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Increases in plant reflectance in the water band are signs of early plant water stress.
That is why the intensity of the water band is decreasing with thermal treatment.
The water band appears at approximately 1630 cm−1, which is similar in all of the synthesized solids.
Adsorbed water bands are located in the region around (~3000-3440 cm−1) [21] and occluded water band at ~1640 cm−1 [22] in all the spectra.
Difference spectra for the water band obtained in the presence of salts suggested that only sulfate systems specifically affect polymer hydrations in the gel phase.
A linear regression based on reflectance at a chlorophyll sensitive wavelength (R683 nm), coupled with a water band index (R970/R900), was able to predict decline with 85% accuracy.
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What supplies go in your Mardi Gras survival kit? A. Water, Band-Aids, Popeyes fried chicken, king cake and vodka.
Infrared spectra of the water-added sample showed dominant water bands of zoisite.
The intensities in the water bands of the zoisite gradually decreased from the sample boundaries to the inner part of the sample.
A more reliable assignation can be made for the water bands at 1620 (bending), and 918 and 687 cm−1 (libration) by analogy with potassium alum [25, 26].
The diffusion coefficient of water in the water-added sample was determined from the gradient of the IR bands around the sample boundary (Fig. 9), which mainly showed water bands in zoisite formed by the reaction between anorthite and water (Eq. 1).
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