Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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124 titrimetric measurement<br />
- + X + Ag Æ AgClØ<br />
(6.3)<br />
Reaction (6.3) is a precipitation titration that can be done with or without<br />
an indica<strong>to</strong>r. Silver as a cation is very reactive and is an oxidizing agent. For<br />
instance, it can oxidize aldehydes, including aldoses (sugars with an aldehyde<br />
functionality). For this reason it is possible <strong>to</strong> obtain inaccurate or misleading<br />
results with titrating a soil extract with silver nitrate.<br />
The most common halogen in soil is chloride while both bromide and iodide<br />
occur but are uncommon [8]. The occurrence of either of these anions in soil<br />
would be cause for concern. Analysis for these other halides could be carried<br />
out using either capillary electrophoresis or high-performance liquid chroma<strong>to</strong>graphy<br />
(HPLC) (see Chapters 8 and 9).<br />
6.9. pH–STAT TITRATIONS<br />
In another type of titration, termed pH–stat, 2 the system is maintained at one<br />
fixed pH during a reaction. This type of titration has been applied <strong>to</strong> bioreac<strong>to</strong>rs<br />
where neither the starting material nor the product of the reaction is<br />
titrated but rather acidic or basic byproducts or coproduced acid or base are<br />
measured. In biological reactions this may be CO 2,HCO 3 - , or CO3 2- .The system,<br />
maintained at a fixed temperature during the reaction of interest, is titrated<br />
with an au<strong>to</strong>matic titra<strong>to</strong>r set <strong>to</strong> maintain the specific pH. Bioreac<strong>to</strong>rs may be<br />
sealed <strong>to</strong> ensure that no liquid or gas is lost or gained, or they may be open<br />
<strong>to</strong> allow the exchange of gases.<br />
The titrant used in pH–stat procedures is usually a dilute (perhaps 0.01<br />
molar) acid or base. Two different sets of data can be obtained from a pH–stat<br />
titration.The amount of a substrate consumed or product formed can be determined<br />
by the <strong>to</strong>tal amount of titrant used. Because the titrant is added over a<br />
period of time, the rate of reaction can also be determined.<br />
Even a small soil sample can be considered as a bioreac<strong>to</strong>r, and so the<br />
pH–stat method is applicable <strong>to</strong> soil. However, although this method is applicable<br />
<strong>to</strong> the study of processes occurring in soil, it is not particularly useful in<br />
routine analysis of soil components [9].<br />
6.10. CONCLUSIONS<br />
The titrimetric determination of soil constituents is most commonly applied<br />
<strong>to</strong> a limited number of soil analyses, namely, organic carbon, nitrogen compounds,<br />
carbonates, and chlorides. Determination of acid content by titration<br />
is seldom done because the titration curves are not amenable <strong>to</strong> typical titra-<br />
2 Stat stands for static and derives from the fact that the pH is held static during the progress of<br />
the reaction.