THE VARIANCE AND THE QUANTITY 2DT IN CAPILLARY ZONE ELECTROPHORESIS

Authors
Citation
R. Virtanen, THE VARIANCE AND THE QUANTITY 2DT IN CAPILLARY ZONE ELECTROPHORESIS, Electrophoresis, 14(12), 1993, pp. 1266-1270
Citations number
10
Categorie Soggetti
Biochemical Research Methods
Journal title
ISSN journal
01730835
Volume
14
Issue
12
Year of publication
1993
Pages
1266 - 1270
Database
ISI
SICI code
0173-0835(1993)14:12<1266:TVATQ2>2.0.ZU;2-F
Abstract
The variance is generally used as a measure of dispersion of zones in capillary zone electrophoresis (CZE). It is a quantitative measure of the separation power of a system and different causes of dispersion ca n be rated by their partial variances, which can be summed up to total variance. However, the additivity is only valid for independent dispe rsion sources, a fact that often seems to be ignored. The ubiquitous d ispersion source diffusion is taken into consideration by the Einstein term 2Dt. Other sources of dispersion are, e.g., injection, detection , thermal gradients, adsorption, and hydrodynamic flow. For each of th ese sources various variance expressions have been derived. The origin of the term 2Dt and its relation to the variance is explained and the calculation of variance in general is discussed. The equivalence of t he diffusion variance and the term 2Dt is verified with some simple in itial forms of sample zone and the additivity of variances in ideal zo ne electrophoresis is demonstrated. The change of conductivity in zone s results in asymmetrical zone forms which is an indication of nonidea lity of a system. It is shown that in such cases the term 2Dt is no lo nger valid and its use as an additive variance component leads to an e rroneous total variance. Because in zone electrophoresis conductivity in a zone always changes more or less, the additivity of variances is never perfectly valid. However, in many cases the nonideality may be s o small that the additivity in practice is still applicable. A general ly valid way to calculate theroretically the total variance of a zone is to derive a functional representation of the distribution and then calculate the variance from it. This is possible only in the simplest cases. Usually the distribution must be calculated by numerical method s.