Modified Diglycolamide Resin: Characterization and Potential Application for Rare Earth Element Recovery

Author:

Romero Junnile L.12ORCID,Tabelin Carlito Baltazar13,Park Ilhwan4ORCID,Alorro Richard D.5ORCID,Zoleta Joshua B.16ORCID,Silva Leaniel C.13,Arima Takahiko4ORCID,Igarashi Toshifumi4,Mhandu Takunda6,Ito Mayumi4,Happel Steffen7,Hiroyoshi Naoki4,Resabal Vannie Joy T.13ORCID

Affiliation:

1. Department of Materials and Resources Engineering and Technology, Mindanao State University—Iligan Institute of Technology, Tibanga, Iligan City 9200, Philippines

2. Helmholtz Zentrum Dresden Rossendorf, Helmholtz Institute Freiberg for Resource Technology, Chemnitzer Strasse 40, 09599 Freiberg, Germany

3. Research Institute of Engineering and Innovative Technology (RIEIT), Mindanao State University—Iligan Institute of Technology, Tibanga, Iligan City 9200, Philippines

4. Division of Sustainable Resources Engineering, Faculty of Engineering, Hokkaido University, Sapporo 060-8629, Japan

5. Western Australia School of Mines, Minerals, Energy and Chemical Engineering, Curtin University, Kent Street, Bentley, WA 6102, Australia

6. Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan

7. International S.A.S., 3 Rue des Champs Géons ZAC de, L’Éperon, 35170 Bruz, France

Abstract

Rare earth elements (REEs) are crucial for green energy applications due to their unique properties, but their extraction poses sustainability challenges because the global supply of REEs is concentrated in a few countries, particularly China, which produces 70% of the world’s REEs. To address this, the study investigated TK221, a modified extraction chromatographic resin featuring diglycolamide (DGA) and carbamoyl methyl phosphine oxide (CMPO), as a promising adsorbent for REE recovery. The elemental composition and functional groups of DGA and CMPO on the polystyrene-divinylbenzene (PS-DVB) support of TK221 were confirmed using scanning electron microscopy with energy dispersive X-ray spectroscopy (SEM-EDX), attenuated total reflectance Fourier transform infrared spectroscopy (ATR-FTIR), and X-ray photoelectron spectroscopy (XPS). The adsorption kinetics of neodymium (Nd), yttrium (Y), cerium (Ce), and erbium (Er) followed the pseudo-second-order kinetic model and Langmuir isotherm, indicating monolayer chemisorption. Furthermore, iron (Fe) adsorption reached apparent equilibrium after 360 min, with consistent Fe adsorption observed at both 360 min and 1440 min. The inclusion of Fe in the study is due to its common presence as an impurity in most REE leachate solutions. The Fe adsorption isotherm results are better fitted with the Langmuir isotherm, implying chemisorption. Maximum adsorption capacities (qmax) of the resin were determined as follows: Nd (45.3 mg/g), Ce (43.1 mg/g), Er (35.1 mg/g), Y (15.6 mg/g), and Fe (12.3 mg/g). ATR-FTIR analysis after adsorption suggested that both C=O and P=O bands shifted from 1679 cm−1 to 1618 cm−1 and 1107 cm−1 to 1142 cm−1 for Y, and from 1679 cm−1 to 1607 cm−1 and 1107 cm−1 to 1135 cm−1 for Ce, implying possible coordination with REEs. These results suggest that TK221 has a huge potential as an alternative adsorbent for REE recovery, thus contributing to sustainable REE supply diversification.

Funder

Department of Science and Technology through the Engineering Research and Development for Technology

Curtin University

Publisher

MDPI AG

Subject

Geology,Geotechnical Engineering and Engineering Geology

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