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The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments

Received: 12 November 2018    Accepted: 27 November 2018    Published: 14 January 2019
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Abstract

This study was aimed at evaluating the effect of mass transfer resistance to the transport of phenol in soil sediments. Batch adsorption experiments were conducted using phenol in homogenous soil sediments (clay and sand). The Physico-chemical properties of the soil sediments were determined and sorption behaviour kinetically modelled using the Pseudo-first order, Pseudo-second order, Intra-particle, Elovich, and Power function models. The sorption behaviour was best modelled with the intra-particle model (R2 ˃ 0.9628). The rate limiting step and mass transfer resistance were determined by the Boyd plot, Homogenous pore diffusion model (HPDM) and the modified Furusawa -Smith equation. The Boyd plots indicated external mass transfer as the rate-determining step for the phenol/clay and phenol/sand systems; the HPDM model gave a poor fit (R2 ≈ 0.6) for the phenol sorbate systems, corresponding with projections from the Boyd plots. From the results of the study, the rate controlling step for phenol sorption in the sediments was predominantly due to external mass transfer resistance. A comparative analysis between the two sediments using the Furusawa -Smith equation gave the mass transfer coefficients for clay and sand to be 2.09205E-14 m s−1 and 4.17537E-12 m s−1 respectively, showing that as the particle size decreased, the more significant the effect of external mass transfer effect on the sorption rate.

Published in American Journal of Environmental Science and Engineering (Volume 2, Issue 4)
DOI 10.11648/j.ajese.20180204.12
Page(s) 56-64
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), 2024. Published by Science Publishing Group

Keywords

Contaminants, Adsorption, Sediment, Adsorbate, Adsorbent, Resistance

References
[1] Owabor, C. N., Agarry, S. E., Ayodele, B. V., Udeh, S. I., and Ehiosun, E. (2013). Comparative Study of the Adsorption and Desorption Behavior of Single and Multi-Ring Aromatics in Sediment Fractions. Advances in Chemical Engineering and Science, 3, 67-73.
[2] Wang, Y. J., Chen, J. H., Cui, Y. X., Wang, S. Q., and Zhou, D. M. (2009). Effects of low-molecular weight organic acids on Cu(II) adsorption onto hydroxyapatite nanoparticles. J Hazard Mater, 162: 1135–1140.
[3] Kookana, R. (2010). The Role of Biochar in Modifying the Environmental Fate, Bioavailability and Efficacy of Pesticides in Soils: A Review. Soil Research, 48 (7), 627-637.
[4] Gebremariam, S. (2011). Mineralization, Sorption and De- sorption of Chlorpyrifos in Aquatic Sediments and Soils, Ph.D. Thesis. Pullman: Washington State University.
[5] Owabor, C., Ogbeide, S., and Susu, A. (2010b). Adsorption and Desorption Kinetics of Naphthalene, Anthracene and Pyrene in Soil Matrix. Petroleum Science and Technology, 28 (5), 504-514.
[6] Ding, L. (2010). Mechanisms Of Competitive Adsorption Between Trace Organic Contaminants And Natural Organic Matter On Activated Carbon,. Ph.D Dissertation Submitted To The University Of Illinois.
[7] Girish, C., and Ramachandra, V. M. (2016). Mass Transfer Studies on Adsorption of Phenol from Wastewater Using Lantana camara, Forest Waste;. International Journal of Chemical Engineering, 6 (2), 11.
[8] Kapur M Mondal M K, (2013) Mass transfer and related phenomena for Cr(VI) adsorption from aqueous solutions onto Mangifera indica sawdust,” Chemical Engineering Journal, vol. 218, pp. 138–146
[9] Osagie, E. I. and Owabor, C. N. (2015) Adsorption of Naphthalene on Clay and Sandy Soil from Aqueous Solution. Advances in Chemical Engineering and Science, 5, 345-351
[10] Ghogomu J. N, Dieudonné, Estella N. Tamungang N B, Ajifack D. L., Ndi J. N, Ketcha M J (2014) Adsorption of phenol from aqueous solutions onto natural and thermallymodified kaolinitic materials Int. J. Biol. Chem. Sci. 8 (5): 2325-2338
[11] Ayanda, O., Fatoki, S., Adekola, F., and Ximba, B. (2013). Kinetics and equilibrium models of the adsorption of tributyltin to nZnO, activated carbon and nZnO/activated carbon composite in artificial seawater. Mar Pollut Bull, 1016, 10.
[12] Vermeulen, T. (1953). Theory for irreversible and constant-pattern solid diffusion. Industrial Eng. Chem, 45, 1664–1670.
[13] Valderrama, C., Gamisans, X., de las Heras, X., and Farr´an b, A. (2008). Sorption kinetics of polycyclic aromatic hydrocarbons removal using granular activated carbon: Intraparticle diffusion coefficient. Journal of Hazardous Materials, 158, 386-396.
[14] Vadivelan, V., and Vasanth Kumar, K. (2005). Equilibrium, kinetics, mechanism, and process design for the sorption of methylene blue onto rice husk. J Colloid Interface Sci, 286, 90–100.
[15] Djebbar M, Djafri. F, Bouchekara M. and Djafri A. (2012) Adsorption of phenol on natural clay African Journal of Pure and Applied Chemistry Vol. 6 (2), pp. 15-25,
[16] Ahmad, M., Puad, N., and Bello, O. (2014). Kinetic, equilibrium and thermodynamic studies of synthetic dye removal using pomegranate peel activated carbon prepared by microwave-induced KOH activation. Water Res Ind, 10 (4), 234-345.
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[18] Nethaji, S., Sivasamy, A., and Mandal, A. B. (2013). Adsorption isotherms, kinetics and mechanism for the adsorptionof cationic and anionic dyes onto carbonaceous particles prepared from Juglans regia shell biomass. International Journal for Environmental Science Technology, 10, 231-242.
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    Eugene Ehidiamhen Yakubu, Chiedu Owabor. (2019). The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments. American Journal of Environmental Science and Engineering, 2(4), 56-64. https://doi.org/10.11648/j.ajese.20180204.12

