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IOSR Journal of Applied Physics (IOSR-JAP)
e-ISSN: 2278-4861.Volume 7, Issue 1 Ver. III (Jan.-Feb. 2015), PP 06-10
www.iosrjournals.org
DOI: 10.9790/4861-07130610 www.iosrjournals.org 6 | Page
FTIR study of second group iodate crystals grown by gel method
Amit. B. Patil
P.G. Department of Physics, Pratap college, Amalner - 425401, (MAH) India
Abstract: The crystals of Strontium iodate, Zinc iodate and Mercuric iodate were grown by a simple gel
method using diffusion technique. The optimum growth conditions were established by varying various
parameters such as pH of the gel solution, gel concentration, gel setting time, concentrations of reactants etc.
The crystals were characterized using FTIR.
Keywords: Gel technique, Strontium iodate, Zinc iodate and Mercuric iodate crystals, FTIR.
I. Introduction
The growth of single crystals in gel at an ambient temperature, which are sparingly soluble in water, is
a fascinating alternative to the techniques involving high temperature and expensive equipments. During the last
few years, successful application of gel growth technique has been demonstrated by the preparation of single
crystals of alkaline earth metal iodate. The gel growth technique appeared quite attractive for growing crystals
of such compounds on account of its unique advantages in terms of crystals produced and the simplicity of
process. Crystals of iodate exhibit nonlinear optical properties and piezoelectric properties. Nonlinear optical
phenomenon have found a wide variety of applications in many areas of modern science, technology and
engineering. The nonlinear devices find large applications in optical communication, image processing, and
wave-guide coupling.
A variety of crystals required for the purpose of research and application can be grown in silica gels.
The gel medium prevents turbulence and being chemically inert, it provides a three-dimensional crucible which
permits the reagents to diffuse at a desirable controlled rate. Its softness and uniform nature of constraining
forces that it exerts upon the growing crystals encourages orderly growth.
In the present work, Second group iodate crystals were grown by gel technique using diffusion method.
Optimum growth conditions for crystals were determined. Optimum conditions were established by varying
various parameters such as pH of gel, gel reactants, concentration programming, effect of neutral gel etc.
II. Materials and Method
Test tubes were used as crystallizing vessels. The silica gel was used as a growth media. Gel was
prepared by using glacial acetic acid and sodium meta silicate having different pH values. The chemicals used
for growth of single crystals of zinc iodate were CH3COOH; Na2SiO3.5H2O; KIO3, NaIO3; SrCl2 ; Sr(NO3)2 ;
ZnCl2 ; Zn(NO3)2 ; HgCl2 ; Hg(NO3)2. All chemicals were of AR grade.
Different molar masses were tried to determine the optimum growth conditions. One of the reactants
having different concentrations was incorporated into the gel. This solution was then transferred to borosil glass
tube of diameter, 2.5 cm and 25 cm in height. The mouth of the tube was covered by cotton plug. After setting
of the gel, it was left for aging for different periods of time. Another reactant having different concentrations
was then added as supernatant over the set gel. Experiments were carried out by changing different
concentrations of the reactants.
The chemical reaction inside the gel can be expressed as
XCl2 + 2YIO3 → X(IO3)2 + 2YCl
OR
X(NO3)2 + 2YIO3 → X(IO3)2 + 2YNO3
Where X = Sr, Zn and Hg and Y = K or Na.
III. Results and discussions
Infrared spectroscopy is one of the most powerful analytical techniques, which offers the possibility of
chemical identification. The technique when coupled with intensity measurements may be used for quantitative
analysis. One of the most advantages of infrared spectroscopy over the usual methods of structural analysis is
that it provides useful information about the structure of molecules quickly without tiresome evaluation
methods. This method solved many problems in organic chemistry and co-ordination chemistry, while in some
other problems infrared data advantageously complement the results obtained by other methods.
FTIR study of second group iodate crystals grown by gel method
DOI: 10.9790/4861-07130610 www.iosrjournals.org 7 | Page
A new method known as Fourier Transform Infrared Spectroscopy (FT-IR) has come in to use more
recently. It is more advanced stage of infrared spectroscopy. It gives more detailed information about the
absorption bands due to presence of water molecules, metal ions, hydroxyl ions, organic molecules, etc.
