VOLUME 19 (Supplement)

SciEnggJ%202026%20Special%20Issue%20265 280 Bautista%20et%20al

SciEnggJ 19 (Supplement) 323-333
available online: 16 October 2026
DOI: https://doi.org/10.54645/202619SupFZF-36

*Corresponding authorr
Email Address: einstineopiso@cmu.edu.ph
Date received: 30 May 2026
Date revised: 21 August 2026
Date accepted: 19 September 2026

ARTICLE

Immobilization of arsenate and fluoride from alkaline industrial wastes via induced hydrotalcite and brucite formation: Implications for the solidification of radioactive waste

Einstine M. Opiso*1, Sheila Mae P. Bulado2, Ma. Catherine Q. Arca1, Liu Xiaoji3, and Tsutomu Sato4

1Civil Engineering Department, College of Engineering, Central Mindanao University, Musuan, Maramag, Bukidnon, 8710 Philippines

2Physics Department, College of Arts and Sciences, Central Mindanao University, Musuan, Maramag, Bukidnon, 8710 Philippines

3CECEP (Feixi) WTE CO., LTD., Hefei 231241, China

4Graduate School of Engineering, Faculty of Engineering, Hokkaido University, Sapporo, 060-0808 Japan

KEYWORDS: Arsenate, Brucite, Coal fly ash, Fluoride, Granulated blast furnace slag, Hydrotalcite, Radionuclide sequestration, Solidification/Stabilization

Coal fly ash and granulated blast furnace slag (GBFS) can potentially be utilized as highly effective binders for the solidification and stabilization of radioactive waste. This study investigated a novel immobilization strategy by inducing the formation of magnesium-bearing minerals, specifically hydrotalcite and brucite, through the addition of magnesium oxide (MgO) and magnesium nitrate [Mg (NO3)2]. Mineralogical transformations were monitored over two weeks with varying Mg-source ratios (10%–30%). Results showed that MgO addition successfully induced stable hydrotalcite and brucite phases, significantly enhancing fluoride removal in GBFS from 53% to over 97%. In contrast, Mg nitrate led to pH reduction and the formation of less stable hydrocalumite. Selective dissolution and leaching tests confirmed that anions co-precipitated with hydrotalcite remained sequestered at pH as low as 5.6, whereas calcium-bearing minerals dissolved at pH 9, releasing sorbed anions. These findings demonstrate that controlling pore-water chemistry through slightly soluble MgO provides a possible long-term sequestration mechanism for arsenate and fluoride as analogues of highly mobile radioactive oxyanions, highlighting the potential of industrial by-product-based binders for radioactive waste solidification applications.

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