Agricultural practices that favour the increase of soil ... · Zero tillage X Reduced residue...
Transcript of Agricultural practices that favour the increase of soil ... · Zero tillage X Reduced residue...
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Agricultural practices that favourthe increase of soil organic matter
Philippe Ciais and Pete Smith
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• Current soil C stocks distribution• Vulnerability of soil C• Land use change• Agricultural practice• Future climate change• Uncertainties and outlook
Outline
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Ecosystem carbon balance
Chapin 2002
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Soil and vegetation ?
<1>>1,000,00077,000,000Sediments &rocks
~5.6(-8.1)-1200 (- >6000)Fossil carbon
-3-5750Atmosphere
601-1000800Vegetation
52 (het.)60-80 total
<1-5,0002300+1600 frozen and wet
Soils
18 (?)2,00037,000Deep ocean
Fluxinto atm. [Pg yr-1]
Turnovertime [yr]
Reservoir size[Pg]
after Reeburgh et al. (1997), Sabine et al. (2004), Canadell (2007), pers. com.
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Global carbon stocks in ecosystems
after Gruber et al. 2004, Lal, 2005, Davidson & Janssens 2006
Most of soil C stock is at high latitudesCroplands hold small amount of soil CGrasslands hold variable amount of soil C
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How soil C is sampled
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Stock vs. sequestration: partitioningbetween vegetation and soil
frac
tion
Soil is a larger C stock but a smaller C sink than vegetation
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Soil carbon stock is large & vulnerable
after Davidson & Janssens 2006
-400
-200
0
200
400
600
800
Stock Current gain percentury
Potential loss bycentury
2000Pg
C
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Climate factors affecting soil C balance
Temperature Waterbalance CO2
N-deposition
Primaryproduction
Soil carbon
Decompo-sition - +
Tempe-rature
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Climate factors affecting soil C balance
Temperature Waterbalance CO2
N-deposition
Primaryproduction
Soil carbon
Decompo-sition - +
Tempe-rature
Human factors affecting soil C balance
tillage
Land use changeFarmers practice
erosion
irrigation
fertilization
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Global changes in biomass and Soil Caffected by climate and land use change
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Former Soviet Union China
Europe
Temperate regions
USA
Contrasted land use histories ;Large depletion of soil C pools in the first half of
20th Century in USA and FSU by agriculture
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Soil C change associated toland use change
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What are our emission reduction targets?
• European target“To reach the 2°C goal, the EU needs to adopt areduction target of at least 30% below 1990 levelsin 2020 and additional action to reduce emissionsin developing countries”
• Corresponds to an emission reduction target of0.3 Pg C y-1
• Corresponds to an emission reduction efforthigher than this
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• EU target means a cumulative emission reduction of 3Billion tC between 2010 and 2020
• If this sequestration had to be realized over Europeanagricultural lands (250 Million ha), it would imply toincrease ecosystem carbon by 12 tC ha-1 in one decade.
• This means an extra sink of 1.2 tC ha-1 y-1 in one decade• This sink need can be compared to the current
‘inadvertent’ C balance of agricultural land(Carboeurope numbers, Schulze et al. 2010)➩ Cropland is a source of 0 - 2.5 t C ha-1 y-1
➩ Grassland is a sink of 0.6 - 0.9 t C ha-1 y-1
Emission reduction targets and currentagricultural land C budgets ?
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How does soil C sequestration work?