Light covering the whole frequency range, typically 4000 – 400 cm-1
, is split in to two beams. Either
one beam is passed through the sample, or both the beams are passed, but one beam is made to traverse longer
path than the other does. Recombination of the two beams produces an inference pattern that is the sum of all
the inference patterns created by each wavelength in the beam. By systematically changing the difference in the
two paths, the inference patterns change to produce a detected signal varying with optical path difference. This
pattern is known as interferogram, and looks nothing like a spectrum. However, Fourier transformation of the
interferogram, converts it in to a plot of % transmittance against wave number, which resembles the usual
spectrum obtained by traditional method. There are several advantages of FT-IR over the traditional method.
Because it is not necessary to scan each wave number successively, the whole spectrum is measured in at most a
few seconds. Moreover, because it is not dependent upon a slit and a prism or grating, high resolution in FT-IR
is easier to obtain without sacrificing sensitivity.
FTIR of gel grown Second group iodate crystals were recorded using SHIMADZU spectrophotometer
at the Department of chemistry, University of Pune. The IR spectrum was recorded in the wave number range
400-4000 cm-1
for KBr line. The FT-IR spectrum of the strontium iodate, zinc iodate and mercuric iodate
crystals are as shown in the figures 1, 2 and 3 respectively.
Figure 1. FT-IR spectrum of strontium iodate
Figure 2. FT-IR spectrum of Zinc iodate
FTIR study of second group iodate crystals grown by gel method
DOI: 10.9790/4861-07130610 www.iosrjournals.org 8 | Page
Figure 3. FT-IR spectrum of Mercuric iodate
The fundamental frequencies of the pyramidal iodate ions as have been reported earlier by Nassau et al,
Dasent and Waddington, Balicheva and petrova, Sanyal and Nag, Nyquist and Kagal, are in good agreement
with the observed values in the present investigation. The various bands observed in the FT-IR analysis of these
crystals are shown in the table 1.
Table 1: Vibrational infrared frequencies:
Fundamental frequencies Strontium iodate (cm-1
) Zinc iodate (cm-1
) Mercuric iodate (cm-1
)
Symmetric stretching frequency, 1 740.69 767.69 688.61
Asymmetric stretching frequency, 2 478.36 405.06 461.00
Symmetric bending frequency, 3 825.56 729.12 800.49
Asymmetric bending frequency, 4 368.42 366.49 368.42
The various bands observed in the FT-IR analysis of the iodate crystals are as follows:
1. Strontium iodate:-
i. The bands at 3416.05 cm-1
and 3444.98 cm-1
are due to O – H stretching with shoulder near 3157.58 cm-
1
due to overtone.
ii. The bands at 1548.89 cm-1
and1
1595.18cm-1
are due to H – O – H bending.
iii. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the
range 740-830 cm-1
.
iv. The fundamental frequencies of the pyramidal iodate ions are observed,
a. Symmetric stretching γ1 at 740.69 cm-1
.
b. Symmetric bending γ2 at 478.36 cm-1
.
c. Asymmetric stretching γ3 at 825.56 cm-1
.
d. Asymmetric bending γ4 at 368.42 cm-1
.
v. The extra bands observed in the range 400-480 cm-1
may be due to metal – oxygen vibration.
vi. One more extra band observed in the range 740-830 cm-1
may also be due to vibration between metal –
iodine – oxygen atoms.
The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the
range 740-830 cm-1
. The fundamental infrared frequencies, observed in all iodate compounds in general, are also
found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 368.42 cm-1
are due to the iodate group. The dominant absorption bands are found at 700-825 cm-1
in all iodate compounds
(Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 . From the spectral
analysis, it is clear that in case of strontium iodate crystals, the bands at 3157 cm-1
, 3416 cm-1
, 3444 cm-1
, 1548
cm-1
and 1595 cm-1
are due to inclusion of one water molecule.
2. Zinc iodate:-
vii. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the
range 675-770 cm-1
.
