EFFECT OF SO IMPURITY ON THE OPTICAL TRANSMISSION OF As S GLASS
1389
2
2 3
After rinsing in high-purity carbon tetrachloride, a
glass sample (12–14 g) was placed in a quartz ampule,
which was then connected to a leak-in system of known
volume (Fig. 1). The volume of the system and ampule
was measured relative to a calibrated volume. After
pumping down the ampule containing glassy arsenic
3
2
7
5
-4
sulfide to a residual pressure of 6.5 × 10 Pa, sulfur
1
dioxide was admitted in an amount sufficient for pro-
6
ducing initial pressure p in the system. Next, the
0
4
ampule was disconnected from the system by sealing
off tube 2, and sulfur dioxide was removed from the
leak-in system. The ampule was heated under static
conditions for 4 h at 650°C and then furnace-cooled. In
this way, we obtained glassy arsenic trisulfide in the
form of a plate 5 mm in thickness, containing sulfur
Fig. 1. Schematic of the apparatus for introducing sulfur
dioxide into glassy arsenic sulfide: (1) ampule containing a
glass sample, (2) tube for sealing off under vacuum;
dioxide. Next, SO was again introduced into the leak-
2
in system, to pressure p , the partition was broken, and
0
(3) manometer; (4) cylinder containing SO ; (5) outlet
2
the residual pressure was measured after SO dissolu-
valve; (6) striker, (7) partition.
2
tion. The difference between the initial and residual
pressures was due to the SO dissolution in arsenic sul-
2
spectrum in this range was deconvoluted into elemen-
tary components as described by Bychkova et al. [7].
As an example, Fig. 3 shows the spectrum of the sample
fide. From this value, we calculated the amount of dis-
solved sulfur dioxide and its concentration in the sam-
ple using the Clapeyron equation. The sulfur dioxide
–
2
containing 0.11 wt % SO
2
and the deconvolution
content of the samples thus prepared was 1.3 × 10 to
results.
–
2
1
2.4 × 10 wt % (Table 2).
At sulfur dioxide contents within 0.12 wt % and
sample lengths no greater than 30 mm, the absorptions
The glass was withdrawn from the ampule, and sev-
eral plane-parallel samples 2–3 mm thick were pre-
pared for IR measurements. A control sample was pre-
pared by the same procedure but without introducing
sulfur dioxide.
–1
at 1361, 1871, 2305, and 2499 cm , due to the funda-
mental and mixed frequencies of SO (Table 1), were
2
missing.
The spectrum of the control sample (2 mm in thick-
Transmission spectra were recorded in the range
ness) shows no bands due to H O or OH groups
2
–
1
5
00–5000 cm with an IFS-113V Fourier transform IR
(
Fig. 2). As seen in Fig. 2, the spectra of the SO -doped
2
spectrometer.
samples contain absorption bands arising from H O
2
–
1
–1
(
1588 and 3590 cm ), CO (2324 cm ), and OH and
The homogeneity of the SO distribution was
2
2
–
1
SH groups (3450 and 2487 cm , respectively). Note
that the intensities of the absorption bands due to H O,
checked by measuring the spectra of samples cut from
the upper and lower portions of the ingot. The spectra
2
showed no variations in absorption with position in the CO
, and OH groups do not correlate with the SO con-
2
2
ingot.
Table 2. Sulfur dioxide content of glassy arsenic sulfide
Sam- Sample weight, ∆p, Pa V, cm3
RESULTS AND DISCUSSION
wt %
2
2
SO × 10
Figure 2 shows the IR absorption spectra of arsenic
sulfide glasses doped with sulfur dioxide in comparison
with the spectrum of the control sample. The effect of
sulfur dioxide on the absorption spectra of the glass is
ple no.
g (±0.001)
(±260) (±0.4)
(±0.5)
1
2
3
4
5
6
7
14.106
14.953
12.556
12.185
13.987
12.470
13.719
650
1560
1950
2990
3120
5460
6370
103.2
95.0
1.3
2.7
–
1
clearly seen in the range 800–1400 cm . The introduc-
tion of sulfur dioxide into the glass gives rise to an
106.9
91.0
4.4
–
1
absorption peaked at 1158 cm (Fig. 2), which
becomes stronger with increasing sulfur dioxide con-
6.1
tent. In addition, the spectra of the SO -doped samples
2
102.0
94.0
6.2
show absorption bands centered at 985, 1053, and
–
1
–1
1
270 cm . The bands at 1053 and 1270 cm are due to
11.2
12.4
As–O vibrations [5, 6]. Since the absorption bands in
98.0
–
1
the range 800–1400 cm have a complex structure, the
INORGANIC MATERIALS Vol. 42 No. 12 2006