Cathodoluminescence imaging on quartz in sandstone

How to study properties of rare-earth doped materials with cathodoluminescence

Posted by Delmic on Feb 20, 2019 3:09:00 PM

Rare-earth elements, also known as REE, are a group of elements, consisting of scandium, yttrium and 15 lanthanide elements. In the last decades there has been a significant growth in the number of devices that use rare-earth metals. They can be found in a wide range of technological areas and are commonly used in lighting and displays, CT scanners and electron microscopes, (fiber) lasers and amplifiers, anti-cancer agents, fluorescent markers, batteries, magnets and catalysists. Rare-earth elements are crucial for modern-day technology and it is important to study rare-earth doped materials at nanoscale to understand them better.

How can optical properties of REE be observed?

Lanthanides series have outer electron shells 5d and 6s, containing 3 electrons, and, most importantly, an outer shell 4f with number of electrons responsible for the optical properties. Most of the transitions that occur in lanthanides ions are called intra-4f transitions, which means that electrons, even being excited, remain their 4f shell, which is shielded by external shells 5s and 5p. Due to that, there is a limited coupling to the outside environment. This means that the transitions are similar in energy regardless of the host material.

In order to perform cathodoluminescence (CL) imaging, rare-earth ions have to be embedded in a crystal host, typically silica, quartz, sapphire, yttrium aluminum garnet, yttrium oxide.

When these materials are excited with electrons, the incoming electrons have enough energy to promote valence electrons from the valence band to the conduction band. Normally, this excitation is supposed to drop back to the valence band. However, if the material is doped with rare-earth ions, the defects inside of the bandgap are created. They draw in the excitation and the resulting emission bears the optical properties of embedded rare-earth elements. This emission then can be observed with various cathodoluminescence techniques, including intensity mapping and hyperspectral imaging.

Microanalysis of REE materials: examples

One of the examples of materials which can be analyzed with cathodoluminescence is YAG:Ce3+, a yttrium aluminum garnet crystal doped with one of the lanthanides species of rare-earth elements (Figure 1). It acts as a very efficient phosphor material and gives a lot of light, which can be observed with CL scan. YAG:Ce3+ is used in LEDs and scintillators and can be studied both in powder and single crystal forms. Cathodolumienscence spectroscopy allows observing particle to particle variations, and also within particles due to high spatial resolution. When this material is studied with cathodoluminescence imaging, it shows a broad spectrum of emission. It means that this crystal can be used to complement a more commonly used in LEDs (In)GaN to produce brighter white light. 

YAG_Cerium-01

Figure 1: Part of the periodic table corresponding to the rare-earth metals. Below a SEM image of YAG:Ce3+ particles is shown together with an RGB CL image which was constructed from three RGB color-filtered CL intensity maps as measured with a PMT. Sample courtesy of Professor Xia.

Both artificial and organic materials, such as geological samples, can contain rare-earth elements that emit light. One of such natural material is zircon, which is commonly studied by geologists because it is robust, chemically inert and can persist for a long time in the earth’s crust. Additionally, zircons are rich in radioactive elements, which makes them so interesting for radiometric isotope dating. Beside those elements, zircons are often rich in lanthanides, which can be observed with CL. Cathodoluminescence imaging allows to see a rich internal structure and features associated with the growth of the crystal. Both hyperspectral and intensity mapping can be used to observe rare-earth elements in zircons. With zircon spectroscopy it is possible to map spectral distribution over large crystal and check differences between bands.

Rare-earth elements can be also used as a stable biocompatible CL emitter to study biological samples. This approach is called correlative cathodoluminescence electron microscopy (CCLEM) [1]. A study made with the use of human lung cells doped with lanthanides nanoparticles demonstrates that introduction of REE allows to observe a robust emission. Additionally, these particles can be introduced in the cell in a non-toxic concentration while the cells are alive. The emission remains stable even when the tissue is stained with osmium.

CCLEM

Figure 2: Cathodoluminescence image of the corresponding area with a pixel size of 20 nm (e) and an overlay image of a bright field-STEM image and the corresponding CL-image, showing co-localization of the particles (f). [1]

These examples show that cathodoluminescence is a fast and powerful technique for microanalysis of REE materials, which can be applied in materials science, optics, geology and life sciences. If you would like to get more details about examples mentioned in this blog post, watch our recent webinar dedicated to rare-earth doped materials:

Rare-earth materials cathodoluminescence webinar

 

References

[1] Tb3+-doped LaF3 nanocrystals for correlative cathodoluminescence electron microscopy imaging with nanometric resolution in focused ion beam-sectioned biological samples. 

Topics: cathodoluminescence, SPARC, cl imaging, cathodoluminescence sem, geological materials, bioimaging