FTIR study of second group iodate crystals grown by gel method
DOI: 10.9790/4861-07130610 www.iosrjournals.org 9 | Page
viii. The fundamental frequencies of the pyramidal iodate ions are observed,
a. Symmetric stretching γ1 at 767.69 cm-1
.
b. Symmetric bending γ2 at 405.06 cm-1
.
c. Asymmetric stretching γ3 at 729.12 cm-1
.
d. Asymmetric bending γ4 at 366.49 cm-1
.
ix. The extra bands observed in the range 400-480 cm-1
may be due to metal-oxygen vibration.
x. One more extra band observed in the range 740-830 cm-1
may also be due to vibration between metal –
iodine – oxygen atoms.
xi. All other extra bands observed in the spectra are may be due to inclusion of sodium meta silicate in the
grown crystals.
The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the
range 670-770 cm-1
. The fundamental infrared frequencies, observed in all iodate compounds in general, are also
found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 366.49 cm-1
are due to the iodate group. The dominant absorption bands are found at 600-800 cm-1
in all iodate compounds
(Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 .
3. Mercuric iodate:-
xii. The bands observed in the range 3281.02 cm-1
to 3583.86 cm-1
are due to O – H stretching with shoulder
near 3198.08 cm-1
due to overtone.
xiii. The bands at 1489.10 cm-1
, 1550.82 cm-1
and 1614.47cm-1
are due to H – O – H bending.
xiv. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the
range 670-800 cm-1
.
xv. The fundamental frequencies of the pyramidal iodate ions are observed,
a. Symmetric stretching γ1 at 688.61 cm-1
.
b. Symmetric bending γ2 at 461.00 cm-1
.
c. Asymmetric stretching γ3 at 800.49 cm-1
.
d. Asymmetric bending γ4 at 368.42 cm-1
.
xvi. The extra bands observed in the range 400-461 cm-1
may be due to metal – oxygen vibration.
xvii. Extra bands observed in the range 670-800 cm-1
may also be due to vibration between metal – iodine –
oxygen atoms.
The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the
range 670-800 cm-1
. The fundamental infrared frequencies, observed in all iodate compounds in general, are also
found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 368.42 cm-1
are due to the iodate group. The dominant absorption bands are found at 700-825 cm-1
in all iodate compounds
(Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 . From the spectral
analysis, it is clear that in case of mercuric iodate crystals, the bands at 3198.08 cm-1
, 3281.02 cm-1
, 3294.53 cm-
1
, 3340.82 cm-1
, 3362.04 cm-1
, 3385.18 cm-1
, 3419.90 cm-1
, 3522.13 cm-1
3562.64 cm-1
, 3583.86 cm-1
, 1550.82
cm-1
and 1614.47 cm-1
are due to inclusion of half water molecule.
IV. Conclusions
From the above studies we observe that
(I) Gel growth technique is suitable for growing iodate crystals.
(II) Different habits of these crystals can be obtained by changing parameters like gel density, gel aging, pH of
gel, Concentration of reactants etc.
(III)Existance of Water of crystallization present in the grown crystals is confirmed by FT-IR analysis.
(IV)Fundamental infrared frequencies observed in all iodate compounds in general, are also found in the present
FT-IR analysis.
Acknowledgements
The authors are greatful to prof. Dr L A Patil, Head of the Department of physics, Pratap College,
Amalner, for providing laboratory facilities. Also we thank Prof. Dr. Sanjay Dhole, Department of physics,
University of pune for providing laboratory facilities of FT-IR analysis.
