05.04.2013 Views

Introduction to Soil Chemistry

Introduction to Soil Chemistry

Introduction to Soil Chemistry

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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)

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!