Research led by the Universities of St Andrews and Brighton reveals newly discovered sources for rare earth metals vital in modern technologies such as renewables production, mobile phones, laptops and televisions.
The research, published in Nature Communications (1 September 2020) investigated alternative sources of much sought after heavy rare earth metals used in every day modern technologies, focussing on subtropical soils in Northern Madagascar.
Modern technologies, such as those producing green energy from renewable resources like wind and water, require many tonnes of rare, so-called e-tech metals. Mining of e-tech metals can be costly, environmentally challenging and energy intensive. This is particularly true for metals sourced from rocks formed in ancient mountain belts or volcanoes, which must be excavated, crushed and then processed to separate valuable metals from the rest.
Sometimes nature lends a helping hand by breaking down naturally hard-to-crack minerals to form softer materials from which valuable commodities can be extracted more efficiently and sustainably.
The research, led by the School of Earth and Environmental Sciences at the University of St Andrews with colleagues at the University of Brighton, focussed on tracing a specific group of metals known as the rare earth elements. These include metals such as neodymium, praseodymium and dysprosium which are crucial components in technologies ranging from phones, computers, military or medical appliances to wind turbines and electric vehicles.
The demand for rare earth metals is set to grow exponentially over the next few decades, as ambitious clean energy projects, such as the European Union’s Green Deal, are being developed globally. However, most economies still find themselves relying heavily on imports from China.
At present, China produces roughly 77% of the world’s supply of rare earth elements. The rarest rare earths, particularly those used in permanent magnets, are primarily sourced from ion adsorption clay deposits, or laterites, formed by tropical weathering of rocks such as granite and syenite in Southern China.
Using an intense x-ray source, called a ‘synchrotron’, the team of researchers reveal at the atomic scale where the rare earths are in the soil. The team found that the rare earths are loosely stuck to the surfaces of clay particles. By comparing samples from a weathered volcanic complex in Madagascar to those mined in China, the study provides key insights into how nature produces easily-leachable, economically viable, rare earth deposits.
Lead author of the study Dr Anouk Borst, from the University of St Andrews, said: “Some have wondered whether the Southern Chinese adsorption deposits are unique, but our study confirms that the Chinese soils are identical to deposits found in Madagascar, and that they formed in similar ways. The race is now on to find other deposits elsewhere in the world.” This information will be an impetus to global exploration for critical metal resources outside China.
The paper Adsorption of rare earth elements in regolith-hosted clay deposits by A M Borst, M Smith, A A Finch, G Estrade, E Marquis, C Villanova-de-Benavent, N J Horsburgh, K Goodenough, P Nason, J Kynicky, C Xu and T Geraki, is published in Nature Communications (2020) and is available online.
Please ensure that the paper’s DOI (doi.org/10.1038/s41467-020-17801-5) is included in all online stories and social media posts, and that Nature Communications is credited as the source.
Raw data for the study is available online under DOI doi.org/10.17630/73e556f7-0fc3-4814-b25c-fa747ceb72a2
Photo 1: one of the field sites in northern Madagascar. Thick clay deposits have formed above rocks formed in an old volcano by the name of Ambohimirahavavy. The volcano was active around 24 million years ago and has since eroded to expose its interior. The rocks closest to the surface weathered to form a clay deposit in which the original minerals were broken down to release their rare metals, which then stuck to the clay minerals. © Kathryn Goodenough and Martin Smith
Photo 2: co-authors Dr Guillaume Estrade, Dr Eva Marquis and Dr Kathryn Goodenough (University of Toulouse, University of Brighton, the British Geological Survey, respectively) taking samples from soil profiles and the volcanic rocks underneath. The soils are of economic interest for their enrichment in rare earth elements. © Guillaume Estrade, Eva Marquis and Kathryn Goodenough
Photo 3: Diamond Light Source at the Harwell Science and Innovation Campus, Didcot, UK. The researchers analysed samples from Madagascar and China at Diamond Light Source in Oxfordshire, the UK’s only national synchrotron facility. A synchrotron light source is like an enormous microscope made up of a large storage ring – over half a kilometre long – in which electrons are accelerated to create an intense beam of x-rays, infrared or ultraviolet light. This powerful energy beam enables scientists to study a wide range of materials too small to see with the naked eye and is roughly 10.000 times more powerful than a traditional microscope.
The study was part of the NERC and EPSRC-funded SOSRARE consortium, a UK-based collaborative project between the Universities of St Andrews, Brighton, Leeds, Sheffield and Exeter (Camborne School of Mines), the British Geological Survey and various international industry and research partners, and was supported by Diamond Synchrotron X-ray facility grants SP14793 and SP15903. The aim of the project was to develop new insights into the natural processes by which rare earth elements are concentrated to extractable levels, and to develop environmentally friendly and economically viable ways to source them.