THERMAL ACTIVATION OF TEBINBULAK TITANOMAGNETITE ORE AS A LOW-COST MAGNETIC SORBENT PRECURSOR: TEMPERATURE–TIME DEPENDENCE OF SPECIFIC SURFACE AREA, CRYSTALLITE GROWTH AND PHASE STABILITY

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Authors
  • Ergashev Muhsinjon Ergashevich UZ

    Department of Agronomy, Navoi State University of Mining and Technologies, Navoi, Uzbekistan
  • Shodiqulov Jurabek Mehriqulovich UZ

    Department of Agronomy, Navoi State University of Mining and Technologies, Navoi, Uzbekistan
  • Doniyorov Kamoliddin Alouddinovich UZ

    Department of Agronomy, Navoi State University of Mining and Technologies, Navoi, Uzbekistan
Keywords:
titanomagnetite thermal activation BET surface area grain growth magnetite oxidation empirical model magnetic sorbent Tebinbulak
Abstract
Natural titanomagnetite can serve as a precursor of magnetically recoverable iron-oxide sorbents, provided that its low initial surface area (≈4–7 m² g⁻¹) is developed without destroying the magnetite phase. Here the thermal activation of titanomagnetite ore from the Tebinbulak deposit (Karakalpakstan, Uzbekistan) was mapped over a full 6 × 5 factorial grid of temperature (500–1000 °C) and holding time (0.5–2.5 h), and the response of BET surface area, crystallite size, external surface and pore volume was described with empirical models. Surface area obeyed SBET = −83.1 + 15.8 ln T + 3.60 ln t (R² = 0.976), with first-order time saturation (τ = 0.31–0.45 h) and a limiting value S∞ that grows from 17.2 to 27.8 m² g⁻¹ between 500 and 1000 °C. Crystallite size followed a power law d ∝ T1.31 t0.12 (R² = 0.992), i.e. coarsening is governed by temperature far more than by time. The surface gained per nanometre of crystallite growth (ΔS/Δd) dropped eightfold, from 0.42 to 0.05 m² g⁻¹ nm⁻¹, across the 500–1000 °C range, with the steepest fall above 700 °C, where the maghemite-to-hematite transformation of magnetite is known to accelerate. Combining these trends, 700 °C for 2.0 h is identified as the upper practical limit of activation: it provides 84 % of the thermally attainable surface (23.67 m² g⁻¹, external 18.80 m² g⁻¹, pore volume 0.120 cm³ g⁻¹) at a crystallite size of 64.86 nm, with the product still predominantly in the spinel phase. The models provide design equations for a sorbent intended for removing Mo, Se, U, As and V oxyanions from saline drainage water.
References

[1] M. Qadir, B. R. Sharma, A. Bruggeman, R. Choukr-Allah, and F. Karajeh, “Non-conventional water resources and opportunities for water augmentation to achieve food security in water scarce countries,” Agricultural Water Management, vol. 87, pp. 2–22, 2007, doi: 10.1016/j.agwat.2006.03.018.

[2] P. Micklin, “The Aral Sea disaster,” Annual Review of Earth and Planetary Sciences, vol. 35, pp. 47–72, 2007, doi: 10.1146/annurev.earth.35.031306.140120.

[3] R. Kulmatov, J. Mirzaev, J. Abuduwaili, and B. Karimov, “Challenges for the sustainable use of water and land resources under a changing climate and increasing salinization in the Jizzakh irrigation zone of Uzbekistan,” Journal of Arid Land, vol. 12, pp. 90–103, 2020, doi: 10.1007/s40333-020-0092-8.

[4] R. S. Ayers and D. W. Westcot, Water Quality for Agriculture, FAO Irrigation and Drainage Paper 29, Rev. 1. Rome, Italy: FAO, 1985.

[5] R. Tornqvist, J. Jarsjo, and B. Karimov, “Health risks from large-scale water pollution: Trends in Central Asia,” Environment International, vol. 37, pp. 435–442, 2011, doi: 10.1016/j.envint.2010.11.006.

[6] K. K. Tanji and N. C. Kielen, Agricultural Drainage Water Management in Arid and Semi-Arid Areas, FAO Irrigation and Drainage Paper 61. Rome, Italy: FAO, 2002.

