Finding Structural Phase Transitions in Barlowite and Claringbullite
POSTER
Abstract
Barlowite (Cu4(OH)6FBr) and claringbullite (Cu4(OH)6FCl) are minerals related to the quantum spin liquid candidate herbertsmithite ZnCu3(OH)6Cl2, the popular S = ½ antiferromagnet with a geometrically perfect kagome lattice. The kagome lattices of claringbullite and barlowite are stacked perfectly on top of one another, separated by planes consisting of Cu2+ and halide ions, and show promise as QSL candidates. Both materials have a hexagonal crystal structure with P63/mmc symmetry and undergo temperature-dependent phase transitions to Pnma symmetry1. Previously we examined the barlowite transitions at 276 K1, but the claringbullite transition occurs much lower. To pinpoint the transition, equipment had to be modeled and aligned.
Chem. Commun., 2019,55,11587-11590
Chem. Commun., 2019,55,11587-11590
*We thank Dr. S. Winter for helpful discussions. APS Sector 15 is supported by the NSF Divisions of Chemistry and Materials Research under NSF/CHE-1346572. Use of the APS was supported under Contract No. DE-AC02-06CH11357. J.A.S. acknowledges support from the Independent Research/Development program while serving at the NSF. The NHMFL was supported by the NSF under DMR-1644779 and the State of Florida. A.H., L.D., and T.S. acknowledge funding from the NSF under DMR-1534818. H.I.R. thanks to the NHMFL for the internship.
Presenters
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Hannah Revell
- National High Magnetic Field Laboratory