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Postdoc ČZU (ESF/MEYS CZ.1.07/2.3.00/30.0040)
Common Chemometric Indicators for
Prediction of Soil Organic Matter
Content and Quality from Soil Spectra:
A Review and Research Perspectives
Department of Soil Science and Soil Protection, Faculty of Agrobilogy, Food and
Natural Resources, Czech University of Life Sciences Prague
Asa Gholizadeh, Luboš Borůvka, M.Mehdi Saberioon
Soil Organic Matter (SOM)
Trend in soil organic matter content ( Brady 1999)
Why focus on SOM?
Managing soil organic matter is the key to air and water
quality and also agricultural higher output.
Conventional Soil Management Techniques
Uniform ManagementHigh Input & Cost Low Output
Time-Consuming LaborEnvironment Pollution
Conventional Methods of Soil Management
Current role of
Vis-NIR and MIR
Pre-treatment,
Calibration and
Validation
Geographical
Scales
Uncertainty and
Accuracy
Objectives
Vis, NIR and MIR Spectroscopy for SOM
Assessment
Olinger & Griffiths (1993)
Vis and NIR are used for the quantitative determination
MIR is used for the qualitative determination
Bartholomeus et al. (2008)
Henderson et al. (1992)
Vis had strong correlation with SOM content
Nocita et al. (2013)
Christy (2008)
NIR had strong correlation with SOM content
Viscarra Rossel et al. (2009)
MIR had strong correlation with SOM content
Cozzolino & Moron (2006)
Cecillon et al. (2009)
Shepherd & Walsh (2002)
Reeves et al. (2006)
Cecillon et al. (2009)
Du & Zhou (2009)
Merry & Janik (2013)
Vis-NIR had strong correlation with SOM quality
MIR had strong correlation with SOM quality
Spectroscopic Pre-treatment, Calibration
and Validation
Calibration Techniques
SMLR: The estimated regression coefficients vary
markedly when the outlying observations are changed
or deleted. Furthermore, the variability of the
estimated regression coefficients becomes inflated.
PCR: The PCs selected are not essentially the best
predictors for the reference data. Moreover, there is no
guarantee that the first PCs will include the spectral
data related to the specific dependent variable that
needs to be modeled.
PLSR: Not appropriate when the nonlinear models is
needed.
ANN: Requires a large number of training data, which
always influence the training speed. The over-fitting
nature is also a difficulty to conquer in order to create a
good result.
Nicolai et al. (2007)
Esbensen et al. (2002)
Nicolai et al. (2007)
Zhang et al. (2008)
Shao et al. (2012)
LS-SVM as Recommended Calibration
Technique
Sonali et al. (2013)
strike the right balance between accuracy attained on a
given finite amount of training patterns and the ability
to generalize to unseen data.
Stevens et al. (2010)
Yasumaru (2011)
It has the capability for linear and nonlinear
multivariate calibration and solves the multivariate
calibration problems in a relatively fast way.
It is a method with high accuracy, simplicity and
robustness.
Chen et al. (2012)
The most valuable properties of SVMs are their ability
to handle large input spaces efficiently.
Shao et al. (2012)
Stevens et al.
(2010)
Viscarra Rossel &
Behrens (2010)
Vohland &
Emmerling (2011)
Predictions of different soil properties by LS-SVM using all Vis-NIR
wavelengths produced the higher R2 and smaller RMSE values.
