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Introduction to Soil Chemistry

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extraction 129<br />

having cation exchange capacity (CEC). There are, however, some soils that<br />

have significant anion exchange capacity, and this possibility must never be<br />

overlooked.<br />

In cation exchange reactions typically both the charge and concentration<br />

of the cation in the extracting solution are important in determining its ability<br />

<strong>to</strong> exchange with cations already on the exchange sites. Generally, the larger<br />

the charge on the cation, the more effective it is in replacing other cations,<br />

especially those with less charge. Cations with less charge but at high concentration<br />

will replace cations with higher charge. This latter approach is generally<br />

the one taken in carrying out analysis involving cation exchange; thus an<br />

extracting solution containing a high concentration of lower charged cation is<br />

used in the extraction [11,12].<br />

In the case of compounds not attracted or attached <strong>to</strong> cation or anion<br />

exchange sites in soil, an aqueous solution containing a ligand or a mixture of<br />

ligands and auxiliary compounds that form an attraction for the compound of<br />

interest and result in the formation of a highly soluble compound, complex,<br />

or species is chosen. A solution of this ligand in distilled water is prepared and<br />

used <strong>to</strong> extract the soil [13–15].<br />

Another approach that has been used is <strong>to</strong> add a surfactant <strong>to</strong> aqueous<br />

extractants, particularly when insoluble components are <strong>to</strong> be extracted or are<br />

present. Typically soaps and both ionic and nonionic surfactants have been<br />

used. Because of the complex nature of some surfactants and their effect on<br />

viscosity, care must be taken <strong>to</strong> make sure that they do not adversely affect<br />

subsequent analytical procedures [16–18].<br />

In a similar fashion organic compounds are typically extracted using organic<br />

solvents or mixtures of organic solvents. In this case, because of the constant<br />

occurrence of water in soil, the solubility of water or the mutual solubility of<br />

the compound of interest and water in the extractant will be an important<br />

consideration.<br />

An attempt <strong>to</strong> circumvent these problems is <strong>to</strong> use mixed solvents, which<br />

are soluble in each other as well as in water. Thus a mixture of ace<strong>to</strong>ne, which<br />

is miscible with water, and hexane, which is a hydrophobic hydrocarbon insoluble<br />

in water, could be used as a soil extractant. The idea is <strong>to</strong> have a solvent<br />

that will dissolve in water and yet also dissolve hydrophobic contaminants in<br />

soil (see Section 7.2.1).<br />

Nonaqueous or hydrophobic extractants can also be used, although typically<br />

their usefulness is limited. Examples of these types of extractants are<br />

halogenated solvents such as the freons and chloroethanes. A problem with<br />

all these types of extractants is that water in nondraining pores is not accessible<br />

<strong>to</strong> them and thus any contaminant surrounded by water will not or will<br />

only partially be extracted.<br />

In the case of all of the above mentioned extractants, there are three important<br />

questions:<br />

1. Will the extractant extract the component or contaminant of interest?<br />

2. Is the extractant compatible with the analytical procedures <strong>to</strong> be used?

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