coupling high spatial resolution data, gis approaches and modelling for reliable estimates of soc...
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Coupling High Spatial Resolution Data, GIS Approaches and Modelling for Reliable Estimates of SOC stocks
and Their Historical Changes in Agricultural Land
UCD School of Biology and Environmental Science and UCD Earth Institute, University College Dublin,
Belfield, Dublin 4, Ireland
M. I. Khalil and B. A. Osborne
GLOBAL SYMPOSIUM ON SOIL ORGANIC CARBON, FAO HQ, ROME, ITALY, 21-23 MARCH 2017
Contamination of waterbodies
More Inputs
More leaching
More GHGs
Trade-off/Offset: SOC
Soil Organic Matter• Soil Quality/Health: Fertility and Productivity• Adsorbent of environmental toxicants• Storehouse of atmospheric CO2: Sequestration• Source of Greenhouse Gases: CO2, CH4 and N2O
Ireland: Annex-I country – obligation for accounting and reporting to UNFCCC: AG + LULUCF = AFOLU
Article 3.3: Aforestration, deforestration and reforestration
Article 3.4: Agricultural soils but also to cover soil C dynamics
Paris agreement: Climate change: temp. rise<2oC
Carbon credits benefits, trade-off relations and offsetting
International Agreements
Uncertainty: Sources of variation & error Sampling error
• Topography• Land use and management• Number of samplings• Consistency in sampling time
Preparation error • Compositing • Homogenization• Grinding, screening, sifting, storage
Analytical error • QA/QC: Standard methods (Org + Inorgorganic = Total)
Principal structure and soil profile sampling scheme
SOC accounting: IPCC default Tier 1 to country-specific Tier 2 mainly
Developed methodologies and models to estimate baseline SOC concentrations, densities and stocks (0-10, 0-30 & 0-100 cm depth) for 2006.
Compiled and analysed databases to identify agricultural land uses, their changes and management practices.
Compiled databases for common agricultural land uses, management practices and inputs.
Estimated reference SOC (SOCref) for 1990 through back calculation and historical changes in SOC stocks (2006-2014) across key agricultural LULUC.
Overlaid LPIS (2000-2014) on NSDB and ISTs using Arc-GIS.
Compiled research and country-specific IPCC emission factors (EFs) for management practices and inputs in relation to SOC sequestration/loss.
STEPS: Soil Carbon Accounting
LU areas and SOC derived from overlaying LPIS, NSDB and ISM
LPIS Map
ISM
Data Acquisition1 km Buffer on Irish National Grid: SOC under a LC contains a Indicative Soil Type (IST) >50% area
Common Soil type
Level of degradation
Major land covers
Acidity Drainage classes
Indicative soil types Depth distribution models x SOCz10 *
R2 CV%
Mineral soil (SOC<10%)
Non-degraded
Grassland Non-Calcareous
Well AminDW, AminSW y = 1.4002e-0.035x 1.0000 30
Poorly AminPD (+AminSP) y = 1.3661e-0.034x 0.9998 31
Calcareous Well BminDW, BminSW y = 1.3719e-0.035x 0.9999 33
Poorly BminPD y = 1.3654e-0.034x 0.9998 26
Tillage Non-Calcareous
Well AminDW, AminSW y = 1.5647e-0.029x 0.9947 29
Poorly AminPD y = 1.5195e-0.026x 0.9928 34
Calcareous Well BminDW, BminSW y = 1.5328e-0.03x 0.9966 63
Poorly BminPD y = 1.5055e-0.025x 0.9920 17
