1988
DOI: 10.1021/j100320a055
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A quantitative infrared spectroscopic method for the study of the hydration of ions in aqueous solutions

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Cited by 76 publications
(75 citation statements)
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“…Thus, taking into account all spectral information we conclude that most of the water molecules absorbed from the atmosphere into the eight RTILs presented in Tables 1 and Table 2 are H-bonded via both hydrogen atoms of water to the two anions of RTILs. Table 1 27 and with studies of isotopically dilute HDO molecules of water 28 shows that the relative order of the interaction of water with anions in the systems containing the same anions as in the RTILs studied here is identical. Our findings are also consistent with the work on the interaction between methanol and various anions, 29 Nevertheless, we cannot exclude the presence of water-water aggregates in these RTILs at higher water concentrations when water is added into these RTILs.…”
Section: Resultssupporting
confidence: 55%
“…Thus, taking into account all spectral information we conclude that most of the water molecules absorbed from the atmosphere into the eight RTILs presented in Tables 1 and Table 2 are H-bonded via both hydrogen atoms of water to the two anions of RTILs. Table 1 27 and with studies of isotopically dilute HDO molecules of water 28 shows that the relative order of the interaction of water with anions in the systems containing the same anions as in the RTILs studied here is identical. Our findings are also consistent with the work on the interaction between methanol and various anions, 29 Nevertheless, we cannot exclude the presence of water-water aggregates in these RTILs at higher water concentrations when water is added into these RTILs.…”
Section: Resultssupporting
confidence: 55%
“…17 By measuring the same concentration of salt in both pure water and water containing 8% HDO, and then subtracting the spectrum of pure water one gets an infrared spectrum of the HDO molecules different from those in the aqueous bulk. By taking the derivative of these spectra Ϭϵ/Ϭm where ϵ denotes the spectrum and m the molality of the solution then subtracting (1/N*M)*Ϭϵ/Ϭm from the spectrum of pure water, where N is the affected number of water and M is the mean molar mass in kg/mol of water and partially heavy water, as described by Kristiansson et al and Gampe et al;[18][19][20] the affected water peaks ascribed to water molecules bound to cations or anions are obtained through PCA. All calculations of the spectra were carried out using GRAMS AI version 8.0 (Thermo-Fisher Scientific) and RAZOR tools (Spectrum Square Associates), and two Array the Basic program YANUZ.AB was used to calculate the derivatives of the spectra.…”
Section: Double Difference Infrared Spectroscopy (Ddir)mentioning
confidence: 99%
“…The position of the anionic peak indicates that selenite ion is a weak structure maker with molecular interaction energy of water ΔU w = -45.2 kJ mol -1 derived from υ OD using the Badger-Bauer rule 27 using calculation procedure described in detail in earlier studies. 18,19 It was possible to separate the contributions from the sodium and selenate ions in the affected DDFTIR spectra, Figure 7. 3 Transforming the υ OD for the affected water peak of the selenate ion to molecular interaction energy of water it becomes ΔU w = -47.4 kJ•mol -1 .…”
Section: Fourier Transform Infrared Spectroscopymentioning
confidence: 99%
“…Such visualization of the spectral changes -i.e. the incomplete subtraction of a reference spectrum, which yielded a positive difference curve in the region of interest, was used successfully by Kristiansson et al [33] and by Stangret and co-workers [34][35][36][37]. The spectra after the subtraction of a reference water spectrum are described as difference spectra in the following text.…”
Section: Data Processingmentioning
confidence: 99%