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High performance capillary electrophoresis - T.E.A.M.

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Principles<br />

Figure 19<br />

Electrodispersion due to mismatched<br />

sample and buffer conductivities<br />

2.3.4.5 Electrodispersion<br />

Differences in sample zone and running buffer conductivities<br />

can have three major effects: 1) skewed peak shapes;<br />

2) solute concentration or focusing (low conductivity<br />

sample), or solute defocusing (high conductivity sample);<br />

3) temporary isotachophoretic states due to excess of a<br />

certain ion (for example, Cl - ).<br />

As described by the Kohlrausch regulating function, when<br />

the solute zone has a higher mobility than the running<br />

buffer, the leading edge of the solute zone will be diffuse<br />

and the trailing edge sharp. Conversely, when the solute<br />

zone has a lower mobility than the running buffer, the leading<br />

edge will be sharp and the trailing edge diffuse. When<br />

the conductivities are equivalent, no such peak distortions<br />

will occur. Schematics of each case are shown in figure 19.<br />

a) b) c)<br />

Low<br />

conductivity<br />

<strong>High</strong><br />

conductivity<br />

Low<br />

conductivity<br />

Equivalent<br />

<strong>High</strong><br />

conductivity<br />

Low<br />

conductivity<br />

<strong>High</strong><br />

conductivity<br />

Sample zone Sample zone Sample zone<br />

E<br />

40

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