References
[1]. Kurtz S K and Perry T T , J. Appl. Phys. 39 3798 (1968)
[2]. Ranadive D, Blank Z, Brenner W and Okamoto Y , Nature 223 829 (1969)
[3]. Morosin B, Bergman J G and Crane G R , Acta Crystallography B29 1067 (1973)
[4]. Sangwal K and Patel A R , J. Crystal growth 23 282 (1974)
FTIR study of second group iodate crystals grown by gel method
DOI: 10.9790/4861-07130610 www.iosrjournals.org 10 | Page
[5]. Bach H and Kuppers H Acta Crystallography B34 263 (1978)
[6]. Joshi M S and Trivedi S G , Indian J. pure & App. Phys. 21 435 (1983)
[7]. Shitole S J and Saraf K B , Bulletin of Material Science 5 461 (2001)
[8]. Garud S L and Saraf K B , Bulletin of Material Science 4 639 (2008)

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FTIR study of second group iodate crystals grown by gel method

  • 1. IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861.Volume 7, Issue 1 Ver. III (Jan.-Feb. 2015), PP 06-10 www.iosrjournals.org DOI: 10.9790/4861-07130610 www.iosrjournals.org 6 | Page FTIR study of second group iodate crystals grown by gel method Amit. B. Patil P.G. Department of Physics, Pratap college, Amalner - 425401, (MAH) India Abstract: The crystals of Strontium iodate, Zinc iodate and Mercuric iodate were grown by a simple gel method using diffusion technique. The optimum growth conditions were established by varying various parameters such as pH of the gel solution, gel concentration, gel setting time, concentrations of reactants etc. The crystals were characterized using FTIR. Keywords: Gel technique, Strontium iodate, Zinc iodate and Mercuric iodate crystals, FTIR. I. Introduction The growth of single crystals in gel at an ambient temperature, which are sparingly soluble in water, is a fascinating alternative to the techniques involving high temperature and expensive equipments. During the last few years, successful application of gel growth technique has been demonstrated by the preparation of single crystals of alkaline earth metal iodate. The gel growth technique appeared quite attractive for growing crystals of such compounds on account of its unique advantages in terms of crystals produced and the simplicity of process. Crystals of iodate exhibit nonlinear optical properties and piezoelectric properties. Nonlinear optical phenomenon have found a wide variety of applications in many areas of modern science, technology and engineering. The nonlinear devices find large applications in optical communication, image processing, and wave-guide coupling. A variety of crystals required for the purpose of research and application can be grown in silica gels. The gel medium prevents turbulence and being chemically inert, it provides a three-dimensional crucible which permits the reagents to diffuse at a desirable controlled rate. Its softness and uniform nature of constraining forces that it exerts upon the growing crystals encourages orderly growth. In the present work, Second group iodate crystals were grown by gel technique using diffusion method. Optimum growth conditions for crystals were determined. Optimum conditions were established by varying various parameters such as pH of gel, gel reactants, concentration programming, effect of neutral gel etc. II. Materials and Method Test tubes were used as crystallizing vessels. The silica gel was used as a growth media. Gel was prepared by using glacial acetic acid and sodium meta silicate having different pH values. The chemicals used for growth of single crystals of zinc iodate were CH3COOH; Na2SiO3.5H2O; KIO3, NaIO3; SrCl2 ; Sr(NO3)2 ; ZnCl2 ; Zn(NO3)2 ; HgCl2 ; Hg(NO3)2. All chemicals were of AR grade. Different molar masses were tried to determine the optimum growth conditions. One of the reactants having different concentrations was incorporated into the gel. This solution was then transferred to borosil glass tube of diameter, 2.5 cm and 25 cm in height. The mouth of the tube was covered by cotton plug. After setting of the gel, it was left for aging for different periods of time. Another reactant having different concentrations was then added as supernatant over the set gel. Experiments were carried out by changing different concentrations of the reactants. The chemical reaction inside the gel can be expressed as XCl2 + 2YIO3 → X(IO3)2 + 2YCl OR X(NO3)2 + 2YIO3 → X(IO3)2 + 2YNO3 Where X = Sr, Zn and Hg and Y = K or Na. III. Results and discussions Infrared spectroscopy is one of the most powerful analytical techniques, which offers the possibility of chemical identification. The technique when coupled with intensity measurements may be used for quantitative analysis. One of the most advantages of infrared spectroscopy over the usual methods of structural analysis is that it provides useful information about the structure of molecules quickly without tiresome evaluation methods. This method solved many problems in organic chemistry and co-ordination chemistry, while in some other problems infrared data advantageously complement the results obtained by other methods.
