Fao longterm trials shepherd dec 2011

World Agroforestry (ICRAF)
World Agroforestry (ICRAF)Knowledge Management Specialist at World Agroforestry Centre um World Agroforestry (ICRAF)
Land Health Surveillance Harnessing science and technology to provide Reliable, comparable, and locally relevant information on land health status, risks and intervention outcomes  Global Research Project 4: Land Health World Agroforestry Centre (ICRAF)
Land Health The  capacity of land to sustain delivery of essential ecosystem services (the benefits people obtain from ecosystems) Widespread degradation is reducing productivity, impeding development , damaging the environment
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Land health surveillance
AfricaSoils.net ,[object Object],African Soil Information Service
AfricaSoils Sentinel Site  based on the  L and  D egradation  S urveillance  F ramework a spatially stratified, h i e r a r c h i c a l ,  r a n d o mized sampling framework Sentinel site (100 km 2 ) 16 Clusters (1 km 2 ) 10 Plots (1000 m 2 ) 4 Sub-Plots (100 m 2 )
Sampling plot  ( 1000 m 2 ) ,[object Object]
 
Infrared Spectroscopy for rapid soil characterization ,[object Object],[object Object],[object Object],[object Object]
What soil properties affect spectral shape?
Soil IR fundamentals 1 = Fingerprint region e.g Si-O-Si stretching/bending 2 = Double-bond region (e.g. C=O, C=C, C=N 3 = Triple bond (e.g. C≡C, C≡N) 4 = X–H stretching (e.g. O–H stretching) NIR = Overtones; key features clay lattice and water OH; SOM affects overall shape
Soil infrared calibrations
Covariates Remote Sensing (RS) and Spatial Data Cost surfaces, etc. Elevation Vegetation Hydrology Topographical  properties Climate Landsat Legacy data ASTER Quickbird MODIS 500 m 250 m 28.5 m 15 m 2.4 m 0.6 m ?
Local (site-level) C ref Examples from UNEP-ICRAF West Africa Drylands Project 10 km
Regional C ref 160 km
Spectral prediction of TOC, POC, Charcoal-C Australian and Kenya soils Janik LJ, Skjemstad JO, Shepherd KD and Spouncer LR (2007) The prediction of soil carbon fractions using mid-infrared-partial least square analysis. Journal of Australian Soil Research 45(2): 73–81. TOC :  alkyl –CH2 stretching modes;  carbohydrate  overtones of the –COH stretch;  carboxylic acid –COOH;  amide  I and II bands;  alkyl –CH2 deformation;  aromatic –CH in  plane deformation; carbohydrate–COH stretch. CHAR :  C=C skeletal  vibrations;  phenolic ,  or COO stretching vibrations; ring C–H   in plane deformations
Spectral prediction of SOC in global alfisols Kamau-Rewe, M., Rasche, F., Cobo, J.G., Dercon, G., Shepherd, K.D., Cadisch, G. (2011). Generic prediction of soil organic carbon in Alfisols using diffuse reflectance Fourier transformed mid-infrared spectroscopy. Soil Science Society of America Journal 75: 2358–2360. Not treated (NT) and with mineral signature subtracted Δ550
Spectral signatures respond to management-induced  changes in soil functional properties NARL long-term experiment, Kenya
Spectral differences in SOC quality in aggregates Verchot, L.V., Dutaur, L., Shepherd, K.D., Albrecht, A. 2011. Organic matter stabilization in soil aggregates: Understanding the biogeochemical mechanisms that determine the fate of carbon inputs in soils. Geoderma 161: 182–193. Microaggregates had similar spectra despite large texture differences Luero  35% sand Teso  76% sand The meso- and macro- aggregates, and macro-aggregates were enriched in carboxylic-C and aromatic-C, indicating the importance of OM decomposition and plant-derived C in the stabilization of larger aggregates.  ,[object Object],[object Object],[object Object],[object Object],[object Object]
Spectral prediction of C mineralization rates in SOC fractions Mutuo PK, Shepherd KD, Albrecht A, and Cadisch G (2006) Prediction of Carbon Mineralization Rates from Different Soil Physical Fractions Using Diffuse Reflectance Spectroscopy. Soil Biology & Biochemistry 38:1658–1664.
Extending to X-ray and laser technology
Aggregate stability using laser diffraction particle size analysis
Results   ( Quantitative x-ray diffraction spectroscopy  Mineral Semi-quant (%) Quartz Montmorillonite Microcline Kaolinite Hematite Ilmenite Gibbsite 76.9 4.0 3.2 10.2 2.9 2.0 0.8
Results   ( Characterise sites relative to AfSIS population
Results   ( Spectral applications in long-term trials ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
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Fao longterm trials shepherd dec 2011

