Measurements have been made of the Raman spectra of aqueous solutions of Be(ClO
4)
2, BeCl
2, (NH
4)
2SO
4 and BeSO
4 to 50 cm
−1. In some cases low concentrations (0.000770 mol⋅kg
−1) have been used and two temperatures (23 and 40 °C) were studied. In BeSO
4(aq), the
ν
1-SO
42-\mathrm{SO}_{4}^{2-} mode at 980 cm
−1 broadens with increasing concentration and shifts to higher wavenumbers. At the same time, a band at 1014 cm
−1 is detectable with this mode being assigned to [BeOSO
3], an inner-sphere complex (ISC). Confirmation of this assignment is provided by the simultaneous appearance of stretching
bands for the Be
2+-OSO
32-\mathrm{Be}^{2+}\mbox{-}\mathrm{OSO}_{3}^{2-} bond of the complex at 240 cm
−1 and for the BeO
4 skeleton mode of the [(H
2O)
3BeOSO
3] unit at 498 cm
−1. The ISC concentration increases with higher temperatures. The similarity of the n
1-SO
42-\nu_{1}\mbox{-}\mathrm{SO}_{4}^{2-} Raman bands for BeSO
4 in H
2O and D
2O is further strong evidence for formation of an ISC. After subtraction of the ISC component at 1014 cm
−1, the n
1-SO
42-\nu_{1}\mbox{-}\mathrm{SO}_{4}^{2-} band in BeSO
4(aq) showed systematic differences from that in (NH
4)
2SO
4(aq). This is consistent with a n
1-SO
42-\nu_{1}\mbox{-}\mathrm{SO}_{4}^{2-} mode at 982.7 cm
−1 that can be assigned to the occurrence of an outer-sphere complex ion (OSCs). These observations are shown to be in agreement
with results derived from previous relaxation measurements. Infrared spectroscopic data show features that are also consistent
with a beryllium sulfato complex such as the appearance of a broad and weak n
1-SO
42-\nu_{1}\mbox{-}\mathrm{SO}_{4}^{2-} mode at ∼1014 cm
−1, normally infrared forbidden, and a broad and asymmetric n
3-SO
42-\nu_{3}\mbox{-}\mathrm{SO}_{4}^{2-} band contour which could be fitted with four band components (including n
3-SO
42-(aq)\nu_{3}\mbox{-}\mathrm{SO}_{4}^{2-}(\mathrm{aq})). The formation of ISCs in BeSO
4(aq) is much more pronounced than in the similar MgSO
4(aq) system studied recently.
相似文献