Compositional Studies of Metals with Complex Order by means of the Optical Floating-Zone Technique

TL;DR

This paper demonstrates the use of the optical floating-zone technique to grow high-quality single crystals with complex compositions and gradients, enabling advanced solid-state research on magnetic and metallurgical properties.

Contribution

It introduces a method for growing complex and gradient single crystals of various metals and compounds using the optical floating-zone technique, expanding experimental possibilities.

Findings

Successfully grew compositional gradient crystals for magnetic studies

Correlated magnetic transition temperatures with sample quality

Produced high-quality crystals of complex diborides

Abstract

The availability of large high-quality single crystals is an important prerequisite for many studies in solid-state research. The optical floating-zone technique is an elegant method to grow such crystals, offering potential to prepare samples that may be hardly accessible with other techniques. As elaborated in this report, examples include single crystals with intentional compositional gradients, deliberate off-stoichiometry, or complex metallurgy. For the cubic chiral magnets Mn$_{1-x}$Fe$_{x}$Si and Fe$_{1-x}$Co$_{x}$Si, we prepared single crystals in which the composition was varied during growth from $x = 0 - 0.15$ and from $x = 0.1 - 0.3$, respectively. Such samples allowed us to efficiently study the evolution of the magnetic properties as a function of composition, as demonstrated by means of neutron scattering. For the archetypical chiral magnet MnSi and the itinerant antiferromagnet CrB$_{2}$, we grew single crystals with varying initial manganese (0.99 to 1.04) and boron (1.95 to 2.1) content. Measurements of the low-temperature properties addressed the correlation between magnetic transition temperature and sample quality. Furthermore, we prepared single crystals of the diborides ErB$_{2}$, MnB$_{2}$, and VB$_{2}$. In addition to high vapor pressures, these materials suffer from peritectic formation, potential decomposition, and high melting temperature, respectively.