Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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oxidative and reductive reactions in the soil solution 85<br />
These constants are determined by mixing a solution of known concentration,<br />
measured in mg/L, with a known amount of soil, measured in kilograms.<br />
After a period of time the solution and solid are separated and the amount of<br />
a given component in solution is measured. From this data a Kd can be calculated.<br />
This procedure is often performed for various periods of time and at<br />
various concentrations of a target compound in solution. In the determination<br />
of K om, the amount of organic matter in the solid phase, namely, soil, is determined<br />
(see Chapter 3), and this amount is used as the kilogram value of<br />
organic matter.<br />
From these two equations, the larger the amount of component sorbed <strong>to</strong><br />
the solid phase, the larger the K d or K om and the less likely it is <strong>to</strong> move in the<br />
soil. Because K d and K om are determined using the compound in a pure<br />
solvent, usually water, and a soil suspension, these constants do not necessarly<br />
give information about how difficult the extraction of a component is likely <strong>to</strong><br />
be when a specific extractant is used, such as mixed solvents or extractants<br />
using specific extracting or complexing agents [7,8].<br />
4.12. OXIDATIVE AND REDUCTIVE REACTIONS IN<br />
THE SOIL SOLUTION<br />
Many chemical reactions occurring in soils are acid–base reactions; however,<br />
oxidation–reduction reactions are more frequently the cause of confusion and<br />
may complicate the interpretation of analytical results. The reason is that<br />
reduced species, for instance, ferrous iron and the bivalent manganese, are<br />
seldom assumed <strong>to</strong> occur in the liquid and solid phases in a well-aerated soil,<br />
although they usually do.<br />
During and after a rainfall the soil will quickly become anaerobic because<br />
microorganisms and plant roots use up dissolved and trapped oxygen. Under<br />
these conditions, reduction of various constituents takes place. When the soil<br />
drains or dries, air replaces the water and there is movement of oxygen back<br />
in<strong>to</strong> the pores. However, not all pores drain immediately, and some pores<br />
never drain at all. Both these situations lead <strong>to</strong> anaerobic zones. Even when<br />
soils become aerobic, the reaction leading <strong>to</strong> oxidation of the reduced species<br />
may not be fast enough <strong>to</strong> remove all reduced species before the next anaerobic<br />
event.<br />
Drying soil at an elevated temperature will result in the loss of water from<br />
these normally filled pores, thereby allowing reactions that would not<br />
otherwise take place. Also, chemical reactions take place faster at higher<br />
temperatures, resulting in reactions taking place much more rapidly than<br />
they normally would in soil. This not only changes the amount of compounds<br />
in the soil sample but will also change the ratios of the components present<br />
and may even lead <strong>to</strong> the formation of compounds not naturally present in<br />
soil at all. For these reasons soil is not dried at elevated temperatures before<br />
analysis [9].