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Introduction to Soil Chemistry

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100 electrical measurements<br />

Standardization is an essential component of soil pH measurement, and<br />

care must be taken <strong>to</strong> ensure good buffers. If the buffers show any indication<br />

of contamination, such as material floating in them, soil, or microbial growth,<br />

they must be discarded and new buffers prepared. All pH buffers will support<br />

microbial growth, which will interfere with electrode function and change the<br />

buffers pH.<br />

Measurements made using pH meters and electrodes are temperaturesensitive;<br />

that is, the pH reading obtained depends on the temperature of the<br />

solution. Some pH meters have a temperature probe such that a temperature<br />

correction is au<strong>to</strong>matically made during the measurement. However, if this is<br />

not the case, the pH meter must be set <strong>to</strong> the proper temperature if accurate<br />

measurements are <strong>to</strong> be obtained.<br />

Fouling of the reference electrode or the reference side of a combination<br />

electrode is a common problem in soil pH measurements. Fouling can be<br />

caused by salts, organic matter, and clay. Each electrode manufacturer will<br />

provide specific cleaning procedures that will help keep electrodes functioning<br />

properly; however, in many cases no amount of cleaning will be effective<br />

and the electrodes will need <strong>to</strong> be replaced.<br />

Depending on the extraction method <strong>to</strong> be used or developed, determination<br />

of pH using a standard method should be used. In different countries<br />

and geographic areas different standard methods will be in common use; for<br />

example, in Ohio (USA), a 1:1 soil:water suspension is used while in<br />

Zimbabwe a 1 : 1 soil : 0.01 M CaCl 2 is commonly used. The pHs determined by<br />

the standard method, used in a particular area, are used in many other procedures<br />

and methods and are used <strong>to</strong> make recommendations and predictions<br />

about the environment. Changing the method will mean that the validity of<br />

all these relationships will need <strong>to</strong> be reestablished or new relationships determined.<br />

For these reasons it is generally not advantageous <strong>to</strong> spend time and<br />

money developing a new methodology for determining soil pH unless there is<br />

a highly significant economic benefit in doing so [4–6].<br />

5.3.2. Ion-Selective Electrodes<br />

Ion measurements, using ion-selective electrodes (ISEs), 2 are very similar <strong>to</strong><br />

pH measurements and typically are carried out using a pH meter capable of<br />

accepting ion-selective electrodes. Each ion requires a specific electrode, some<br />

of which will be combination electrodes similar <strong>to</strong> combination pH electrodes,<br />

while others will be only the sensing electrode, called a half-cell. For these halfcell<br />

electrodes, special reference electrodes, which have a high flow of reference<br />

electrode solution, are used. There are two important differences<br />

between pH and ion-selective measurements: (1) the latter may require that<br />

the solution be separated from the soil before measurement is made and (2)<br />

2<br />

Ion-selective electrodes were originally called ion-specific electrodes, and this term may still be<br />

encountered.

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