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Published on: February 21, 2017
Microbially formed Mn(IV) oxide as a novel adsorbent for removal of Radium
Kazuya Tanaka1, Keiko Yamaji2, Hayato Masuya3
1Advanced Science Research Center, Japan Atomic Energy Agency, 2-4 Shirakata, Tokai, Ibaraki, 319-1195, Japan; Ningyo-toge Environmental Engineering Center, Japan Atomic Energy Agency, Kagamino, Tomata, Okayama, 708-0698, Japan.
Microbially formed manganese(IV) oxide effectively removes radioactive radium (Ra) from contaminated water. This biogenic manganese oxide (BMO) shows high efficiency in treating mine water, offering a promising solution for radium removal in water treatment.
Area of Science:
- Environmental Science
- Geochemistry
- Microbiology
Background:
- Radioactivity of radium (Ra) isotopes in natural waters poses environmental risks.
- Controlling radium-226 (²²⁶Ra) concentrations in uranium mill tailings ponds is crucial for waste management.
Purpose of the Study:
- To evaluate microbially formed manganese(IV) oxide (BMO) as an adsorbent for radium removal from water.
- To assess the efficiency of BMO in treating radium-contaminated mine water.
Main Methods:
- Biogenic manganese(IV) oxide (BMO) was synthesized using the fungus Coprinopsis urticicola.
- Adsorption experiments using strontium (Sr) and barium (Ba) as radium surrogates were conducted.
- Extended X-ray absorption fine structure (EXAFS) analysis was used to determine adsorption mechanisms.
Main Results:
- Distribution coefficients for Ba and Sr onto BMO were high (∼10⁶.⁵ and ∼10⁴.³, respectively).
- EXAFS analysis confirmed inner-sphere complex adsorption of Ba and Sr onto BMO.
- A small amount of BMO (7.6 mg) removed over 98% of ²²⁶Ra from 3 L of mine water, yielding a distribution coefficient of 10⁷.⁴ mL/g.
Conclusions:
- Biogenic manganese(IV) oxide is highly effective for radium removal in water treatment.
- The high distribution coefficient indicates practical applicability for BMO in managing radium-contaminated water.
- Manganese(IV) oxide plays a significant role as a carrier and host phase for radium in natural environments.

