Abstract

The diverse properties of rare earth elements have seen broad and growing applications in clean energy technologies, hybrid vehicles, pollution control, optics, refrigeration, and so on. This study presents a “cradle-to-gate” life cycle assessment of the energy use, resource depletion, and global warming potential resulting from the production of rare earth elements (REEs) using the Bayan Obo rare earth operation in Inner Mongolia, China, as a representative system. The study aggregates data from the literature, LCI databases, and reasonable estimations. A novel economic value-based allocation method for the multiple coproducts of the process is proposed. It is found that four of the high priced REEs scandium, europium, terbium, and dysprosium have very high GWPs from production relative to the rest. A mass-based allocation is also provided for comparison. Impacts on immediate local environment from waste streams that can be toxic are not included in this study.

Highlights

  • Rare earth elements (REEs) or RE metals are technically defined as the 15 elements in the lanthanide (La) series, yttrium (Y), and scandium (Sc)

  • Contrary to a lay persons’ understanding, REs are not rare in natural occurrence, though REEs have much less tendency to become concentrated in exploitable ore deposits [2], in particular Heavy rare earth elements (HREEs)

  • The principal goal of this study is to investigate the cradle-togate energy use, water use, and global warming impact of REEs produced in Bayan Obo, China

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Summary

Introduction

Rare earth elements (REEs) or RE metals are technically defined as the 15 elements in the lanthanide (La) series, yttrium (Y), and scandium (Sc). Y and Sc are considered REEs since they mostly occur in the same ore deposits and have similar chemical properties. (i) Light rare earth elements (LREEs): lanthanum (La), cerium (Ce), praseodymium (Pr), neodymium (Nd), and promethium (Pm). (ii) Medium rare earth elements (MREEs): samarium (Sm), europium (Eu), and gadolinium (Gd). (iii) Heavy rare earth elements (HREEs): terbium (Tb), dysprosium (Dy), holmium (Ho), erbium (Er), thulium (Tm), ytterbium (Yb), lutetium (Lu), scandium (Sc), and yttrium (Y). There are about 200 known rare-earth containing mineral deposits, mostly as carbonatites spread around the world. Bastnasite deposits in China and the United States constitute the largest percentage of the world’s rare-earth economic resources [3]

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