Various Pre-treatment Strategies Results on
the Same SOM Data
Spectroscopy for SOM Assessment
No. Vis/NIR/MIR Sample Data Processing
Validation
Set
SEP (%) Range in µm Reference
1 Vis-NIR Lab/Fresh PLSR 70% 0.39 0.4-2.5
Van Vuuren et al.,
2006
2 NIR
Lab/Ground
(Moisturized)
MLR 33% 0.19 1.65-2.5
Sudduth &
Hummel, 1993
3 Vis-NIR
Lab (Oven
Dried)/Ground
1stD- PLSR LooCV 4.6 0.4-2.5
Rinnan & Rinnan,
2007
4 NIR Field/On-the-go SNV- 1stD- PCR LooCV 0.4 0.7-1.7 Christy, 2008
5 Vis-NIR
Field/Hole and
Trench
MSC-1stD- PLS 22% 2.1 0.4-2.45
Ben-Dor et al.,
2008
6 MIR
Lab (Oven
Dried)/Ground
PLSR LooCV 0.72 2.5-25
Masserschmidt et
al., 1999
Calibration Scales: Field, Regional or Global
Accuracy and Uncertainty in Soil
Spectroscopy
Conclusions
 For the determination of SOM quantity and quality, MIR spectroscopy is
often more accurate and produces more robust calibrations than Vis-NIR
spectroscopy.
 Finding suitable data pre-treatment and calibration strategies for the
application of Vis-NIR or MIR spectroscopy is dramatically eye-catching.
 Smoothing (mostly Savitzky-Golay) and LS-SVM algorithms lead to over-
optimistic performance in the assessment of SOM.
 A global soil spectral libraries will improve the predictive ability of
spectroscopy for soil quantity and quality attributes whatever the soil type.
 Inaccuracy and uncertainties occur in different steps within the prediction
procedure such as soil sampling, spectra collecting, building the prediction
model (number of training samples and model parameters) and final spatial
prediction.
Future Works
 Standardization of Vis-NIR and MIR spectroscopy calibration is
needed and it would allow the identification of soil properties including
SOM quantity and quality that are possibly spectroscopy predictable and
would lead to an enhanced acceptance of Vis–NIR and MIR spectroscopy
in soil analyses.
 Internal standards, a standard protocol and controlled conditions can
assist in sharing and comparing soil spectra worldwide with higher
accuracy.
 An urgent research need is the development of global soil spectral
libraries.
Thank you
Postdoc ČZU (ESF/MEYS CZ.1.07/2.3.00/30.0040)

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Predicting Soil Organic Matter from Spectra

  • 1. Postdoc ČZU (ESF/MEYS CZ.1.07/2.3.00/30.0040) Common Chemometric Indicators for Prediction of Soil Organic Matter Content and Quality from Soil Spectra: A Review and Research Perspectives Department of Soil Science and Soil Protection, Faculty of Agrobilogy, Food and Natural Resources, Czech University of Life Sciences Prague Asa Gholizadeh, Luboš Borůvka, M.Mehdi Saberioon
  • 2. Soil Organic Matter (SOM) Trend in soil organic matter content ( Brady 1999)
  • 3. Why focus on SOM? Managing soil organic matter is the key to air and water quality and also agricultural higher output.
