Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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164 spectroscopy<br />
these make analysis of some components mixed with water difficult or<br />
impossible.<br />
Infrared spectroscopy is most frequently used for the identification of<br />
organic compounds. Some organic functional groups, particularly alcohol, acid,<br />
carbonyl, double bonds, triple bonds, and amines, have unique, strong, and<br />
easily identifiable absorptions in the IR spectrum. Both methyl and methylene<br />
groups are insensitive <strong>to</strong> their environments and absorb strongly in narrow<br />
frequency ranges, making them easily identifiable and useful for quantification<br />
(see discussion of hydrocarbon analysis below). However, since these groups<br />
are almost always present in organic compounds, their absorptions are seldom<br />
useful in identifying specific compounds. Carbonyl groups also have a strong,<br />
sharp absorption that is usually the strongest in the spectrum, which also<br />
makes their absorption behavior useful for identification.<br />
A correlation chart giving the important and unique absorptions of various<br />
organic functionalities can be found in many books on infrared spectroscopy.<br />
These charts are useful, but the user needs <strong>to</strong> be familiar with the shape and<br />
size of typical functional group absorptions before using them with any degree<br />
of accuracy. A broad absorption between 2500 and 3650cm -1 shows the presence<br />
of —OH. However, the absorption of alcohol —OH is very different from<br />
that of acid, as can be seen in Figure 8.11. Another example is the carbonyl<br />
absorption, which occurs in the 1700cm -1 region of the spectrum. It is important<br />
<strong>to</strong> know not only that these are sharp absorptions but also that they are<br />
the strongest absorptions in the spectrum of aldehydes, ke<strong>to</strong>nes, and acids as<br />
seen in Figure 8.11. If there is an absorption in this region but it is not the<br />
strongest absorption in the entire spectrum or is not sharp, then it is not from<br />
a typical aldehyde, ke<strong>to</strong>ne, or acid but may be from a double bond, although<br />
this is not common. Table 8.1 lists some important functional group absorptions<br />
for the MIR region of the spectrum.<br />
Infrared is not typically used in common soil analytical procedures,<br />
although it has been used <strong>to</strong> investigate various soil components, the most<br />
common of which are humus and its various subcomponents (see Figure 8.12).<br />
It has also been used <strong>to</strong> identify soil clays, both crystalline and amorphous.<br />
Spectra can be accessed on the Web at http://speclab.cr.usgs.gov<br />
particularly see splib04a.<br />
There is one case, in environmental work, where the methyl and methylene<br />
absorptions are both useful and used. This is in the USEPA method for the<br />
determination of <strong>to</strong>tal recoverable petroleum hydrocarbons (TRPHs) in a soil<br />
or other extract. Here a supercritical carbon dioxide extraction of a<br />
hydrocarbon-contaminated soil is made (USEPA Method 3560) (see also<br />
Chapter 7). The extracted hydrocarbons are dissolved in tetrachloroethylene,<br />
which is transparent in the region of the IR spectrum where methyl and methylene<br />
groups absorb. The infrared —CH 3, —CH2—, absorptions in the<br />
2800–3000cm -1 region are related <strong>to</strong> the amount of hydrocarbons in the soil<br />
extract through standard curves constructed, as described above, for the<br />
method [20–26].