presentation on land-use management
TRANSCRIPT
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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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