  • 2. FTIR study of second group iodate crystals grown by gel method DOI: 10.9790/4861-07130610 www.iosrjournals.org 7 | Page A new method known as Fourier Transform Infrared Spectroscopy (FT-IR) has come in to use more recently. It is more advanced stage of infrared spectroscopy. It gives more detailed information about the absorption bands due to presence of water molecules, metal ions, hydroxyl ions, organic molecules, etc. Light covering the whole frequency range, typically 4000 – 400 cm-1 , is split in to two beams. Either one beam is passed through the sample, or both the beams are passed, but one beam is made to traverse longer path than the other does. Recombination of the two beams produces an inference pattern that is the sum of all the inference patterns created by each wavelength in the beam. By systematically changing the difference in the two paths, the inference patterns change to produce a detected signal varying with optical path difference. This pattern is known as interferogram, and looks nothing like a spectrum. However, Fourier transformation of the interferogram, converts it in to a plot of % transmittance against wave number, which resembles the usual spectrum obtained by traditional method. There are several advantages of FT-IR over the traditional method. Because it is not necessary to scan each wave number successively, the whole spectrum is measured in at most a few seconds. Moreover, because it is not dependent upon a slit and a prism or grating, high resolution in FT-IR is easier to obtain without sacrificing sensitivity. FTIR of gel grown Second group iodate crystals were recorded using SHIMADZU spectrophotometer at the Department of chemistry, University of Pune. The IR spectrum was recorded in the wave number range 400-4000 cm-1 for KBr line. The FT-IR spectrum of the strontium iodate, zinc iodate and mercuric iodate crystals are as shown in the figures 1, 2 and 3 respectively. Figure 1. FT-IR spectrum of strontium iodate Figure 2. FT-IR spectrum of Zinc iodate
  • 3. FTIR study of second group iodate crystals grown by gel method DOI: 10.9790/4861-07130610 www.iosrjournals.org 8 | Page Figure 3. FT-IR spectrum of Mercuric iodate The fundamental frequencies of the pyramidal iodate ions as have been reported earlier by Nassau et al, Dasent and Waddington, Balicheva and petrova, Sanyal and Nag, Nyquist and Kagal, are in good agreement with the observed values in the present investigation. The various bands observed in the FT-IR analysis of these crystals are shown in the table 1. Table 1: Vibrational infrared frequencies: Fundamental frequencies Strontium iodate (cm-1 ) Zinc iodate (cm-1 ) Mercuric iodate (cm-1 ) Symmetric stretching frequency, 1 740.69 767.69 688.61 Asymmetric stretching frequency, 2 478.36 405.06 461.00 Symmetric bending frequency, 3 825.56 729.12 800.49 Asymmetric bending frequency, 4 368.42 366.49 368.42 The various bands observed in the FT-IR analysis of the iodate crystals are as follows: 1. Strontium iodate:- i. The bands at 3416.05 cm-1 and 3444.98 cm-1 are due to O – H stretching with shoulder near 3157.58 cm- 1 due to overtone. ii. The bands at 1548.89 cm-1 and1 1595.18cm-1 are due to H – O – H bending. iii. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the range 740-830 cm-1 . iv. The fundamental frequencies of the pyramidal iodate ions are observed, a. Symmetric stretching γ1 at 740.69 cm-1 . b. Symmetric bending γ2 at 478.36 cm-1 . c. Asymmetric stretching γ3 at 825.56 cm-1 . d. Asymmetric bending γ4 at 368.42 cm-1 . v. The extra bands observed in the range 400-480 cm-1 may be due to metal – oxygen vibration. vi. One more extra band observed in the range 740-830 cm-1 may also be due to vibration between metal – iodine – oxygen atoms. The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the range 740-830 cm-1 . The fundamental infrared frequencies, observed in all iodate compounds in general, are also found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 368.42 cm-1 are due to the iodate group. The dominant absorption bands are found at 700-825 cm-1 in all iodate compounds (Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 . From the spectral analysis, it is clear that in case of strontium iodate crystals, the bands at 3157 cm-1 , 3416 cm-1 , 3444 cm-1 , 1548 cm-1 and 1595 cm-1 are due to inclusion of one water molecule. 2. Zinc iodate:- vii. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the range 675-770 cm-1 .
