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Introduction to Soil Chemistry

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extract cleanup 141<br />

Table 7.3. Some Common Extraction Cleanup Methods<br />

Method Based on<br />

Sorbent Used Advantages Disadvantages<br />

Alumina Diffferent pH and activity May decompose or<br />

ranges available for irreversibly sorb<br />

different cleanup needs compounds<br />

Florisil Cleanup of chlorinated Has basic properties and<br />

hydrocarbons, nitrogen, may not be compatible<br />

and aromatic compounds with acids<br />

Silica gel Separation on the basis Components with the<br />

of differing polarity same polarity will not<br />

be separated<br />

Gel permeation Components separated Different components of<br />

on the basis of size the same size will not<br />

be separated<br />

procedures; however, the former has the advantage of both separating the<br />

component of interest from other materials and concentrating it.<br />

In either case materials commonly used as sorbants are stationary phases<br />

used in chroma<strong>to</strong>graphy. Because of their common chroma<strong>to</strong>graphic use,<br />

these sorbants are well described in the literature and their characteristics and<br />

sorbtive capacities known. Thus all three aluminas—acid, neutral, and basic—<br />

have been used, along with silica gel, Florisil, and gel permeation for different<br />

compounds and environmental samples.<br />

Solid-phase cleanup separates and concentrates components of interest.<br />

However, care must be taken <strong>to</strong> ensure that the capacity of the column is not<br />

exceeded. If it is, some of the component of interest will not be retained on<br />

the column and thus lost, resulting in analytical results lower that the true<br />

amounts present.<br />

7.5.3. Water Removal<br />

Water is always present in soil; even air dry soil contains a significant amount<br />

of water. The temptation is <strong>to</strong> remove all water before analysis, but <strong>to</strong> accomplish<br />

this, soil must be dried at a temperature above 100°C. This procedure<br />

works but causes irreversible changes in soil characteristics such that its extraction<br />

and subsequent analytical results are inaccurate, at least when compared<br />

with the results obtained on “fresh” unheated soil samples. The issue then<br />

becomes how <strong>to</strong> circumvent these problems.<br />

The most common and standard method is <strong>to</strong> allow soil <strong>to</strong> dry naturally at<br />

room temperature or sometimes a little above room temperature (35°C<br />

maximum) before extraction or analysis. This will result in a soil sample con

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