Applications of IR Spectroscopy to Inorganic Molecules
Tuesday, July 15th, 2008
Many so-called inorganic compounds are in reality largely organic, and for these we look for the same functional group bands in the IR as we do for purely organic compounds. However, the infrared spectra of relatively simple, purely inorganic compounds containing only a few atoms–specifically, inorganic salts containing polyatomic (complex) ions–are quite distinctive and can be used to rapidly identify the ions. Consider a simple inorganic salt, such as KNO2. On the basis of the empirical formula, we might naively expect there to be a total of 3(4)-6 = 6 normal modes of vibration associated with this material. However, this assumes that KNO2 is covalent. In fact, KNO2 consists of an ionic lattice of K+ and NO2- ions arranged in an infinite and very regular array. The crystal consists of essentially isolated K+ ions and NO2- ions. Thus we are able to consider the vibrational modes of the cation and anion independently of one another. In this case, since the potassium ions are monatomic, they have no vibrations (3(1)-3 = 0), so we need only consider the nitrite anions. The VSEPR (Valence Shell Electron Pair Repulsion) Theory predicts a bent structure for the nitrite ion. We thus anticipate three normal vibrational modes for NO2-, corresponding to the diagrams drawn earlier for H2O, and they should all be infrared active. Indeed, three bands are observed in the IR spectrum of KNO2: the symmetric stretch at 1335 cm-1, the asymmetric stretch at 1250 cm-1, and the bending vibration at 830 cm-1 (bending vibrations occur in general at lower frequencies than stretching vibrations). The frequencies of these vibrations are about the same regardless of counter ion, substantiating the independence of the anion and cation in the crystal. (This independence is only an approximation, but we will not worry about the complicating factors now.) We can, therefore, diagnose the presence of nitrite ion in a salt from the infrared spectrum of the material. This diagnostic application can be implemented only when the spectrum of the material is relatively uncomplicated, but despite this restriction it is an enormously useful application.
Let us turn now to the somewhat more complex case of NaNO3. Here we anticipate 3(4)-6 = 6 normal vibrational modes. The infrared spectrum, however, exhibits only three fundamental bands, at 831, 1405, and 692 cm-1. Why? There is no doubt that there are 6 normal vibrational modes. The formula is always valid. In the case of NO3-, however, the symmetric stretch is not IR active because it does not cause a change in the dipole moment of the ion, and so cannot give rise to absorption of IR radiation. This eliminates one of the anticipated bands from the IR spectrum. Among the remaining 5, there are two sets of doubly degenerate vibrations–i.e., two instances in which 2 vibrations occur with exactly the same frequency. Thus although 5 vibrations absorb IR radiation, they are manifested in only three spectral bands. However, these absorptions can be used diagnostically just as for nitrite. In similar fashion, other relatively simple anionic (and cationic) species can be identified via their IR spectra.
Many so-called inorganic compounds are in reality largely organic, and for these we look for the same functional group bands in the IR as we do for purely organic compounds. However, the infrared spectra of relatively simple, purely inorganic compounds containing only a few atoms–specifically, inorganic salts containing polyatomic (complex) ions–are quite distinctive and can be used to rapidly identify the ions. Consider a simple inorganic salt, such as KNO2. On the basis of the empirical formula, we might naively expect there to be a total of 3(4)-6 = 6 normal modes of vibration associated with this material. However, this assumes that KNO2 is covalent. In fact, KNO2 consists of an ionic lattice of K+ and NO2- ions arranged in an infinite and very regular array. The crystal consists of essentially isolated K+ ions and NO2- ions. Thus we are able to consider the vibrational modes of the cation and anion independently of one another. In this case, since the potassium ions are monatomic, they have no vibrations (3(1)-3 = 0), so we need only consider the nitrite anions. The VSEPR (Valence Shell Electron Pair Repulsion) Theory predicts a bent structure for the nitrite ion. We thus anticipate three normal vibrational modes for NO2-, corresponding to the diagrams drawn earlier for H2O, and they should all be infrared active. Indeed, three bands are observed in the IR spectrum of KNO2: the symmetric stretch at 1335 cm-1, the asymmetric stretch at 1250 cm-1, and the bending vibration at 830 cm-1 (bending vibrations occur in general at lower frequencies than stretching vibrations). The frequencies of these vibrations are about the same regardless of counter ion, substantiating the independence of the anion and cation in the crystal. (This independence is only an approximation, but we will not worry about the complicating factors now.) We can, therefore, diagnose the presence of nitrite ion in a salt from the infrared spectrum of the material. This diagnostic application can be implemented only when the spectrum of the material is relatively uncomplicated, but despite this restriction it is an enormously useful application.
Let us turn now to the somewhat more complex case of NaNO3. Here we anticipate 3(4)-6 = 6 normal vibrational modes. The infrared spectrum, however, exhibits only three fundamental bands, at 831, 1405, and 692 cm-1. Why? There is no doubt that there are 6 normal vibrational modes. The formula is always valid. In the case of NO3-, however, the symmetric stretch is not IR active because it does not cause a change in the dipole moment of the ion, and so cannot give rise to absorption of IR radiation. This eliminates one of the anticipated bands from the IR spectrum. Among the remaining 5, there are two sets of doubly degenerate vibrations–i.e., two instances in which 2 vibrations occur with exactly the same frequency. Thus although 5 vibrations absorb IR radiation, they are manifested in only three spectral bands. However, these absorptions can be used diagnostically just as for nitrite. In similar fashion, other relatively simple anionic (and cationic) species can be identified via their IR spectra.