The infra-red behaviour of sodium fluorideRaman, C.
doi: 10.1007/BF03046295pmid: N/A
Twelve spectrophotometer records of the absorption by NaF plates are reproduced covering the wavelength range between 7µ and 23µ for absorption paths ranging from 21 mm. down to 0·18 mm. The octave of the fundamental mode of highest frequency records itself as a sharply-defined absorption at 18·2µ. This gives 275 cm.−1 as the fundamental frequency, in fair agreement with the theoretically computed value of 281 cm.−1 It also fits in with the observed infra-red reflexion maximum at 36µ.
Kinetic studies in ester hydrolysisAnantakrishnan, S.; Radhakrishnamurti, P.
doi: 10.1007/BF03046300pmid: N/A
The study of hydrolyses of the diesters of benzene dicarboxylic acids as a consecutive reaction and of the sodium salt of the half ester in mixed solvents clearly indicates that both in the first and in the second stage the reaction is only of the ion-dipole type. Calculations of the dimensions of the reactant species show that the most reasonable values are given by the Laidler approach while the Ingold calculations probably give the dimensions of the solvated transition state.
On the preparation of the neutron-deficient Nb92 in high specific activityGopinathan, K.
doi: 10.1007/BF03046302pmid: N/A
The extraction of niobium by di-isobutyl ketone from hydrochloric acid solutions is investigated. This method is made use of in the preparation of the neutron-deficient Nb92 in high specific activity. Nb92 is produced by (n, p) reaction in Mo92 using natural molybdenum irradiated in the reactor. The effect of (n, p) reactions in other naturally present isotopes of molybdenum, on the radiochemical purity of the sample, is discussed.
Manganese in the shelf sediments off east coast of IndiaRao, M.
doi: 10.1007/BF03046304pmid: N/A
The distributional pattern of manganese in the shelf sediments off east coast of India has been determined. It is found that sediments from the immediate vicinity of river confluences, those of finer texture, and also those that are brownish in colour are generally more enriched in manganese. Manganese content decreases in a direction that is seaward from the coast and away from river confluences. An inverse relationship between the manganese content and the carbonate content of these sediments has been established, the richer the sediment in carbonate content the less the manganese concentration.