Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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cations 201<br />
Manganese does, however, have some unusual characteristics. It is very<br />
unusual <strong>to</strong> find soil situations where iron is <strong>to</strong>xic, whereas manganese <strong>to</strong>xicity<br />
is known.As noted above, iron is found in only two oxidation states while manganese<br />
can have three oxidation states. However, the situation is found <strong>to</strong> be<br />
much more complex than this when soil is analyzed for the species of manganese<br />
present. A simple analysis for manganese might indicate an oxidation<br />
state of +3.5, indicating that the material analyzed contains an unknown<br />
mixture of the common oxidation states of soil manganese. This then creates<br />
problems in understanding the chemistry of manganese and thus reactions<br />
leading <strong>to</strong> its deficiency, <strong>to</strong>xicity, biological availability, and movement in the<br />
environment.This is an issue and problem which has received significant attention<br />
and research [10].<br />
10.1.2.3 Chromium<br />
Chromium has numerous oxidation states, some of which are strongly oxidizing.<br />
The most highly oxidized species is Cr 6+ , and the reduced ion is Cr 3+ .In<br />
soil, because of its strong oxidizing characteristics and oxidizable species<br />
present, Cr 6+ is rapidly reduced <strong>to</strong> Cr 3+ . Chromium species of intermediate oxidation<br />
states can exist in soil; however, the +3 state is the most common. As<br />
with the other metals, all the possible combinations of species with other components<br />
are possible and must be kept in mind when carrying out an analysis<br />
for chromium species in soil [11–13].<br />
10.1.2.4 Mercury<br />
Mercury is unusual in that it is found in the environment as both oxidized<br />
mercury ions and reduced methyl mercury. The mercurous (Hg + ) ion is unstable<br />
and not likely <strong>to</strong> be found in soil, while mercuric (Hg 2+ ) ions and methyl<br />
mercury compounds are. All forms of mercury are of environmental concern,<br />
and mercury ions can form the same types of interactions with soil constituents<br />
as those described for other multi-oxidation-state metals. Mercury in all its<br />
forms is <strong>to</strong>xic and thus of concern; however, methyl mercury, which can form<br />
in soil under anaerobic conditions, is particularly dangerous because of its<br />
extreme <strong>to</strong>xicity.<br />
Mercury has several other characteristics that render it of particular environmental<br />
concern and make it likely <strong>to</strong> be found as many different species.<br />
It is a natural constituent of soil, although it occurs at low concentrations. It<br />
is widely used in both industry and in the labora<strong>to</strong>ry, making it a common contaminant<br />
of reference materials. Metallic mercury has a relatively high vapor<br />
pressure, which means that it can occur in measurable amounts in the soil<br />
atmosphere.<br />
Analysis of mercury is difficult, and specialized sampling and instrumental<br />
techniques are generally required <strong>to</strong> carry out an accurate analysis. Although