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Modelling regolith depth in the Mt Lofty
Ranges, SA: towards an Australian regolith map

Mark Thomas, CSIRO Land and Water
John Wilford, Geoscience Australia
John Gallant, CSIRO Land and Water
Regolith – what is it, why is it
                    important?
• “Soil” is often only thought of as the upper 0.3 – sometimes to 1.5 m - of ground surface
      •   Traditionally a strong agricultural focus
• Regolith is all weathered bedrock material mantling hard bedrock, including soil
• Has critical biophysical function, moderating interactions of
      •   Hydrology: storage, movement, quality ….
      •   Biology: fauna, flora, biodiversity ….
      •   Energy: absorption, emission, transfer
      •   Biogeochemistry: C, N, P, trace elements, gaseous exchange (H2O, O2, CO2, NOx …) …..
      •   Cultural: land use patterns, farming, urban, conservation
      •   These are integrated functions
• We need a broader understanding of regolith - beyond just soil, beyond agriculture focus - for
biophysical modelling
• Regolith mapping is in short supply
      •   Only small % of Australia covered at 1:250,000 scale or better
      •   Most maps show nature and composition, rarely depth
      •   Mapping is inconsistent
• We’re making a start towards a consistent national coverage by researching how to map regolith depth
Study area: Mount Lofty Ranges
• Controls on regolith depth:
    • Complex geology
    • Complex weathering, long
      landscape history
           Recently exposed (fresh, shallow)
             residual mantles (Tertiary,
            ancient and deep)
    • Neotectonic history
    • Range of landforms
• MLR contains many analogues of
southern Australian landscapes, so a
good place to start
Site data, depth to hard bedrock
• Strong reliance on existing, “legacy” regolith data
• Borehole logs
     •   Mineral exploration, groundwater, geotechnical
     •   > 14,000
• New site observations
     •   Road cuttings
     •   Creek beds to exposed bedrock
     •   Issue: biased landscape positions
• New drilling
     •   Focused on areas where our field knowledge was
         poor/incomplete
     •   Drilled in clusters, along toposequences
     •   < 9 m, 60 mm in tact cores removed
• 714 useable depth records
• 128,000 ha study area
     •   ~ 1 observation per 180 ha
Modelling regolith depth
• An environmental correlation approach
     •   Using readily available environmental parameters (digital grid
         maps) to predict other, less easy to measure environmental
         parameters
     •   The environmental parameters correlate to soil properties, e.g.
         relationships between elevation and hillslope soil depth
• Environmental parameters from national data infrastructure,
including
     •   Topographic parameters: ref John Gallant’s talk, including
         MrVBF, topographic wetness index, aspect, slope …
     •   Climatic parameters: rainfall, evaporation, ….
     •   Geochemical parameters: geology, gamma radiometrics,
         weathering intensity index, ….
     •   28 used
     •   Grids standardised to 30 m ground resolution
• Piecewise, multi linear regression modelling (“Cubist” software)
     •   Model produces a decision tree, consisting of
              Branches, the rules/conditions (“piecewise”)
              Leaves , the linear regression models
• Cubist makes models explicit for expert evaluation
• Model result
     •   R2 0.64
Next?
• Working towards a seamless, consistent national regolith map
    •   An enduring piece of national data infrastructure for all Australian/international biophysical
        modellers
    •   With estimates of uncertainty
    •   Presented /served via
          •   Discoverable through the TERN Data Discovery Portal http://portal.tern.org.au
          •   Visible through the TERN Soil Portal http://www.asris.csiro.au/viewer/tern
          •   Downloadable from CSIRO Data Access Portal https://data/csiro/dap
• Phase 2 - testing the approach in the Burdekin catchment (on-going)
    •   New biophysical region with new national analogues
    •   Complements the spatial disaggregation approach (Nathan Odgers’ talk), which will be used for
        method benchmarking
          •   Multiple lines of evidence, testing multiple approaches towards the best national data product(s)
• National approaches may vary, depending on
    •   Biophysical regions, landscape histories
    •   Quality, density of useable site observations
    •   The local “power” of specific environmental parameters
    •   National regolith map: a stitched patchwork of multiple biophysical regolith models/maps (?)
• New regolith map themes
    •   Whole-of-profile or layer-by-layer stocks
          •   Plant available water
          •   C, N, P, trace elements ….
          •   clay content, salinity, pH …
          •   …
Acknowledgements
• CRC Forestry
• SA Government (DWLBC)