Organic carbon source
Add to soil
C in soil
CO2
Some C is stabilisedin the soil
Soil
Soil C cycle
e.g. residue management,organic amendments, increased plant C input…
Increase C inputs…e.g. restore & rewet farmedorganic soils
...or reduce C losses
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= microbe C = C inside aggregate
C
No-till
C
C
CC
C
C
Tillage
Tillage breaksopen aggregates
= weatheringKey:
COrganic material (C)more exposed to microbial attack and weathering
How does soil C sequestration work? –reduced disturbance
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Activity Practice Specific management change Increase C inputs
Decrease C losses
Reduce disturbance
Cropland management Agronomy Increased productivity XRotations XCatch crops XLess fallow XMore legumes XDeintensification XImproved cultivars X
Nutrient management Fertilizer placement XFertilizer timing X
Tillage / residue management Reduced tillage XZero tillage XReduced residue removal X XReduced residue burning X X
Upland water management Irrigation XDrainage X
Set-aside and land use change Set aside X XWetlands X X
Agroforestry Tree crops inc. Shelterbelts etc. X XGrazing land management Livestock grazing intensity Livestock grazing intensity X
Fertilization Fertilization XFire management Fire management XSpecies introduction Species introduction XMore legumes More legumes XIncreased productivity Increased productivity X
Organic soils Restoration Rewetting / abandonment X XDegraded lands Restoration Restoration X X X
Mechanisms for soil C sequestration in agriculture
Smith et al. (2008)
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Manure – large & long-lasting effects
Rothamsted Hoosfield – Jenkinson 1998
0
20
40
60
80
100
1850 1890 1930 1970
Year
Organic C in Soil(t ha-1)
Farmyard manure annually
Farmyard manure 1852-1871 nothing thereafter
Unmanured
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Carbon depleted soils have large potential toaccumulate C in early recovery stage
Conclusions• Farmland abandonment
caused C sink• ~0.5 tC ha-1 y-1 over past
decade
Cereals Steppe
Former Soviet Union
20 Mha abandonnedfrom 1990 to 2000
7
Example : the largest LUC change in the northern hemisphere !
This process causes net Caccumulation in soils
Vuichard et al, Glob. Biogeoch. Cycl. (2008)
Year after abandonment
gC m
-2
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Grass biofuel production vs. C sequestration
Future climate changeimpacts the results
8
How many years until biofuel cultivation overpasses passive Cseuestration by return to natural steppe ?
-200
0
200
400
600
800
1000
0 10 20 30 40 50
Nombre d'années de production
Gai
n ca
rbon
é cu
mul
é (g
C m
-2)
Avec évolution climatique simuléepar IPSL-CM4
Sans évolution climatique
Vuichard et al, 2010
+50%Current climate
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Global mitigation potential in agriculture
-200
0
200
400
600
800
1000
1200
1400
1600
Crop
land
man
agem
ent
Wat
er m
anag
emen
t
Rice
man
agem
ent
Setas
ide,
LUC
&ag
rofo
restr
y
Graz
ing
land
man
agem
ent
Resto
re c
ultiv
ated
orga
nic s
oils
Resto
re d
egra
ded
lands
Bioe
nerg
y (so
ilsco
mpo
nent
)
Live
stock
Man
ure
man
agem
ent
Mitigation measure
Glob
al b
ioph
ysic
al m
itiga
tion
pote
ntia
l (M
t CO2-e
q. y
r-1)
N2OCH4CO2
Smith et al. (2008)
A potential sink of 0.9 Pg C y-1
Compared to :• Global land sink today 4.7 ± 1.2 Pg C y-1
• Global land use source 1.2 ± 0.7 Pg C y-1
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-200
0
200
400
600
800
1000
1200
1400
1600
1800
Sout
heas
t Asi
a
Sout
h A
mer
ica
East
Asi
a
Sout
h A
sia
East
ern
Afr
ica
Rus
sian
Fed
erat
ion
Nor
th A
mer
ica
Wes
tern
Eur
ope
Wes
tern
Afr
ica
Cen
tral A
sia
Nor
ther
n Eu
rope
Mid
dle
Afr
ica
East
ern
Euro
pe
Oce
ania
Sout
hern
Eur
ope
Cen
tral A
mer
ica
Nor
ther
n A
fric
a
Wes
tern
Asi
a
Sout
hern
Afr
ica
Car
ribe
an
Japa
n
Poly
nesi
a
Region
Mt C
O2-
eq. y
r-1
Smith et al. (2007)
High and low estimates of the mitigation potentialin each region
A potential European sink 200 Tg C y-1
Current sink in European agricultural land 20 Tg C y-1
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Effect of C price on implementation
Smith et al. (2007)
0
200
400
600
800
1000
1200
1400
Res
tore
cul
tivat
edor
gani
c so
ils
Cro
plan
dm
anag
emen
t
Gra
zing
land
man
agem
ent
Res
tore
deg
rade
dla
nds
Ric
e m
anag
emen
t
Live
stoc
k
Seta
side
, LU
C &
agro
fore
stry
Man
ure
man
agem
ent
Measure
Mt C
O2-
eq. y
r-1
up to 20 USD t CO2-eq.-1up to 50 USD t CO2-eq.-1up to 100 USD t CO2-eq.-1
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Global mitigation potential in agriculture(Mt CO2-eq. yr-1)
Price range (USD t CO2-eq. -1)
Scenario 0-20 0-50 0-1000->>100 (technical
potential)
B1 1925 2384 3149 5480
A1b 1982 2439 3254 5670
B2 2047 2495 3330 5844
A2 2119 2549 3330 5957
Smith et al. (2007)
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Energy supply
0
1
2
3
4
5
6
7
<20<50
<100
<20<50
<100
GtCO2-eq
Transport Buildings Industry Agriculture Forestry Waste
Non-OECD/EITEITOECDWorld total
US$/tCO2-eq
Global economic mitigation potential fordifferent sectors at different carbon prices
IPCC WGIII (2007)
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How do we cut GHG emissions andhow much will it cost?
