Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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118 titrimetric measurement<br />
Because of the complex nature of soil and the soil solution, it is rarely possible<br />
<strong>to</strong> directly determine specific soil constituents by titrating soil or soil solutions<br />
using a pH meter, selective ion electrode, or a platinum electrode (with<br />
appropriate reference electrode (see Chapter 5 for more details on this<br />
subject) [3].<br />
6.3. ORGANIC MATTER<br />
<strong>Soil</strong> organic matter can be divided in<strong>to</strong> many fractions; however, the first distinction<br />
between fractions is the active fraction, that is, the fraction undergoing<br />
active decomposition and the stable fraction, namely, the fraction that is<br />
relatively stable, mostly humus. The most common method of determining soil<br />
organic matter does not differentiate between these two types. All organic<br />
matter is oxidized using a strong oxidizing agent, most often potassium or<br />
sodium dichromate in sulfuric acid. To effect complete oxidation, heating,<br />
which can be done using a hotplate or by mixing the acidic and dichromate<br />
solutions, is required. When the reaction is completed, unreacted dichromate<br />
is titrated, in an oxidation–reduction titration, and the difference is used as the<br />
amount of organic matter present.<br />
This titration uses an indica<strong>to</strong>r, the color of which is difficult <strong>to</strong> see because<br />
of the soil present. The indica<strong>to</strong>r, however, is much easier <strong>to</strong> see with natural<br />
rather than fluorescent lighting.<br />
Other methods for determination of soil organic matter are available [4];<br />
however, they are not as commonly used as is dichromate oxidation, commonly<br />
called the Watley–Black method. Usually these methods are both more<br />
time-consuming and less accurate than is the dichromate oxidation titration<br />
method. Keep in mind that the dichromate oxidation of organic matter is the<br />
standard by which all other methods of determining soil organic matter must<br />
be compared [4,5].<br />
Caution: Chromates, including potassium and sodium dichromate,<br />
are hazardous materials, as are sulfuric and phosphoric acid used in<br />
the oxidation of soil organic matter. Great care must be exercised in<br />
using these chemicals.<br />
6.4. AMMONIA<br />
Ammonia is a gas that reacts with water <strong>to</strong> form ammonium as follows:<br />
H 3N + H 2O<br />
NH 4 + + – OH<br />
(6.1)