Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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speciation 197<br />
vivid example of this is thalidomide, which exists in two optical isomers, one<br />
relieving nausea the other causing birth defects.<br />
Inorganic and metallorganic compounds also have conformations and<br />
isomers, including optical isomers. It is expected that these various conformers<br />
and isomers will also have varying biological activities.<br />
There are many other reasons why speciation might be important. Among<br />
these are plant nutrient availability, biological contamination by metals, human<br />
or animal <strong>to</strong>xicity, movement of species in the environment, biological accumulation<br />
or amplification, obtaining data needed for models, understanding a<br />
species’ role in the reactions and fates of various environment components,<br />
and development of a basic understanding of a species’ chemistry. Any one of<br />
these by itself is an important reason <strong>to</strong> understand speciation, and often<br />
several of these reasons will be important at the same time.<br />
Why might one be specifically interested in the species of components in<br />
soil? From a positive perspective it is desirable <strong>to</strong> provide plants with nutrients<br />
in forms that are available and yet are not present in concentrations high<br />
enough <strong>to</strong> cause environmental harm. From a negative aspect, some species<br />
of certain components are more and some less <strong>to</strong>xic. Some species are biologically<br />
available; some are not. Some species may accumulate in biological<br />
tissue; others will not. When a species is detected in the environment, it is<br />
important <strong>to</strong> know which of the categories described above it falls in<strong>to</strong>.<br />
A first step in deciding on an analytical procedure or a species <strong>to</strong> look for<br />
is <strong>to</strong> understand that the species of interest may be in one of, four “compartments”<br />
in soil (see Figure 10.3): the solid (both inorganic and organic), the<br />
liquid (soil solution), the gaseous (soil air), or the biological (living cells) compartment.<br />
It is important <strong>to</strong> remember that species are constantly moving both<br />
between compartments and between species.<br />
Once the compartment is decided on, then the species, as illustrated in<br />
Figure 10.1, <strong>to</strong> be analyzed for can be decided on. In this case it is important<br />
Solid<br />
Gaseous<br />
Biological<br />
Figure 10.3. <strong>Soil</strong> compartments.<br />
Solution