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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

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