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    ACS Style

    Eugene Ehidiamhen Yakubu; Chiedu Owabor. The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments. Am. J. Environ. Sci. Eng. 2019, 2(4), 56-64. doi: 10.11648/j.ajese.20180204.12

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    AMA Style

    Eugene Ehidiamhen Yakubu, Chiedu Owabor. The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments. Am J Environ Sci Eng. 2019;2(4):56-64. doi: 10.11648/j.ajese.20180204.12

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  • @article{10.11648/j.ajese.20180204.12,
      author = {Eugene Ehidiamhen Yakubu and Chiedu Owabor},
      title = {The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments},
      journal = {American Journal of Environmental Science and Engineering},
      volume = {2},
      number = {4},
      pages = {56-64},
      doi = {10.11648/j.ajese.20180204.12},
      url = {https://doi.org/10.11648/j.ajese.20180204.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajese.20180204.12},
      abstract = {This study was aimed at evaluating the effect of mass transfer resistance to the transport of phenol in soil sediments. Batch adsorption experiments were conducted using phenol in homogenous soil sediments (clay and sand). The Physico-chemical properties of the soil sediments were determined and sorption behaviour kinetically modelled using the Pseudo-first order, Pseudo-second order, Intra-particle, Elovich, and Power function models. The sorption behaviour was best modelled with the intra-particle model (R2 ˃ 0.9628). The rate limiting step and mass transfer resistance were determined by the Boyd plot, Homogenous pore diffusion model (HPDM) and the modified Furusawa -Smith equation. The Boyd plots indicated external mass transfer as the rate-determining step for the phenol/clay and phenol/sand systems; the HPDM model gave a poor fit (R2 ≈ 0.6) for the phenol sorbate systems, corresponding with projections from the Boyd plots. From the results of the study, the rate controlling step for phenol sorption in the sediments was predominantly due to external mass transfer resistance. A comparative analysis between the two sediments using the Furusawa -Smith equation gave the mass transfer coefficients for clay and sand to be 2.09205E-14 m s−1 and 4.17537E-12 m s−1 respectively, showing that as the particle size decreased, the more significant the effect of external mass transfer effect on the sorption rate.},
     year = {2019}
    }
    

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  • TY  - JOUR
    T1  - The Effect of Mass Transfer Resistance on the Adsorption Rate of Phenol in Soil Sediments
    AU  - Eugene Ehidiamhen Yakubu
    AU  - Chiedu Owabor
    Y1  - 2019/01/14
    PY  - 2019
    N1  - https://doi.org/10.11648/j.ajese.20180204.12
    DO  - 10.11648/j.ajese.20180204.12
    T2  - American Journal of Environmental Science and Engineering
    JF  - American Journal of Environmental Science and Engineering
    JO  - American Journal of Environmental Science and Engineering
    SP  - 56
    EP  - 64
    PB  - Science Publishing Group
    SN  - 2578-7993
    UR  - https://doi.org/10.11648/j.ajese.20180204.12
    AB  - This study was aimed at evaluating the effect of mass transfer resistance to the transport of phenol in soil sediments. Batch adsorption experiments were conducted using phenol in homogenous soil sediments (clay and sand). The Physico-chemical properties of the soil sediments were determined and sorption behaviour kinetically modelled using the Pseudo-first order, Pseudo-second order, Intra-particle, Elovich, and Power function models. The sorption behaviour was best modelled with the intra-particle model (R2 ˃ 0.9628). The rate limiting step and mass transfer resistance were determined by the Boyd plot, Homogenous pore diffusion model (HPDM) and the modified Furusawa -Smith equation. The Boyd plots indicated external mass transfer as the rate-determining step for the phenol/clay and phenol/sand systems; the HPDM model gave a poor fit (R2 ≈ 0.6) for the phenol sorbate systems, corresponding with projections from the Boyd plots. From the results of the study, the rate controlling step for phenol sorption in the sediments was predominantly due to external mass transfer resistance. A comparative analysis between the two sediments using the Furusawa -Smith equation gave the mass transfer coefficients for clay and sand to be 2.09205E-14 m s−1 and 4.17537E-12 m s−1 respectively, showing that as the particle size decreased, the more significant the effect of external mass transfer effect on the sorption rate.
    VL  - 2
    IS  - 4
    ER  - 

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Author Information
  • Department of Chemical Engineering, University of Benin, Benin City, Nigeria

  • Department of Chemical Engineering, Federal University of Petroleum Resources Effurun, Effurun, Nigeria

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