Reinterpretation of an EPR experiment on Cu<sup>2+</sup> with regard to the structure of rhombohedral Zn-Cl boracite

Rivera, Jean-Pierre; Bill, Hans; Lacroix, Roger

doi:10.1080/00150197808237220

Scientific article

English

Reinterpretation of an EPR experiment on Cu²⁺ with regard to the structure of rhombohedral Zn-Cl boracite

ContributorsRivera, Jean-Pierre; Bill, Hans; Lacroix, Roger

Published inFerroelectrics, vol. 20, no. 1, p. 225-227

Publication date1978

Abstract

EPR of Cu²⁺ in Zn—Cl boracite has already been studied by several authors. Two models were proposed for the structure of rhombohedral phase of the boracite. The obtained EPR results demonstrate that one of the models is suitable to explain this phase of Zn—Cl boracite.

Affiliation entities

Faculté des sciences / Section de chimie et biochimie / Département de chimie physique

Research groups

Groupe Bill

Citation (ISO format)

RIVERA, Jean-Pierre, BILL, Hans, LACROIX, Roger. Reinterpretation of an EPR experiment on Cu²⁺ with regard to the structure of rhombohedral Zn-Cl boracite. In: Ferroelectrics, 1978, vol. 20, n° 1, p. 225–227. doi: 10.1080/00150197808237220

Article (Published version)

Identifiers

PID : unige:3134
DOI : 10.1080/00150197808237220

Journal ISSN0015-0193

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Reinterpretation of an EPR experiment on Cu2+ with regard to the structure of rhombohedral Zn-Cl boracite

EPR of Cu2+ in Zn—Cl boracite has already been studied by several authors. Two models were proposed for the structure of rhombohedral phase of the boracite. The obtained EPR results demonstrate that one of the models is suitable to explain this phase of Zn—Cl boracite.

Technical informations

Reinterpretation of an EPR experiment on Cu²⁺ with regard to the structure of rhombohedral Zn-Cl boracite

EPR of Cu²⁺ in Zn—Cl boracite has already been studied by several authors. Two models were proposed for the structure of rhombohedral phase of the boracite. The obtained EPR results demonstrate that one of the models is suitable to explain this phase of Zn—Cl boracite.