1. Depth distribution models for the estimation of SOC across soil depths for IST and key agricultural land covers in Ireland (Khalil et al., 2013)
Common Soil type
Level of degradation
Major land covers
Acidity Drainage classes
Indicative soil types Depth distribution models x SOCz10 *
R2 CV%
Organo-mineral soil (SOC 10-20% and >20% at <30cm depth)
Non-degraded(SOC >20% at <30cm depth)
Rough grazing, Grassland, Tillage
Non-Calcareous
Mixed, Poorly major
AminSRPT,(AminPDPT,AlluvMIN, AminPD, AminDW, AminSW)**
y = 1.5652e-0.042x 0.9999 09
Calcareous Mixed, well major
BminPDPT (BminDW, BminPD, BminSW)**
y = 1.6084e-0.041x 0.9996 10
Degraded(SOC 10-20% at <30cm depth)
Grassland, Rough grazing, Tillage
Non-Calcareous
Mixed, Poorly major
AminPDPT, AminSRPT,(AminPD, AminDW)** AlluvMIN?); If SOC10cm: 10-20% (y1)/<10% (y2)
y1 = 2.3718e-0.038x 0.9703 27
y2 = 3.5709e-0.035x 0.8843 27
Calcareous Well BminPDPT, BminSRPT, (BminDW, BminSW)** If SOC10cm: 10-20% (y1)/<10% (y2)
y1 = 2.7101e-0.037x 0.9485 10
y2 = 4.9308e-0.031x 0.7630 12
Organic soil (SOC >20% and 10-20% at >30cm depth
Non-degraded (SOC >20% at >30cm depth)
Rough grazing, Grassland, Tillage***
Non-Calcareous
Undefined Cut y = -0.164ln(x)+ 1.4431
0.9217 38
Undefined BkPt y = -0.066ln(x)+ 1.2306
0.5798 13
Degraded (SOC 10-20% at >30cm depth)
Rough grazing, Grassland, Tillage
Non-Calcareous
Undefined Cut = if SOC10cm: 10-20% y = 0.2692ln(x)+ 0.3866
0.5347 35
Undefined BkPt = if SOC10cm: 10-20%
y = 0.4357ln(x)- 0.0383
0.6080 12
Undefined Cut = if SOC10cm: <10% y = 1.1682ln(x)- 1.0111
0.6838 36
Undefined BkPt = if SOC10cm: <10% y = 1.3518ln(x)- 1.6659
0.7232 13
2. Depth distribution models for the estimation of SOC across soil depths for IST and key agricultural land covers in Ireland (Khalil et al., 2013)
Common Soil type
Level of degradation
Major land covers
Acidity Drainage classes
Indicative soil types
y = PTF, x = SOCz * R2 SSE MSE RMSE
Organo-mineral soil (SOC 10-20% and >20% at <30cm depth)
Non-degraded(SOC >20% at <30cm depth)
Rough grazing,Grassland
Non-Calcareous
Mixed, Poorly major
AminSRPT, (AminPDPT, AlluvMIN, AminDW, SW, PD,)**
y = 0.2170+1.0763e-0.080x 0.76 2.043 0.028 0.166
Rough grazing, Grassland
Calcareous Mixed, well major
BminPDPT,SRPT BminDW, SW,)**
y = 0.1067+1.4473e-0.072x 0.99 <0.001
<0.001 0.003
Degraded(SOC 10-20% at <30cm depth)
Grassland, Rough grazing
Non-Calcareous
Mixed, Poorly major
AminPDPT, SRPT, (AminDW, SW,PD, AlluvMIN,)**
y = 0.2012+1.1592e-0.081x 0.67 8.037 0.028 0.166
Grassland Calcareous Well BminPDPT, SRPT (BminDW, SW)**
y = 0.3749+0.9901e-0.119x 0.89 1.191 0.005 0.071
Organic soil (SOC >20% and 10-20% at >30cm depth
Non-degraded(SOC>20% at >30cm depth)
Rough grazing, Grassland Tillage***
Non-Calcareous
Undefined Cut y = 0.1235+2.5048e-0.085x 0.75 0.190 0.003 0.053
Tillage***Rough grazing, Grassland
Undefined BkPt y = 0.1437+5.7679e-0.121x 0.83 0.251 0.002 0.048
Degraded(SOC 10-20% >30cm depth)
Rough grazing Grassland
Non-Calcareous
Undefined Cut y = -0.0751+1.5674e-0.042x 0.91 0.293 0.011 0.104
Rough grazing Grassland
Undefined BkPt y = -0.2125+1.7592e-0.031x 0.87 0.341 0.014 0.119
2. Pedo-transfer functions for soil bulk density estimation across depths for IST and key agricultural land covers in Ireland (Khalil et al., 2013).
