Journal
JOURNAL OF SOLID STATE CHEMISTRY
Volume 184, Issue 12, Pages 3319-3323Publisher
ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jssc.2011.10.015
Keywords
CdCu3(OH)(6)Cl-2; Herbertsmithite; Kapellasite; Pseudopolyatomic; Kagome; Paratacamite
Funding
- NSF [DMR 0819762]
- DOE [DE-FG02-04ER46134]
- Division Of Materials Research
- Direct For Mathematical & Physical Scien [819762] Funding Source: National Science Foundation
Ask authors/readers for more resources
A new transition metal hydroxide chloride containing kagome layers of magnetic ions, CdCu3(OH)(6)Cl-2, has been synthesized and structurally characterized. The actual low symmetry P2(1)/n structure can be derived from the ideal trigonal one with a change in cation distribution and coherent distortions of the anion framework. The result is a fundamentally different Cu2+ kagome framework than found in the related Herbertsmithite and Kapellasite minerals. Magnetization measurements show no transition to long range magnetic order above T=2 K, despite strong antiferromagnetic interactions with a Weiss temperature of theta(w)= -150 K. Furthermore, we show that the structure of CdCu3(OH)(6)Cl-2 and related hydroxide chlorides can be rationalized on the basis of [(OH)(3)Cl](4-) pseudopolyatomic anions that pack and rotate, in much the same way as do traditional polyatomic anions. This opens the door to rational design of new and useful hydroxide chloride materials. (C) 2011 Elsevier Inc. All rights reserved.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available