Abstract
Enrichment of 13C by chemical exchange between CO2 and amine carbamate in nonaqueous solvents has been mathematically modelled in two ways. The height equivalent to a theoretical plate and steady-state separation, based on the two models, have been obtained. If only the isotopic exchange between CO2 gas and amine carbamate is considered, the model can estimate the process performance for pressures close to the atmospheric one and room temperature. For process analysis at pressures higher than the atmospheric one and lower temperatures, a two-step model has been used. Using the two models the effects of pressure have been studied.
Similar content being viewed by others
References
S. DRONCA, D. AXENTE, A. BÂLDEA, C. TEACă, Rev. Chim., 51 (2000) 65.
J. P. AGRAWAL, Separ. Sci., 6 (1971) 831.
J. P. AGRAWAL, Separ. Sci., 6 (1971) 819.
K. TAKESHITA, A. KITAMOTO, J. Chem. Eng. Japan, 22 (1989) No. 5, 447.
A. KITAMOTO, K. TAKESHITA, Proc. Intern. Symp. on Isotope Separation and Chemical Exchange Uranium Enrichment, 1992, Tokyo, T.I.T., p. 376.
S. DRONCA, D. AXENTE, A. BÂLDEA, M. ABRUDEAN, Rev. Chim., 49 (1998) 775.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Raica, P., Axente, D. Enrichment of 13C by chemical exchange between CO2and amine carbamate in nonaqueous solvents. Journal of Radioanalytical and Nuclear Chemistry 251, 443–449 (2002). https://doi.org/10.1023/A:1014838410235
Issue Date:
DOI: https://doi.org/10.1023/A:1014838410235