Common Soil type
Level of degradation
Major land covers
Acidity Drainage classes
Indicative soil types
y = PTF, x = SOCz * R2 SSE MSE RMSE
Mineral soil (SOC<10%)
Non-degraded
Grassland Non-Calcareous
Well AminDW, AminSW y = 0.7468+0.6559e-0.260x 0.70 9.290 0.011 0.105
Poorly AminPD(+AminSP) y = 0.2882+1.1420e-0.106x 0.90 1.644 0.003 0.056
Calcareous Well BminDW, BminSW y = 0.5041+0.8982e-0.146x 0.92 1.487 0.002 0.047
Poorly BminPD y = -0.0275+1.4995e-0.083x 0.99 0.001 <0.001 0.003
Tillage Non-Calcareous
Well AminDW, AminSW y = 0.4827+0.9227e-0.153x 0.80 0.091 0.002 0.049
Poorly AminPD y = 0.9302+0.6003e-0.209x 0.99 0.004 <0.001 0.010
Calcareous Well BminDW, BminSW y = -0.0154+1.6219e-0.125x 0.99 0.001 <0.001 0.003
Poorly BminPD y =-0.0977+1.6157e-0.063x 0.99 <0.001
<0.001 0.003
1. Pedo-transfer functions for soil bulk density estimation across depths for IST and key agricultural land covers in Ireland (Khalil et al., 2013).
Proportion of area under management and inputs across LUS and the IPCC EFs
Tillage/Arable
Management Ppn (A)
Inputs Ppn (A)
EFs
Mineral soil only
Full tillage 0.80 Low 0.23 0.63/0.69/0.73
Reduced tillage 0.15 Medium 0.34 0.69/0.75/0.79No tillage 0.05 High 0.33 0.77/0.83/0.88
High +manure 0.10 0.99/1.07/1.14
Temp grass
Management Ppn (A)
Inputs Ppn (A)
EFs
Mineral (0.86)& Organo-mineral (0.14) soil
Full tillage 0.95 Low 0.23 0.78/0.84Reduced tillage 0.05 Medium 0.34 0.85/0.92
High 0.33 0.94/1.02High +manure 0.10 1.22/1.32
Grazing Ppn (A)
Ppn (A)
Mineral & Organo-mineral
0.91 Mineral 0.76 Pasture 0.56Organo-mineral
0.24 Hay 0.06
Organic 0.09 Silage 0.26Rough grazing 0.12
Management Inputs Ppn (A) EFs (G/R)Mineral & Organo-mineral
Non-degraded Low 0.38 1.00/1.00Improved Medium 0.40 1.14/1.14
High 0.22 1.27Organic Degraded Low 0.08 0.95/0.95
Non-degraded Medium 0.30 1.00/0.95Improved High 0.40 1.14/1.14
0.22 1.27
Proportion of area under management and inputs across LUS and the IPCC EFs
SOC density for estimated (1990) and measured (2006) values
Proportion of land use change between 1990 and 2014
Source: EPA, CSO and Our works
Conclusions Coupled GIS and modelling approach provides a robust estimate of
SOC concentration and density/stocks for Tier 2 development. IPCC approaches should be re-evaluated for more robust accounting
systems:o that track the actual rate of stock change with management o that correctly account for agricultural management activities.
Based on the IPCC default EFs used, the SOC sources and sinks in agricultural soils is balanced/neutral.
Options to achieve a carbon neutral agricultural sector by 2050: (i) Advanced GHG mitigation strategies: Technological limitation?? (ii) Carbon sequestration: Improved management and higher C in
agricultural soils: strategy for beyond 30 cm depth? (iii) Afforestation (1.25 M ha) may raise concerns if this involves the
replacement of agricultural land – but use marginal lands?
(Source: CGIAR, 2011)
THANK YOU
AcknowledgementsIrish Environmental Protection Agency (EPA) for funding
Phillip O’Brien, EPA for providing relevant data
John Muldowney, DAFM for input