Exploring rare earth elements in coalmine overburden: nanoscale insights from FESEM, TEM and XPS analysis
Binud Attry1,2, K S V Subramanyam3, Virendra M Tiwari1,2
1CSIR-North East Institute of Science & Technology Jorhat 785006 Assam India bksaikia@neist.res.in bksaikia@gmail.com.
RSC Advances
|June 9, 2025
Summary
Coal mine waste, known as overburden (OB), is a newly identified potential source for rare earth elements and yttrium (REY). This study explored Makum coalfield in India, revealing significant REY concentrations in OB and coal, suggesting future recovery possibilities.
Area of Science:
- Geochemistry
- Economic Geology
- Materials Science
Background:
- Rare earth elements and yttrium (REY) are critical for advanced technologies and economic growth.
- Coal and its by-products are potential sources of REY, but coal mine overburden (OB) remains largely unexplored.
- The Makum coalfield in India's Northeastern Region (NER) is examined for REY potential.
Purpose of the Study:
- To investigate the existence, distribution, and depositional conditions of REY in coal and coal mine OB.
- To analyze the geochemical behavior and potential commercial viability of REY in the study area.
- To assess the suitability of OB as a future source for REY recovery.
Main Methods:
- Analysis of REY content in coal and OB samples from the Makum coalfield.
- Utilizing advanced analytical techniques including nanoscale morphology, Field Emission Scanning Electron Microscopy (FE-SEM), and High-Resolution Transmission Electron Microscopy (HR-TEM).
- Evaluation of geochemical indicators such as light (LREY) to heavy (HREY) ratio, and anomalies of Europium (δEu), Cerium (δCe), and Gadolinium (δGd).
Main Results:
- Coal and coal mine OB samples from the Makum coalfield are identified as promising sources of REY.
- The average REY concentration is 167.66 mg kg-1, with a mean LREY to HREY ratio of 37.67.
- Significant Europium (δEu = 3.20), Cerium (δCe = 0.71), and Gadolinium (δGd = 5.30) anomalies were observed, indicating specific depositional conditions.
Conclusions:
- The coal-forming conditions (slightly oxidizing, highly reducing, M-type enrichment) are favorable for REY preservation.
- The absence of anaerobic microbial activity aided in preserving organic matter and REY.
- Coal mine OB and coal deposits in the Makum coalfield represent a viable opportunity for future REY exploration and recovery.


