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Presentation by Ross Searle and Mike Grundy
          representing the TERN Soils Facility




The Need for Effective Soil
Information Infrastructure
TERN Soils Collaborations
Soils facility is highly collaborative

  •State agencies
  •Universities
  •Geoscience Australia
  •CSIRO
  •TERN Facilities
The Australian Soil & Landscape Grid
             Infrastructure to move from ‘soil information’ to
             soil spatio-temporal systems:
             Soil information which:
                 • is consistent, reliable, functional and
                   comprehensive
                 • is at an appropriate scale and resolution
                 • describes soil variability in x,y,z (i.e. the soil
                   volume)
                 • integrates with earth observation, climate
                   biogeochemical models and monitoring
                   systems
                 • Improves the quality of ecosystem research
                 • Reduces uncertainty in models, integrated
                   systems and land management decisions
             Current soil information does not meet this need
             – it does not provide the right kind of
             ‘infrastructure’
Why?
I assume you assume that Australia - a 1st world
country has 1st world soil information
no
what would 1st world info allow?
     • provide soil information you need:
     • what you want, where you want it and with the
       quality you need
what we have:
     • a patchwork / collage and little of what you need
Benefits of the New Infrastructure
•ASRIS has highlighted the need
•Poor or inadequate infrastructure ensures
duplication and inefficiency – example later
•Discourages emergent activities
•Readily updateable
•Is explicit and transparent about quality
Topographic parameters
(available now)


•Slope, aspect, curvature
•Relief
•Slope/relief classification
•MrVBF valley bottom flatness index
•Topographic position index
•Topographic wetness index (TWI or CTI)
•Solar radiation


     John Gallant
Specifications – Soil properties
    Six Depths              Key soil properties
     0 - 5 cm         1. Organic Carbon (g/kg)
     5 – 15 cm        2. Sand (g/kg), Silt (g/kg), Clay (g/kg)
     15 – 30 cm          coarse fragments (g/kg)
                      3. pH
     30 – 60 cm       4. Depth to restricting layer (cm)
                      5. Depth of regolith (cm)
                      6. Total P (%)
     60-100 cm        7. Bulk Density (Mg/m3)
                      8. Available Water Capacity (given in mm/m)
     100-200 cm       9. ECEC (Cations plus exchangeable acidity mmol/kg)
     Depth to bedrock 10. EC (Electrical conductivity mS/m)
     and              From these attributes, ecosystem model parameters
     Effective depth will be predicted using an embedded inference
                      system


 Slide Credit: Alfred Hartemink
Building on Existing Soils Data
                  Environmental Correlation




Raphael Viscarra-Rossel
Building on Existing Soils Data
                Spatial Disaggregation




Nathan Odgers
David Clifford
Get - - http://www.asris.csiro.au/viewer/tern
  Viewhttps://data/csiro/dap
  Discover - http://portal.tern.org.au




Peter Wilson & David Jacquier
The Need For a Soil Infrastructure...
The need for a Soil
Infrastructure...
One off solution

Had to develop a purpose
built soils framework
Manual interpretation of soil
parameters
Manual development of
parameter files
Little provenance
No estimate of reliability
Extrapolation                Supersites - We know a lot about small areas
             Supersites      Other facilities – we know a little about a
                             large area eg TERN Soils, AusCover

                             By combining we can move toward sophisticated
                             national environmental accounting


                                                      National accounting




TERN Soils

                  AusCover
Key Contacts For Soils Facility
• the info - Peter Wilson
• the science – Raphael Viscarra Rossel, Ross Searle
• the program – Mike Grundy

                           the team
          David Clifford              Linda Gregory
          Melisa Dobbie               Nathan Odgers
          David Jacquier              Karen Holmes
          John Gallant                Liz Stower
          Jen Austin                  John Wilford
          Mark Thomas                 Jason Morris

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Ross Searle_The need for effective soil information infrastructure: TERN's Soil and Landscape Grid of Australia

  • 1. Presentation by Ross Searle and Mike Grundy representing the TERN Soils Facility The Need for Effective Soil Information Infrastructure
  • 2. TERN Soils Collaborations Soils facility is highly collaborative •State agencies •Universities •Geoscience Australia •CSIRO •TERN Facilities
  • 3. The Australian Soil & Landscape Grid Infrastructure to move from ‘soil information’ to soil spatio-temporal systems: Soil information which: • is consistent, reliable, functional and comprehensive • is at an appropriate scale and resolution • describes soil variability in x,y,z (i.e. the soil volume) • integrates with earth observation, climate biogeochemical models and monitoring systems • Improves the quality of ecosystem research • Reduces uncertainty in models, integrated systems and land management decisions Current soil information does not meet this need – it does not provide the right kind of ‘infrastructure’
  • 4. Why? I assume you assume that Australia - a 1st world country has 1st world soil information no what would 1st world info allow? • provide soil information you need: • what you want, where you want it and with the quality you need what we have: • a patchwork / collage and little of what you need
  • 5.
  • 6. Benefits of the New Infrastructure •ASRIS has highlighted the need •Poor or inadequate infrastructure ensures duplication and inefficiency – example later •Discourages emergent activities •Readily updateable •Is explicit and transparent about quality
  • 7. Topographic parameters (available now) •Slope, aspect, curvature •Relief •Slope/relief classification •MrVBF valley bottom flatness index •Topographic position index •Topographic wetness index (TWI or CTI) •Solar radiation John Gallant
  • 8. Specifications – Soil properties Six Depths Key soil properties 0 - 5 cm 1. Organic Carbon (g/kg) 5 – 15 cm 2. Sand (g/kg), Silt (g/kg), Clay (g/kg) 15 – 30 cm coarse fragments (g/kg) 3. pH 30 – 60 cm 4. Depth to restricting layer (cm) 5. Depth of regolith (cm) 6. Total P (%) 60-100 cm 7. Bulk Density (Mg/m3) 8. Available Water Capacity (given in mm/m) 100-200 cm 9. ECEC (Cations plus exchangeable acidity mmol/kg) Depth to bedrock 10. EC (Electrical conductivity mS/m) and From these attributes, ecosystem model parameters Effective depth will be predicted using an embedded inference system Slide Credit: Alfred Hartemink
  • 9. Building on Existing Soils Data Environmental Correlation Raphael Viscarra-Rossel
  • 10. Building on Existing Soils Data Spatial Disaggregation Nathan Odgers
  • 12. Get - - http://www.asris.csiro.au/viewer/tern Viewhttps://data/csiro/dap Discover - http://portal.tern.org.au Peter Wilson & David Jacquier
  • 13. The Need For a Soil Infrastructure...
  • 14. The need for a Soil Infrastructure...
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  • 16. One off solution Had to develop a purpose built soils framework Manual interpretation of soil parameters Manual development of parameter files Little provenance No estimate of reliability
  • 17. Extrapolation Supersites - We know a lot about small areas Supersites Other facilities – we know a little about a large area eg TERN Soils, AusCover By combining we can move toward sophisticated national environmental accounting National accounting TERN Soils AusCover
  • 18. Key Contacts For Soils Facility • the info - Peter Wilson • the science – Raphael Viscarra Rossel, Ross Searle • the program – Mike Grundy the team David Clifford Linda Gregory Melisa Dobbie Nathan Odgers David Jacquier Karen Holmes John Gallant Liz Stower Jen Austin John Wilford Mark Thomas Jason Morris