Research Papers by Christian Larchet

It is found that the DBL near an ionexchange membrane is formed quasi-instantly under natural convection and follows the variation in solution concentration drop through the DBL (Dc): d ~ (Dc)–0.2. The fact that the value of power differs from the value predicted by Levich (–0.25) is explained by th

It is found that under certain conditions (a dilute solution, a relatively small inter-membrane distance, and a significant forced convection), the contribution of the gravitational convection in the ion transfer is negligible. Considerable electroconvective mixing of the depleted solution starts at