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Frans_M_Everaerts_Isotachophoresis_378342.pdf

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PROCEDURE OF COMPUTATION<br />

A.3. PROCEDURE OF COMPUTATION<br />

For a separation boundary between the zones U- 1 and U, eqn. A1 gives<br />

u- 1 U<br />

~u-i * 2 (mA,+mB)cA,,U-i =E,* C (mAr+mB)cAr,U (A71<br />

r= 1 r=l<br />

Combining eqns. A7 and A6 gives<br />

JI<br />

In fact, this is a modification of the ‘Dole polynomals’ [ 1,8] and solutions for the<br />

equations are valid if<br />

If the composition of the leading electrolyte and the sample solution are known, all<br />

parameters can be computed with the equations given above. The velocity of the concen-<br />

tration boundaries can be neglected.<br />

In the first instance, the concentrations of the ionic species in the last sample zone<br />

are taken to be equal to the original concentrations in the sample. Although this assump-<br />

tion is not correct, the ratio between the concentrations in the sample remains constant<br />

in the zones, according to eqn. A2, which gives<br />

(It is assumed that the velocity of the concentration boundary can be neglected.)<br />

Using eqns. AS and A9, flu-] ,u can be calculated if all mobilities are known. With<br />

flu- ,u and eqn. A6, all concentrations of the zone U- 1 can be calculated, and thus all<br />

concentrations and values can be calculated for all zones.<br />

The concentration of the ionic species in the first sample zone can be calculated in<br />

two ways, either with the equations given above or using the isotachophoretic condition<br />

as described in Chapter 4. In the first computation, we chose arbitrarily as concentrations<br />

for the ionic species in the last sample zone those concentrations present in the original<br />

sample solution, and all quantities could be obtained. If the parameters of the first zone<br />

obtained in this way did not agree with those obtained by the isotachophoretic method,<br />

we re-computed from the first to the last zone with the quantities obtained with the<br />

isotachophoretic condition, using the 0 values from the moving-boundary procedure. By<br />

this calculation, new concentrations for the sample zones can be proposed and new<br />

/3 values can be calculated. This procedure of ‘iteration’ must be repeated until the<br />

P values and concentrations fit.<br />

389

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