  • 1. Land Health Surveillance Harnessing science and technology to provide Reliable, comparable, and locally relevant information on land health status, risks and intervention outcomes Global Research Project 4: Land Health World Agroforestry Centre (ICRAF)
  • 2. Land Health The capacity of land to sustain delivery of essential ecosystem services (the benefits people obtain from ecosystems) Widespread degradation is reducing productivity, impeding development , damaging the environment
  • 3.
  • 4.
  • 5. AfricaSoils Sentinel Site based on the L and D egradation S urveillance F ramework a spatially stratified, h i e r a r c h i c a l , r a n d o mized sampling framework Sentinel site (100 km 2 ) 16 Clusters (1 km 2 ) 10 Plots (1000 m 2 ) 4 Sub-Plots (100 m 2 )
  • 6.
  • 7.  
  • 8.
  • 9. What soil properties affect spectral shape?
  • 10. Soil IR fundamentals 1 = Fingerprint region e.g Si-O-Si stretching/bending 2 = Double-bond region (e.g. C=O, C=C, C=N 3 = Triple bond (e.g. C≡C, C≡N) 4 = X–H stretching (e.g. O–H stretching) NIR = Overtones; key features clay lattice and water OH; SOM affects overall shape
  • 12. Covariates Remote Sensing (RS) and Spatial Data Cost surfaces, etc. Elevation Vegetation Hydrology Topographical properties Climate Landsat Legacy data ASTER Quickbird MODIS 500 m 250 m 28.5 m 15 m 2.4 m 0.6 m ?
  • 13. Local (site-level) C ref Examples from UNEP-ICRAF West Africa Drylands Project 10 km
  • 14. Regional C ref 160 km
  • 15. Spectral prediction of TOC, POC, Charcoal-C Australian and Kenya soils Janik LJ, Skjemstad JO, Shepherd KD and Spouncer LR (2007) The prediction of soil carbon fractions using mid-infrared-partial least square analysis. Journal of Australian Soil Research 45(2): 73–81. TOC : alkyl –CH2 stretching modes; carbohydrate overtones of the –COH stretch; carboxylic acid –COOH; amide I and II bands; alkyl –CH2 deformation; aromatic –CH in plane deformation; carbohydrate–COH stretch. CHAR : C=C skeletal vibrations; phenolic , or COO stretching vibrations; ring C–H in plane deformations
  • 16. Spectral prediction of SOC in global alfisols Kamau-Rewe, M., Rasche, F., Cobo, J.G., Dercon, G., Shepherd, K.D., Cadisch, G. (2011). Generic prediction of soil organic carbon in Alfisols using diffuse reflectance Fourier transformed mid-infrared spectroscopy. Soil Science Society of America Journal 75: 2358–2360. Not treated (NT) and with mineral signature subtracted Δ550
  • 17. Spectral signatures respond to management-induced changes in soil functional properties NARL long-term experiment, Kenya
  • 18.
  • 19. Spectral prediction of C mineralization rates in SOC fractions Mutuo PK, Shepherd KD, Albrecht A, and Cadisch G (2006) Prediction of Carbon Mineralization Rates from Different Soil Physical Fractions Using Diffuse Reflectance Spectroscopy. Soil Biology & Biochemistry 38:1658–1664.
  • 20. Extending to X-ray and laser technology
  • 21. Aggregate stability using laser diffraction particle size analysis
  • 22. Results ( Quantitative x-ray diffraction spectroscopy Mineral Semi-quant (%) Quartz Montmorillonite Microcline Kaolinite Hematite Ilmenite Gibbsite 76.9 4.0 3.2 10.2 2.9 2.0 0.8
  • 23. Results ( Characterise sites relative to AfSIS population
  • 24.

Hinweis der Redaktion

  1. Third, use of infrared spectroscopy for rapid soil characterization. Using only light, this a rapid, low cost and high reproducible methods, which can predict not only carbon but a number of other soil functional properties.