Modeling of formation and prevention of a pure water zone in capillary isoelectric focusing with narrow pH range carrier ampholytes

• Published in: Electrophoresis Vol. 38; no. 5; pp. 677 - 688
• Main Authors: Takácsi‐Nagy, Anna, Kilár, Ferenc, Thormann, Wolfgang
• Format: Journal Article
• Language: English
• Published: Germany Wiley Subscription Services, Inc 01-03-2017
• Subjects: Ampholyte Mixtures - chemistry; Amphoterics; Anodes; Atmospheric models; Carbon dioxide; Carbonic acid; Carbonic Acid - chemistry; Carrier ampholytes; Carriers; Catholytes; Computer Simulation; Electrophoresis, Capillary - methods; Formations; Hydrogen-Ion Concentration; Isoelectric focusing; Isoelectric Focusing - methods; Mathematical models; Migration; Modelling; Narrow pH gradient; Neutrality; Simulation; Water - chemistry; Water zone; Water zone; Carrier ampholytes; Isoelectric focusing; Simulation; Carbonic acid; Narrow pH gradient
• ISSN: 0173-0835; 1522-2683
• DOI: 10.1002/elps.201600314

This paper comprises a continuation of computer simulation studies dealing with carrier ampholyte based CIEF in presence of narrow pH gradients. With this technique, amphoteric sample components with pI values outside the pH gradient are migrating isotachophoretically toward the cathode or anode whereas components with pI values within the gradient become focused. In order to understand the processes occurring in presence of the electric field, the behavior of both carrier ampholytes and amphoteric sample components is investigated by computer modeling. Characteristics of two pH unit gradients with end components having pI values at or around 7.00 and conditions that lead to the formation of a water zone at neutrality were investigated. Data obtained reveal that a zone of water is formed in focusing with carrier ampholytes when the applied pH range does not cover the neutral region, ends at pH 7.00 or begins at pH 7.00. The presence of additional amphoteric components that cover the neutrality region prevent water zone formation under current flow. This situation is met in experiments with narrow pH gradients that end or begin around neutrality. Simulation data reveal that no water zone evolves when atmospheric carbon dioxide dissolved in the catholyte causes the migration of carbonic acid (in the form of carbonate and/or hydrogen carbonate ions) from the catholyte through the focusing structure. An electrolyte change in the electrode solution does not have an impact on the focusing part but does change the isotachophoretic pattern migrating behind the leading ion.