  • 4. FTIR study of second group iodate crystals grown by gel method DOI: 10.9790/4861-07130610 www.iosrjournals.org 9 | Page viii. The fundamental frequencies of the pyramidal iodate ions are observed, a. Symmetric stretching γ1 at 767.69 cm-1 . b. Symmetric bending γ2 at 405.06 cm-1 . c. Asymmetric stretching γ3 at 729.12 cm-1 . d. Asymmetric bending γ4 at 366.49 cm-1 . ix. The extra bands observed in the range 400-480 cm-1 may be due to metal-oxygen vibration. x. One more extra band observed in the range 740-830 cm-1 may also be due to vibration between metal – iodine – oxygen atoms. xi. All other extra bands observed in the spectra are may be due to inclusion of sodium meta silicate in the grown crystals. The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the range 670-770 cm-1 . The fundamental infrared frequencies, observed in all iodate compounds in general, are also found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 366.49 cm-1 are due to the iodate group. The dominant absorption bands are found at 600-800 cm-1 in all iodate compounds (Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 . 3. Mercuric iodate:- xii. The bands observed in the range 3281.02 cm-1 to 3583.86 cm-1 are due to O – H stretching with shoulder near 3198.08 cm-1 due to overtone. xiii. The bands at 1489.10 cm-1 , 1550.82 cm-1 and 1614.47cm-1 are due to H – O – H bending. xiv. The bands due to vibrations involving metal, iodine and oxygen atoms are found predominantly in the range 670-800 cm-1 . xv. The fundamental frequencies of the pyramidal iodate ions are observed, a. Symmetric stretching γ1 at 688.61 cm-1 . b. Symmetric bending γ2 at 461.00 cm-1 . c. Asymmetric stretching γ3 at 800.49 cm-1 . d. Asymmetric bending γ4 at 368.42 cm-1 . xvi. The extra bands observed in the range 400-461 cm-1 may be due to metal – oxygen vibration. xvii. Extra bands observed in the range 670-800 cm-1 may also be due to vibration between metal – iodine – oxygen atoms. The bands due to vibration involving metal, iodine and oxygen atoms are found predominantly in the range 670-800 cm-1 . The fundamental infrared frequencies, observed in all iodate compounds in general, are also found in the present FT-IR analysis, which confirm the iodate group of grown crystals. The bands at 368.42 cm-1 are due to the iodate group. The dominant absorption bands are found at 700-825 cm-1 in all iodate compounds (Nakamoto 1970) and can be expected to contain ν1, ν3 as well as possible splitting of ν3 . From the spectral analysis, it is clear that in case of mercuric iodate crystals, the bands at 3198.08 cm-1 , 3281.02 cm-1 , 3294.53 cm- 1 , 3340.82 cm-1 , 3362.04 cm-1 , 3385.18 cm-1 , 3419.90 cm-1 , 3522.13 cm-1 3562.64 cm-1 , 3583.86 cm-1 , 1550.82 cm-1 and 1614.47 cm-1 are due to inclusion of half water molecule. IV. Conclusions From the above studies we observe that (I) Gel growth technique is suitable for growing iodate crystals. (II) Different habits of these crystals can be obtained by changing parameters like gel density, gel aging, pH of gel, Concentration of reactants etc. (III)Existance of Water of crystallization present in the grown crystals is confirmed by FT-IR analysis. (IV)Fundamental infrared frequencies observed in all iodate compounds in general, are also found in the present FT-IR analysis. Acknowledgements The authors are greatful to prof. Dr L A Patil, Head of the Department of physics, Pratap College, Amalner, for providing laboratory facilities. Also we thank Prof. Dr. Sanjay Dhole, Department of physics, University of pune for providing laboratory facilities of FT-IR analysis. References [1]. Kurtz S K and Perry T T , J. Appl. Phys. 39 3798 (1968) [2]. Ranadive D, Blank Z, Brenner W and Okamoto Y , Nature 223 829 (1969) [3]. Morosin B, Bergman J G and Crane G R , Acta Crystallography B29 1067 (1973) [4]. Sangwal K and Patel A R , J. Crystal growth 23 282 (1974)
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