Thank you
Dr Mark Thomas
CSIRO Land and Water
mark.thomas@csiro.au
08 8303 8471

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Mark Thomas_A digital soil mapping approach for regolith thickness in the complex Mt Lofty Ranges regolith-landscape setting: towards a consistent Australian regolith map

  • 1. Modelling regolith depth in the Mt Lofty Ranges, SA: towards an Australian regolith map Mark Thomas, CSIRO Land and Water John Wilford, Geoscience Australia John Gallant, CSIRO Land and Water
  • 2. Regolith – what is it, why is it important? • “Soil” is often only thought of as the upper 0.3 – sometimes to 1.5 m - of ground surface • Traditionally a strong agricultural focus • Regolith is all weathered bedrock material mantling hard bedrock, including soil • Has critical biophysical function, moderating interactions of • Hydrology: storage, movement, quality …. • Biology: fauna, flora, biodiversity …. • Energy: absorption, emission, transfer • Biogeochemistry: C, N, P, trace elements, gaseous exchange (H2O, O2, CO2, NOx …) ….. • Cultural: land use patterns, farming, urban, conservation • These are integrated functions • We need a broader understanding of regolith - beyond just soil, beyond agriculture focus - for biophysical modelling • Regolith mapping is in short supply • Only small % of Australia covered at 1:250,000 scale or better • Most maps show nature and composition, rarely depth • Mapping is inconsistent • We’re making a start towards a consistent national coverage by researching how to map regolith depth
  • 3. Study area: Mount Lofty Ranges • Controls on regolith depth: • Complex geology • Complex weathering, long landscape history  Recently exposed (fresh, shallow)  residual mantles (Tertiary, ancient and deep) • Neotectonic history • Range of landforms • MLR contains many analogues of southern Australian landscapes, so a good place to start
  • 4. Site data, depth to hard bedrock • Strong reliance on existing, “legacy” regolith data • Borehole logs • Mineral exploration, groundwater, geotechnical • > 14,000 • New site observations • Road cuttings • Creek beds to exposed bedrock • Issue: biased landscape positions • New drilling • Focused on areas where our field knowledge was poor/incomplete • Drilled in clusters, along toposequences • < 9 m, 60 mm in tact cores removed • 714 useable depth records • 128,000 ha study area • ~ 1 observation per 180 ha
  • 5. Modelling regolith depth • An environmental correlation approach • Using readily available environmental parameters (digital grid maps) to predict other, less easy to measure environmental parameters • The environmental parameters correlate to soil properties, e.g. relationships between elevation and hillslope soil depth • Environmental parameters from national data infrastructure, including • Topographic parameters: ref John Gallant’s talk, including MrVBF, topographic wetness index, aspect, slope … • Climatic parameters: rainfall, evaporation, …. • Geochemical parameters: geology, gamma radiometrics, weathering intensity index, …. • 28 used • Grids standardised to 30 m ground resolution • Piecewise, multi linear regression modelling (“Cubist” software) • Model produces a decision tree, consisting of  Branches, the rules/conditions (“piecewise”)  Leaves , the linear regression models • Cubist makes models explicit for expert evaluation • Model result • R2 0.64
  • 6.
  • 7. Next? • Working towards a seamless, consistent national regolith map • An enduring piece of national data infrastructure for all Australian/international biophysical modellers • With estimates of uncertainty • Presented /served via • Discoverable through the TERN Data Discovery Portal http://portal.tern.org.au • Visible through the TERN Soil Portal http://www.asris.csiro.au/viewer/tern • Downloadable from CSIRO Data Access Portal https://data/csiro/dap • Phase 2 - testing the approach in the Burdekin catchment (on-going) • New biophysical region with new national analogues • Complements the spatial disaggregation approach (Nathan Odgers’ talk), which will be used for method benchmarking • Multiple lines of evidence, testing multiple approaches towards the best national data product(s) • National approaches may vary, depending on • Biophysical regions, landscape histories • Quality, density of useable site observations • The local “power” of specific environmental parameters • National regolith map: a stitched patchwork of multiple biophysical regolith models/maps (?) • New regolith map themes • Whole-of-profile or layer-by-layer stocks • Plant available water • C, N, P, trace elements …. • clay content, salinity, pH … • …
  • 8. Acknowledgements • CRC Forestry • SA Government (DWLBC) Thank you Dr Mark Thomas CSIRO Land and Water mark.thomas@csiro.au 08 8303 8471