  • 4. Conventional Soil Management Techniques Uniform ManagementHigh Input & Cost Low Output Time-Consuming LaborEnvironment Pollution Conventional Methods of Soil Management
  • 5. Current role of Vis-NIR and MIR Pre-treatment, Calibration and Validation Geographical Scales Uncertainty and Accuracy Objectives
  • 6. Vis, NIR and MIR Spectroscopy for SOM Assessment Olinger & Griffiths (1993) Vis and NIR are used for the quantitative determination MIR is used for the qualitative determination Bartholomeus et al. (2008) Henderson et al. (1992) Vis had strong correlation with SOM content Nocita et al. (2013) Christy (2008) NIR had strong correlation with SOM content Viscarra Rossel et al. (2009) MIR had strong correlation with SOM content Cozzolino & Moron (2006) Cecillon et al. (2009) Shepherd & Walsh (2002) Reeves et al. (2006) Cecillon et al. (2009) Du & Zhou (2009) Merry & Janik (2013) Vis-NIR had strong correlation with SOM quality MIR had strong correlation with SOM quality
  • 8. Calibration Techniques SMLR: The estimated regression coefficients vary markedly when the outlying observations are changed or deleted. Furthermore, the variability of the estimated regression coefficients becomes inflated. PCR: The PCs selected are not essentially the best predictors for the reference data. Moreover, there is no guarantee that the first PCs will include the spectral data related to the specific dependent variable that needs to be modeled. PLSR: Not appropriate when the nonlinear models is needed. ANN: Requires a large number of training data, which always influence the training speed. The over-fitting nature is also a difficulty to conquer in order to create a good result. Nicolai et al. (2007) Esbensen et al. (2002) Nicolai et al. (2007) Zhang et al. (2008) Shao et al. (2012)
  • 9. LS-SVM as Recommended Calibration Technique Sonali et al. (2013) strike the right balance between accuracy attained on a given finite amount of training patterns and the ability to generalize to unseen data. Stevens et al. (2010) Yasumaru (2011) It has the capability for linear and nonlinear multivariate calibration and solves the multivariate calibration problems in a relatively fast way. It is a method with high accuracy, simplicity and robustness. Chen et al. (2012) The most valuable properties of SVMs are their ability to handle large input spaces efficiently. Shao et al. (2012) Stevens et al. (2010) Viscarra Rossel & Behrens (2010) Vohland & Emmerling (2011) Predictions of different soil properties by LS-SVM using all Vis-NIR wavelengths produced the higher R2 and smaller RMSE values.
  • 10. Various Pre-treatment Strategies Results on the Same SOM Data
  • 11. Spectroscopy for SOM Assessment No. Vis/NIR/MIR Sample Data Processing Validation Set SEP (%) Range in µm Reference 1 Vis-NIR Lab/Fresh PLSR 70% 0.39 0.4-2.5 Van Vuuren et al., 2006 2 NIR Lab/Ground (Moisturized) MLR 33% 0.19 1.65-2.5 Sudduth & Hummel, 1993 3 Vis-NIR Lab (Oven Dried)/Ground 1stD- PLSR LooCV 4.6 0.4-2.5 Rinnan & Rinnan, 2007 4 NIR Field/On-the-go SNV- 1stD- PCR LooCV 0.4 0.7-1.7 Christy, 2008 5 Vis-NIR Field/Hole and Trench MSC-1stD- PLS 22% 2.1 0.4-2.45 Ben-Dor et al., 2008 6 MIR Lab (Oven Dried)/Ground PLSR LooCV 0.72 2.5-25 Masserschmidt et al., 1999
  • 12. Calibration Scales: Field, Regional or Global
  • 13. Accuracy and Uncertainty in Soil Spectroscopy
  • 14. Conclusions  For the determination of SOM quantity and quality, MIR spectroscopy is often more accurate and produces more robust calibrations than Vis-NIR spectroscopy.  Finding suitable data pre-treatment and calibration strategies for the application of Vis-NIR or MIR spectroscopy is dramatically eye-catching.  Smoothing (mostly Savitzky-Golay) and LS-SVM algorithms lead to over- optimistic performance in the assessment of SOM.  A global soil spectral libraries will improve the predictive ability of spectroscopy for soil quantity and quality attributes whatever the soil type.  Inaccuracy and uncertainties occur in different steps within the prediction procedure such as soil sampling, spectra collecting, building the prediction model (number of training samples and model parameters) and final spatial prediction.
  • 15. Future Works  Standardization of Vis-NIR and MIR spectroscopy calibration is needed and it would allow the identification of soil properties including SOM quantity and quality that are possibly spectroscopy predictable and would lead to an enhanced acceptance of Vis–NIR and MIR spectroscopy in soil analyses.  Internal standards, a standard protocol and controlled conditions can assist in sharing and comparing soil spectra worldwide with higher accuracy.  An urgent research need is the development of global soil spectral libraries.
  • 16. Thank you Postdoc ČZU (ESF/MEYS CZ.1.07/2.3.00/30.0040)