Spectrochimica Actq Vol. 45A, No. 8, pp. 877-878, Printed in Great Brilain.
1989. 0
TECHNICAL INFRARED
AND POLARIZED
1989 Maxwell
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NOTE
RAMAN SPECTRA
OF KAINITE
(Received 20 May 1988; in final form 21 January 1989; accepted 30 January 1989) Abstract-The i.r. and Raman spectra of KMgClS0,.3H,O and its deuterated compound KMgClS0;3D,O have been recorded and analysed. Due to site symmetry effects the i.r. inactive modes appear as sharp bands in the i.r. spectrum. Water bands indicate strong hydrogen bonding and show the presence of three crystallographically distinct water molecules in the unit cell.
Kainite is a mineral [l] with chemical formula KMgClS0,.3H,O. The space group of this compound is determined as CZ/m [2], but detailed crystal structure data such as bond lengths and bond angles are not available. In the present paper, i.r. and Raman spectroscopic techniques
have been used as a probe to determine the nature of the SOi- ion and hydrogen bond in this compound. Crystals suitable for the polarization study were prepared by the slow evaporation of an aqueous solution containing equimolar ratios of KCI and MgS0,.7H,O at room tem-
Table 1. Spectral data and band assignments (cm-‘) of KMgClS0,.3H,O/D,O KMgClSO,. 3H,O Raman i.r. B* A, 3408 3330 3292
3348 3308
3258 3162 3080
3244 3168 3089
1720 1697 1655
1720 1670 1644
1162 1138 1110 1093
1173 1138 1122 1094
3000-3500
1700b
1140b 1090 b
1048
SAA45:8-G
2500 2470 2445
KMgClSO,. 3D,O i.r.
Assignments
H,O(D,O) H,O(D,O)
I II III
H,O(D,O) “3
22OG2600
2420 2340 2300
“1
H,O(D,O) H,O(D,O) H,O(D,O)
I II III
1270 1250 1218
“2
1225 b
H,O(D,O) H,O(D,O) H,O(D,O)
III II I
1150b
SOa
1175 1150 1125 1080
1080 b
1020 980 m
988
990
945
918
890 815
853 808 784
860 b
740
750 b
700
746 721 705
662 644 633 612
647 630 621
630 m 608 sh
590 525 503
599
585 sh
472 460
470 461 442
440m
420 365
390 m
415 388 315 284 242
Raman
984
980 m
945
WWW)
298 240m
560 530
650 635 600
“1
H,WW)
“4
so4
“2
so4
615 b
435 400
465 445
440m External modes of H,O(D,O) and M-O stretching
265 230 811
878
Technical Note Table 1 KMgCISO;3H,O Raman Ail B* 195 151 125
147 131
88
76
i.r.
Raman
(continued)
KMgCISO,.3D,O i.r.
175 115
Assignments
SO, rotational SO, translational
b, broad; m, medium; sh, shoulder; C, combination; r,t,w, rocking, twisting and wagging modes of water. perature (300 K) [3]. The deuterated compound KMgCIS0,.3D,O was obtained by using heavy water as solvent, and was recrystallized several times in a vacuum desiccator. Only polycrystalline samples were obtained for the deuterated compound. Infrared spectra were recorded on a Perkin-Elmer 580 spectrophotometer with the samples prepared as KBr discs. Polarized Raman spectra were recorded on a Spex Ramalog 1401 double monochromator equipped _ _. with a Spectra-Physics model 165 Ar+ laser. KMgCISO,.3HiO crystallizes in the monoclinic system with mace aroun C2/mC?. and z = 16. As the lattice is’not prim&e, oily eight molecules are considered for the analysis of the spectra. The atoms (K, Mg and Cl), SOi- ion and the water molecule are at C, sites. Factor group analysis [4] at k = 0 gives 408 modes and they split into l- = 102A, + 1028, + 102A, + 102B,. An isolated SOi- ion with Td symmetry has its normal vibrations at 981 (vi(A,)), 451 (vJE)), 1104 (v3(F2)) and 613 (v., (F2)) cm- ’ [S]. All these modes are Raman active, while v1 and vI are i.r. inactive. Observed bands and their assignment to different modes are given in Table 1. Degeneracies of va, vs and vq modes are completely lifted in the Raman spectrum, and the i.r. inactive modes appear as sharp bands in the i.r. spectrum. This is attributed to site symmetry effects, as the symmetry of the anion is lowered from Td to Ci. In the internal mode region one expects 18 Raman active bands to appear in each species (A, and 83. But only 11 bands are observed in both the species. This can occur due to negligible splittings and overlapping of bands. In the i.r. spectrum only a few bands are observed due to poor resolution. A free water molecule absorbs at 3756 (vs), 3652 (vi) and 1595 (va) cm-’ [6]. In the present investigation a number of broad bands with frequencies considerably shifted from the free state values have been observed, indicating strong hydrogen bonding. The strengths of these hydrogen bonds are comparable with those observed in Tutton salts [7-93. The bands observed in the stretching and bending regions show the presence of three crystallographically distinct water molecules in the unit cell. This is also confirmed by the corresponding bands obtained in the deuterated compound with an isotopic ratio of 1.3-1.36. Bands indicating the formation of HDO are not observed in the spectra. The external modes of H,O molecules, SOi- ion and metal-oxygen stretching bands are observed below
400 cm- i. Sulphate bands are tentatively assigned by considering the fact that rotatory modes appear at higher frequencies with larger intensities than translatory modes in the Raman spectrum [lo, 111. The weak bands observed in the 230-420 cm- r region are assigned to the translational modes of water [12] and to the metal&oxygen stretching modes. Department of Physics Deva Matha College Kuravilangad 686 633 Kottayam, Kerala, India
XAVIER MATHEW
Department of Physics University of Kerala Kariavattom, Trivandrum 695581 Kerala, India
V. U.
NAYAR*
REFERENCES
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[8] G.
SEKAR, V. RAMAKRISHNANand G. ARULDHAS,.I.
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[9] V. S. [lo]
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[12] J. E. BERTIE,H. J. LABBE and Phys. %I,4501 (1969).
E. WHALLEY, J. them.
*To whom correspondence should be addressed.