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Quantification of soil C stocks is hampered by spatial and temporal variability.
Characterization and quantification of soil properties are important for the optimum use and management our soil.
Quantification of soil respiration (Rs) is an essential step in modelling soil carbon fluxes associated with stand structure and management.
In this situation, quantification of soil loss and delineation of degraded areas is necessary for effective conservation planning (Yadav and Sidhu 2010).
The plasticity characteristics of fine-grained soil are used as fundamentals in classification processes and indirect quantification of soil swell potential.
X-ray microtomography, through quantification of soil structure at the microscale, could greatly facilitate the current understanding of soil hydrodynamic behaviour.
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Methods for quantification of the soil moisture are classified into three main groups: (i) measurement with remote sensing, (ii) estimation via (soil water balance) simulation models, and (iii) measurement in the field (ground based).
Quantification of the soil erosion is necessary for designing efficient degradation control strategies.
The technique could be modified for detection and quantification of all soil borne parasitic nematodes.
Also, it is important to assess the most appropriate spectral range for quantification of specific soil property.
In this study, we tested the potential of visible-near infrared (VNIR, 350 2500 nm) and mid-infrared spectroscopy (MIR, 2500 15,000 nm) for quantification and prediction of soil parameters to support the Saxon Permanent Soil Monitoring Program.
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