological regulators &

    ecosystem engineers Promote generalist

    predators above ground

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    Conclusion Of CroplandsClear agri-intensification have negative

    consequences

    At local scales (increase erosion, lower

    soil fertility)

    Regional scales(pollution of groundwater)

    Global scales (reduce climate regulation)

    Cultivation systems long-term effectOn microbial community structures

    Soil communities in general

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    Urbanlands

    Cities-expanding faster than populations

    Consist-highly modified habitats Covered by pavement and buildings

    Soil-subject to sealing and compaction Face environmental stresses - air & heav

    metal pollution, increased temperature

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    Buildings & pavedarea modify -

    Chemical &physicalequilibrium of soils

    Connectivity toother ecosystems

    Remaining space

    Involve nature, treeslanes, lawn, cultivated

    areas and parks, urbanforests, wetlands, lakesand streams

    Face intensivemanagement anddisturbance, involving

    intensive chemical sue

    Urbanlands

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    Sealed areas Non-sealed areas

    Have severely depleted

    soil biodiversity Stop exchanges between

    soil fauna and externalinputs

    Chemical engineers go indormancy

    Bacteria-dorminated

    High chemical inputs forpest control

    Biological regulatorsdominated by

    microarthropods

    Earthworms absent-onlyin urban parks or forests

    Urban lands

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    Each land(m2) face some to many changes

    Involve an initial disturbance phase before a

    new ecosystem equilibrium Modify quality and quantity of available

    organic & mineral inputs Leads to a redistribution of soil community

    Occur large biodiversity changes locally

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    Soil community

    Native soil community-experiencereduction in diversity and abundance

    Non-native-sometimes invasive

    Species - find suitable conditions andresources

    Replace native species

    In new ecosystem:

    Biodiversity more/equally/less

    abundant than previous one

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    Impact of the main land-use changes

    Forests

    grasslands Grasslands crop lands

    Agricultural lands

    urban areas

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    Impact of the main land-use changes

    A sharp switch from one soil typecommunity to another occur

    Greater when forests to agriculturallands or urban areas

    A general decline in soil biodiversity

    occur during transition phase

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    A switch within a fungi-dominated

    system

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    Increased disturbance -results - lower soilmicrobial activity

    Reduced activity of anecic earthworms -hiders - their movement

    Reduction in activity of chemical engineers- reinforced

    Communities of biological & ecosystemengineers - more diverse

    Switch-reduces nutrient cycling, regulation

    of carbon flux and climate control services

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    A switch from low to moderate or

    high management intensity

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    Render available previously protectedorganic matter

    Provoke local bursts of microbialactivity and significant losses in soil C

    Machinery use and low food availability

    - reduces abundance of springtails &earthworms

    - some field - no earthworms

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    Disrupt chemical engineers andearthworm communities

    Hinder nutrient cycling, carbon regulation &climate control

    Communities of mutualist and non-

    pest microbes and biologicalregulators become poor Reduce plant protection and growth, impacting

    soil fertility The change in chemical engineers

    communities -alter - self-regulation

    ecosystem

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    The prevalence of soil sealing

    G l d/ l d U b l d

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    Grassland/cropland Urban land

    Abundance and diversity of all native

    soil species reduces dramatically Some exotic soil species or some urban

    exploiters may flourish

    Sewage sludge deplete

    Soil invertebrate communities and

    soil trophic structureMainly parasitic and predatory mites

    Predatory and omnivorous

    nematodes

    O ll d li i ll t f

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    Overall decline in all components ofsoil biodiversity - result - loss of

    almost all services Litter decompositionmade redundant

    Reduced litter quantity and man-

    made management practices involved

    Carbon storage and climate controlservices impaired

    Reduction in natural water regulation

    fully not compensated

    Urban forest

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    Represent havens of soil biotic activityHave little organic residues and litter

    Heavily impacted by humans Favor earthworms to dig down to deep

    organic matter stores

    Urban forest

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    Spatial Scale Temporal Scale

    S ti l S l

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    Impact soil foodwebs and biotic

    interactions Thus dynamic

    equilibriumwithin a soilcommunity

    Dispersal-key factor

    Determine amount

    and type of transfersof soil biotas

    Non- native species-colonize newecosystem andpotentially become

    invasive

    Spatial Scale

    The importance of landscape scale

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    The importance of landscape scale

    Soil services-still provided over whole

    To maintain biodiversity and ecosystemservices

    Creating refuges for living organisms

    Focusing on stocks of seeds in soil

    Biodiversity Sources ofliving organism

    Increaseresilience of

    ecosystem

    Provide Crucial

    Temporal Scale

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    Temporal Scale

    Organisms living on plant

    roots days to months

    Land-usechange &its effect

    Each change comes

    -further modifications- potential damages tosoil diversity

    Cumulative

    Occur after a certain

    time lag

    Mineralizing microbes

    survive for years

    Soil biodiversity restoration

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    Soil biodiversity restoration

    Not all groups reach equilibrium numberat the same pace.

    Restoration not easy task

    Loweringintensity ofland use

    practices

    soilbiodiversityenhance

    This process takes several years to take effect.

    Future Trends

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    Future Trends

    2020 2035

    Arable landdecrease 5%

    Total forest areaincrease -5%

    Urban areas

    increase 1%

    Grasslandsdecrease 10%

    Agriculture surfacedecrease slightly

    Organic agriculture

    surfaces-increase

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    Rural AreasLand use

    changing faster

    Urban AreasSoil biodiversity

    poor

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