Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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surface features 35<br />
Because different components are held <strong>to</strong> soil components by different<br />
types of bonding and attractions, the interaction can be relatively strong or<br />
weak. Thus extraction procedures must be capable of extracting the desired<br />
component when it is held by different forms of bonding <strong>to</strong> different<br />
components.<br />
2.2.7. Other Ways of Investigating Bonding<br />
Bonding and other interactions between the components in soil (i.e., the clays)<br />
and organic components can be investigated by conducting adsorption experiments.<br />
An organic molecule is added <strong>to</strong> a suspension of clay and the amount<br />
adsorbed after a fixed amount of time is determined. The amount adsorbed is<br />
plotted against the amount added <strong>to</strong> produce adsorption isotherms. The shape<br />
of the graph is then used <strong>to</strong> indicate the type of interaction between the molecule<br />
and the clay. With this type of investigation, various types of adsorption<br />
phenomona can be distinguished.<br />
Two of the most common ways of handling such data is <strong>to</strong> try <strong>to</strong> fit the data<br />
<strong>to</strong> either a Langmuir or a Freundlich type of equation, or alternatively <strong>to</strong><br />
simply determine which of these two equations best describes the data<br />
obtained. Although some useful information can be obtained about the interactions<br />
between the components being studied, neither provides specific information<br />
about the type of bonding in terms of orbitals, or interactions such as<br />
those discussed in the previous sections. Spectroscopy, as discussed in Chapter<br />
7, is typically the method used <strong>to</strong> determine bonding details [11,12].<br />
SOIL COMPONENTS IN COMBINATION<br />
2.3. SURFACE FEATURES<br />
Both sand and silt surfaces are dominated by oxygen and its lone pairs of electrons<br />
in p orbitals. In some instances broken surfaces may also have siliconhybridized<br />
sp 3 orbitals 4 available for bonding. Comparison of sand, silt, and<br />
clay reveals the surface area of sand and silt <strong>to</strong> be low and the interaction<br />
between surface bonding orbitals and components in the surrounding medium<br />
relatively weak.<br />
As a first approximation, the surfaces of the clays can be grouped in<strong>to</strong> three<br />
types: (1) surfaces consisting exclusively of oxygens with their lone pairs or<br />
electrons, in p orbitals, extending at an angle away from the surface in<strong>to</strong> the<br />
surrounding medium; (2) surfaces containing —OH groups with the partially<br />
positive hydrogens extending in<strong>to</strong> the surrounding medium—because of the<br />
4 This would be a hybridized orbital formed by the hybridization of one s and three p orbitals as<br />
opposed <strong>to</strong> 2s,2p hybridization in carbon.