CF4/C2F6 Gases Emissions During Rare Earth Electrolysis

Rare earth elements (REE) have become vital in our daily life because they are used as a key component in a variety of the advanced technology applications [1]. Large scale REE exploitation is a waste-generating process that causes serious environmental problems and forces industrialised countries to turn to alternative resources for RE, such as recycling of the elements from end-of-life (EOL) products [1]. Fluoride-based molten salts are widely used in the RE molten salt electrolysis (MSE) because of their distinct advantages such as continuous production and short process flow [2]. However, this electrolyte media is associated with the consumption of anode, and emission of greenhouse gases (GHGs), CO/CO2 and perfluorocarbon gases (PFCs), mainly CF4 and C2F6. Our work in this area has led to the development of a new process for the recovery of REE from EOL magnets. Pyrometallurgical treatment of spent NdFeB magnets was used to produce the magnet recycling derived oxides (MRDO), a REE containing product. The subsequent fluoride-based MSE of the produced MRDO was carried out to recover REE from EOL magnets [2,3]. Continuous monitoring of PFC emissions by in-situ FTIR-spectrometry during the RE recovery from NdFeB EOL magnets by MSE was the main objective of this study. The RE electrolysis from fluoride-based molten salts composed of NdF3+PrF3+LiF with MRDO was carried out using molybdenum (Mo) as a cathode, tungsten (W) as a reference electrode, and a glassy carbon (GC) electrode as an anode. The FTIR results show that the anode gas products were composed mainly of CO and CO2, while CF4 has been detected before the full anode effect and C2F6 at and after this phenomenon. The anode reactions in the fluoride-based melts after the dissolution of RE oxides are most likely the result of the oxide or fluoride complexes formed in the electrolyte, on whose very formation the subsequent reactions at the GC anode depend. The generated oxygen reacts with GC to produce CO and CO2. Upon fluoride salt dissolution produced F− ions, can also react with GC anode and generate PFC compounds such as CF4 and C2F6. The content of CF4 during constant potentiostatic electrolysis was on average 0.3 ppm except for spikes that were detected periodically, and then the highest concentration was around 1 ppm, while C2F6 was not detected.

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RWTH Publications (RWTH Aachen)
Published
2025-01-01
Primary Topic
Geochemistry and Geologic Mapping
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article

CF4/C2F6 Gases Emissions During Rare Earth Electrolysis

RWTH Publications (RWTH Aachen)
Geochemistry and Geologic Mapping
article

CF4/C2F6 Gases Emissions During Rare Earth Electrolysis

article en

Abstract

Rare earth elements (REE) have become vital in our daily life because they are used as a key component in a variety of the advanced technology applications [1]. Large scale REE exploitation is a waste-generating process that causes serious environmental problems and forces industrialised countries to turn to alternative resources for RE, such as recycling of the elements from end-of-life (EOL) products [1]. Fluoride-based molten salts are widely used in the RE molten salt electrolysis (MSE) because of their distinct advantages such as continuous production and short process flow [2]. However, this electrolyte media is associated with the consumption of anode, and emission of greenhouse gases (GHGs), CO/CO2 and perfluorocarbon gases (PFCs), mainly CF4 and C2F6. Our work in this area has led to the development of a new process for the recovery of REE from EOL magnets. Pyrometallurgical treatment of spent NdFeB magnets was used to produce the magnet recycling derived oxides (MRDO), a REE containing product. The subsequent fluoride-based MSE of the produced MRDO was carried out to recover REE from EOL magnets [2,3]. Continuous monitoring of PFC emissions by in-situ FTIR-spectrometry during the RE recovery from NdFeB EOL magnets by MSE was the main objective of this study. The RE electrolysis from fluoride-based molten salts composed of NdF3+PrF3+LiF with MRDO was carried out using molybdenum (Mo) as a cathode, tungsten (W) as a reference electrode, and a glassy carbon (GC) electrode as an anode. The FTIR results show that the anode gas products were composed mainly of CO and CO2, while CF4 has been detected before the full anode effect and C2F6 at and after this phenomenon. The anode reactions in the fluoride-based melts after the dissolution of RE oxides are most likely the result of the oxide or fluoride complexes formed in the electrolyte, on whose very formation the subsequent reactions at the GC anode depend. The generated oxygen reacts with GC to produce CO and CO2. Upon fluoride salt dissolution produced F− ions, can also react with GC anode and generate PFC compounds such as CF4 and C2F6. The content of CF4 during constant potentiostatic electrolysis was on average 0.3 ppm except for spikes that were detected periodically, and then the highest concentration was around 1 ppm, while C2F6 was not detected.

RWTH Publications (RWTH Aachen)
Openalex Percentile: Top 68%
Geochemistry and Geologic Mapping
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