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Introduction to Soil Chemistry

Introduction to Soil Chemistry

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ph titration of soil 115<br />

Figure 6.2. Setup for titrating and recording pH change using a pH meter card in a lap<strong>to</strong>p<br />

computer.<br />

pH<br />

<strong>Soil</strong> Titration With Calcium Hydroxide<br />

7.5<br />

7.3<br />

7.1<br />

6.9<br />

6.7<br />

6.5<br />

6.3<br />

6.1<br />

5.9<br />

5.7<br />

5.5<br />

0 50 100 150 200 250 300<br />

mL of titrant<br />

Figure 6.3. Stepwise titration of acidic soil with calcium hydroxide.<br />

The initial pH rise as shown in Figure 6.3 and fallback is interpreted <strong>to</strong> be<br />

a result of two reactions. The initial rapid pH increase is a result of neutralization<br />

of free acid in the soil solution. Often this is represented as H + ;<br />

however, in aqueous solutions it is better represented as H3O + , the hydronium<br />

ion. The slower subsequent decrease in pH is a result of reequilibration

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