Abstract:iron counters and reducing the source background to 50% and the cosmic background to 0.1 of its present value (advanced model). A further precision increase can be obtained by using a 1.5-mCi source and reducing the total background to 0.1 of the present one (optimum model).
CONCLUSIONThe apparatus described previously shows the following advantages: (a) possibility of nondestructive testing of liquids, solid, gaseous, and chromatogram samples; (b) no necessity of sample preparation; (c) no need for highly sk… Show more
“…The frequencies of the peak maxima for all of the isotopically substituted water systems are collected in Table 6, together with the experimental ones. [20][21][22][23][24][25][26][27] It can be seen that the frequencies of the peak maxima, as far as they have been measured, are in reasonable agreement with the experimental values. The ratios of the vibrational frequency maxima, ν′ max / ν max , for H 2 O to D 2 O and D 2 O to T 2 O from the simulations are equal to 1.38, 1.37, and 1.37 and 1.20, 1.19, and 1.19 for the symmetric stretching, asymmetric stretching, and bending motions, respectively, and reproduce the ideal isotopic ratios 1.37 and 1.19.…”
Section: Resultssupporting
confidence: 65%
“…The ones for the H 2 O + HDO + D 2 O and D 2 O + DTO + T 2 O mixtures are quite similar to those shown in Figure but differ, of course, in the positions of the peak maxima. The frequencies of the peak maxima for all of the isotopically substituted water systems are collected in Table , together with the experimental ones. − It can be seen that the frequencies of the peak maxima, as far as they have been measured, are in reasonable agreement with the experimental values. The ratios of the vibrational frequency maxima, ν‘ max /ν max , for H 2 O to D 2 O and D 2 O to T 2 O from the simulations are equal to 1.38, 1.37, and 1.37 and 1.20, 1.19, and 1.19 for the symmetric stretching, asymmetric stretching, and bending motions, respectively, and reproduce the ideal isotopic ratios 1.37 and 1.19.…”
The hindered translational motions, the librations around the
principal axes, and the intramolecular vibrations
have been calculated from molecular dynamics simulations of water by
Fourier transformations of the
corresponding velocity autocorrelation functions for all possible
hydrogen-isotope-substituted molecules at
room temperature. The flexible BJH model for water has been
employed in the simulations. The frequencies
for the hypothetical liquids HDO, HTO, and DTO as well as the
stretching vibrations of T2O are predicted.
“…The frequencies of the peak maxima for all of the isotopically substituted water systems are collected in Table 6, together with the experimental ones. [20][21][22][23][24][25][26][27] It can be seen that the frequencies of the peak maxima, as far as they have been measured, are in reasonable agreement with the experimental values. The ratios of the vibrational frequency maxima, ν′ max / ν max , for H 2 O to D 2 O and D 2 O to T 2 O from the simulations are equal to 1.38, 1.37, and 1.37 and 1.20, 1.19, and 1.19 for the symmetric stretching, asymmetric stretching, and bending motions, respectively, and reproduce the ideal isotopic ratios 1.37 and 1.19.…”
Section: Resultssupporting
confidence: 65%
“…The ones for the H 2 O + HDO + D 2 O and D 2 O + DTO + T 2 O mixtures are quite similar to those shown in Figure but differ, of course, in the positions of the peak maxima. The frequencies of the peak maxima for all of the isotopically substituted water systems are collected in Table , together with the experimental ones. − It can be seen that the frequencies of the peak maxima, as far as they have been measured, are in reasonable agreement with the experimental values. The ratios of the vibrational frequency maxima, ν‘ max /ν max , for H 2 O to D 2 O and D 2 O to T 2 O from the simulations are equal to 1.38, 1.37, and 1.37 and 1.20, 1.19, and 1.19 for the symmetric stretching, asymmetric stretching, and bending motions, respectively, and reproduce the ideal isotopic ratios 1.37 and 1.19.…”
The hindered translational motions, the librations around the
principal axes, and the intramolecular vibrations
have been calculated from molecular dynamics simulations of water by
Fourier transformations of the
corresponding velocity autocorrelation functions for all possible
hydrogen-isotope-substituted molecules at
room temperature. The flexible BJH model for water has been
employed in the simulations. The frequencies
for the hypothetical liquids HDO, HTO, and DTO as well as the
stretching vibrations of T2O are predicted.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.