[7] C. A. Hejase, K. A. Weitzel, S. C. Stokes, et al., “Opportunities for treatment and reuse of agricultural drainage in the United States,” ACS ES&T Engineering, vol. 2, pp. 292–305, 2022, doi: 10.1021/acsestengg.1c00277.

[8] B. A. Manning, S. E. Fendorf, and S. Goldberg, “Surface structures and stability of arsenic(III) on goethite: Spectroscopic evidence for inner-sphere complexes,” Environmental Science & Technology, vol. 32, pp. 2383–2388, 1998, doi: 10.1021/es9802201.

[9] S. Goldberg and C. T. Johnston, “Mechanisms of arsenic adsorption on amorphous oxides evaluated using macroscopic measurements, vibrational spectroscopy, and surface complexation modeling,” Journal of Colloid and Interface Science, vol. 234, pp. 204–216, 2001, doi: 10.1006/jcis.2000.7295.

[10] D. Peak and D. L. Sparks, “Mechanisms of selenate adsorption on iron oxides and hydroxides,” Environmental Science & Technology, vol. 36, pp. 1460–1466, 2002, doi: 10.1021/es0156643.

[11] J. P. Gustafsson, “Modelling molybdate and tungstate adsorption to ferrihydrite,” Chemical Geology, vol. 200, pp. 105–115, 2003, doi: 10.1016/S0009-2541(03)00161-X.

[12] T. B. Scott, G. C. Allen, P. J. Heard, and M. G. Randell, “Reduction of U(VI) to U(IV) on the surface of magnetite,” Geochimica et Cosmochimica Acta, vol. 69, pp. 5639–5646, 2005, doi: 10.1016/j.gca.2005.07.003.

[13] D. E. Latta, C. A. Gorski, M. I. Boyanov, E. J. O’Loughlin, K. M. Kemner, and M. M. Scherer, “Influence of magnetite stoichiometry on U(VI) reduction,” Environmental Science & Technology, vol. 46, pp. 778–786, 2012, doi: 10.1021/es2024912.

[14] A. C. Scheinost and L. Charlet, “Selenite reduction by mackinawite, magnetite and siderite: XAS characterization of nanosized redox products,” Environmental Science & Technology, vol. 42, pp. 1984–1989, 2008, doi: 10.1021/es071573f.

[15] C. A. Gorski and M. M. Scherer, “Influence of magnetite stoichiometry on Fe(II) uptake and nitrobenzene reduction,” Environmental Science & Technology, vol. 43, pp. 3675–3680, 2009, doi: 10.1021/es803613a.

[16] C. T. Yavuz, J. T. Mayo, W. W. Yu, et al., “Low-field magnetic separation of monodisperse Fe₃O₄ nanocrystals,” Science, vol. 314, pp. 964–967, 2006, doi: 10.1126/science.1131475.

[17] R. D. Ambashta and M. Sillanpää, “Water purification using magnetic assistance: A review,” Journal of Hazardous Materials, vol. 180, pp. 38–49, 2010, doi: 10.1016/j.jhazmat.2010.04.105.

[18] J. T. Mayo, C. Yavuz, S. Yean, et al., “The effect of nanocrystalline magnetite size on arsenic removal,” Science and Technology of Advanced Materials, vol. 8, pp. 71–75, 2007, doi: 10.1016/j.stam.2006.10.005.

[19] S. Goldberg, H. S. Forster, and C. L. Godfrey, “Molybdenum adsorption on oxides, clay minerals, and soils,” Soil Science Society of America Journal, vol. 60, pp. 425–432, 1996, doi: 10.2136/sssaj1996.03615995006000020013x.

[20] J.-H. Huang, F. Huang, L. Evans, and S. Glasauer, “Vanadium: Global (bio)geochemistry,” Chemical Geology, vol. 417, pp. 68–89, 2015, doi: 10.1016/j.chemgeo.2015.09.019.

How to Cite

Ergashevich, E. M., Mehriqulovich, S. J., & Alouddinovich , D. K. (2026). THERMAL ACTIVATION OF TEBINBULAK TITANOMAGNETITE ORE AS A LOW-COST MAGNETIC SORBENT PRECURSOR: TEMPERATURE–TIME DEPENDENCE OF SPECIFIC SURFACE AREA, CRYSTALLITE GROWTH AND PHASE STABILITY. Innovative: International Multidisciplinary Journal of Applied Technology (2995-486X), 4(10), 203-212. https://doi.org/10.51699/gdxn4e26