Spectroscopic and voltammetric characteristics of α-Zn2SiO4:V luminophor


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

Single-phase luminophor Zn2SiO4:V with willemite structure is prepared by hydrothermal method. It is found that the Zn: Si: V ratio between cations is 2: 0.9: 0.1. It is shown that the inclusion of vanadium in the willemite structure reduces the width of the bandgap by ΔEg ≈ 2 eV. Using a combination of spectroscopic and voltammetric techniques, it is found the zinc silicate matrix contains vanadium ions with charge states V5+, V4+, and V3+. In addition, magnetic ions form clusters.

About the authors

T. I. Krasnenko

Institute of Solid State Chemistry, Ural Branch

Author for correspondence.
Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

M. Yu. Yanchenko

Institute of Solid State Chemistry, Ural Branch; Ural State Mining University

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990; Yekaterinburg

N. A. Zaitseva

Institute of Solid State Chemistry, Ural Branch; Ural State Mining University

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990; Yekaterinburg

E. V. Zabolotskaya

Institute of Solid State Chemistry, Ural Branch

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

I. V. Baklanova

Institute of Solid State Chemistry, Ural Branch

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

L. Yu. Buldakova

Institute of Solid State Chemistry, Ural Branch

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

T. A. Onufrieva

Institute of Solid State Chemistry, Ural Branch

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

R. F. Samigullina

Institute of Solid State Chemistry, Ural Branch

Email: krasnenko@ihim.uran.ru
Russian Federation, Yekaterinburg, 620990

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2017 Pleiades Publishing, Ltd.