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Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer

Received: 31 May 2026     Accepted: 10 June 2026     Published: 11 August 2026
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Abstract

Bauxite mining in Guinea, particularly in the Boke region, generates significant risks of groundwater contamination by metals and acidification. This paper develops a deterministic coupled groundwater flow and reactive solute transport model applied to the N'Dangara and Boundou Wande bauxite plateaus (CBG concession, Sangaredi, Guinea). The steady-state flow equation and the transient advection-dispersion-reaction equation are discretised using three numerical methods: finite differences (FDM), finite volumes (FVM), and finite elements (FEM). Model parameters are taken from three field campaigns that provided piezometric measurements and physico-chemical analyses. The field data show dispersed flow directions controlled by topography and water table depths between 1.09 m and 17.39 m. Water quality analyses indicate acidic groundwater with pH values as low as 4.84--5.13. Numerical results show that FVM gives the best mass conservation (error < 0.1 \%) and sharpest fronts, FEM is most accurate on irregular geometries, and FDM is fastest but suffers from numerical dispersion. The calibrated model predictions agree well with field observations. This work offers a validated deterministic framework for groundwater risk assessment in Guinean bauxite mining and provides practical guidance for method selection in data-sparse regions.

Published in Mathematics and Computer Science (Volume 11, Issue 4)
DOI 10.11648/j.mcs.20261104.12
Page(s) 71-77
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2026. Published by Science Publishing Group

Keywords

Groundwater Flow, Contaminant Transport, Finite Differences, Finite Volumes, Finite Elements, Bauxite Mining, Guinea, Boke, Acid Mine Drainage

References
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Cite This Article
  • APA Style

    Kamano, M. F., Diallo, M. N., Ndiaye, M., Dinakhaby, A. (2026). Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer. Mathematics and Computer Science, 11(4), 71-77. https://doi.org/10.11648/j.mcs.20261104.12

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    ACS Style

    Kamano, M. F.; Diallo, M. N.; Ndiaye, M.; Dinakhaby, A. Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer. Math. Comput. Sci. 2026, 11(4), 71-77. doi: 10.11648/j.mcs.20261104.12

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    AMA Style

    Kamano MF, Diallo MN, Ndiaye M, Dinakhaby A. Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer. Math Comput Sci. 2026;11(4):71-77. doi: 10.11648/j.mcs.20261104.12

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  • @article{10.11648/j.mcs.20261104.12,
      author = {Michel Faya Kamano and Mouhamadou Nassirou Diallo and Mariama Ndiaye and Aboubakary Dinakhaby},
      title = {Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer},
      journal = {Mathematics and Computer Science},
      volume = {11},
      number = {4},
      pages = {71-77},
      doi = {10.11648/j.mcs.20261104.12},
      url = {https://doi.org/10.11648/j.mcs.20261104.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.mcs.20261104.12},
      abstract = {Bauxite mining in Guinea, particularly in the Boke region, generates significant risks of groundwater contamination by metals and acidification. This paper develops a deterministic coupled groundwater flow and reactive solute transport model applied to the N'Dangara and Boundou Wande bauxite plateaus (CBG concession, Sangaredi, Guinea). The steady-state flow equation and the transient advection-dispersion-reaction equation are discretised using three numerical methods: finite differences (FDM), finite volumes (FVM), and finite elements (FEM). Model parameters are taken from three field campaigns that provided piezometric measurements and physico-chemical analyses. The field data show dispersed flow directions controlled by topography and water table depths between 1.09 m and 17.39 m. Water quality analyses indicate acidic groundwater with pH values as low as 4.84--5.13. Numerical results show that FVM gives the best mass conservation (error < 0.1 \%) and sharpest fronts, FEM is most accurate on irregular geometries, and FDM is fastest but suffers from numerical dispersion. The calibrated model predictions agree well with field observations. This work offers a validated deterministic framework for groundwater risk assessment in Guinean bauxite mining and provides practical guidance for method selection in data-sparse regions.},
     year = {2026}
    }
    

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  • TY  - JOUR
    T1  - Comparing FDM, FVM, and FEM for Coupled Flow-Transport in a Guinean Bauxite Mining Aquifer
    AU  - Michel Faya Kamano
    AU  - Mouhamadou Nassirou Diallo
    AU  - Mariama Ndiaye
    AU  - Aboubakary Dinakhaby
    Y1  - 2026/08/11
    PY  - 2026
    N1  - https://doi.org/10.11648/j.mcs.20261104.12
    DO  - 10.11648/j.mcs.20261104.12
    T2  - Mathematics and Computer Science
    JF  - Mathematics and Computer Science
    JO  - Mathematics and Computer Science
    SP  - 71
    EP  - 77
    PB  - Science Publishing Group
    SN  - 2575-6028
    UR  - https://doi.org/10.11648/j.mcs.20261104.12
    AB  - Bauxite mining in Guinea, particularly in the Boke region, generates significant risks of groundwater contamination by metals and acidification. This paper develops a deterministic coupled groundwater flow and reactive solute transport model applied to the N'Dangara and Boundou Wande bauxite plateaus (CBG concession, Sangaredi, Guinea). The steady-state flow equation and the transient advection-dispersion-reaction equation are discretised using three numerical methods: finite differences (FDM), finite volumes (FVM), and finite elements (FEM). Model parameters are taken from three field campaigns that provided piezometric measurements and physico-chemical analyses. The field data show dispersed flow directions controlled by topography and water table depths between 1.09 m and 17.39 m. Water quality analyses indicate acidic groundwater with pH values as low as 4.84--5.13. Numerical results show that FVM gives the best mass conservation (error < 0.1 \%) and sharpest fronts, FEM is most accurate on irregular geometries, and FDM is fastest but suffers from numerical dispersion. The calibrated model predictions agree well with field observations. This work offers a validated deterministic framework for groundwater risk assessment in Guinean bauxite mining and provides practical guidance for method selection in data-sparse regions.
    VL  - 11
    IS  - 4
    ER  - 

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