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Frans_M_Everaerts_Isotachophoresis_378342.pdf

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ISOTACHOPHORESIS 13<br />

2.4. PRINCIPLE OF iSOTACHOPHORESIS<br />

2.4.1. Introduction<br />

We shall consider here the separation of anionic species in narrow-bore tubes. For<br />

the separation of anionic species, the narrow-bore tube and anode compartment are<br />

filled with the so-called leading electrolyte, the anions of which must have a mobility<br />

that is higher than that of any of the sample anionic species. The cations of the leading<br />

electrolyte must have a buffering capacity at the pH at which the analyses will be<br />

performed. The cathode compartment is filled with the terminating electrolyte, the<br />

anions of whch must have a mobility that is lower than that of any of the sample<br />

anionic species. The sample is introduced between the leading and terminating<br />

electrolyte, e.g., by means of a sample tap or a micro-syringe.<br />

#en an electric current is passed through such a system (see Fig.2.5a), a uniform<br />

electric field strength over the sample zone occurs and hence each sample anionic species<br />

will have a different migration velocity according to eqn. 2.1. The sample anionic species<br />

with the highest effective mobility will run forwards and those with lower mobilities will<br />

remain behind. Hence, both in front of and behind the original sample zone, the moving-<br />

boundary procedure results in two series of mixed zones (comparable with the Tiselius<br />

method). In the series of mixed zones, the sample anionic species are arranged in order<br />

of their decreasing effective mobilities (see Fig.2.5b),<br />

The anionic species of the leading electrolyte can never be passed by sample anions,<br />

because its effective mobility is chosen so as to be higher. Similarly, the terminating<br />

anions can never pass the anionic species of the sample. In this way, the sample zones<br />

are sandwiched between the leading and terminating electrolyte. In the mixed zones of<br />

the sample (see Fig.2.5b), the separation continues and, after some time, when the<br />

separation is complete, a series of zones is obtained in which each zone contains only one<br />

anionic species of the sample if no anionic species with identical effective mobilities are<br />

present in the sample. Of course, this series of zones is still sandwiched between leading<br />

and terminating electrolyte (see Fig.2.5~).<br />

The first sample zone contains the anionic species of the sample with the highest<br />

effective mobility, the last zone that with the lowest effective mobility. After this stage,<br />

no further changes to the system occur and a steady state has been reached. In such a<br />

case, we can speak of an isotachophoretic separated system. (Of course, one or more<br />

unmixable ‘mixed zones’, i.e., zones that contain one or more anionic species with<br />

identical effective mobilities, may still be present.) In this state, all of the zones must run<br />

connected together, in contrast to zone electrophoresis, where all zones release. Here the<br />

zones cannot release as there is no background electrolyte that can support the electric<br />

current (a requirement for the solvent is that its self-conductance must be negligible; see<br />

section 5.2 .)* .<br />

*If it is assumed that the zones release, then the concentration of the ionic species at that position will<br />

decrease, the electric field strength will increase (working at a constant current density) and hence the<br />

migration velocity of the ionic species involved will be higher. Therefore, finally these ionic species will<br />

reach the preceding zone.

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