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Introduction to Soil Chemistry

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halogen ion determination 123<br />

6.7. CARBONATE DETERMINATION<br />

Carbonates decompose under acidic conditions with the release of carbon<br />

dioxide:<br />

CaCO + 2HCl<br />

Æ CaCl + CO ≠+ H O<br />

3 2 2 2<br />

CO + 2NaOH<br />

Æ Na CO + H O<br />

2 2 3 2<br />

(6.2a)<br />

(6.2b)<br />

To determine the carbonate, a soil sample can be placed in an Erlenmeyer<br />

flask and a 0.1 molar solution of hydrochloric acid (HCl) is added until no<br />

more carbon dioxide is released. The amount of HCl consumed is used <strong>to</strong> calculate<br />

the amount of carbonate present.The reaction shown is for calcium carbonate;<br />

however, all carbonates in the soil will also be decomposed, and thus<br />

this is a method for determining the <strong>to</strong>tal carbonate content, not just the<br />

calcium carbonate. Additionally, inaccuracies can be caused by other components<br />

in soil that can react with the HCl.<br />

Another approach would be <strong>to</strong> measure the amount of carbon dioxide<br />

produced either by measuring the volume of gas released or by reacting the<br />

carbon dioxide, in a separate flask, with base and determining the amount of<br />

base remaining after all the carbonate has precipitated and been removed<br />

from the solution.<br />

Alternatively, the weight lost when the carbonate is reacted with HCl can<br />

be determined. Heating carbonates results in their decomposition. Thus soils<br />

containing carbonate can be heated <strong>to</strong> the appropriate temperature and the<br />

weight loss measured. In this approach the loss of organic matter and water<br />

of hydration of various components in soil must be corrected for in order <strong>to</strong><br />

determine the weight of carbon dioxide lost [7].<br />

6.8. HALOGEN ION DETERMINATION<br />

Inorganic halogen containing compounds are usually very soluble salts. They<br />

commonly occur as simple, single, negatively charged anions in soil. There are<br />

two common exceptions <strong>to</strong> this generalization. First, fluorine is commonly<br />

found bonded <strong>to</strong> phosphate in insoluble minerals called apatites, which are<br />

calcium phosphate fluorides. The second are halogens, which are sigmabonded<br />

<strong>to</strong> carbon.<br />

The halogen anions are easily leached from soil with water and can be<br />

determined using silver nitrate as a titrant. The letter X is commonly used <strong>to</strong><br />

represent halogens and thus may be interpreted <strong>to</strong> be any of them (i.e., F, Cl,<br />

Br, or I) but is not generally used for At. The following reaction of silver with<br />

halogen X - ignores other possible counterions, namely, nitrate and the cation<br />

associated with the halide:

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