Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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in Cooperation with on an Cooperation-Score of 37%

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  • 2023Towards remote sensing of Rare Earth Element resources – first steps: spectroscopy of synthetic REE mineralscitations

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Deon, Fiorenza
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Van Ruitenbeek, Frank
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Dijkstra, Arjan
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2023

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  • Deon, Fiorenza
  • Van Ruitenbeek, Frank
  • Dijkstra, Arjan
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document

Towards remote sensing of Rare Earth Element resources – first steps: spectroscopy of synthetic REE minerals

  • Bakker, Wim Harry
  • Deon, Fiorenza
  • Van Ruitenbeek, Frank
  • Dijkstra, Arjan
Abstract

Rare Earth Elements (REE) are essential for low-carbon energy solutions for the Energy Transition. Hyperspectral satellite- or UAV-based remote sensing of REE-resources, and proximal hyperspectral imagingspectroscopy (e.g., drill core imaging), such as drill core imaging, have a high potential as tools to support exploration, because of the unique spectral properties of the REE. However, to date, high-quality reflectance spectra of REE-minerals with controlled compositions are lacking.<br/><br/>To address this research gap, we synthesized a series of single-, dual- and mixed-REE minerals. These include hydrated phosphates (rhabdophane) and anhydrous phosphates (, monazite and , xenotime). We also synthesized La-Nd solid solution monazites to constrain the effect of Nd concentrations on the spectral properties, and calcite-monazite mixtures to simulate REE-bearing rocks. Recently we also succeeded in synthesizing single-REE carbonates (hydroxylbastnäsite). We also prepared calcite-monazite mixtures to simulate REE-bearing rocks. PProducts were confirmed by X-ray powder diffraction and structural refinement, and reflectance spectra in the wavelength range 350-2500 nm were measured.<br/><br/>The strong intensities of the absorption features found hold promise for REE-exploration by hyperspectral remote sensing. Moreover, the data confirm that most REE’s have a distinct spectral signature – including in the shortwave IR part of the spectrum. These signatures are largely independent of the host mineral, (because the 4f-electrons involved are relatively shielded). This contrasts with most other minerals, in which the excitation energies of electronic transitions in ions are strongly affected by the surrounding crystal field. This means that in the case of REE there exists a unique potential to detect chemical elements, or maybe even concentrations, rather than mineral (groups) by proximal and remote sensing techniques. There are, however, subtle spectral differences between minerals, e.g., monazite-(Nd) v. bastnäsite-(Nd), which can be resolved in imaging spectroscopy applications.

Topics
  • mineral
  • Carbon
  • spectroscopy
  • rare earth metal