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Dry and wet soil spectra were the default soil spectra in a PROSAIL model (Jacquemoud et al. 2009).
The results showed that EPO minimized the variability of soil spectra induced by moisture.
This method generally benefits from complexity, with which the soil spectra are treated.
These difficulties could be handled more appropriately by the prediction models based on the LWIR soil spectra.
Although there are several studies using soil spectra measured by satellites, soil evaluation through LST is still scarce.
Munsell soil color and soil order were predicted from soil spectra and used to characterize the MU.
Similar(35)
We conclude that HF treatment was more effective than dry ashing and NaOCl oxidation to accentuate organics in the soil DRIFT spectra, since it provided mineral interference free spectra with in general least affected organic bands.
However, valuable structural information is likely stored in the soil Raman spectra.
Moisture is the single most important factor that affects soil reflectance spectra, particularly for field applications.
The culmination of these processes alters the optical properties of surface materials by reddening and darkening soil reflectance spectra and attenuating characteristic absorption bands (Hapke 2001; Clark et al. 2002; Chapman 2004).
This study illustrates that soil Raman spectra contain information of soil constituents even in the presence of fluorescence interference; moreover, it demonstrates that this contained information can play a vital role in the characterization of symmetric structures of SOM, which can provide complementary knowledge to understand molecular structure of SOM that infrared spectroscopy cannot offer.
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