Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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156 spectroscopy<br />
8.6. ULTRAVIOLET AND VISIBLE SPECTROSCOPY<br />
Information about a soil extract can be obtained from the ultraviolet and<br />
visible regions of the spectrum. These are wavelengths ranging within 190–400<br />
and 400–900nm, respectively (wider ranges of wavelengths are available on<br />
some instruments). The two regions of the spectrum are used very differently<br />
in soil analysis, although they are commonly found <strong>to</strong>gether in UV–Vis<br />
(ultraviolet–visible) spectrometers. The ultraviolet region can be used <strong>to</strong><br />
obtain spectra of soil extracts; however, it is most commonly used as a detec<strong>to</strong>r<br />
for high-performance liquid chroma<strong>to</strong>graph (HPLC). The visible region is<br />
used for colorimetric analysis, discussed below.<br />
Common solvents, such as water, ace<strong>to</strong>nitirile, and heptane, are transparent<br />
over both the ultraviolet and visible regions. Because these represent both<br />
hydrophilic and hydrophobic solvents, a very broad range of compounds can<br />
be easily analyzed by UV.<br />
Adsorption in both regions involves promotion of electrons in double or<br />
triple bonds or nonbonding pairs of electrons in elements such as those on<br />
oxygen or nitrogen, <strong>to</strong> higher energy levels. Conjugated double bonds and nonbonding<br />
pairs conjugated with double bonds absorb at longer wavelengths<br />
than do isolated double bonds or nonbonding electron pairs. The more highly<br />
conjugated a system the longer the wavelength of the maximum absorption<br />
called the lambda max (l max) (see Figure 8.6). This means that all aromatic<br />
compounds have strong ultraviolet adsorption bands as well as terpenes and<br />
other conjugated systems. Unconjugated aldehydes, ke<strong>to</strong>nes, amides, acids,<br />
esters, and similar compounds also have ultraviolet absorptions, although they<br />
are not as strong.<br />
Any extract of soil containing large amounts of organic matter may have<br />
multiple absorption bands in the UV–Vis region of the spectrum. A UV–Vis<br />
spectrum of a simple aqueous, low-organic-matter, soil extract is shown in<br />
Figure 8.6. As seen in this spectrum, even a simple soil extract can have significant<br />
absorptions that can mask other potential absorptions of interest.<br />
Absorptions can also result in interferences with an ultraviolet and/or visible<br />
determination of a component or the derivative of a component.<br />
An interesting application of this region of the spectrum is the determination<br />
of nitrate and nitrite in soil extracts. Nitrate is very soluble in water and<br />
can be extracted using a simple water extraction procedure. Nitrate absorbs<br />
at 210nm and nitrite are 355nm and can be quantified using these absorption<br />
maxima (l max). Other materials extracted from soil as noted above, however,<br />
can obscure this region, and thus caution must be exercised <strong>to</strong> determine<br />
whether there are any interfering components in the extract [11,12,15–17].<br />
8.6.1. Ultraviolet Sample Preparation<br />
Samples are analyzed dissolved in a solvent, commonly ace<strong>to</strong>nitrile, heptane,<br />
hexadecane, or water. A scan of the pure solvent in the sample cell, typically<br />
made of quartz (A in Figure 8.7), is first obtained. The dissolved sample is