Introduction to Soil Chemistry
Introduction to Soil Chemistry
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