FRACTIONATION OF HEAVY HYDROGEN ISOTOPES IN DYNAMICAL SYSTEMS

Abstract

The possibility of using mineral adsorbents for cleaning the moderator of heavy water reactors from tritium is determined. Three dynamic systems have been created using montmorilonite, sepiolite and palygorskite clays, and zeolite (systems M-Z, S-Z and P-Z) as composite membranes. At the first stage, deuterium-tritium water (DTO) was filtered through mineral membranes, and at the second stage, these membranes were washed with protium water (Н 2 О). In the process of such two-stage filtration, the effect of separation of tritium and deuterium in the filtrate was first established. At the first stage of the experiment, the content of deuterium and tritium in the DTO filtrate in the system with the M-Z membrane was equally re- duced and at the end of the filtration was slightly more than 50% of the initial concentrations. The separation coefficient of heavy hydrogen isotopes in this system did not exceed K T = 0.99. When DTO was filtered through the C-Z membrane, the fraction of tritium in the filtrate at the end of filtra- tion decreased by 10% relative to the initial concentration, which is less than the fraction of deuterium, and the hydrogen isotope separation coefficient was K T = 1.15. In the P-C system, the residual fraction of deuterium in the DTO filtrate was 3% higher than the residual fraction of tritium and the hydrogen isotope separation coefficient was determined at the level of K T = 0.96. A different process is observed when filtering protium water (Н 2 О) through clay-zeolite adsorbents after their interaction with the DTO solution. In all the studied mineral adsorbents, the manifestations of frac- tionation of heavy hydrogen isotopes with coefficients KD = 13.2, 3.2 and 3.6 were established respectively for montmorillonite-zeolite, sepiolite-zeolite and palygorskite-zeolite composites with a predominant deuterium content in the filtrate, which indicates the possibility of using clay-zeolite mineral adsorbents for the purification of heavy water from tritium.