4.5 Article

Raman spectroscopic study of the selenite mineral: ahifeldite, NiSeO3•2H2O

期刊

JOURNAL OF RAMAN SPECTROSCOPY
卷 40, 期 5, 页码 509-512

出版社

WILEY-BLACKWELL
DOI: 10.1002/jrs.2075

关键词

selenite; Raman spectroscopy; ahlfeldite; chalcomenite; clinochalcomenite; cobaltomenite; marthozite; mandarinoite

资金

  1. Queensland University of Technology Inorganic Materials Research Program of the School of Physical and Chemical Sciences
  2. Australian Research Council (ARC)

向作者/读者索取更多资源

Raman spectroscopy has been used to study the selenite mineral ahifeldite. A comparison is made with the Raman spectra of chalcomenite, cobaltomenite and clinochalcomenite. Selenite minerals are characterised by the position of the symmetric stretching mode which is observed at higher wavenumbers than the anti-symmetric stretching mode. The selenite ion has C-3V symmetry and four modes, 2A(1) and 2E. These modes are observed at 813, 472 cm(-1) (A(1)) and 685, 710, 727 and 367 and 396 cm(-1) (E). Bands assigned to the water stretching vibrations are observed for ahifeldite at 3385 cm(-1), for chalcomenite at 2953, 3184 and 3506 cm(-1) and for clinochalcomenite at 2909, 3193 and 3507 cm(-1). A comparison of the Raman spectra of chalcomenite, clinochalcomenite and cobaltomenite is made. The position of these bands enabled hydrogen bond distances in the selenite structure to be estimated. Hydrogen bond distances for ahifeldite, chalcomenite and clinochalcomenite were determined to be similar. Copyright (c) 2008 John Wiley & Sons, Ltd.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据