Abstract:Infrared spectra of aqueous solutions of U(VI), Np(VI), Pu(VI), and Am(VI) show conclusively that these ions exist as symmetrical and linear, or nearly linear, XO2++. The spectra of Np(V) and Am(V) show that they are probably XO2+ ions. Force constants and estimated distances are given for the X—O bonds. For the XO2++ series, the X—O force constant is expressed as a parabolic function of atomic number, with the maximum occurring at NpO2++. This is contrary to behavior expected if there were a regular contracti… Show more
“…The υ 3 mode of the fully hydrated NpO 2 + species is observed at 820 cm −1 . 42 The same species is dominant under the prevailing sorption conditions, that is, 0.1 M NaCl, D 2 O, pH 8, N 2 (cf. Figure 3A).…”
Section: ■ Experimental Sectionmentioning
confidence: 99%
“…This is due to a decrease of the NpO force constant as a result of complexation with Fe 2 O 3 units of the mineral phase in the equatorial plane. 29,42 The in situ vibrational data of Np(V) sorbed onto oxides of Ti, Si and Zn may serve as a reference, 29 as the experiments were performed under identical experimental conditions, that is, 0.1 M NaCl, D 2 O, pH 8, N 2 . A comparison of the data sets demonstrates that the frequency of the υ 3 of the sorbed Np(V) species is observed at ∼790 cm −1 irrespective of the sorbing surface.…”
Hematite plays a decisive role in regulating the mobility of contaminants in rocks and soils. The Np(V) reactions at the hematite-water interface were comprehensively investigated by a combined approach of in situ vibrational spectroscopy, X-ray absorption spectroscopy and surface complexation modeling. A variety of sorption parameters such as Np(V) concentration, pH, ionic strength, and the presence of bicarbonate was considered. Time-resolved IR spectroscopic sorption experiments at the iron oxide-water interface evidenced the formation of a single monomer Np(V) inner-sphere sorption complex. EXAFS provided complementary information on bidentate edge-sharing coordination. In the presence of atmospherically derived bicarbonate the formation of the bis-carbonato inner-sphere complex was confirmed supporting previous EXAFS findings.1 The obtained molecular structure allows more reliable surface complexation modeling of recent and future macroscopic data. Such confident modeling is mandatory for evaluating water contamination and for predicting the fate and migration of radioactive contaminants in the subsurface environment as it might occur in the vicinity of a radioactive waste repository or a reprocessing plant.
“…The υ 3 mode of the fully hydrated NpO 2 + species is observed at 820 cm −1 . 42 The same species is dominant under the prevailing sorption conditions, that is, 0.1 M NaCl, D 2 O, pH 8, N 2 (cf. Figure 3A).…”
Section: ■ Experimental Sectionmentioning
confidence: 99%
“…This is due to a decrease of the NpO force constant as a result of complexation with Fe 2 O 3 units of the mineral phase in the equatorial plane. 29,42 The in situ vibrational data of Np(V) sorbed onto oxides of Ti, Si and Zn may serve as a reference, 29 as the experiments were performed under identical experimental conditions, that is, 0.1 M NaCl, D 2 O, pH 8, N 2 . A comparison of the data sets demonstrates that the frequency of the υ 3 of the sorbed Np(V) species is observed at ∼790 cm −1 irrespective of the sorbing surface.…”
Hematite plays a decisive role in regulating the mobility of contaminants in rocks and soils. The Np(V) reactions at the hematite-water interface were comprehensively investigated by a combined approach of in situ vibrational spectroscopy, X-ray absorption spectroscopy and surface complexation modeling. A variety of sorption parameters such as Np(V) concentration, pH, ionic strength, and the presence of bicarbonate was considered. Time-resolved IR spectroscopic sorption experiments at the iron oxide-water interface evidenced the formation of a single monomer Np(V) inner-sphere sorption complex. EXAFS provided complementary information on bidentate edge-sharing coordination. In the presence of atmospherically derived bicarbonate the formation of the bis-carbonato inner-sphere complex was confirmed supporting previous EXAFS findings.1 The obtained molecular structure allows more reliable surface complexation modeling of recent and future macroscopic data. Such confident modeling is mandatory for evaluating water contamination and for predicting the fate and migration of radioactive contaminants in the subsurface environment as it might occur in the vicinity of a radioactive waste repository or a reprocessing plant.
“…2 (upper panel). The m 3 (UO 2 ) mode of the fully hydrated UO 2þ 2 species, present in highly acidic aqueous solution, shows an absorption maximum at 961 cm -1 (Jones and Penneman, 1953;Quilès and Burneau, 2000). With increasing pH, hydrolysis reactions occur, monomeric and polymeric species are formed which, above all, strongly depend on the prevailing uranyl(VI) concentration (Grenthe et al, 1992;Guillaumont et al, 2003).…”
“…There are number of reports on the properties of perchloric acid in detail using spectroscopic, analytical and physical methods [1][2][3][4][5][6] . The dependence of viscosity of aqueous perchloric acid and chemical shifts of NMR as a function of concentration has been reported 7,8 .…”
Viscosity ƞ and density ρ of aqueous concentrated perchloric acid 1.0moldm −3 to 9.0moldm −3 were measured at 297.65K. The viscosity data were used to calculate the value of A and B-coefficient of Jones-Dole equation. The value of B-coefficient is positive which suggests the strong ion-solvent interaction in aqueous perchloric acid. The three concentration regions of perchloric acid having value of B-coefficient (measure of ion-solvent interaction or structure making capacity) in the order 1.0 to 4.0moldm −3 < 4.0 to 6.0moldm −3 < 6.0 to 9.0moldm −3 has been proposed.
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