From: McKinsey (2009) - Pathways to a low-carbon economy Version 2 of the GlobalGreenhouse Gas Abatement Cost Curve
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How do we cut GHG emissions andhow much will it cost?
From: McKinsey (2009) - Pathways to a low-carbon economy Version 2 of the GlobalGreenhouse Gas Abatement Cost Curve
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Smith (2008) International Journal ofAgricultural Sustainability 6(3),169–170
• “There are a number of well rehearsed arguments against reliance oncarbon sequestration for tackling climate change, involving saturationof the carbon sink (the carbon is only removed from the atmospherewhile the tree is growing or until the soil reaches a new equilibriumsoil carbon level; Smith, 2005), permanence (carbon sinks can bereversed at any stage by deforestation or poor soil management;Smith, 2005), leakage/displacement (e.g. planting trees in one arealeads to deforestation in another; Intergovernmental Panel on ClimateChange (IPCC), 2000), verification issues (can the sinks be measured;Smith, 2004), and total effectiveness relative to emission reductiontargets (only a fraction of the reduction can be achieved throughsinks; IPCC, 2007)”.
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Soil CVegetation C
Time since management change
C s
tock
Management change
Saturation – the time course of Csequestration
• Sink saturation ~ 20-100 years• Sink strength declines towards new equilibrium
Smith (2004a)
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Permanence
25
35
45
55
65
75
85
1844 1894 1944 1994 2044 2094
Year
Tota
l SO
C to
23
cm (t
C h
a-1)
Management change
Conversion to low-input cropland
Manure treatment in red, Woodland in blue Smith (2005)
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Leakage / displacement: are we actuallysequestering carbon or just moving it about?
Farm with more manure Farm with less manure
Manure Manure Mineral N
More manure here….but……..less manure here
Effect over the whole cropland area = zero
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Value of C sequestered
No. of samples required to demonstrateincrease in soil C
Cost
Zero return
Verification issues
Smith (2004b)
Value of C sequestered
Accuracy of estimate(or precision if only a change is verified)
Cost
Zero return
Minimum accuracyrequired for verification
Progress in measurement
technology
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“Trying to sequester the geosphere inthe biosphere”
• The C we release through fossil fuel burning has been locked up for~300 Million years and was accumulated over many millions of years –we are trying to lock that up over years / decades – it does not addup!
• “It is easier to leave the marbles in the jar than to tip them out andtry to pick them all up again” W.H. (Bill) Schlesinger
• Soil C sequestration is time limited, non-permanent, difficult to verifyand is no substitute for GHG emission reduction
• Soil C sequestration may have a role in reducing the short termatmospheric CO2 concentration, and buying us time to developlonger term solutions, largely in the energy sector
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Conclusions
• Soil C sequestration globally has a large, cost-competitive mitigation potential
• Useful to meet short / medium term targets –especially if these are high (e.g. in UK)
• Many co-benefits – soil fertility, workability,water-holding capacity etc. (see other talk)
• Uncertainties are very large on long termsequestered C ; verification is not in place
• Don’t forget the limitations: time limited, notpermanent, doesn’t replace genuine emissionreduction