Abstract

Rare earth-bearing gypsum tailings from the fertilizer industry are a potential source for an economically viable and sustainable production of rare earth elements. Large quantities are generated inter alia in Catalão, Brazil, as a by-product in a fertilizer production plant. Hitherto, the gypsum has been used as soil conditioner in agriculture or was dumped. The cooperative project, “Catalão Monazite: Economical exploitation of rare earth elements from monazite-bearing secondary raw materials,” intends to extract rare earth elements from these gypsum tailings. In this paper, a chemical process route to obtain a mixed rare earth carbonate from a monazite concentrate, was investigated. The results of the digestion, leaching, and precipitation experiments are presented and discussed herein. This includes reagent choice, process parameter optimization through experimental design, mineralogical characterization of the feed material and residues, purification of the leach solution, and precipitation of the rare earth as carbonates. The results showed that a rare earth extraction of about 90% without the mobilization of key impurities is possible during a sulfuric acid digestion with two heating stages and subsequent leaching with water. In the following purification step, the remaining impurities were precipitated with ammonium solution and the rare earth elements were successfully recovered as carbonates with a mixture of ammonium solution and ammonium bicarbonate.

Highlights

  • The rare earth elements (REEs) are a group of elements with similar properties

  • The results of this section showed that a high REE yield up to 95% could be achieved at low temperatures

  • The immobilization of thorium is possible at higher temperatures but leads to REE losses of around 10%

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Summary

Introduction

The rare earth elements (REEs) are a group of elements with similar properties. They include scandium (atomic number 21), yttrium (atomic number 39), and the lanthanides (atomic numbers57–71) [1]. High growth rates are observed for the elements neodymium and dysprosium due to their application in neodymium-iron-boron-magnets, which are used inter alia in electromobility and wind turbines [3]. Despite their name, REEs are relatively abundant in the Earth’s crust, but economically minable concentrations are less common than for most other ores. Either igneous or sedimentary phosphate rock is used as raw material in fertilizer plants. The fertilizer plant in Catalão uses the less common apatite-containing igneous phosphate rock [9]. A precipitate of calcium sulfate, phosphogypsum, is formed as by-product according to Equation (1) [6].

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