Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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onding considerations 33<br />
The two oppositely charged species then attract each other, forming a compound.<br />
Although the seminal characteristic of compounds held <strong>to</strong>gether by<br />
ionic bonds is that they dissolve in water, giving a solution containing ions, it<br />
is essential <strong>to</strong> keep in mind that many ionic compounds are insoluble. The solubility<br />
of these compounds depends on the relative strength of solvation and<br />
bonding energy.<br />
Some ionic compounds contain a combination of bonds. For instance, in<br />
polya<strong>to</strong>mic ions such as ammonium (NH4 + ), the hydrogens are bonded <strong>to</strong> the<br />
nitrogen by polar covalent bonds. The ionic bond is thus between this covalently<br />
bonded moiety and another ion.<br />
Ionic bonds are typical of inorganic compounds, and thus the mineral or<br />
inorganic components of soil often contain ionic bonds and are soluble in<br />
water. This means two things: (1) the soil solution should always be expected<br />
<strong>to</strong> contain salts and their corresponding ions and (2) the inorganic components<br />
of soil should be expected <strong>to</strong> dissolve in the soil solution, some at a very slow<br />
rate, resulting in their ions being present in low concentrations.<br />
The third aspect of this is that analysis of inorganic or ionic compounds<br />
must take in<strong>to</strong> account not only their solubility in the soil solution but also<br />
the possibility that they may be present as exchangeable ions. Extraction procedures<br />
designed for inorganic components thus need <strong>to</strong> take these two characteristics<br />
in<strong>to</strong> account [7].<br />
2.2.3. Ion Exchange Interactions<br />
The soil colloids, both inorganic (i.e., clay) and organic (i.e., humus), contain<br />
charges that are balanced by cations and anions associated with the charged<br />
sites. Most soil clays and humus contain a predominance of negative charges<br />
and thus act as cation exchangers. Some clays also have significant numbers<br />
of positive charges and will act as anion exchangers. Thus soil can have both<br />
cation exchange capacity (CEC) and anion exchange capacity (AEC).<br />
When considering cation or anion exchange capacity the pH of the soil<br />
solution is extremely important. There will be competition for binding sites<br />
between H 3O + and other cations in the soil solution. In addition, some surface<br />
a<strong>to</strong>ms may become pro<strong>to</strong>nated, thus decreasing the available negative sites on<br />
these surfaces. Therefore, the observed CEC will be less at high pro<strong>to</strong>n concentrations,<br />
that is, at low or acid pH levels, and higher at basic pH levels. Thus<br />
the CEC of the soil at the pH being used for extraction is the important value,<br />
not a CEC determined at a higher or lower pH.<br />
Exchangeable cations must be removed from the exchange sites <strong>to</strong> be<br />
detected and quantified. To accomplish this, the soil sample is extracted with<br />
a solution containing a cation having multiple charges or present at high concentration.<br />
At the same concentration, cations having more positive charges<br />
will replace those on exchange sites having smaller charge. This condition can<br />
be overcome if the less charged cation is in high concentration when even a<br />
cation with one positive charge can replace a cation with multiple charges.