1985
DOI: 10.1007/bf00956782
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Continuous absorption in the IR spectra of sulfate solutions in 100% sulfuric acid

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Cited by 2 publications
(6 citation statements)
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“…Because no HCl was added (0 titrant equivalent) and almost no H + is present in the solution (pH = 6.27), the acidic water retrieved by IR spectroscopy must be attributed to water in strong interaction with the glycine zwitterion. Excess acidic water has long been estimated by the so-called “continuum of absorption”. We also reported similar results for IR titrations of phosphoric and malic acids. , This acidic water cannot be attributed to free protons (H + or H 3 O + ) and must be attributed to the solvated solute species. Hence, the aqueous glycine zwitterion spectrum (Figure D z ) must be corrected for its acidic water, as well as for malic acid 27 (see Appendix A).…”
Section: Resultssupporting
confidence: 60%
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“…Because no HCl was added (0 titrant equivalent) and almost no H + is present in the solution (pH = 6.27), the acidic water retrieved by IR spectroscopy must be attributed to water in strong interaction with the glycine zwitterion. Excess acidic water has long been estimated by the so-called “continuum of absorption”. We also reported similar results for IR titrations of phosphoric and malic acids. , This acidic water cannot be attributed to free protons (H + or H 3 O + ) and must be attributed to the solvated solute species. Hence, the aqueous glycine zwitterion spectrum (Figure D z ) must be corrected for its acidic water, as well as for malic acid 27 (see Appendix A).…”
Section: Resultssupporting
confidence: 60%
“…Excess acidic water has long been estimated by the so-called "continuum of absorption". [17][18][19][20][21][22][23][24][25][26] We also reported similar results for IR titrations of phosphoric and malic acids. 7,27 This acidic water cannot be attributed to free protons (H + or H 3 O + ) and must be attributed to the solvated solute species.…”
Section: Resultssupporting
confidence: 54%
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“…The 3700−1800 cm -1 region is dominated by four weak broad bands situated at 3500, 2930, 2580, and 1995 cm -1 (Figure ). Because of its continuous formation, this diffuse absorption is sometimes referred to as the “continuum of absorbance”. However, this absorption is associated with the presence of water for two reasons: no H 3 O + is present in the solution, and the absorption in the 3700−1800 cm -1 region is much more intense than in solid malic acid where there is no water (Figure d,d‘). The second derivative technique allowed us to see three very weak bands situated at 2940, 2895, and possibly one at 2840 cm -1 , which we assign to CH 2 antisymmetric and symmetric and CH stretch bands.…”
Section: Resultsmentioning
confidence: 99%