Skip to content
DraconiticResearch
Search Sources API
203,234 studies31 sourcesUpdated 53 min ago
Peer-reviewedCC BY 4.0Mathematics

Mathematical Modeling of the Influence of Non-Uniform Electrical Conductivity of an Ion-Exchange Membrane on Salt Ion Transport in a Desalination Channel with Forced Convection

  1. 1Faculty of Architecture and Civil Engineering, RheinMain University of Applied Sciences and Arts, 65197 Wiesbaden, Germany
  2. 2Faculty of Computer Technologies and Applied Mathematics, Kuban State University, 350040 Krasnodar, Russia

Abstract

In this work, the influence of the electrical heterogeneity of the surface of an ion-exchange membrane on salt ion transport in a desalination channel with forced convection in the potentiodynamic mode is studied for the first time by the successful combined application of various mathematical methods: mathematical modeling based on a boundary value problem for the coupled system of the Navier–Stokes, Nernst–Planck, and Poisson equations; the finite element method for its numerical solution; an approximate analytical solution of the Stokes equations constructed by the method of images, in which the flow at the junction of the conducting and non-conducting regions is described as a flow induced by a point torque (rotlet); and a first-order relaxation model describing the growth of the vortex size. Since such problems have not been considered before, a new mathematical apparatus for their solution has been developed. It is established that the presence of electrical heterogeneity on the membrane surface leads to the formation of a heteroelectroconvective vortex at the conducting/non-conducting boundary, which arises as a result of space-charge accumulation at the junction point and the emergence of a significant non-potential electric force that swirls the fluid. It is shown that the radius of the heteroelectroconvective vortex is empirically described by exponential saturation toward an asymptotic value over the sampled interval of 190–290 s, that its stabilization occurs before the appearance of ordinary electroconvective vortices, and that it is described quite accurately by the first-order relaxation model. With a further increase in the potential drop and the development of ordinary electroconvection, cyclic destruction and restoration of the heteroelectroconvective vortex occur. The influence of the non-conducting island length on vortex dynamics and desalination is examined; among the six lengths considered, 0.05 mm gives the highest computed degree of desalination (42.044%). Direct comparisons of longitudinal velocity give NMAE values of 2.50%, 14.73%, and 1.63% at three representative cross-sections, with the largest discrepancy near the vortex center.

Related

  1. Subdivision-based collocation methods for time fractional convection diffusion reaction equation with environmental and biomedical applications
    Saima Bibi, Syeda Tehmina Ejaz
    Scientific ReportsPeer-reviewedCC BY-NC-ND 4.0Full textGeneral mathematicsCrossref
  2. 1D Convection-Diffusion in Porous Media: A Unified Solution from Bounded Domain to Half-Space
    Koffi Ognandon Ayena, Amah Séna D'almeida
    arXivPreprintarXiv licenceFull textAnalysis & PDEsarXiv
  3. On the optimal decay rate of global solutions to the convection-diffusion equation with zero-mass initial data
    Yi C. Huang, Ryunosuke Kusaba
    arXivPreprintarXiv licenceFull textAnalysis & PDEsarXiv
  4. A stabilized scheme satisfying the discrete maximum principle for a time fractional convection-diffusion-reaction equation
    Christos Pervolianakis
    arXivPreprintCC BY-NC-ND 4.0Full textNumerical analysis & scientific computingarXiv
  5. Leak localisation with a measure source convection-diffusion model
    Thi Tam Dang, Tuomo Valkonen
    arXivPreprintarXiv licenceFull textAnalysis & PDEsOptimisation & controlarXiv
BibTeX
@article{kirillova2026mathematical,
  title = {{Mathematical Modeling of the Influence of Non-Uniform Electrical Conductivity of an Ion-Exchange Membrane on Salt Ion Transport in a Desalination Channel with Forced Convection}},
  author = {Evgenia Kirillova and Anastasia Tarasova and Anna Kovalenko and Makhamet Urtenov},
  journal = {Mathematics},
  year = {2026},
  month = nov,
  doi = {10.3390/math14213984},
  url = {https://www.mdpi.com/2227-7390/14/21/3984},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Mathematical Modeling of the Influence of Non-Uniform Electrical Conductivity of an Ion-Exchange Membrane on Salt Ion Transport in a Desalination Channel with Forced Convection
AU  - Evgenia Kirillova
AU  - Anastasia Tarasova
AU  - Anna Kovalenko
AU  - Makhamet Urtenov
PY  - 2026
DA  - 2026/11/01
JO  - Mathematics
DO  - 10.3390/math14213984
UR  - https://www.mdpi.com/2227-7390/14/21/3984
AB  - In this work, the influence of the electrical heterogeneity of the surface of an ion-exchange membrane on salt ion transport in a desalination channel with forced convection in the potentiodynamic mode is studied for the first time by the successful combined application of various mathematical methods: mathematical modeling based on a boundary value problem for the coupled system of the Navier–Stokes, Nernst–Planck, and Poisson equations; the finite element method for its numerical solution; an approximate analytical solution of the Stokes equations constructed by the method of images, in which the flow at the junction of the conducting and non-conducting regions is described as a flow induced by a point torque (rotlet); and a first-order relaxation model describing the growth of the vortex size. Since such problems have not been considered before, a new mathematical apparatus for their solution has been developed. It is established that the presence of electrical heterogeneity on the membrane surface leads to the formation of a heteroelectroconvective vortex at the conducting/non-conducting boundary, which arises as a result of space-charge accumulation at the junction point and the emergence of a significant non-potential electric force that swirls the fluid. It is shown that the radius of the heteroelectroconvective vortex is empirically described by exponential saturation toward an asymptotic value over the sampled interval of 190–290 s, that its stabilization occurs before the appearance of ordinary electroconvective vortices, and that it is described quite accurately by the first-order relaxation model. With a further increase in the potential drop and the development of ordinary electroconvection, cyclic destruction and restoration of the heteroelectroconvective vortex occur. The influence of the non-conducting island length on vortex dynamics and desalination is examined; among the six lengths considered, 0.05 mm gives the highest computed degree of desalination (42.044%). Direct comparisons of longitudinal velocity give NMAE values of 2.50%, 14.73%, and 1.63% at three representative cross-sections, with the largest discrepancy near the vortex center.
SN  - 2227-7390
ER  -