J. Phys. IV France 126 (2005) 17-21DOI: 10.1051/jp4:2005126004
Growing of SixGe
O
single crystals with
-quartz structure and their characterization
V.S. Balitsky1, D.V. Balitsky2, A.N. Nekrasov1 and L.V. Balitskaya1 1
Institute of Experimental Mineralogy RAS, Russia
2
Montpellier University II, France
Abstract
Crystals of
-Si
Ge
O2 solid
solution is a new material with relatively high piezoelectric coefficients
and temperature stability. Theoretical and experimental study on the
development of reliable and reproducible method of
-Si
Ge
O2 crystal growth under hydrothermal conditions will be proposed
in the report. Influence of the composition of solutions, T-P parameters,
growth rates of different faces, capture and distribution of Si and Ge on
morphology and internal structure of the crystals, and the basic
crystallochemical characteristics and properties of the crystals have been
investigated.
The most important result of the performed investigations is an experimental
proof of the growth of

-Si

Ge

O
2 single crystals
with

-quartz structure under conditions of the stable existence of
trigonal quartz and tetragonal germanium oxide phases. The maximum GeO
2
content (38,78 mass%) has been attained while crystal growth in aqueous
solutions of ammonium fluoride at temperature of 700

C and pressure of
the order of 180MPa. Crystals grown in alkaline solutions at similar T-P
parameters are characterized by the maximum GeO
2 content of 25
mass%. A temperature of the

polymorphous transition of

-Si

Ge

O
2 with GeO
2 content of 38 mass%
has reached 840

C (instead 573

C of

-quartz).
GeO
2 portion increases in

-Si

Ge

O
2
crystals at temperature and growth rates rise. The highest GeO
2 content
belongs to the growth sectors of positive and negative rhombohedra; the
minimum - belongs to the growth sectors of hexagonal prism. A regular rise
of the unit cell parameters and refraction indices are observed at GeO
2
portion increase in

-Si

Ge

O
2 crystals. An
appearance of new absorption bands was found in IR-spectra, caused by a
formation of Si-O-Ge bridge bonds. A shifting of practically all bands in
the IR-spectra of the combinational scattering for a distance of 10-15 cm

into the region of short-wave vibrations seems to be related to this
very fact. The basic piezoelectric constants d
11 and d
14 of

-Si

Ge

O
2 crystals have increased as compared to
quartz by approximately two times.
This work has been supported by the Russian Basic Research Foundation (Grant
No 03-02-16613).
© EDP Sciences 2005