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Frans_M_Everaerts_Isotachophoresis_378342.pdf

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Fig.6.31. Isotachopherograms for the separation of some anions that lack W absorbance. (a)<br />

Creatinine, for which the molaf absorptivity of creatinine is function of the pH. Leading electrolyte<br />

= HCl(O.01 M, pro analysi grade) t creatinine (purified); pH = 4.5. Terminating electrolyte =<br />

morpholinoethanesulphonic acid (MES) (re-crystallized three times). (b) Counter ion for which the<br />

change in pH of a zone does not influence the molar absorptivity (p-alanine). Leading electrolyte<br />

= HCl (0.01 M, pro analysi grade) t e-aminocaproic acid (purified); pH = 4.5. Terminating<br />

electrolyte = MES (re-crystallized three times). Non-W-absorbing ions can thus be detected by the<br />

‘indirect UV method‘. A = Increasing UV absorption; R = increasing electric resistance; t = time. The<br />

current was stabilised in both instances at 30pA. The chart paper speed was 2 cm/min. An injection<br />

was made of 1 pl of the sample 0.01 Mchlorate t 0.01 Macetate + 0.01 M formate + 0.01 M<br />

glutamate. Peaks: 1 = chloride; 2 = chlorate; 3 = formate; 4 = acetate; 5 = glutamate; 6 = MES. In (a)<br />

the lower pH of the glutamate zone with respect to the zone preceding it and following it is clearly<br />

visible. From this isotachopherogram, the pH can easily be checked as it can be calculated with the<br />

computer program discussed in Chapter 4. The difference in the step height as found in the linear<br />

conductivity trace, due to the difference in the counter ion, should be noted. The conductimeter<br />

used is discussed elsewhere (Fig.6.18); the measuring electrodes were mounted equiplanar. Various<br />

impurities commonly present in the chemicals can be observed in the traces from both the UV and<br />

conductivity detectors.<br />

167

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